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1 Mawson Resources Limited Progress Report On The Geology, Mineralization And Exploration Activities On The Rompas-Rajapalot Gold- Uranium Project, Peräpohja Schist Belt Lapland, Finland Michael Hudson, FAusIMM, MAIG, MSEG 8/27/2014

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Page 1: Mawson Resources Limited Progress Report On The …tupa.gtk.fi/karttasovellus/mdae/references/189_Rompas/...The veins (amphibole-pyroxene-quartz-carbonate ± native gold, uraninite)

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Mawson Resources Limited

Progress Report On The Geology, Mineralization And Exploration Activities On The Rompas-Rajapalot Gold-

Uranium Project, Peräpohja Schist BeltLapland, Finland

 

Michael Hudson, FAusIMM, MAIG, MSEG 

8/27/2014 

  

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Table of Contents Table of Contents ............................................................................................................................ 2 

List of Tables .................................................................................................................................. 3 

List of Appendices .......................................................................................................................... 3 

1.  Summary ................................................................................................................................ 4 

2.  Introduction ........................................................................................................................... 6 

3.  Reliance on Other Experts .................................................................................................... 6 

4.  Property Description and Location...................................................................................... 6 

5.  Accessibility, Climate, Local Resources, Infrastructure and Physiography .................. 12 

6.  History .................................................................................................................................. 12 

7.  Geological Setting and Mineralization .............................................................................. 13 

a)  Regional Geological Setting .............................................................................................. 13 

b)     Rompas Area Geology ...................................................................................................... 16 

c)  Mineralization .................................................................................................................... 18 

Deposit Types .............................................................................................................................. 21 

8.  Exploration ........................................................................................................................... 21 

10.  Drilling .............................................................................................................................. 27 

11.  Sample Preparation, Analyses and Security ................................................................. 37 

12.  Data Verification .............................................................................................................. 40 

13.  Mineral Processing and Metallurgical Testing ............................................................. 41 

14.  Mineral Resource Estimates ........................................................................................... 41 

15.  Mineral Reserve Estimates .............................................................................................. 41 

16.  Mining Methods ............................................................................................................... 41 

17.  Recovery Methods ............................................................................................................ 41 

18.  Project Infrastructure ..................................................................................................... 41 

19.  Market Studies and Contracts ........................................................................................ 41 

20.  Environmental Studies, Permitting and Social or Community Impact ...................... 42 

21.  Capital and Operating Costs .......................................................................................... 43 

22.  Economic Analysis ........................................................................................................... 43 

23.  Adjacent Properties ......................................................................................................... 43 

24.  Other Relevant Data and Information ........................................................................... 44 

25.  Interpretation and Conclusions ...................................................................................... 44 

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List of Tables Table 1: Status of Mawson’s Claims in Finland as of August 2014. ............................................. 8 

Table 2: Lithostratigraphy of the Peräpohja Belt (Prave, 2013) .................................................. 15 

Table 3: Drill statistics from the Rompas-Rajapalot, August 2014 ............................................. 27 

Table 4: Comparison of J. Nebocat Samples (2011) with AREVA & Mawson Samples ........... 41 

Table 5: Recommended company-wide budget for August 2014 - August 2015 ........................ 46 

Table 6: Exploration budget for August 2014-August 2015 ....................................................... 47 

List of Figures Figure 1: Rompas Project Finland Index Map ................................................................................ 7 

Figure 2: Rompas Claims and Prospects ........................................................................................ 8 

Figure 3: Rompas Geology and Structure ..................................................................................... 17 

Figure 4: Rompas Rajapalot Prospect -Basaltic Host Rocks ....................................................... 19 

Figure 5: Rajapalot Overview Map with IP Chargeability .......................................................... 20 

Figure 6: Rompas Heavy Mineral Sampling ............................................................................... 22 

Figure 7: Rompas Levelled A Horizon and C Horizon Till Au-W Geochemistry ...................... 26 

Figure 8: North Rompas Drilling Plan .......................................................................................... 30 

Figure 9: South Rompas Drilling Plan .......................................................................................... 31 

Figure 10: South Rompas Cross Section 7373780N.................................................................... 32 

Figure 11: South Rompas Long Section ....................................................................................... 33 

Figure 12: South Rompas Log Grade vs. Width ........................................................................... 34 

Figure 13: Palokas Drilling Plan ................................................................................................... 35 

Figure 14: Palokas Cross Section ................................................................................................. 36 

Figure 15: Palokas Longitudinal Drill Section ............................................................................. 37 

List of Appendices Appendix 1: List of Mawson’s Claims at Rompas/Finland. ........................................................ 50 

Appendix 2: List of Drill Holes Collars Drilled by Mawson to Date at Rompas ......................... 71 

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1. Summary The Rompas-Rajapalot gold-uranium project is located in the Ylitornio and Rovaniemi municipalities of northern Finland at 66.45ºN and 24.75ºE, approximately 50 kilometres (“km”) west of the Rovaniemi town.

The Rompas project is a new camp-scale discovery where high-grade gold and uranium have been found within an area approaching 10km by 10km. Mawson acquired the project in April 2010 and outlined the initial hydrothermal nuggety gold vein discovery over a 6.0 kilometres strike and 200-250 metres width. In 2013, a new style of disseminated gold mineralization was drilled at Rajapalot, 8 kilometres east of the Rompas vein system.

Mawson is focused on two target areas at Rompas-Rajapalot:

1. A primary target of disseminated gold mineralization at Rajapalot, where discovery of high grade and thick core sample results include 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006 and 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres) and 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005. This disseminated mineralization is coincident with geophysical anomalies that extend for more than 4 kilometres and has only been drilled to 30 metres maximum depth with a hand portable core sampler.

2. The Company’s secondary target is the Rompas vein-style target area. The first drill program at South Rompas included the highlight of 6 metres at 617 g/t gold from 7 metres in drill hole ROM0011 which includes 1 metre at 3,540 g/t gold from 11 metres depth. The second drill program, conducted over the winter (December 2012 - January 2013) confirmed the presence and variable continuity within metabasalts of high grade, nuggety gold at both North and South Rompas and included results from North Rompas of 0.4 m at 395 g/t gold and 0.41% uranium (“U308”) in drill hole ROM0052 and at South Rompas the top 24% all assays from trenches and drilling now grade 100 g/t or more.

The Rompas-Rajapalot property consists of 108 granted claims and 2 granted exploration permits (currently under one administrative appeal by a non-governmental organization) of 1,462 hectares and 1,292 hectares respectively at Rompas/Rajapalot (Table 1). The Company has staked additional claim applications, exploration permit applications and reservations in the Rompas area with potential for gold.

Core sample results in October 2013 at Rajapalot include 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006 and 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres) and 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005. The disseminated mineralization is coincident with a VTEM geophysical conductor that extends for more than 500 metres through an area with <1% outcrop, and forms part of a 3.5 kilometre target horizon between basaltic and quartzitic rocks.

Results from the maiden drill program at the Rompas vein system returned 6 metres at 617 g/t gold from 7 metres in drill hole ROM0011 including 1 metre at 3,540 g/t gold in August 2012. In February 2013, the first drill results from North Rompas, located 5km from South Rompas included 0.4m at 395 g/t Au and 0.41% U3O8 from 41m. The project lies within the Peräpohja Schist Belt, a Paleoproterozoic supracrustal sequence of quartzites, mafic volcanics and volcaniclastics, carbonate rocks, black shales, mica schists and greywackes. At Rajapalot fine disseminated hydrothermal gold mineralization occurs within magnesian chlorite-biotite-tourmaline-pyrrhotite-scheelite bearing rocks, located near the contact between mafic rocks and relatively oxidized muscovite and hematite-bearing quartzites. The initial discovery area, Rompas, is a hydrothermal system of carbonate-calcsilicate-quartz veins hosted in poly-deformed amphibolite facies metabasalts, with some bituminous carbon. Detailed examination of the gold and uraninite in polished thin section reveals a series of complex overprinting relationships and the origin of the mineralization

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remains unclear. At this early stage of exploration, it is difficult to find a global analogue for mineralization. Within the vein system, gold and uranium mineralization is hosted by a carbonate-calcsilicate-quartz vein array and albitic vein breccias. The veins (amphibole-pyroxene-quartz-carbonate ± native gold, uraninite) and alteration selvages (biotite-amphibole-K-feldspar) have been metamorphosed to amphibolite facies, following a structural episode of flattening within high strain zones. It is interpreted that the mineralized veins are either pre- or syn-deformational, but that the high-grade mineralization is likely a result of redistribution during syn-metamorphic deformation and perhaps superposition of new gold late in the metamorphic history. The disseminated mineralization differs in that it is more sulphidic and continuous than the vein-style mineralization, and comprises fine disseminated gold mineralization within magnesian chlorite-biotite-tourmaline-pyrrhotite-scheelite rocks. The mineralized zone lies structurally between mafic rocks and relatively oxidized quartzites.

Importantly, about 90% of the Rompas-Rajapalot project area is below soil and till cover which, at up to 5m thick, is too thick for the discovery of near-surface radiometric occurrences and exploration is at its very earliest of stages.

A continuing program is recommended at Rompas-Rajapalot with the main goal over the next year to attempt to define the first NI 43-101 resource on the project and continue to derisk adjacent prospect areas for deep drill testing. Specifically the recommended work program should address the following items:

1. Pole-Dipole Induced Polarization (“IP”) at 100 metre spacing over the main Rajapalot trend from Hirvimaa, Palokas to Rumajärvi prospects;

2. Gradient Array IP over the Joki prospect;

3. Maxwell modelling of the VTEM airborne geophysical survey at Rajapalot;

4. Deep till and basement grid drilling over the Raja prospect area to the east of the Natura 2000

5. Subject to final permitting, aim to define by diamond drilling an initial resource at Rajapalot on 100 metre drill sections at 50 metre down dip spacing over 2 kilometre strike. Approximately 500 metres per section over 2 kilometre strike would amount to a recommended 10,000 metres drill campaign;

6. Metallurgical test work on Palokas drill core;

An exploration and company-wide budget to carry out these programs is estimated at CDN$6M.

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2. Introduction This report was prepared for the Company by Michael Hudson, a non-independent Qualified Person (as defined under NI 43-101) and the Chairman, President and Chief Executive Officer and a director of Mawson and a Fellow of the Australasian Institute of Mining and Metallurgy.

The technical report documents the geology, mineralization and exploration activities conducted by the Issuer on the property during 2010 - 2014. The Issuer conducted all the work described within this report either through direct employees of the Issuer or by specialized contractors.

Sources of information include maps and presentation material provided by AREVA; claim statistics and maps provided by the Finnish Ministry of Employment and Economy; topographic maps found online at the Citizen’s Map Site--National Land Survey of Finland; GTK, the Geological Survey of Finland website; two geological bulletins for map sheet 3612 (Rovaniemen) and map sheets 2631/2633 (Törmäsjärvi and Koivu); updated 1:25,000 scale regional geology map by GTK (2010); structural interpretation by independent consulting geologist; in-house digital compilation maps of Finland and project area presented in Mapinfo format and provided by the Issuer; in-house analytical databases, sampling protocols, press releases, up to August 13, 2014, and various Management Discussion and Analyses (“MD&A’s”) by the Issuer.

The Rompas-Rajapalot property has been continually examined by the author since April 2010, with the last field made on August 21 to August 26, 2014.

The effective date of this report is August 27, 2014. The effective date for technical data is August 27, 2014.

3. Reliance on Other Experts No sections of this report were drawn from the opinions of independent experts.

4. Property Description and Location On April 30, 2010, Mawson entered into an agreement with AREVA Finland whereby the Issuer acquired 100% of AREVA Finland’s mineral properties and exploration database in exchange for €1 million. AREVA subscribed, via a private placement, for 4,696,698 common shares of the Issuer at a price of $0.29 per share for a total purchase price of €1 million. Fifty percent of the shares from the private placement will remain in voluntary escrow until the final granting of certain claim applications.

In addition, AREVA received 4,217,012 share purchase warrants, exercisable for 4 years after closing, to purchase an equivalent number of common shares of the Issuer for $1.00 per share. The share purchase warrants expired in full on May 12, 2014.

There exists no underlying royalties, back-in rights or other underlying agreements or encumbrances that this property may be subject to.

The Rompas-Rajapalot property consists of 108 granted claims and 2 granted exploration permits (currently under one administrative appeal by a non-governmental organization) of 1,462 hectares and 1,292 hectares respectively at Rompas/Rajapalot (Table 1). The Company has staked additional claim applications, exploration permit applications and reservations in the

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Rompas area with potential for gold. Figure 2 shows the locations of the claims described above. Appendix 1 lists all of Mawson claims.

.

Figure 1: Rompas Project Finland Index Map Date: 27 August 2014, Modified Public Domain Map, North Parallel to Longitude Lines to Top of Map

Rompas is centered roughly at coordinates 3,403,100E by 7,375,550N of the Finnish national coordinate system (KKJ), Zone 3 (Figure 1).

The Finnish national coordinate system, KKJ is derived from the Finnish national adjustment (1966) of the ED50 (European Datum 1950) coordinate system by shifting and rotating ED50 plane coordinates so, that they optimally fit to KKJ's predecessor VVJ, Helsinki System. KKJ-coordinates can be presented in geographical (latitude, longitude) or in rectangular grid-coordinates (northing, easting). The reference ellipsoid used with KKJ is International 1924 ellipsoid, also known as Hayford ellipsoid. Gauss-Krüger projection formula is used to convert

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between KKJ-geographical and KKJ-grid-coordinates. KKJ-grid consists of six zones, each 3 degrees wide. Very often only zones 1-4 are represented because these zones almost cover entire Finland. This grid system, with six 3 degrees wide zones, is called 'Basic Coordinate System', in Finnish 'Peruskoordinaatisto'. Parameters for zone 3 are also used countrywide and is then called 'Uniform Coordinate System', in Finnish 'Yhtenäiskoordinaatisto' or YKJ. In topographic maps the Basic Coordinate Systems grid-lines are printed black and Uniform Coordinate Systems grid-lines are printed red.

Table 1: Status of Mawson’s Claims in Finland as of August 2014.

Number of

Claims

Number of

Reservations

Area

(ha)

Status

Rompas 108 - 10,330 Granted Claims1

Rompas 710 - 63,468 Applied Claims1

Rumavuoma* 13 - 1,292 Granted Claims1

Kairamaat 2-3* 4 1,462 Exploration Permit2

Kairamaat 1, Kultamaat, Hirvimaa, Raja 1 5,355 Exploration Permit Application2

*Under administrative appeal

1. Old Mining Act (pre July 1, 2011)

2. New Mining Act (post Jul 1, 2011)

Figure 2: Rompas Claims and Prospects

Date: 27 August 2014, Author M.R Hudson, North to top of map

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Finland introduced a new Mining Act (“new Act”) in force from 1 July 2011. The Issuer’s current claim applications were submitted under the previous Act; however, some sections of the new Act will apply. The Company’s new exploration permits and application were submitted under the current Mining Act. Under Finnish Mining Law, prospecting is considered part of the so-called “everyman's right”, a Nordic tradition, giving public access to all land, public or private. Geological mapping, as well as limited sampling, and prospecting can be carried out everywhere, provided that no damage is done to the landowner's property or to the environment. The old Act, core claims at Rompas were granted on October 31, 2011 and came into legal force until on October 15, 2012. A decision was made in early July 2014 by TUKES (the Finnish Safety and Chemical Agency) to grant modified and renewed exploration claims titled Kairamaat 2 and 3 that cover a surface area of 1,462 hectares at Mawson's Rajapalot gold project in northern Finland, that entitles Mawson drill access during winter conditions within Natura 2000 biodiversity areas. The decision will take legal effect after a standard public appeal process

Under the new Act, an area not already reserved or with an ore prospecting permit or application, may be reserved for a period of up to 24 months. This reservation (“Varaus”) gives the reserving party priority to apply for an ore prospecting permit. Some exploration may be conducted on a reservation, if the landholder approves, if the work would not harm people’s health, other commercial activity or the environment, and exploration is not for uranium or thorium. Geological mapping, some types of sampling and prospecting can be carried out if these conditions are met. Minor sampling and non-disturbing exploration such as soil/till sampling by hand, induced polarization, ground magnetic and electromagnetic surveys are allowed whilst under application and without landholder approval.

An ore prospecting permit allows the holder to conduct exploration. Ore prospecting fees are payable to the landholder, beginning at €20 per ha, per year, for the first four years, then rising.

Collateral, determined on a case by case basis, to cover potential environmental damage is lodged with the Ministry. Permits can be valid for 3 to 4 years, and may be extended for a maximum of three years at a time. In total, the permit may remain valid for a maximum of 15 years, if certain conditions are met.

A mining concession is granted if a deposit is shown to be technically and economically exploitable.

No special permits are required for surface exploration once the “claim reservation” has been accepted as an “ore prospecting permit.”

The author is aware that Mawson has been dealing with certain Finnish environmental authorities in regards to work completed during the 2010 and 2011 field programs (refer to press release dated June 26, 2013). The issue involves allegations that the Company's hand dug trenches from these programs have affected the nature values of the area where the work was undertaken. The Company has now been informed that the investigative process is complete and the prosecutor has reviewed the investigative material and referred the matter to trial, with the case to be heard in the Kemi-Tornio District Court on October 14-15 2014. Mawson is pleased the case is advancing and will be handled through a formal legal process. Mawson believes the claims made are without merit and will vigorously defend itself and its employees. Mawson has always maintained that hand digging has no material impact on the nature values of the area in question. Mawson believes it conducted its operations within the intent and law of the Mining and Nature Conservation Acts.

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There is no record of any previous mining activity on the property.

Finland has legislated the following acts and laws:

Forest Act 1996

This act promotes utilization of the forestry areas for economic profit but at the same time maintaining the “biological diversity” in the area.

Water Services Act 2001

This act aims to provide clean water to the citizens of Finland, in order to protect their health.

Waste Act 2004

This act promotes the use of natural resources in a rational manner, in order to hazardous (sic) material from harming people as well as the environment.

Waste Oil Charge Act

The state will collect hazardous waste in order to cover expenses from waste oil management.

Nature Conservation Act 1996

This act aims to maintain biological diversity, promote scientific research, and conserve the natural beauty of the area.

Parts of the Rompas area are subject to decrees which pre-date the Nature Conservation Act 1996 (with amendments). These are the Bog Protection Decree (933/1981) and the Grove Protection Decree (522/1992). Exploration is allowed in the areas of the decrees, with landholder permission.

Natura 2000

Finland, as a member of the EU, supports the EEC ‘Habitats’ Directive 92/43/CEE. Article 6 of the Directive plays a crucial role in the management of the sites that make up the Natura 2000 network - a biodiversity program.

Certain areas of the Rompas-Rajapalot areas (namely claim areas Kairamaat 1-3) are defined as European Union Natura 2000 designated areas. Natura 2000 sites cover about 10% of Finland and approximately 30% of Northern Finland. Natura 2000 is the centrepiece of EU nature and biodiversity policy. It is an EU-wide ecological network of nearly 26,000 sites in the 27 EU countries, established under the 1992 Habitats Directive and covering almost 18% of the EU’s land area. The aim of the network is to assure the long-term survival of Europe’s most valuable and threatened species and habitats. Natura 2000 is not a system of strict nature reserves where all human activities are excluded. Whereas the network will certainly include nature reserves, most of the land is likely to continue to be privately-owned and the emphasis will be on ensuring that future management is sustainable, both ecologically and economically.

Part of the property lies within a Natura 2000 area. The Natura 2000 network is in place to conserve important biotopes and species throughout Europe. The purpose of the Natura 2000 program is to preserve nature’s diversity.

For the most part the areas Finland has suggested as Natura 2000 areas are protected areas, wilderness areas and areas taking part in nature conservation programs. The network also aims to protect the natural features which have not been conserved in the past.

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http://www.metsa.fi/sivustot/metsa/en/NaturalHeritage/ProtectedAreas/Natura2000Sites/Sivut/Natura2000AreasEstablishedtoProtectBiotopesandSpecies.aspx.

In 2014 the Finnish Government updated the Guide to Exploration in protected areas, the Sámi homeland and the reindeer managing area:

http://www.tukes.fi/Tiedostot/kaivokset/TEM_Opas_MEKO_en.pdf

For the 10,580 hectares at Rompas, the Company is entitled to 100% of the mineral rights over the entire claim with certain limitations on exploration methods that can be completed in Natura 2000 areas (approximately 20% of the Company’s granted claim area) within the exploration claims, including no large scale drilling or trenching. A decision was made in early July 2014 by TUKES (the Finnish Safety and Chemical Agency) to grant modified and renewed exploration claims titled Kairamaat 2 and 3 that cover a surface area of 1,462 hectares at Mawson's Rajapalot gold project in northern Finland, that entitles Mawson drill access during winter conditions within Natura 2000 biodiversity areas. The decision will take legal effect after a standard public appeal process.

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5. Accessibility, Climate, Local Resources, Infrastructure and Physiography

The topography is a fairly gently rolling to almost flat, heavily glaciated and inundated with numerous post-glacial lakes, till, eskers, lacustrine and fluvial deposits. The mean elevation on the property is in the neighborhood of 100 m ASL according to the regional topographic map, and the ridge underlying the showings ranges between 100 m and 200 m ASL.

Lodgepole pine, spruce and fir are common coniferous species. Low-lying shrubs are common; probably some species of blueberry or lingon berry, and sphagnum moss blankets the forest floor throughout. Alders and poplars were recognized as a common deciduous tree along waterways, and stands of white birches form groves randomly interspersed with the coniferous trees.

Rompas is located about 45 km WSW of the city of Rovaniemi in southern Lapland, Finland. Access by road from Rovaniemi is via highway E75 (4) southwesterly for 24 km to the junction of highway 930, just past the town of Muurola. Heading westerly on highway 930 for about 28 km, the property is accessed via a secondary/tertiary gravel road that heads northerly from the village of Kaitajärvi. This is roughly the south-central boundary of the property which extends for several kilometers to the north-northwest; Rompas lies about 10 km south of the Arctic Circle.

Alternately, the property is accessible by highways from either southern Finland or via Sweden; the Swedish border is only about 1 hour’s drive to the west.

Rovaniemi is the largest city in Lapland with a population of 59,000. Several daily flights link the city with Helsinki, and train travel takes from 9 to 12 hours.

The climate is classified as subarctic with an average temperature of +0.20C. Annual rainfall is 535 mm, and snow stays on the ground 183 days per year on average. The type of work performed on the property would be dictated by the seasons somewhat, but effectively, some kind of work could be done throughout the year.

Skilled labour is readily available in Rovaniemi and surrounding communities. There is adequate raw material (water, gravel, timber) and infrastructure--forestry roads inundate the entire area. The smaller communities along highway 930 are serviced with electricity. As mining is an established and recognized industry in Finland, there would appear to be no hindrances to surface rights. The terrain is suitable for a mine/processing plant, dumps, tailings and storage facilities.

6. History During the 1950s the GTK performed some exploration for molybdenum and uranium SW from the general Rompas area, and additional exploration for copper and tungsten was performed in the northern part of the area during the 1970s. The Rautaruukki Company performed uranium exploration south of this area, resulting in the discovery of the Mustamaa uranium prospect, currently held under tenure by the Issuer, located about 15 km south of the Rumavuoma area (Vanhanen, 2010).

It appears that the area was discovered by an airborne radiometric survey. Follow-up exploration was conducted by geologists who had previous GTK experience in the area. GTK had drilled a fence of stratigraphic holes to the south, along strike from the Rumavuoma claim. Radioactivity

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was first discovered by GTK on what is now the Rumavuoma claims (southern spur of Rompas) in the early 2000’s.

AREVA began reconnaissance exploration in June 2007, mostly ground radiometric surveys. They collected 32 rock/colluvium samples mostly from pits excavated in areas of strong scintillometer readings over a distance roughly 13 km NW-SE by 12 km E-W. Uranium values ranged from 12 ppm to 249,000 ppm (24.9%) and gold results ranged from 0.05 ppm to 12,800 ppm (>373 oz/ton). Of these 31 samples, 9 ran higher than 1,000 ppm (0.1%) U and 7 ran greater than 100 ppm (~3 oz/ton) Au. Further work was completed in 2008 with some follow-up work done in 2009. More than 150 new, separate occurrences of high uranium and extremely high gold contents were located in bedrock. At that time, however, AREVA decided to reduce activities in Finland and started negotiations with the Issuer.

Between August and September 2009, the Issuer spent several days examining the mineralized zones discovered by AREVA and took several check samples from their pits and from a few other sites. A total of twenty-one samples were collected by the Issuer from the northwestern showings on the Rompas/Rumavuoma claims during this time. The Issuer’s samples were analyzed for multi-elements in addition to specific techniques for Au and U.

Uranium values ranged from 2 ppm to 435,000 ppm (43.5%), averaging 36,088 ppm (3.6%) and six of the samples were in the percentage range. Similarly, gold values ranged from trace levels to 1,830 ppm (g/t), or just over 53 oz/ton, and averaged 224 g/t (6.5 oz/ton). Of the 32 samples AREVA collected, 20 came from these northwestern showings. These 20 samples yielded uranium levels from 13 ppm to 249,000 ppm (24.9%), averaging 27,292 ppm (2.7%), and gold values ranged from 0.1 g/t to 12,800 g/t (373.3 oz/ton), averaging 1,146 g/t (33.4 oz/ton). Rompas was a new discovery made by AREVA; there is no evidence of prior exploration, development or production.

7. Geological Setting and Mineralization a) Regional Geological Setting The Baltic Shield is characterized as the Precambrian part of Fennoscandia; it covers Norway, Sweden, Finland and the western parts of Russia. Estonia, Latvia, Lithuania and parts of Poland and Norway are covered with Phanerozoic rocks.

The Baltic Shield was created by the accretion of different micro-continents onto the Achaean core of Fennoscandia during the late Achaean and early Proterozoic. The age of the Baltic Shield decreases from the northeast to the southwest.

The Achaean Domain is located in the northeastern part of the Baltic Shield and comprises the Kola, Belomorian and Karelian Provinces, separated by early Proterozoic thrust faults. The oldest preserved rocks on the Baltic Shield, which can be found in the Karelian Province, have been referred to the Saamian Orogeny between 3.1 and 2.9 Ga. In the southwestern part of the Karelian Province Saamian rocks mainly consist of granitoids with a tonalite-trondhjemite-granodiorite composition and intermediary granulite belts. Gaál & Gorbatschev (1987) assumed that these granitoids can also be found within the basement of the other provinces. The eastern part of the Karelian Province consists of numerous greenstone belts, formed during the Lopian Orogeny. They contain a substantial amount of komatiites and are intruded by Lopian granitoids http://geoguide.geoversum.info/?page=geology2.

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Rompas is situated within the Karelian Province of the Achaean Domain (craton). The general area was mapped at 1:400,000 scale in the early 1900s. A review of the bulletin showed that the accompanying geology maps were compiled as one 1:1,600,000 scale map, and this map is quite outdated. The Geological Survey of Finland (GTK) conducted geological mapping in the Törmäsjärvi map-sheet area (2631) between 1973 and 1978, and in the Koivu map-sheet area (2633) between 1978 and 1983. Some local revisions have been made later. A national geological map was compiled by GTK at 1:1,000,000 scale and released in 1997. The entire area of the Koivu map-sheet and most of the Törmäsjärvi map-sheet area are composed of rocks of the Paleoproterozoic Peräpohja schist belt (PSB). The bedrock of the northwestern part of the Törmäsjärvi map-sheet belongs to the Central Lapland Granitoid Complex (CLGC). The few outcrops in the zone between the PSB and CLGC consist of sheared, brecciated, and mylonitic rocks belonging to the Mellajoki Suite (MS); a large fault separates the PSB to the southeast from the MS and CLGC to the northwest. The stratigraphy of the PSB was first published by Perttunen (1991) who divided the belt into eight formations that unconformably overlie the Achaean Pudasjärvi complex. The stratigraphy was re-interpreted by Perttunen and Hanski (2003), who divided the supracrustal rocks of the belt into two major groups: Kivalo and Paakkola. The current stratigraphic interpretation by Hanski, et al (2005) has expanded the number of formations from eight to thirteen (Lauri, 2011).

The Peräpohja Schist Belt (PSB), located in the Northern Finland comprises a sequence of Paleoproterozoic supracrustal rocks unconformably deposited on the Achaean Pudasjärvi complex, which lies on the southern side of the PSB. In the north the PSB is bordered by the Paleoproterozoic Central Lapland Granitoid Complex (CLGC). The western margin of the PSB is defined by the Tornionjoki River, on the western side of which no supracrustal rocks comparable to the PSB are found. Supracrustal rocks consist of quartzites, mafic volcanics and volcaniclastics, carbonate rocks, black shales, mica schists and greywackes. Basement for the PSB consists of Achaean granitoids, remnants of the greenstone belts and Paleoproterozoic layered intrusions. Maximum deposition age for the PSB has been constrained by the 2.44 Ga mafic layered intrusions, which were partly eroded when the oldest sediments started to accumulate. A minimum age of 1.88 Ga has been interpreted from the Haparanda series synorogenic monzonite intrusions that cut the youngest sediments in the PSB (Perttunen & Vaasjoki, 2001).

The rocks of the PSB have undergone polyphase deformation. They are metamorphosed under greenschist facies in the southern parts of the belt. The metamorphic grade is higher in the northern and eastern parts, where amphibolite facies conditions prevail. In the northeastern margin the rocks of the PSB are locally migmatized (Hanski et al., 2005), whereas based on our observations in the field the northern margin of the belt is most probably defined by a fault that separates the non-migmatitic rocks of the PSB from migmatitic rocks of the CLGC.

Table 2 lists these groups, formations and relevant ages, where known.

The lower Kivalo Group consists of quartzite and dolomite formations intercalated with mafic lavas and tuffs. Quartzite prevails in the rocks of the Sompujärvi, Palokivalo, Santalampi, and Kvartsimaa Formations, while the Poikkimaa and Rantamaa Formations are mainly dolomitic. The volcanic formations contain mafic lava (the Runkaus and Jouttiaapa Formations) or mafic tuffite (the Tikanmaa, Hirsimaa, and Lamulehto Formations). The rocks in the outcrops of the Santalampi Formation are pyroclastic, but many apparently local boulders exhibit distinct pillow structures.

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The overlying rocks of the upper Paakkola Group consist of turbiditic greywackes and mafic pillow lavas. The formations separating the upper and lower groups are marked by black schists with anomalous uranium and copper contents (Perttunen, 2007). The most extensive unit of the Paakkola Group is the Martimo Formation. Mica schists and black schists characterize that formation. The mostly volcanic Väystäjä Formation is stratigraphically highest in the Törmäsjärvi map-sheet area. (Perttunen & Hanski, 2003).

Table 2: Lithostratigraphy of the Peräpohja Belt (Prave, 2013)

The supracrustal rocks are cut by diabase sills and dykes (2.2 and 2.1 Ga) as well as felsic plutons (1.88 - 1.90 Ga), which are comprised mainly of granodioritic, and in lesser amounts, syenitic rocks. The felsic intrusives indicate that all of the lower part of the Lapland Triangle, or PS, are older than 1.9 Ga. Correspondingly, the sedimentation and volcanism of the lower part of the PS took place between 2.44 and 2.1 Ga, as manifested by the ages of the layered intrusions and mafic dykes (Vanhanen, 2010).

The bulk of the Rompas claims underlie sheets 2632 and 2634 which were not mapped in detail by the Geological Survey of Finland (GTK). A correlation between the 1:1,000,000 scale map with the more detailed geology to the south suggests that the western part of the claims are underlain by quartzites of the Mellajoki Suite, part of the CLGC. They are described as medium to coarse-grained and white or grey, schistose and often tightly folded.

Adjacent to the quartzite to the east and straddling the central part of the claims is a unit described as “carbonate and calc-silicate rocks, black schists and metavolcanic” rocks on the 1:1,000,000 scale map. Mica schist, black schist, conglomerate and arkosite occur central to this unit, but lie mostly north and south of the property. Both of these units are collectively mapped on the 1:100,000 scale maps as part of the Martimo Formation belonging to the Paakola Group. The Martimo is described as a mica schist containing intercalations of graphite- and pyrite-bearing phases (suggested by airborne electromagnetic data). No mention of calcsilicates,

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metavolcanics or BIF’s is made in the publication by Perttunen & Hanski, 2003. Their mapping on sheet 2631 shows a section of the Väystäjä Formation occurring southwest of the property and selvaged between the CL to the northwest and the PS to the southeast. The Väystäjä Formation is described as pillowed tholeiitic basalts with minor tuffites, some dolomite and mica schists plus a felsic volcanic rock among the mafic volcanics. The author is suggesting that the unit described as containing “metavolcanics” in the 1,000,000 scale map might be correlative with the Väystäjä Formation.

Along the eastern side of the Rompas claims the calc-silicate/metavolcanic unit is in contact with mafic and felsic metavolcanics to the south. Further south these metavolcanics join with the Jouttiaapa Formation on map grid 2633. This formation is described as dominantly amygdaloidal basalts containing quartz, chlorite, epidote and calcite amygdales. Individual flows range from 0.5 m to 20 m in thickness and are estimated in number somewhere between one and two dozen. Very minor amounts of quartzitic sediments have been noted between individual flows. Internally the flows are fairly massive and medium to coarse grained, while the flow tops are amygdaloidal. Metamorphic minerals include actinolite, albite, epidote and chlorite.

Sandwiched between the Runkaus Formation to the east and the Martimo Formation to the west is a narrow section mapped as Kvartsimaa Formation on sheet 2633; the southernmost part of the Rompas claims overlies this area. The formation is described by Perttunen & Hanski as typically a light pink or white orthoquartzite including sericite, tourmaline and rounded zircon grains. The texture is mostly granoblastic without signs of original clastic textures. Thin intercalations of siltstone and dolostone occur locally.

b) Rompas Area Geology The Rompas prospect area is dominated by a north-trending ridge comprising metabasalt, inferred volcaniclastics, carbonate-rich rocks and black graphitic metapelites (Figure 3). On the ridge crest these rocks either crop out, or are covered by a thin glacial till cover (generally less than 1 m). Either side of the ridge, small lakes, peat bogs and thicker till are abundant with isolated bedrock outcrops. However, mineralization is known to continue under the deeper till cover. The calc-silicate vein-style mineralization at Rompas is nearly all hosted by a metabasalt.

Regional folds, inferred to be related to D2 and D3 deformational events, dominate the Rompas area geology. The D1 event in the Rompas area is difficult to identify, but regional work suggests it is now present as transposed isoclinal folds with a high temperature foliation parallel or sub-parallel to the D2 foliation. D2 formed upright N-striking tight to isoclinal folds at Rompas that are in turn folded about upright open to tight E-trending D3 folds. Of significance at Rompas is that the D2 foliation is quite variable in intensity, with an increase towards South Rompas to such an extent that any original basaltic rock textures are destroyed.

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OVER PAGE

Figure 3: Rompas Geology and Structure Date: 27 August 2014, Author L. Dahlenborg, North to top of map

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3,410,000 mE3,405,000 mE3,400,000 mE3,395,000 mE

7,38

0,00

0 m

N7,

370,

000

mN

7,36

5,00

0 m

N7,

375,

000

mN

Ma�c dykes (magnetic andnon-magnetic)

Non/weakly magnetic granitoid

Pyroxenite to meta-komatite

Garnet-mica schist

Strongly magnetic granitoid

Tremolite-quartz +/- mica schist

Albite Breccia bodies (structurally hosted)

Felsic meta-volcanic

Mica Schist(magnetic and non magnetic)

Amphibolite

Magnetic metasediment(mixed Po -bearing BSH, calc-silicate, quartz)

Ma�c meta-volcanic(intrudes A + B of Rompas)

Calcsilicate (including mapped skarn rocks)

Quartzite +/- calcsilicate + mica schist(including altered quartzite)

F1 folds

F2 folds

F3 folds

Magnetic highs

0 20001000meters

Granted Claims

MAWSON RESOURCES LTD

SCALE:

Finnish KKJ Zone 3

GEOLOGY AND STRUCTURE Geology compiled by L. Dahlenborg

after L. Lauri, (2010) and L.Rankin (2010)

see grid

ROMPAS PROJECT FINLAND

ROMPAS TREND

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Amphibolite facies metamorphism has accompanied the development of the S2 foliation with biotite and amphibole (largely hornblende) defining the fabric. Biotite is an important part of the most foliated metabasalts, providing evidence of early potassic alteration. Within the metabasalts, variably oriented large amphibole grains up to 8 mm long grow across the S2 foliation throughout the North and South Rompas prospect areas. These may be in the cummingtonite or anthophyllite amphibole groups, in addition to ‘more normal’ hornblende compositions. Indeed, some samples are found to contain hornblende, cummingtonite and anthophyllite.

Comparison of the geochemical composition of the Rompas metabasalts with other mafic rocks within the PSB by Mustonen (2012) reveals a geochemical similarity with the Runkaus Formation, the oldest basalt within the Peräpohja stratigraphy. U-Pb dating of secondary titanite from the Runkaus gives a minimum age of approximately 2.25 Ga (Huhma et al., 1990) implying a similar minimum age of the Rompas basalts. Near Rompas, zircons have been separated from rocks mapped as the Martimo Formation, a graphitic schist inferred to occur within the Paakkola Group.

The dilemma at Rompas is that no unconformity has yet been recognized in the sequence and that the metamorphic age based on uraninite textures apparently synchronous with metamorphism (see below) is less than the maximum age of the Martimo Fm. The Martimo Formation appears to have enjoyed the same metamorphic history as the metabasalts. At the time of writing, this dilemma remains unsolved.

c) Mineralization The Rompas-Rajapalot project is a new discovery in Northern Finland where high-grade gold and uranium have been found within an area approaching 10km by 10km.

Gold and uranium distribution within the initial discovery area at Rompas is nuggety. Thin and very high-grade drill intercepts are common, matching the many hundred surface trench exposures of significant grades found over the 6 kilometre trend. What is clear from the drilling and trenching at North and South Rompas is the strong host rock control on mineralization – a distinctive metabasalt (Figure 4). Uraninite and gold are found within or marginal to carbonate-calcsilicate-quartz veins in metabasaltic host rocks. Vein densities in the adjacent metasedimentary rocks are similar to the metabasalt, but to date lack any significant gold (“Au”) or uranium (“U”) intersections. Thus, wallrock interaction with the basalt is inferred to be the key control on gold and uraninite formation, although the actual mechanisms remain the subject of much debate.

The gold itself is of high fineness (>95% Au), with minor Te, Ag and Cu recorded (Nancy/CEGRU research work). Drilling up to 100 metres depth has not revealed any variation in fineness. Petrographic examination by a number of workers agrees that the gold is paragenetically later than the uraninite, commonly occupying cracks within uraninite. Sulphide minerals are not commonly directly associated with gold and uraninite. Fine pyrrhotite is a ubiquitous trace component of the metabasalt, resulting in a stronger IP chargeability response than the adjacent rocks. Trace gold with fine molybdenite has also been observed within the ROM0011 intersection (pers. comm. Molnar and others, GTK).

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Figure 4: Rompas Rajapalot Prospect -Basaltic Host Rocks Date: 27 August 2014, Author M.R. Hudson, North to top of map

Uraninite is the predominant uranium-bearing mineral, with two varieties observed in petrographic work by Nancy/CEGRU researchers. Paragenetically late gummite is locally present in surface samples occurring between uraninite grains. Radiogenic galena is also observed associated with the uraninite.

Due to the recent discovery history at Rajapalot (Figure 5), much less information has been collected. However, the mineralization differs in that is more sulphidic with strong potassic alteration and is predominantly of a disseminated, replacement style and is therefore directly targetable by IP chargeability. Four prospect areas have been defined within topographic highs within a predominantly swampy area. These areas are the Hirvimaa, Palokas, Joki and Rumajärvi prospects and located within a 2 km by 2 km area, within the hinge of a complex fold structure within the contact zone between quartzitic and basaltic rocks which are geochemically distinct from the Rompas area. The style of mineralization in the Hirvimaa and Joki areas is similar to Rompas and consists of calc-silicate veins in albitized quartzites and basalts, with more pyrite and magnetite than observed in Rompas. Mineralization at Palokas and Rumajärvi appears to be a new style and consists of highly altered quartzites with albite, carbonate, amphibole, sericite and biotite with disseminated and stockworks of pyrite. Gold mineralization appears to be

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disseminated, replacement style, within the host rock, with no obvious associated calc-silicate veining.

Figure 5: Rajapalot Overview Map with IP Chargeability Date: 27 August 2014, Author J. Kinnunen

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Deposit Types The mineralization at Rompas-Rajapalot comprises two different styles: firstly, a nuggety style where gold and uranium is found within quartz-carbonate-calc-silicate veins or their wallrocks in metabasaltic host rocks. Uranium is largely located in uraninite and gold is found both within cracks in uraninite and as free gold adjacent to uraninite, often associated with pyrobitumen. The second style of gold-uranium mineralization is of a more sulphidic, potassic and disseminated character hosted in metabasaltic and quartzitic rocks.

The precipitation mechanism for both styles of mineralization and their relationship is still unclear and debate continues as to the exact genesis of this deposit. Elements of the Rompas mineralized trend, namely the metasomatic alteration, could just as easily have been caused by a hydrothermal event, but as yet, no direct evidence of an underlying, nearby, mineralizing intrusive has been discovered. Early evidence is just emerging suggests that organic matter also plays an important role in precipitating the high-grade gold-uranium Rompas-Rajapalot prospect in the Peräpohja Schist Belt.

Due to the lack of detailed work that has been done on this relatively new discovery, little is understood about the nature of the mineralizing controls, as yet. In any event, it would appear that the target would be of a large, bulk-tonnage, fracture-controlled nature at Rajapalot and potentially economic high grade vein array at Rompas.

8. Exploration Rompas Vein Style

The initial discovery area, Rompas, is a hydrothermal vein style system defined over a 6.0 kilometres strike and 200-250 metres width. Exploration on the project started in May 2010. During that year, 80 channel samples averaged 0.59 metres @ 203.66 g/t gold and 0.86% uranium oxide and during 2011 the weighted average of all 74 channel intervals was 1.40 m @ 51.9 g/t gold and 0.13% uranium oxide. Unrepresentative grab sample results include values up to 33,200ppm gold and 56.6% uranium oxide at Rompas.

As discussed further in Section 10, from mid-2011 to the end of the period Mawson has drilled 8,164 m in 90 holes at Rompas. This has comprised 2,462.8 m in 29 drill holes at North Rompas; 2,436.2 m in 29 drill holes in the northern block at South Rompas; 2,504.3 m in 24 holes within the southern block at South Rompas; and 761.5 m in 8 drill holes at Northern Rajapalot.

In August 2012, results from the first drill program at Rompas returned 6 metres at 617 g/t gold in drill hole ROM0011 including 1 metre at 3,540 g/t gold and 1 metre at 114.5 g/t gold in drill hole ROM0015. These results confirmed the significance of the hundreds of significant grade surface occurrences that were channel sampled during 2010 and 2011.

A second drill program commenced in December 2012. At North Rompas the best results include 0.4 metres at 395 g/t gold and 0.41% U3O8 from 41.0 metres in drill hole ROM0052, the most southerly drill hole of the program; and 1.1 metres at 9.8 g/t gold and 0.16% U3O8 from 78.5 metres in drill hole ROM0053.

In September 2012, Mawson announced a new discovery at the Rajapalot area located 8 kilometres to the east of the Rompas trend. The style of mineralization at Rajapalot is predominately sulphidic and of a disseminated or replacement style, which differs from the vein style observed at Rompas. Highlights from this work include prospecting grab samples taken

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from outcrop that returned 2,817 g/t gold, 2,196 g/t gold, 1,245 g/t gold, 933 g/t gold, 151 g/t gold and 135.5 g/t gold. A total of 52 grab samples from the Rajapalot prospect to date average 152.8 g/t gold and range from 0.001 g/t to 2,817 g/t gold.

The completion of a LIDAR airborne survey at the end of 2012 gave Mawson’s field geologists the ability to prospect and map Rompas much more rapidly and effectively. With this new technology, outcrops that previously took weeks to locate and then map in 2011 and 2012, can now be identified and mapped in days.

Other sampling programs include a heavy mineral orientation program at South and North Rompas (Figure 6).

Figure 6: Rompas Heavy Mineral Sampling Date: 27 August 2014, Author M.R. Hudson, North to top of map

Five non-selective, 5 litre heavy mineral samples were collected, with one from South Rompas returning one of the largest accumulations of gold nuggets ever identified within a heavy mineral sample from the Fennoscandian Shield. This sample contained 5,000 gold nuggets, with 40-50 gold grains in the 0.5-2 mm fraction. Other samples included one sample up-ice direction with 18 nuggets, 100 m north-west of the last outcrop in North Rompas (Figure 6). The three other samples contained 100, 1,000 and 100 nuggets respectively. Eighty additional regional heavy mineral samples have been collected and will be processed to further test this as a suitable method for locating further blind gold mineralization.

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All the geochemical programs in combination with other datasets suggests Rompas is shaping up at all scales with 58 gold anomalous target areas from surficial sampling and prospecting identified within the broad Rompas area for follow up during the 2013 field season.

Since acquiring the project in April 2010, the Issuer has collected 80 channel samples that averaged 0.59 metres @ 203.66 g/t gold and 0.86% uranium oxide in 2010. During 2011 the weighted average of all 74 channel intervals was 1.40 m @ 51.9 g/t gold and 0.13% uranium oxide. Unrepresentative grab sample results include values up to 33,200ppm gold and 56.6% uranium oxide at Rompas.

Mawson has collected a total of 2,808 surficial soil and till samples over an area exceeding 55 km by 30 km. Sample spacing has ranged from 1 km to 250 m. Mawson’s geochemical rock chip, grab and channel sample database over this large area now contains 1,171 samples which average 212 g/t gold and 0.8% U3O8. Of the 1,171 samples, 84 samples assay more than 100 g/t gold. Gold values range from 33,320 g/t gold to <0.001 g/t gold and U3O8 values from 49.5% to <4 ppm. Channel samples are considered representative of the in-situ mineralization sampled, while grab samples are selective by nature and are unlikely to represent average grades on the property.

Geophysical surveys conducted at Rompas include:

A 3,279 line-km airborne radiometric-magnetic survey was in 2010;

A 28 line-km gradient IP and a 5 line-km dipole-dipole IP survey were completed in 2011;

In 2012, Mawson completed 62 line kilometres of gradient array induced polarization geophysical surveying;

A 48.3 km of magnetic and 35.3 km of electromagnetic (“EM – Slingram”) ground-based geophysical surveys at Rajapalot;

A 827 line-km helicopter-borne VTEM Plus electromagnetic, magnetics and radiometric geophysical survey over the Rajapalot area in 2013 (results pending);

A small Mise-La-Masse electric survey at South Rompas in 2013;

A small radiometric probe survey at North Rompas;

A 40m spaced 6 kilometre gravity traverse across the Rompas trend in 2013 (results pending).

Rajapalot Disseminated Style

Rajapalot is located 8 kilometres to the east of the Rompas vein trend. The style of mineralization at Rajapalot is predominately sulphidic and of a disseminated or replacement style, which differs from the nuggety vein style observed at Rompas. Rajapalot is the primary target area for the Company.

Surface sample highlights Rajapalot include prospecting grab samples taken from outcrop that returned 2,817 g/t gold, 2,196 g/t gold, 1,245 g/t gold, 933 g/t gold, 151 g/t gold and 135.5 g/t gold. A total of 52 grab samples from the Rajapalot prospect to date average 152.8 g/t gold and

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range from 0.001 g/t to 2,817 g/t gold. All samples are prospecting grab samples. These are selective by nature and are unlikely to represent average grades on the property.

Discovery grab samples from the Rajapalot project returned gold mineralization from three distinct areas, namely the Palokas, Joki and Rumajärvi prospects. The areas were targeted with regional geophysics and surface soil geochemistry. Rumajärvi lies 1.5 kilometres south of Palokas, while Joki is located 1 kilometre southeast of Palokas. Each prospect area is characterized by minor outcrop on a topographic high, within a predominantly swampy terrain and therefore very little in situ bedrock has been located. Little outcrop has been found between the prospect areas. As the same mineralized rock types occur in outcrop, the glacial boulders sampled and reported here are considered to be proximal to their source.

In October 2013, Mawson announced the first core test of Rajapalot from the Palokas prospect. Drilling intersected 9 metres at 10.2 g/t gold from surface, including 3 metres at 27.5 g/t gold in hole PRAJ0003. Palokas is part of the Rajapalot area, located 7 kilometres east of our drilling in the vein style mineralization at Rompas. Further high grade, thick and near-surface core sample results in November 2013 and January 2014, and included 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006; 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres); 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005; 19.0m @ 2.3 g/t gold from 8.0 metres from PRAJ0022; and 8.7m @ 4.6 g/t gold from 16.9 metres from PRAJ0025.

Multi-element analyses from all core sample holes from the Palokas project at Rajapalot (holes PRAJ0003 to PRAJ0025) shows consistently low uranium (weighted average through quoted intersections is 36ppm uranium and 5.2g/t gold) and high cobalt grades associated with gold mineralization. Cobalt also forms a broader halos around lower (>0.1 g/t) grade gold mineralized zones. The low uranium grades drilled at Palokas also support the concept of both gold-rich and uranium-rich styles occurring within the Rompas-Rajapalot mineral field.

Geochemical sampling at Rajapalot is coincident with a versatile time domain electromagnetic (“VTEM”) geophysical conductor that extends for more than 500 metres through an area with <1% outcrop, and forms part of a 3.5 kilometre target horizon between basaltic and quartzitic rocks. In addition, 26 line kilometres gradient array induced polarization ("IP"), 480 metres of pole-dipole IP and 27 line kilometres of ground magnetic surveys were completed at Rajapalot during the quarter. The geophysical surveys tested 5 kilometres of target horizon along strike from the drill area at Palokas. Interpretation of the surveys identified multiple near-surface and high priority targets that extend to depth immediately along strike, and extending up to 4 kilometres from the drilled high grade and thick drill results discovered from surface Pole-dipole induced polarization geophysical anomalies extend beyond the 150 metre nominal depth limit of the survey.

These core sample results have produced the widest and most consistent gold grades with low uranium grades at Rompas to date. In context with the extensive VTEM, induced polarization and magnetic geophysical anomalies, Palokas forms a strong exploration target.

Fine disseminated gold mineralization at Palokas occurs within calcsilicate-biotite-tourmaline-pyrrhotite rocks in a contact zone between mafic rocks and relatively oxidized quartzites. The true thicknesses of the mineralized intervals is interpreted to be approximately 80% of the sampled thickness.

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Mawson announced the extension of the Rajapalot mineralized system with the discovery of high grade gold and uranium surface grab samples located immediately along strike and approximately 2 kilometres from Palokas in Feb 2014. In summary:

seventy-four prospecting grab samples taken from outcrop and glacial boulders, with better results including:

3,220g/t gold and 0.3 uranium; 248 g/t gold and 0.7% uranium; 43.1 g/t gold and 27.4% uranium; 9.8 g/t gold and 1.2% uranium; 1.8 g/t gold and 1.7% uranium; 0.3 g/t gold and 1.5% uranium;

in total 9 project areas have now been defined at Rajapalot within an area extending over 2.5 kilometres by 3.5 kilometres; and

at least two styles of gold mineralization now exist at Rajapalot, the first with extremely low uranium grades (Palokas), the second with higher uranium grades as evidenced by the new surface sample results.

New samples are all prospecting grab samples which are selective by nature and are unlikely to represent average grades on the property.

Mineralization from the new area is hosted in sulphide and biotite rich metasedimentary and volcanic rocks, with gold occurring as a disseminated or replacement style. The glacial boulders sampled and reported are the same lithologies as nearby outcrops and appear to form boulder trains, and are thus considered to be proximal to their source. Of note are the high uranium grades discovered in these new areas, suggesting the presence of gold only and uranium- dominant mineralized styles at Rajapalot. Like most of the Rajapalot area, the new prospect areas are within a predominantly swampy terrain and therefore very little in-situ bedrock has been located.

A 26 line kilometre survey by Geovista AB of Lulea, Sweden of gradient array induced polarization (“IP”), 480 metres of pole-dipole IP and 27 line kilometres of ground magnetic surveys were reported at Rajapalot during March 2014.

Chargeable, low resistive and magnetic anomalies define multiple high priority target areas, for follow-up beneath the predominant thin 2 to 5 metre thick glacial soils, for more than 4 kilometres of strike. Chargeable and low resistive anomalies discovered below drilled gold mineralization extend beyond the 150 metre nominal depth limits of the survey technique. Airborne electromagnetic (“VTEM”) anomalies generated from a survey flown late last year similarly shows conductors that extend immediately below drilled near-surface mineralization, to at least 400 metres depth. The VTEM conductors correlate well with many of the IP chargeable and low resistive anomalies.

A total of 120 drill holes were completed by independent drilling contractor Ludvika BorrTeknik AB, within an area of 2.5 kilometres by 0.5 kilometres. during the April-May 2014 at the Hirvimaa prospect, which is located 600-1300 metres along strike from the Palokas prospect drill area. The aim of the program was to map and define gold anomalous bedrock beneath glacial soils that cover 98% of the area and to refine targets for deeper drilling. The average depth of each drill hole was 7.3 metres and the average thickness of glacial soil overburden was 3.9 metres. An additional in-house diamond drill rig with capability to drill deeper was mobilized at

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the end of the program to complete 16 holes for 116.65 metres. The boulders that were drilled are large (average 0.85m3), angular and considered to be locally sourced from their original position. Best results returned from the shallow diamond drill program included 0.6 metres @ 21.3 g/t gold and 0.8 metres @ 13.1 g/t gold, from a large mineralized boulder. Boulders have the same mineralization style as the Palokas prospect, where recent drill results included 19.5 metres @ 7.4 g/t gold from 1.3 metres. The bedrock source for the gold-bearing boulders remains to be identified. The shallow drill program also defined a 600 metre long mineralized trend, defined by lower tenor gold anomalism in bedrock, with the best result being 1 metre @ 0.12 g/t gold.

Regional Sampling

The extensive data collected from Rompas during the last 3 field seasons has provided an excellent understanding of the exploration potential. Mawson has collected a total of 2,808 surficial soil and till samples over an area exceeding 55 km by 30 km. Sample spacing has ranged from 1 km to 250 m (Figure 7). Known gold mineralization correlates well with surficial soil anomalies and many untested surface targets remain over a larger area.

Figure 7: Rompas Levelled A Horizon and C Horizon Till Au-W Geochemistry Date: 27 August 2014, Author M.R. Hudson, North to top of map

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10. Drilling From mid-2011 to August 2014, Mawson has drilled 11,912.5 m in 357 diamond drill holes at Rompas-Rajapalot with an average depth of 33.4 metres as per Table 3 below. (Figures 8-15; Appendix 2).

Table 3: Drill statistics from the Rompas-Rajapalot, August 2014

Prospect  Number of Holes Metres  Best Result 

Palokas  28           573.7   19.5m @ 7.4 g/t gold from 1.3 metres (PRAJ0006) 

South Rompas  55       5,149.5   6 metres at 617 g/t gold from 7 metres (ROM0011) 

North Rompas  29       2,463.1   0.4 metres at 395 g/t gold 41 metres (ROM0052) 

Shallow North Rompas  28           156.7   2.05m @ 0.1 g/t Au from 2.1 metres (NROM024) 

Kaita  13           784.2   1m @ 4.9 g/t gold from 49 metres (KD0009) 

Kaita Shallow  37           451.6  0.3m @ 16.3 g/t from 8.2 metres (PROM0017) 

Hirvimaa Shallow  120       1,050.9   0.6 metres @ 21.3 g/t gold(drilled boulder) 

Hirvimaa Regional  8           757.1   3.1 metres @ 0.4 g/t Au from 6 metres in PAL003B 

Rajapalot Regional  39           525.8   1m @ 0.68 g/t Au from 17 metres (PRAJ0049) 

TOTAL  357    11,912.5    

Rajapalot

In October 2013, Mawson announced the first core test of Rajapalot from the Palokas prospect. Drilling intersected 9 metres at 10.2 g/t gold from surface, including 3 metres at 27.5 g/t gold in hole PRAJ0003. Palokas is part of the Rajapalot area, located 7 kilometres east of our drilling in the vein style mineralization at Rompas. Further high grade, thick and near-surface core sample results in November 2013 and January 2014, and included 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006; 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres); 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005; 19.0m @ 2.3 g/t gold from 8.0 metres from PRAJ0022; and 8.7m @ 4.6 g/t gold from 16.9 metres from PRAJ0025 (Figures 13-15).

A total of 120 drill holes were completed by independent drilling contractor Ludvika BorrTeknik AB, within an area of 2.5 kilometres by 0.5 kilometres during April-May 2014 at the Hirvimaa prospect, which is located 600-1300 metres along strike from the Palokas prospect drill area. The aim of the program was to map and define gold anomalous bedrock beneath glacial soils that cover 98% of the area and to refine targets for deeper drilling. The average depth of each drill hole was 7.3 metres and the average thickness of glacial soil overburden was 3.9 metres. An additional in-house diamond drill rig with capability to drill deeper was mobilized at the end of the program to complete 16 holes for 116.65 metres. The boulders that were drilled are large (average 0.85m3), angular and considered to be locally sourced from their original position. Best results returned from the shallow diamond drill program included 0.6 metres @ 21.3 g/t gold and 0.8 metres @ 13.1 g/t gold, from a large mineralized boulder. Boulders have the same mineralization style as the Palokas prospect, where recent drill results included 19.5 metres @ 7.4 g/t gold from 1.3 metres. The bedrock source for the gold-bearing boulders remains to be identified. The shallow drill program also defined a 600 metre long mineralized trend, defined by lower tenor gold anomalism in bedrock, with the best result being 1 metre @ 0.12 g/t gold.

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“PRAJ” Core sampling at Rajapalot was undertaken by Mawson Staff who provided EW (25.2 mm) diameter core. Core recoveries were excellent and average close to 100% in fresh rock. After photographing and logging, core intervals averaging 1 metre in length were cut in half at the Geological Survey of Finland (GTK) core facilities in Rovaniemi, Finland. These half-core one metre samples weigh less than 0.7 kilograms. The remaining half core is retained on site for verification and reference purposes. Analytical samples were transported by Mawson or GTK personnel from GTK to the Labtium Oy ("Labtium") laboratory in Rovaniemi, Finland where they were prepared and analyzed for Au by 705P techniques and multi-element analysis by XRF technique (pellet), method +175X. The QA/QC program of Mawson consists of the systematic insertion of certified standards of known gold content, with blanks at the beginning of each batch. In addition, Labtium inserts a number of blanks and standards into the analytical process.

Rompas

In early 2011 Mawson conducted one small shallow (“till”) stratigraphic drill program. A total 155.65 m were drilled in 28 holes located along two traverse lines located 100 m and 300 m to the north of the North Rompas mineralized zone (Appendix 2). The stratigraphic drill program was designed to test for the presence of the host rock sequence undercover to the north of Rompas and not to drill beneath known mineralized zones. The program was successful in proving the altered host sequence continues at least 350 m undercover from the last mineralized site at North Rompas. Glacial cover averaged 3 m to 5 m over the area drilled while drill holes averaged 5.5 m depth.

To date from the deeper diamond drilling, the most encouragement has come from the northern block of South Rompas (Figure 9 and 10), with both prospect scale shallow drilling and trenching defining a coherent mineralized sequence. South Rompas is characterized by gold mineralization constrained to one specific host rock type (metabasalt) within a broader uranium halo. Within this halo the:

The top 24% of all trench and drill assays above the lower cut of 0.5 g/t Au or 100 ppm U3O8, have a grade of 100 g/t or more and the top 24% of all intersections have a grade of 0.42% U3O8 or higher (Figure 12);

Top 25% of drill intersections only have a grade of 7.7 g/t or higher;

The highest grade drill hole intersection is 3,540 g/t gold over 1 m. The highest grade uranium intersection is 3.6% U3O8 over 0.6 m in a trench. The highest grade drill intersection grade of 0.7% U3O8 over 1.0 m;

Mineralization in the vein system, to date, is characterized by narrow intersection widths of 1-2m with an average of 0.9 m thickness;

Drilling, to date, has been shallow with 46% of intersections at 20 m down hole depth or less;

11 out of 13 holes drilled in 2013 winter drill program at South Rompas had at least one intersection that exceeded lower cut 0.5 g/t gold or 100 ppm U3O8.

Mawson is now evaluating further drilling or bulk sampling programs in order to best determine the gold grade in this nuggety and high-grade gold system.

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All drilling at Rompas has been NQ or HQ diameter drill core. Drill recoveries are excellent and average close to 100% in fresh rock. After photographing and logging, core intervals averaging between 0.7 to 1.0 metres in length were cut in half at the Geological Survey of Finland core facilities in Rovaniemi, Finland. These half core one metre samples weigh less than three kilograms. Drill intersections are estimated to be 70 to 90 per cent of the true width.

Drilling at the Kaita prospect at the most southern end of the Rompas vein system did not intersect mineralization of economic interest. A 13 diamond drill hole program for 784.2 metres campaign was conducted during September-October of 2013. The best diamond drill result was 1m @ 4.9 g/t gold from 49 metres in KD0009. Better surface diamond cut trench results from Kaita included 1.65 metres @ 29.1 g/t gold in TR107465; 1.2 m @ 27 g/t gold in TR118401, 0.4 m @ 132 g/t gold in TR118407 and 1.5 m @ 42.2 g/t gold in TR118425.

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OVER PAGE Figure 8: North Rompas Drilling Plan

Date: 27 August 2014, Author M.R. Hudson, North to top of map

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3,399,650 mE3,399,500 mE 3,399,550 mE 3,399,600 mE3,399,350 mE 3,399,400 mE 3,399,450 mE3,399,300 mE7,

378,

400

mN

7,37

8,45

0m

N7,

378,

500

mN

7,37

8,35

0m

N7,

378,

300

mN

3,399,650 mE3,399,500 mE 3,399,550 mE 3,399,600 mE3,399,350 mE 3,399,400 mE 3,399,450 mE3,399,300 mE7,

378,

400

mN

7,37

8,45

0m

N7,

378,

500

mN

7,37

8,55

0m

N7,

378,

350

mN

7,37

8,30

0m

N

0 5 10

metres

20 Scale 1:1,000

ROM0043

ROM0048

ROM0046

ROM0064

ROM0042

ROM0056ROM0047

ROM0045

ROM0040

ROM0055

ROM0067

ROM0068

ROM0052

ROM0051

ROM0053

ROM0049ROM0050

ROM0044

ROM0041

ROM0054

ROM0061

ROM0057

ROM0058

ROM0059

ROM0065

ROM0066

TR108559

TR108924

TR108562

TR108560

TR104754

TR107438

TR107440

TR108572

TR107446

TR107447

TR108563

TR108565

TR108564

TR10744B

TR10744CTR107451

TR108566

TR104742

TR104742C

TR104743b

TR104744

TR104745

TR104746

TR108569

TR108571

TR108570

TR104749

1.30 5.40 1949

1.53 2.94 1490.28 21.60 1155

1.00 1.54 19

1.40 2528.78 50705

1.14 36.60 1999

1.20 37.39 152

5.00 0.60 38

1.00 1.43 25

0.28 220.00 6272

2.05 15.28 746

0.69 87.11 3528

1.50 1.43 7

3.00 0.26 7

width Au g/t U3O8ppm

1.14 9.82 2490.65 4.09 24490.13 3.66 4115

0.20 10.95 2146

1.50 1.35 51.55 11.59 728

TR108566

TR104742TR104742C

TR107444B

TR108563

TR107446

TR107440

TR108559

TR104749TR104745TR104744

TR108571

TR108569TR108570

TR107447TR107451

TR107437

TR108560

TR108572TR108915

TRENCH

HoleID Depth Depth Width Au g/t U308ppmfrom to

ROM0042 2.4 3.1 0.7 1.00 50ROM0044 19.7 20.4 0.7 0.14 161ROM0044 21.8 22.5 0.7 0.51 3ROM0044 23.9 24.6 0.7 0.82 71ROM0047 35.4 36.8 1.4 0.01 395ROM0047 44.6 46.0 1.4 0.00 181ROM0047 51.9 56.1 4.2 0.00 306ROM0048 26.0 26.7 0.7 1.15 40ROM0049 25.9 26.6 0.7 0.34 166ROM0050 7.1 7.8 0.7 3.51 67ROM0050 19.6 20.3 0.7 0.55 91ROM0052 41.0 41.4 0.4 395.00 4118ROM0052 61.5 62.2 0.7 0.00 179ROM0053 13.7 14.4 0.7 1.14 24ROM0053 34.7 35.4 0.7 0.67 15ROM0053 78.5 79.6 1.1 9.81 1519ROM0053 79.0 79.6 0.6 17.95 1059ROM0057 43.2 43.4 0.2 0.05 212ROM0065 77.8 78.4 0.6 0.11 310ROM0067 20.2 20.7 0.5 0.01 136ROM0067 52.9 53.6 0.7 0.00 171ROM0068 30.3 31 0.7 2.46 1403

March 2013Figure 3: Plan View of Drillholes from North Rompas with Surface Sampling. New Asssy Results from Drillholes ROM0061 - ROM0068.

0 25 50

metres

Trench Trace

Rock Chip Sample

>100 10 to 1001 to 10<1

Drill Collar and Trace

Quoted assay interval above cut o�

Quoted assay interval above cut o�

3,399,400 mE 3,399,500 mE

7,37

8,60

0m

N7,

378,

700

mN

7,37

8,50

0m

N

3,399,200 mE 3,399,300 mE

7,37

8,30

0m

N7,

378,

400

mN

ROM0060

ROM0061

ROM0062

ROM0063

MAP AREA

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OVER PAGE Figure 9: South Rompas Drilling Plan

Date: 27 August 2014, Author M.R. Hudson, North to top of map

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7,37

3,65

0m

N7,

373,

700

mN

7,37

3,75

0m

N7,

373,

800

mN

7,37

3,85

0m

N3,401,400 mE 3,401,450 mE 3,401,500 mE 3,401,550 mE3,401,350 mE3,401,250 mE 3,401,300 mE

0 5 10

metres

20 Scale 1:1,000

3,401,450 mE 3,401,550 mE7,

373,

850

mN

3,401,250 mE 3,401,350 mE7,

373,

750

mN

7,37

3,65

0m

N

0 5 10

metres

20 Scale 1:1,000

basalt

basalt

basa

lt

basalt

basa

lt

basalt

basalt

basalt

TR107581

TR107580

TR108534

TR107577

107578

TR107575

TR107574

TR104731

TR104739

TR107752

TR104738

TR104730

TR104737

TR108535

TR107582

ROM0036 ROM0035

ROM0020

ROM0018

ROM0022

ROM0013

ROM0009

ROM0075

ROM0077

ROM0074ROM0073+

ROM0080

ROM0028

ROM0079

ROM0082

ROM0025

ROM0070ROM0012

ROM0069

ROM0014ROM0071+ROM0072

ROM0037ROM0011

ROM0017ROM0010

ROM0015

0 25 50

metres

Projection Finnish KK3

March 2013

Trench Trace

Rock Chip Sample

>100 10 to 1001 to 10<1

Drill Collar and Trace

Figure 2: Plan View of Drillholes from South Rompas with Surface Sampling. New Assay Results from Drillholes ROM0069 - ROM0082.

Quoted assay interval above cut o�

Quoted assay interval above cut o�

Geological ContactTR107590 0.70 800.15 40639

TR107588 0.60 1256.14 36095TR107588C 0.15 871.83 32352

TR104724B 1.6 257.10 14619

TR107587 0.29 1.46 876

TR107752 0.56 103.84 2279

TR104731 0.84 88.96 465

TR104730 0.45 4.67 221

TR104737 0.97 244.97 4271

TR104738 0.95 1424.22 15298

TR107574 0.25 1012.72 23645

TR104739 0.08 217.30 9208

TR107575 0.35 1040.35 20273

TR107577 1.07 1.02 166

TR107580 0.67 3.51 4787

TR108535 0.50 4.76 43

TR107581 0.38 20.67 12343

TR107578 0.35 1459.87 15882

TR107579 0.60 47.00 4662

TR107582 0.44 34.19 2319

TR108534 1.90 2.52 37

width Au g/t U3O8ppmTRENCH

HoleID Depth Depth Width Au g/t U308ppmfrom to

ROM0007 36 37 1 1.60 204

ROM0008 100 101 1 0.55 16.2ROM0009 46 47 1 1.70 43.1ROM0010 29 30 1 10.80 367ROM0011 7 8 1 22.80 1130ROM0011 8 9 1 0.10 4.4ROM0011 9 10 1 0.00 1.5ROM0011 10 11 1 0.00 1ROM0011 11 12 1 3540.00 1770ROM0011 12 13 1 137.00 650ROM0011 87 88 1 9.70 338ROM0012 17.8 18.8 1 6.30 409

ROM0013 36.3 37.6 1.4 0.56 18.2ROM0015 14 15 1 2.50 3.7ROM0015 44 45 1 114.50 2830ROM0017 15 16 1 0.90 95.4ROM0017 23 24 1 6.60 95.4ROM0018 9 10 1 0.60 27.3ROM0022 10 11 1 0.70 1.5ROM0022 22 23 1 0.60 2.1ROM0022 145 146 1 1.00 29.3

ROM0034 98 99 1 2.95 7370ROM0037 17 18 1 4.33 38.3ROM0037 68 69 1 3.18 1.7ROM0070 17.7 18.2 0.5 1.90 104ROM0071 16 17.4 1.4 0.86 27ROM0071 25.8 27.2 1.4 1.23 2ROM0072 18.7 20.1 1.4 0.80 19ROM0072 41.8 42.5 0.7 2.29 118ROM0073 0.55 1.4 0.85 0.79 33ROM0073 4.2 5.6 1.4 1.30 14ROM0074 16.45 16.95 0.5 148.00 4162ROM0076 41.35 41.85 0.5 0.39 120ROM0077 10.3 10.8 0.5 0.14 672ROM0077 31.9 32.4 0.5 0.15 219ROM0078 55.4 56.1 0.7 3.07 215ROM0079 5.8 7.2 1.4 17.64 270ROM0080 32 33.4 1.4 9.19 20ROM0081 41.3 42.5 1.2 7.74 267

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Figure 10: South Rompas Cross Section 7373780N Date: 27 August 2014, Author M.R. Hudson, Section Looking North

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OVER PAGE

Figure 11: South Rompas Long Section Date: 27 August 2014, Author M.R. Hudson, North the right of map

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100mR

L200m

RL

150mR

L7,373,750mN

7,373,750mN

7,373,700mN

7,373,700mN

100m

RL

7,373,800mN3,401,350mE

7,373,850mN

7,373,850mN

7,373,800mN3,401,350mE20

0mR

L15

0mR

L

ROM0025

ROM0070ROM007

5

VG

ROM0081

VG

VG

VG

VGVG

VG

VG

VG

ROM0074

VG

ROM0080ROM0079

ROM0011

ROM0037

ROM0077

ROM0076

ROM0009

ROM0073

0 5 10

metres

20 Scale 1:750

0 5 10 20

metres

7,37

3,70

0 m

N7,

373,

800

mN

3,401,200 mE 3,401,300 mE 3,401,400 mE

7373680N

7373720N

7373750N7373765N

7373780N

7373800N

7373820N

7373840N

BasaltBasalt

Drill Hole & Gamma >20cps

Drill hole & gold intercept > 0.5g/t Au

VG Visible Gold

Trench with gold intercept > 0.5g/t Au

Long Section

Surface samples> 0.5 ppm Au

VG

VG

VG

VG VG

VG

ROM0025ROM0070

ROM0079

ROM0081

ROM0080 ROM0073

ROM0074

ROM0011 ROM0077

ROM0037

ROM0075

ROM0076

ROM0009

7.1 ppm Au

2,177.1 ppm Au158.9 ppm Au

7,719.7 ppm Au

1.14 ppm Au

0.1 @ 217.3 g/t Au

0.95 @ 1424.2 g/t Au0.25 @ 1012.7 g/t Au

0.97 @ 245.0 g/t Au 0.45 @ 4.7g/t Au 0.8 @ 88.9 g/t Au0.4 @ 0.95 g/t Au

0.1 @ 217.3 ppm Au

0.5m @ 1.9 g/t Au

1.4m @ 17.6 g/t Au

1.4m @ 9.2 g/t Au1.2m @ 7.7 g/t Au

0.85m @ 0.79 g/t Au1.4m @ 1.3 g/t Au

0.5 m@ 148 g/t Au

1.0m @ 0.78 g/t Au

1.0m @ 9.7 g/t Au

1.0m @ 22.8 g/t Au1.0 m @ 4.33 g/t Au

1.0 m @ 3.18 g/t Au

1.0 m @ 1.73 g/t Au

1.0 m @ 3540 g/t Au1.0 m @ 137 g/t Au

1.0 m@ 0.67 g/t Au

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Figure 12: South Rompas Log Grade vs. Width Note Log Scale of Au ppm

Date: 27 August 2014, Author M.R. Hudson

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Figure 13: Palokas Drilling Plan

Date: 27 August 2014, Author M.R. Hudson

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Figure 14: Palokas Cross Section

Date: 27 August 2014, Author M.R. Hudson

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Figure 15: Palokas Longitudinal Drill Section

Date: 27 August 2014, Author M.R. Hudson

11. Sample Preparation, Analyses and Security 1 (a) No documentation of the sampling methodology was provided by AREVA; the best record of their activities is their sample sites. With few exceptions, all samples were taken of colluvium or sub-cropping angular rock at a few 10’s of cm depth.

In October 2009, Nebocat (2011) attempted to sample only the host/wall rock from the pits and/or outcroppings and this is reflected in some of the sample results when compared to the original samples; however, two of the samples did yield highly anomalous Au values (4.37 ppm & 76.8 ppm) plus one anomalous value in U (2,020 ppm).

Channel sampling done by the Issuer was usually with a group of 2 to 4 persons. After the surface was cleaned, the channel cut and interval length was marked out with chalk. A motorized diamond saw and water pump were used to cut the channel; the sample was extracted by use of a hammer and chisel. The sample is placed into a double paper, and this is in turn put into a larger plastic bag along with the sample ticket. At the end of each day the samples are stored in a shed at the Issuer’s base camp. The channel sample site is marked with a permanent tag.

Subcrop samples are collected in 50 cm pieces after excavating site with a plastic shovel and removing surficial weathered bedrock. Occasionally taken with a hammer or saw if surface is irregular, then categorized as a “grab” sample.

Till samples were collected from the C-horizon at varying depths, depending on the local soil profile. A 500 g sample was collected and placed in a plastic bag along with the sample number ticket.

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Similarly, 500 g of material were collected for the organic soil samples. Samples were taken from the A0, or upper part of the A-horizon from an average depth of 20 cm from surface.

All samples were taken and/or prepared by employees of the Issuer. Ten samples each were placed into sacks that were sealed, tagged and labeled. The samples were delivered by truck to the ALS Chemex lab in Pitea, Sweden by employees of the Issuer.

1 (b) AREVA’s samples were assayed at the Labtium Oy laboratory in Rovaniemi, Finland by methods 511P and 704P. The details of the sample preparation are extensive and will not be discussed here; a web-link is provided.

Http://www.labtium.fi/en/geology-and-mining-industry/sample-preparation.

Method 511P employs aqua regia digestion of the sample and multi-element determinations using ICP-OES instrumentation.

Methods 704/705 are used to determine ore grade assays of gold and the platinum metals by high-precision classical lead oxide (litharge)/fire assay method using either 25 g or 50 g subsamples, combined with alternative finishes (FAAS, ICP-OES, gravimetric).

Labtium Oy is a FINAS-accredited testing laboratory T025 and calibration laboratory K056 meeting the requirements of standard SFS-EN ISO/IEC 17025:2005

The Issuer’s earlier suites of samples were analyzed by ME-MS81, U-XRF05, XRF-10, Au-GRA21 and Au-AA25 techniques by ALS Chemex Ltd's laboratories in Pitea, Sweden and Vancouver, Canada. The samples were crushed in the Piteå laboratory, and the pulps were shipped to the Vancouver, Canada laboratory for analyses. Crushing methods are fairly standard--a 250 g split of the crushed material is pulverized in a ring grinder such that greater than 85% of the material passes through a 75-micron screen. For further details of all the procedures employed by ALS, the reader is referred to the following website:

Http://www.alsglobal.com/mineralServicesOverview.aspx

All the samples were determined by ALS’s “ME-MS81” package (multi-element mass spectrometer) which reports 38 elements including U and Th. The samples are digested with lithium borate fusion prior to dissolution in acid.

Uranium was determined by the “U-XRF05” X-ray fluorescence (XRF) package. A pressed pellet is used for certain elements not easily solubilized by acid digestion techniques. A finely ground sample powder (20 g minimum) is mixed with a few drops of liquid binder, compressed in a pellet press then analyzed by XRF spectrometry. The detection range for U is 4 to 10,000 ppm.

Most of the Au determinations were done by the “Au-AA25” package. This is a conventional fire assay-atomic absorption method using a 30 g nominal sample weight. The detection range is from 0.01 to 100 ppm,

Samples that yielded much higher values for Au and U using the methods described above were determined again using different techniques. High grade U was determined by ALS’s “XRF-10” package after digestion with lithium borate fusion. The detection range for U is 0.01% to 15%.

For high grade Au the “Au-GRA21” package was used. It also uses a 30 g sample, but the finish is done gravimetrically (weighed) rather than the gold bead being dissolved and determined by atomic absorption technique.

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Subsequent samples were also analyzed using “ME-MS41u”, “PGM-ICP27” and “ME-MS61u” techniques. ME-MS41u is a multi-element, mass spectrometry method the tests for 51 elements plus U (0.05 ppm - 10,000 ppm). The ME-MS61u method is very similar but analyzes just 48 elements plus (0.1 ppm - 10,000 ppm).

PGM-ICP27 is an ore grade method for determining Au, Pt and Pd by fire assay and either ICP-AES, or ICP-MS finish. A nominal 30 g sample weight is used, and the detection ranges for Au, Pt and Pd are 0.03-100 ppm.

ALS Chemex’s North Vancouver laboratory is ISO/IEC 17025:2005 accredited for precious and base metal assay methods.

Certain samples contained too much radioactive material to be prepared by ALS in Sweden due to national occupational health and safety regulations. These samples were sent securely to the laboratory of the Saskatchewan Research Council (SRC) located in Saskatoon, Canada. The samples were analyzed for multi-elements using ICP (inductively coupled plasma spectrometry) technique. Some of the elements were only partially digested using a 0.5 g pulp digested in 2.25 ml of 8:1 HNO3: HCl for 1 hour at 950C. The elements analyzed by the total digestion method had a 0.125 g pulp digested in a heated mixture of HF/HNO3/HClO4 until dry, and the residue is dissolved in dilute HNO3. The uranium was also determined by ICP. A 1.00 g pulp is digested with 24 ml of HCl: HNO3 for 1 hour at 950C; the result was reported as percent U3O8.

SRC is an ISO/IEC 17025:2005 accredited laboratory.

All three laboratories are independent of the Issuer.

1 (c) The SRC lab did one repeat assay for all the determinations and used two standards: one for the high grade U, another for the total digestion multi-element ICP determinations.

ALS generally inserted 2 standards each for the multi-element ICP, U and Au determinations. Normally just 1 blank and 1 duplicate were inserted, but on sample submissions containing more than 10 samples, 2 duplicate checks were run. The results of the duplicate analyses appear to be acceptable.

The internal duplicate, standard and/or blank introduction done Labtium Oy, or those introduced by AREVA, is not known.

For the regional till sampling program of 2010, the Issuer collected field duplicates at every 50th sample site. The standard procedure was to sample a separate pit about 1 m from the original pit. In addition to this standards, were inserted on a 1:25 basis.

For the channel sampling, a blank was introduced as the first sample within a given batch, and every 25th sample was a standard. The Issuer introduced up to five different analytical standards depending on the type of sample and projected grades. One lower level Au standard was used for the regional till survey (520 ppb), one low grade Au (2 ppm Au, 433 ppm Cu, 495 ppm Ag) and a higher grade Au (11.79 ppm), and two different levels of U (135 ppm and 662 ppm) were used.

A plot created by the Issuer of U ppm values for the original vs. duplicate field samples shows a strong correlation with all analytical methods used (5) except for one. For Au, 3 of 4 methods used showed a good correlation. However, not all duplicate samples were analyzed by the same techniques, so an exact comparison is not possible.

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1 (d) The author is of the opinion that the sampling, security and quality assurance/quality control procedures employed by the Issuer are well documented and are more than satisfactory.

12. Data Verification The author sampled with Nebocat (2011) who took five samples from three different areas at Rompas (2009) over a distance of about 5 km. These samples were all checks of some of the higher grade samples: four of AREVA’s and one of the Issuer’s. Two samples were collected near the southern end of the Rompas zone, another about 1 km to the north and two more about 5 km to the NNW. The samples ranged from 5 ppm to 2,020 ppm U and from 0.19 ppm to 76.8 ppm Au. Some of these samples corresponded closely to the original samples, others were considerably lower. Nebocat’s (2011) samples consisted of the metavolcanic wallrock, not of the carbonate bearing vein material previously sampled by the Issuer and AREVA.

The Issuer’s sample site that was examined was covered with snow and could not be located exactly. Instead, a sample was taken over 0.4 m across a fracture in a nearby outcrop that yielded a strong scintillometer reading.

Nebocat (2011) attempted to sample only the host/wall rock from the pits and/or outcroppings and this is reflected in some of the sample results when compared to the original samples; the following table documents these check samples.

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Table 4: Comparison of J. Nebocat Samples (2011) with AREVA & Mawson Samples

AREVA/Mawson Sample

AREVA/ Mawson-U

(ppm)

AREVA/ Mawson-Au

(ppm)

J. Nebocat Sample

J. Nebocat U (ppm)

J. Nebocat Au (ppm)

BBT-070-01 249,000 12,800 73880 34.8 4.37104209* 2 0.19 73881* 5.09 0.19

EJV-013-03 135,000 4,800 73882 2,020 76.8

TIH-064-02 24.1 0.51 73883 25.9 0.29BBT-056-00 111,000 2,620 73884 7.44 0.34

* Mawson Resources sample

Three samples taken by AREVA are considerably higher in U and Au than those taken by the Nebocat (2011) at the same sites. As stated previously, some of the sampling done by AREVA and the Issuer was focused on determining the nature of the mineralization and is not meant to be representative of the average tenure of the rock over measurable widths. The corresponding samples taken by the author of mostly the host/wall rock yielded considerably lower levels in U and Au; nonetheless, sample 73882 still assayed 76.8 ppm Au (2.24 oz/ton). Two of the original samples that yielded low levels in both U and Au ran similar results in Nebocat (2011)’s.

13. Mineral Processing and Metallurgical Testing No mineral processing or metallurgical testing has been conducted on this property so far.

14. Mineral Resource Estimates There are no known mineral resource estimates for this property.

15. Mineral Reserve Estimates Not applicable to this report.

16. Mining Methods Not applicable to this report.

17. Recovery Methods Not applicable to this report.

18. Project Infrastructure Not applicable to this report.

19. Market Studies and Contracts Not applicable to this report.

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20. Environmental Studies, Permitting and Social or Community Impact

For the 10,580 hectares at Rompas, the Company is entitled to 100% of the mineral rights over the entire claim with certain limitations on exploration methods that can be completed in Natura 2000 areas (an EU biodiversity program) within the exploration claims, including no drilling or trenching due to the presence of specific flora. Mawson is entitled to apply for a modification of this decision by conducting an environmental program (a Natura 2000 assessment) to address these observations in order to obtain permission to conduct drilling and trenching in these areas. Approximately 80% of Mawson’s highest priority targets at Rompas are within European Union defined biodiversity areas (Natura 2000) where the Company is not yet permitted to drill. Natura 2000 defined areas cover 30% of Northern Finland. These targets include the extensive disseminated style mineralization discovered in 2012 at Rajapalot.

Mawson commissioned Golder Associates of Finland to complete a one and a half year-long Natura 2000 Assessment that mapped and reported in detail the floral distribution and natural habitat types of the area. The assessment also defines the impact that Mawson’s exploration work will have on the biodiversity values. The key consultant who performed all the mapping was one of the biologists who mapped the Rompas Natura 2000 area when it was defined in the late 1990s. He is widely considered as the biodiversity expert for the project area. The report stated that at this stage of exploration, a managed program will have no significant environmental effects on the area. The Company formally submitted the study to the competent authority, the Centre for Economic Development, Transport and the Environment (“ELY”) in Lapland on 26th June, 2013. ELY submitted their comments on this study after 8 months of review to the Finnish Mining Authorities (“TUKES”). TUKES are the ultimate decision-makers to modify Mawson’s claims to allow drilling in the Natura 2000 areas. A final decision from TUKES on the permit to allow drilling in the Natura 2000 biodiversity areas is expected shortly. Additionally, the Issuer has received a decision from the Regional Administrative Court on a temporary stop work order requested by ELY during the permit application period on the Issuer's hand-portable core sampling in Natura 2000 areas, including the Palokas prospect. This decision does not affect drilling outside of these areas. The Issuer appealed this temporary stop work order after receiving interpretation from TUKES that the method satisfied the current claim permit conditions as originally outlined by TUKES. The Administrative Court has subsequently overturned ELY's stop work order and returned the matter to ELY for new handling. The court ruled that the matter must be resolved. Mawson sees this as a balanced decision which allows it an opportunity to discuss and resolve these matters rationally with the relevant authorities.

Over the last year Mawson has also commissioned the Geological Survey of Finland to complete a detailed first stage of a base line geochemical water survey. The aim of the study was to investigate the pre-exploration state of the area. Groundwater, surface water (streams), stream sediments and mosses were studied. Groundwater samples were collected from the wells of the study area, including drilled wells, excavated wells and springs used as household water. Samples of stream water and organic stream sediments were collected from streams in a natural state. Samples of mosses were also collected. Physical-chemical properties (anions and elements) and concentrations of radon (Rn-222) of waters, and elements of the stream sediments and mosses were analyzed. It was found surface, groundwater and moss quality was good and

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elemental concentrations can be regarded as background values, while variations can be interpreted to be related to the natural variation in the area. Follow-up surveys will be carried out at three year intervals.

Additionally, the Company has continued to regularly meet all stakeholders including local groups, municipalities and administrative bodies to update them on the Company’s work plans. For the most part the stakeholders have been supportive of the Company's work programs and how it has dealt with compliance issues; however there have been some objections and opposition to the Company's work plans and environmental efforts. The Company has been dealing with allegations made by certain Environmental Authorities into the Company’s hand dug trenches completed during the 2010 and 2011 work programs. The Company has met with all relevant authorities multiple times during the work period and since the objections were raised and believes it conducted its operations within the intent and law of the Mining and Nature Conservation Acts. The Company has been working with all authorities in a transparent and open manner and strongly believes that all allegations against the Company will be refuted when the facts emerge at the end of the investigation, believed to be at the end of 2013.

21. Capital and Operating Costs Not applicable to this report.

22. Economic Analysis Not applicable to this report.

23. Adjacent Properties There are a few properties nearby controlled by other parties but none that appear to be owned by public companies that report on an exchange.

Information on five nearby showings was obtained from a website maintained by GTK: http://en.gtk.fi/Geoinfo/DataProducts/latest/

Vinsa: (free to stake) is an orogenic copper-gold occurrence with no resource estimate available. It comprises a 0.5-2 m wide, >250 m long quartz vein and enveloping alteration halo in a dolerite. Native gold (?) associated with chalcopyrite, pyrite and pyrrhotite.

Petäjävaara: (open for acquisition) is an orogenic copper-gold occurrence with no resource estimate available. It comprises a set of quartz veins in a sheared, SW-trending, contact zone between dolerite and quartzite, and is chiefly hosted by the dolerite. Gold only in the quartz veins?

Kivimaa: (Endomines Oy, owner) is an orogenic copper-gold deposit with an in situ pre-mining resource estimate of 106 kg gold and 1160 t copper (no JORC-compliant resource calculation is available). In 1969, 18,600 t of ore was mined by Outokumpu Oy, and only 37 kg gold and 223 t Cu recovered. Kivimaa comprises a 1-6 m wide, >350 m long quartz vein and enveloping alteration halo in an E-W trending dip-slip fault in a dolerite. Native gold as inclusions in arsenopyrite and, possibly, as free gold. All gold appears to be in the quartz vein.

Sivakkajoki: (Endomines Oy, owner) close to the Kivimaa deposit, is an orogenic gold occurrence with no resource estimate available. It comprises a set of carbonate-quartz veins

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and enveloping alteration halo in an E-W trending fault in a dolerite. Apparently, gold only in the quartz veins.

Vähäjoki: (Pyhäsalmi Mine Oy) possibly is an iron oxide-copper-gold deposit. It includes 14 magnetite bodies with an historic resource estimate totaling at 10.5 Mt, with a variable copper, cobalt and gold content. The best gold lodes are 0.1 Mt, 0.23 Mt and 1.0 Mt in size and contain 0.5 g/t Au, 0.03-0.5% Co, 0.05-1% Cu (no JORC-compliant resource calculation is available). In addition, there are at least 15 magnetite bodies which are not included into the resource estimate. The magnetite bodies form a N-S trending array possibly indicating the trend for a controlling structure (shear or fault zone). Host rocks are Fe-metasomatic products of altered mafic volcanic rocks and dolomitic marbles. Mineral assemblages suggest mineralization under 465°C, 2-4 kbar conditions. No intrusive rocks have been detected in the vicinity of Vähäjoki. Native gold, mostly as inclusions in cobaltite, locally also associated with arsenopyrite.

24. Other Relevant Data and Information There is no other relevant data or information pertinent to this report.

25. Interpretation and Conclusions The Rompas-Rajapalot project is a new camp-scale discovery where high-grade gold and uranium have been found within an area approaching 10km by 10km. Mawson acquired the project in April 2010 and outlined the initial hydrothermal nuggety gold vein discovery over a 6.0 kilometres strike and 200-250 metres width. In 2013, a new style of disseminated gold mineralization was drilled at Rajapalot, 8 kilometres east of the Rompas vein system.

Mawson is focused on two target areas at Rompas-Rajapalot:

1. A primary target of disseminated gold mineralization at Rajapalot, where discovery of high grade and thick core sample results include 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006 and 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres) and 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005. This disseminated mineralization is coincident with geophysical anomalies that extend for more than 4 kilometres and has only been drilled to 30 metres maximum depth with a hand portable core sampler.

2. The Company’s secondary target is the Rompas vein-style target area. The first drill program at South Rompas included the highlight of 6 metres at 617 g/t gold from 7 metres in drill hole ROM0011 which includes 1 metre at 3,540 g/t gold from 11 metres depth. The second drill program, conducted over the winter (December 2012 - January 2013) confirmed the presence and variable continuity within metabasalts of high grade, nuggety gold at both North and South Rompas and included results from North Rompas of 0.4 m at 395 g/t gold and 0.41% uranium in drill hole ROM0052 and at South Rompas the top 24% all assays from trenches and drilling now grade 100 g/t or more.

Core sample results in October 2013 at Rajapalot include 19.5m @ 7.4 g/t gold from 1.3 metres from PRAJ0006 and 5.4m @ 37.6 g/t gold from 2.5 metres from PRAJ0009 (including 1.0m @ 189.0 g/t gold from 6.9 metres) and 12.6m @ 3.6 g/t gold from 6.7 metres in PRAJ0005. The disseminated mineralization is coincident with a VTEM geophysical conductor that extends for

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more than 500 metres through an area with <1% outcrop, and forms part of a 3.5 kilometre target horizon between basaltic and quartzitic rocks.

Results from the maiden drill program at the Rompas vein system returned 6 metres at 617 g/t gold from 7 metres in drill hole ROM0011 including 1 metre at 3,540 g/t gold in August 2012. In February 2013, the first drill results from North Rompas, located 5km from South Rompas included 0.4m at 395 g/t Au and 0.41% U3O8 from 41m. At this early stage of exploration, it is difficult to find a global analogue for mineralization. Within the vein system, gold and uranium mineralization is hosted by a carbonate-calcsilicate-quartz vein array and albitic vein breccias. The veins (amphibole-pyroxene-quartz-carbonate ± native gold, uraninite) and alteration selvages (biotite-amphibole-K-feldspar) have been metamorphosed to amphibolite facies, following a structural episode of flattening within high strain zones. It is interpreted that the mineralized veins are either pre- or syn-deformational, but that the high-grade mineralization is likely a result of redistribution during syn-metamorphic deformation and perhaps superposition of new gold late in the metamorphic history. The disseminated mineralization differs in that it is more sulphidic and continuous than the vein-style mineralization, and comprises fine disseminated gold mineralization within magnesian chlorite-biotite-tourmaline-pyrrhotite-scheelite rocks. The mineralized zone lies structurally between mafic rocks and relatively oxidized quartzites.

Importantly, about 90% of the Rompas-Rajapalot project area is below soil and till cover which, at up to 5m thick, is too thick for the discovery of near-surface radiometric occurrences and exploration is at its very earliest of stages.

Recommendations

A continuing program is recommended at Rompas-Rajapalot with the main goal over the next year to attempt to define the first NI 43-101 resource on the project and continue to derisk adjacent prospect areas for deep drill testing. Specifically the recommended work program should address the following items:

1. Pole-Dipole Induced Polarization (“IP”) at 100 metre spacing over the main Rajapalot trend from Hirvimaa, Palokas to Rumajärvi prospects;

2. Gradient Array IP over the Joki prospect;

3. Maxwell modelling of the VTEM airborne geophysical survey at Rajapalot;

4. Deep till and basement grid drilling over the Raja prospect area to the east of the Natura 2000;

5. Subject to final permitting, aim to define by diamond drilling an initial resource at Rajapalot on 100 metre drill sections at 50 metre down dip spacing over 2 kilometre strike. Approximately 500 metres per section over 2 kilometre strike would amount to a recommended 10,000 metres drill campaign;

6. Metallurgical test work on Palokas drill core.

An exploration and company-wide budget to carry out these programs is estimated at CDN$6M as show in the Tables 5 and 6 below.

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Table 5: Recommended company-wide budget for August 2014-August 2015:

Cost Centre CDN$ %

Exploration* 2,425,000* 29

Permits and Environmental 500,000 12

Finland Personnel 1,400,000 11.5

Canada Personnel 200,000 8

Office and Listing Costs 156,670 6.3

PR 100,000 3.9

Computers, vehicles, consumables 100,000 3.4

Travel 100,000 3.3

Office 80,000 2.7

Contractors 300,000 2.7

Board 62,500 2.5

Contingency 542,417 10

TOTAL 5,966,587 100

*See Table 6 for Exploration Budget

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Table 5: Exploration budget for August 2014-August 2015:

Task Budget (CDN$)

1. Pole-Dipole Induced Polarization (“IP”) at 100 metre spacing over the main Rajapalot trend from Hirvimaa, Palokas to Rumajärvi prospects;

150,000

2. Gradient Array IP over the Joki prospect; 30,000

3. Maxwell modelling of the VTEM airborne geophysical survey at Rajapalot;

15,000

4. Deep till and basement grid drilling over the Raja prospect area to the east of the Natura 2000;

200,000

5. Subject to final permitting, diamond drill out an initial resource at Rajapalot on 100 metre drill sections at 50 metre down dip spacing over 2 kilometre strike. Approximately 500 metres per section over 2 kilometre strike is 10,000 metres;

2,000,000

6. Metallurgical test work on Palokas drill core; 30,000

TOTAL 2,425,000

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1.0 References

Ashley, P.M., 2011, Petrographic Report on Four Rock Samples from Scandinavia: unpublished report, unpublished report, 12 p.

_________, 2011, Petrographic Report on Fifty-Five Rock Samples from the Rompas Area, Peräpohja Schist Belt, Finland, unpublished report, 87 p.

_________, 2009, Petrographic Report on Fifteen Rock Samples From Peräpohja Schist Belt, Finland: unpublished report, 40 p.

Dahlenborg, L., 2011, Comparison of till Geochemistry and Structural targets at the Rompas Project, NW Finland, unpublished report, 11 p.

Dahlenborg, L., 2012, Ah sampling 2012, QAQC, Results, Context with other surface exploratory datasets, Proposal for further work at the Rompas Project, NW Finland, unpublished report, 6 p.

_________, 2010, Interpretation of geochemical results from regional program, Peräpohja Schist Belt, unpublished report, 20 p.

Gaál, G., & Gorbatschev, R., 1987, An outline of the Precambrian Evolution of the Baltic Shield: Precambrian Research, v. 35, pp 15-52.

Huhma, H., Cliff, R., Perttunen, V. And Sakko, M. 1990. Sm-Nd and Pb isotopic study of mafic rocks associated with early Proterozoic continental rifting: the Peräpohja schist belt in northern Finland. Contributions to Mineralogy and Petrology 104, 367-379.

Lauri, L. S., 2011, Geological Mapping of the Rompas Rumavuoma Area, 2011: Geological Survey of Finland, 28 p.

_________, 2010, Geological Mapping of the Rompas Rumavuoma Area, 2010: Geological Survey of Finland, 55 p.

Lees, T., 2011, vice-president of exploration, Mawson Resources Limited until February 1, 2013.

Mawson Resources Limited, 2010-2014: various press releases and MD&A’s.

Mustonen, M, 2012. Geochemistry and petrography of the volcanic rocks in the Rompas area, Ylitornio, northern Finland. M.Sc. thesis, University of Oulu, 63pp.

Nebocat, J., 2011, Progress Report on the Geology, Mineralization and Exploration Activities on the Rompas Gold-Uranium Property Southern Lapland, Finland. Prepared for Mawson Resources Limited Effective Date: November 2, 2011

Perttunen, V. & Hanski, E., 2003, Explanation to the maps of Pre-Quaternary rocks, sheets 2631 and 2633, Summary: Pre-Quaternary rocks of the Törmäsjärvi and Koivu map-sheet areas: GTK, ESPOO 2003, 92 p.

Pitkänen, T., 2011, Ground geophysical survey, Northern Finland, Rompas: Gradient IP and Resistivity Survey: Geovista AB, unpublished report, 10 p.

Prave, T, 2013, A Synthesis of The Geology of The Peräpohja Schist Belt: A Field Excursion, 16-21 June, 2013 University St Andrews For Mawson Resources Limited.

Rankin, L.R., 2011, Rompas Au-U Project: 2011 Field Mapping & Geophysical Interpretation, unpublished report, 74 p.

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_________, 2010, Rompas District, Central Finland: Geological Interpretation of Detailed Airborne Geophysical Data, 46 p.

Richard, P., & Carrier, A., 2008, Technical Report On The Lavoie Property and “ L” Uranium Deposit (Otish Area, Quebec): NI 43-101 Report For Abitex Resources, 85 P.

Sarala, P., 2010, Quaternary geology and till geochemistry in the Rompas-Rumavuoma area and its surroundings in the central Peräpohja Schist Belt: Geological Survey of Finland.

Vanhanen, 2010, Report of the Field Studies of the Rumavuoma-Romppaanvuoma (Rompas) Area During 2007-2008: AREVA NC, 41p.

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Appendix 1: List of Mawson’s Claims at Rompas/Finland.

Granted Claims Old Act

Name of the claim Mining registry Area in Date of Date granted Date of

number/Claim hectares application expiry

identification

Karsikkovaara 1 8837/1 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 2 8837/2 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 3 8837/3 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 4 8837/4 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 5 8837/5 96.83 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 6 8837/6 90.90 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 7 8837/7 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 8 8837/8 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 9 8837/9 97.74 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 10 8837/10 84.85 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 11 8837/11 91.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 12 8837/12 95.11 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 13 8837/13 62.36 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 14 8837/14 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 15 8837/15 100.00 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 16 8837/16 83.71 2009-10-15 2011-10-31 2014-10-30

Karsikkovaara 17 8837/17 52.87 2009-10-15 2011-10-31 2014-10-30

Rompas 1 8837/18 89.29 2009-10-15 2011-10-31 2014-10-30

Rompas 2 8837/19 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 3 8837/20 93.57 2009-10-15 2011-10-31 2014-10-30

Rompas 4 8837/21 99.49 2009-10-15 2011-10-31 2014-10-30

Rompas 5 8837/22 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 6 8837/23 98.56 2009-10-15 2011-10-31 2014-10-30

Rompas 7 8837/24 99.28 2009-10-15 2011-10-31 2014-10-30

Rompas 8 8837/25 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 9 8837/26 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 10 8837/27 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 11 8837/28 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 12 8837/29 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 13 8837/30 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 14 8837/31 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 15 8837/32 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 16 8837/33 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 17 8837/34 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 18 8837/35 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 19 8837/36 100.00 2009-10-15 2011-10-31 2014-10-30

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Rompas 20 8837/37 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 21 8837/38 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 22 8837/39 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 23 8837/40 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 24 8837/41 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 25 8837/42 99.64 2009-10-15 2011-10-31 2014-10-30

Rompas 26 8837/43 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 27 8837/44 99.99 2009-10-15 2011-10-31 2014-10-30

Rompas 28 8837/45 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 29 8837/46 99.64 2009-10-15 2011-10-31 2014-10-30

Rompas 30 8837/47 98.78 2009-10-15 2011-10-31 2014-10-30

Rompas 31 8837/48 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 32 8837/49 99.32 2009-10-15 2011-10-31 2014-10-30

Rompas 33 8837/50 99.99 2009-10-15 2011-10-31 2014-10-30

Rompas 34 8837/51 99.58 2009-10-15 2011-10-31 2014-10-30

Rompas 35 8837/52 99.94 2009-10-15 2011-10-31 2014-10-30

Rompas 36 8837/53 100.00 2009-10-15 2011-10-31 2014-10-30

Rompas 37 8837/54 98.93 2009-10-15 2011-10-31 2014-10-30

Rompas 38 8837/55 97.75 2009-10-15 2011-10-31 2014-10-30

Rompas 39 8837/56 98.97 2009-10-15 2011-10-31 2014-10-30

Rompas 40 8837/57 97.54 2009-10-15 2011-10-31 2014-10-30

Rompas 41 8837/58 49.72 2009-10-15 2011-10-31 2014-10-30

Rompas 42 8837/59 99.91 2009-10-15 2011-10-31 2014-10-30

Rompas 45 8837/62 98.03 2009-10-15 2011-10-31 2014-10-30

Rompas 46 8837/63 99.90 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 1 8837/64 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 2 8837/65 72.98 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 3 8837/66 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 4 8837/67 92.42 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 5 8837/68 99.79 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 6 8837/69 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 7 8837/70 83.67 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 8 8837/71 99.99 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 9 8837/72 99.99 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 10 8837/73 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 11 8837/74 99.99 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 12 8837/75 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 13 8837/76 84.85 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 14 8837/77 97.31 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 15 8837/78 95.06 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 16 8837/79 96.91 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 17 8837/80 97.50 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 18 8837/81 75.00 2009-10-15 2011-10-31 2014-10-30

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Kaunismaa 19 8837/82 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 20 8837/83 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 21 8837/84 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 22 8837/85 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 23 8837/86 75.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 24 8837/87 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 25 8837/88 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 26 8837/89 68.41 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 27 8837/90 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 28 8837/91 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 29 8837/92 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 30 8837/93 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 31 8837/94 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 32 8837/95 83.29 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 33 8837/96 66.57 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 34 8837/97 98.34 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 35 8837/98 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 36 8837/99 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 37 8837/100 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 38 8837/101 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 39 8837/102 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 40 8837/103 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 41 8837/104 96.80 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 42 8837/105 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 43 8837/106 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 44 8837/107 98.10 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 45 8837/108 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 46 8837/109 100.00 2009-10-15 2011-10-31 2014-10-30

Kaunismaa 47 8837/110 75.00 2009-10-15 2011-10-31 2014-10-30

Rumavuoma 1 8526/1 92.21 2007-11-27 2013-05-27 under appeals

Rumavuoma 2 8526/2 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 3 8526/3 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 4 8526/4 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 5 8526/5 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 6 8526/6 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 7 8526/7 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 8 8526/8 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 9 8526/9 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 10 8526/10 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 11 8526/11 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 12 8526/12 100 2007-11-27 2013-05-27 under appeals

Rumavuoma 13 8526/13 100 2007-11-27 2013-05-27 under appeals

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Claim Applications Old Act

Claim application Mining registry Area in Date of

name number/Claim hectares application

identification

Kaitajärvi 1 8965/1 98.01 2010-04-30

Kaitajärvi 2 8965/2 99.82 2010-04-30

Kaitajärvi 3 8965/3 99.23 2010-04-30

Kaitajärvi 4 8965/4 99.18 2010-04-30

Kaitajärvi 5 8965/5 99.92 2010-04-30

Kaitajärvi 6 8965/6 98.63 2010-04-30

Kaitajärvi 7 8965/7 99.31 2010-04-30

Kaitajärvi 8 8965/8 98.42 2010-04-30

Kaitajärvi 9 8965/9 99.89 2010-04-30

Kaitajärvi 10 8965/10 99.96 2010-04-30

Kaitajärvi 11 8965/11 87.28 2010-04-30

Kaitajärvi 12 8965/12 99.93 2010-04-30

Kaitajärvi 13 8965/13 99.55 2010-04-30

Kaitajärvi 14 8965/14 96.31 2010-04-30

Kaitajärvi 15 8965/15 99.95 2010-04-30

Liikamaa 1 8966/1 100 2010-04-30

Liikamaa 2 8966/2 99.01 2010-04-30

Liikamaa 3 8966/3 100 2010-04-30

Liikamaa 4 8966/4 100 2010-04-30

Liikamaa 5 8966/5 100 2010-04-30

Kotavaara 1 8967/1 99.62 2010-04-30

Kotavaara 2 8967/2 99.66 2010-04-30

Kotavaara 3 8967/3 99.38 2010-04-30

Kotavaara 4 8967/4 99.94 2010-04-30

Kotavaara 5 8967/5 99.51 2010-04-30

Kotavaara 6 8967/6 98.11 2010-04-30

Lylymaa 1 9256/1 87.36 2011-05-02

Lylymaa 2 9256/1 100.00 2011-05-02

Lylymaa 3 9256/1 93.21 2011-05-02

Lylymaa 4 9256/1 60.27 2011-05-02

Lylymaa 5 9256/1 79.82 2011-05-02

Lylymaa 6 9256/1 62.48 2011-05-02

Lylymaa 7 9256/1 37.61 2011-05-02

Lylymaa 8 9256/1 100.00 2011-05-02

Lylymaa 9 9256/1 100.00 2011-05-02

Lylymaa 10 9256/1 100.00 2011-05-02

Lylymaa 11 9256/1 100.00 2011-05-02

Lylymaa 12 9256/1 12.62 2011-05-02

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Lylymaa 13 9256/1 100.00 2011-05-02

Lylymaa 14 9256/1 50.00 2011-05-02

Lylymaa 15 9256/1 100.00 2011-05-02

Lylymaa 16 9256/1 100.00 2011-05-02

Lylymaa 17 9256/1 50.00 2011-05-02

Lylymaa 18 9256/1 100.00 2011-05-02

Lylymaa 19 9256/1 100.00 2011-05-02

Lylymaa 20 9256/1 100.00 2011-05-02

Lylymaa 21 9256/1 100.00 2011-05-02

Lylymaa 22 9256/1 100.00 2011-05-02

Lylymaa 23 9256/1 100.00 2011-05-02

Lylymaa 24 9256/1 52.77 2011-05-02

Lylymaa 25 9256/1 95.42 2011-05-02

Lylymaa 26 9256/1 100.00 2011-05-02

Lylymaa 27 9256/1 74.53 2011-05-02

Lylymaa 28 9256/1 99.93 2011-05-02

Lylymaa 29 9256/1 44.13 2011-05-02

Jänkävaara 1 9256/1 40.33 2011-05-02

Jänkävaara 2 9256/1 98.29 2011-05-02

Jänkävaara 3 9256/1 100.00 2011-05-02

Jänkävaara 4 9256/1 100.00 2011-05-02

Jänkävaara 5 9256/1 100.00 2011-05-02

Jänkävaara 6 9256/1 93.73 2011-05-02

Jänkävaara 7 9256/1 55.96 2011-05-02

Jänkävaara 8 9256/1 100.00 2011-05-02

Jänkävaara 9 9256/1 100.00 2011-05-02

Jänkävaara 10 9256/1 100.00 2011-05-02

Jänkävaara 11 9256/1 100.00 2011-05-02

Jänkävaara 12 9256/1 100.00 2011-05-02

Jänkävaara 13 9256/1 100.00 2011-05-02

Jänkävaara 14 9256/1 100.00 2011-05-02

Jänkävaara 15 9256/1 100.00 2011-05-02

Jänkävaara 16 9256/1 100.00 2011-05-02

Jänkävaara 17 9256/1 100.00 2011-05-02

Jänkävaara 18 9256/1 100.00 2011-05-02

Jänkävaara 19 9256/1 100.00 2011-05-02

Jänkävaara 20 9256/1 87.90 2011-05-02

Jänkävaara 21 9256/1 100.00 2011-05-02

Jänkävaara 22 9256/1 100.00 2011-05-02

Jänkävaara 23 9256/1 100.00 2011-05-02

Jänkävaara 24 9256/1 93.58 2011-05-02

Jänkävaara 25 9256/1 55.51 2011-05-02

Jänkävaara 26 9256/1 99.25 2011-05-02

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Jänkävaara 27 9256/1 100.00 2011-05-02

Jänkävaara 28 9256/1 94.48 2011-05-02

Jänkävaara 29 9256/1 57.72 2011-05-02

Jänkävaara 30 9256/1 100.00 2011-05-02

Jänkävaara 31 9256/1 100.00 2011-05-02

Jänkävaara 32 9256/1 100.00 2011-05-02

Jänkävaara 33 9256/1 100.00 2011-05-02

Jänkävaara 34 9256/1 100.00 2011-05-02

Jänkävaara 35 9256/1 100.00 2011-05-02

Jänkävaara 36 9256/1 100.00 2011-05-02

Jänkävaara 37 9256/1 100.00 2011-05-02

Jänkävaara 38 9256/1 74.19 2011-05-02

Jänkävaara 39 9256/1 100.00 2011-05-02

Jänkävaara 40 9256/1 100.00 2011-05-02

Jänkävaara 41 9256/1 100.00 2011-05-02

Jänkävaara 42 9256/1 100.00 2011-05-02

Jänkävaara 43 9256/1 100.00 2011-05-02

Jänkävaara 44 9256/1 100.00 2011-05-02

Jänkävaara 45 9256/1 100.00 2011-05-02

Jänkävaara 46 9256/1 100.00 2011-05-02

Jänkävaara 47 9256/1 99.44 2011-05-02

Jänkävaara 48 9256/1 100.00 2011-05-02

Jänkävaara 49 9256/1 100.00 2011-05-02

Jänkävaara 50 9256/1 100.00 2011-05-02

Jänkävaara 51 9256/1 100.00 2011-05-02

Jänkävaara 52 9256/1 100.00 2011-05-02

Jänkävaara 53 9256/1 100.00 2011-05-02

Jänkävaara 54 9256/1 100.00 2011-05-02

Jänkävaara 55 9256/1 100.00 2011-05-02

Jänkävaara 56 9256/1 100.00 2011-05-02

Jänkävaara 57 9256/1 100.00 2011-05-02

Jänkävaara 58 9256/1 100.00 2011-05-02

Jänkävaara 59 9256/1 100.00 2011-05-02

Jänkävaara 60 9256/1 100.00 2011-05-02

Jänkävaara 61 9256/1 100.00 2011-05-02

Jänkävaara 62 9256/1 100.00 2011-05-02

Jänkävaara 63 9256/1 100.00 2011-05-02

Jänkävaara 64 9256/1 100.00 2011-05-02

Jänkävaara 65 9256/1 100.00 2011-05-02

Jänkävaara 66 9256/1 63.69 2011-05-02

Jänkävaara 67 9256/1 99.82 2011-05-02

Jänkävaara 68 9256/1 100.00 2011-05-02

Jänkävaara 69 9256/1 95.72 2011-05-02

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Jänkävaara 70 9256/1 100.00 2011-05-02

Jänkävaara 71 9256/1 100.00 2011-05-02

Jänkävaara 72 9256/1 95.94 2011-05-02

Jänkävaara 73 9256/1 28.98 2011-05-02

Kuusivaara 1 9256/1 ?? 2011-05-02

Kuusivaara 2 9256/1 50.26 2011-05-02

Kuusivaara 3 9256/1 ?? 2011-05-02

Kuusivaara 4 9256/1 25.66 2011-05-02

Kuusivaara 5 9256/1 100.00 2011-05-02

Kuusivaara 6 9256/1 100.00 2011-05-02

Kuusivaara 7 9256/1 99.25 2011-05-02

Kuusivaara 8 9256/1 100.00 2011-05-02

Kuusivaara 9 9256/1 ?? 2011-05-02

Kuusivaara 10 9256/1 90.40 2011-05-02

Kuusivaara 11 9256/1 ?? 2011-05-02

Kuusivaara 12 9256/1 100.00 2011-05-02

Kuusivaara 13 9256/1 99.79 2011-05-02

Kuusivaara 14 9256/1 100.00 2011-05-02

Kuusivaara 15 9256/1 100.00 2011-05-02

Kuusivaara 16 9256/1 94.28 2011-05-02

Kuusivaara 17 9256/1 63.47 2011-05-02

Kuusivaara 18 9256/1 77.83 2011-05-02

Kuusivaara 19 9256/1 33.92 2011-05-02

Kuusivaara 20 9256/1 75.88 2011-05-02

Kuusivaara 21 9256/1 74.82 2011-05-02

Kuusivaara 22 9256/1 99.00 2011-05-02

Kuusivaara 23 9256/1 ?? 2011-05-02

Kuusivaara 24 9256/1 99.88 2011-05-02

Kuusivaara 25 9256/1 59.60 2011-05-02

Kuusivaara 26 9256/1 49.69 2011-05-02

Kuusivaara 27 9256/1 69.25 2011-05-02

Kuusivaara 28 9256/1 25.33 2011-05-02

Kuusivaara 29 9256/1 78.68 2011-05-02

Kuusivaara 30 9256/1 36.99 2011-05-02

Kuusivaara 31 9256/1 64.29 2011-05-02

Kuusivaara 32 9256/1 98.75 2011-05-02

Kuusivaara 33 9256/1 98.41 2011-05-02

Kuusivaara 34 9256/1 96.19 2011-05-02

Kuusivaara 35 9256/1 100.00 2011-05-02

Kuusivaara 36 9256/1 72.21 2011-05-02

Kuusivaara 37 9256/1 80.54 2011-05-02

Kuusivaara 38 9256/1 100.00 2011-05-02

Kuusivaara 39 9256/1 71.97 2011-05-02

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Kuusivaara 40 9256/1 98.65 2011-05-02

Kuusivaara 41 9256/1 81.16 2011-05-02

Kuusivaara 42 9256/1 86.79 2011-05-02

Kuusivaara 43 9256/1 92.07 2011-05-02

Kuusivaara 44 9256/1 16.46 2011-05-02

Kätkävaara 1 9256/1 100.00 2011-05-02

Kätkävaara 2 9256/1 100.00 2011-05-02

Kätkävaara 3 9256/1 100.00 2011-05-02

Kätkävaara 4 9256/1 96.55 2011-05-02

Kätkävaara 5 9256/1 100.00 2011-05-02

Kätkävaara 6 9256/1 100.00 2011-05-02

Kätkävaara 7 9256/1 100.00 2011-05-02

Kätkävaara 8 9256/1 59.95 2011-05-02

Kätkävaara 9 9256/1 100.00 2011-05-02

Kätkävaara 10 9256/1 100.00 2011-05-02

Kätkävaara 11 9256/1 100.00 2011-05-02

Kätkävaara 12 9256/1 100.00 2011-05-02

Kätkävaara 13 9256/1 99.64 2011-05-02

Kätkävaara 14 9256/1 100.00 2011-05-02

Kätkävaara 15 9256/1 100.00 2011-05-02

Kätkävaara 16 9256/1 49.28 2011-05-02

Kätkävaara 17 9256/1 100.00 2011-05-02

Kätkävaara 18 9256/1 100.00 2011-05-02

Kätkävaara 19 9256/1 100.00 2011-05-02

Kätkävaara 20 9256/1 80.66 2011-05-02

Kätkävaara 21 9256/1 100.00 2011-05-02

Kätkävaara 22 9256/1 97.98 2011-05-02

Kätkävaara 23 9256/1 61.74 2011-05-02

Kätkävaara 24 9256/1 94.05 2011-05-02

Kätkävaara 25 9256/1 89.81 2011-05-02

Kätkävaara 26 9256/1 78.13 2011-05-02

Kätkävaara 27 9256/1 90.73 2011-05-02

Kätkävaara 28 9256/1 100.00 2011-05-02

Kätkävaara 29 9256/1 100.00 2011-05-02

Kätkävaara 30 9256/1 100.00 2011-05-02

Kätkävaara 31 9256/1 99.38 2011-05-02

Kätkävaara 32 9256/1 100.00 2011-05-02

Kätkävaara 33 9256/1 100.00 2011-05-02

Kätkävaara 34 9256/1 47.43 2011-05-02

Kätkävaara 35 9256/1 56.56 2011-05-02

Kätkävaara 36 9256/1 100.00 2011-05-02

Kätkävaara 37 9256/1 85.61 2011-05-02

Kätkävaara 38 9256/1 100.00 2011-05-02

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Kätkävaara 39 9256/1 96.85 2011-05-02

Kätkävaara 40 9256/1 68.59 2011-05-02

Kätkävaara 41 9256/1 94.58 2011-05-02

Kätkävaara 42 9256/1 47.79 2011-05-02

Kätkävaara 43 9256/1 90.08 2011-05-02

Kätkävaara 44 9256/1 82.60 2011-05-02

Kätkävaara 45 9256/1 46.84 2011-05-02

Kätkävaara 46 9256/1 94.49 2011-05-02

Kätkävaara 47 9256/1 94.98 2011-05-02

Kätkävaara 48 9256/1 85.09 2011-05-02

Kätkävaara 49 9256/1 36.22 2011-05-02

Kätkävaara 50 9256/1 98.29 2011-05-02

Kätkävaara 51 9256/1 100.00 2011-05-02

Kätkävaara 52 9256/1 99.68 2011-05-02

Kätkävaara 53 9256/1 77.79 2011-05-02

Kätkävaara 54 9256/1 86.85 2011-05-02

Kätkävaara 55 9256/1 78.66 2011-05-02

Kätkävaara 56 9256/1 21.45 2011-05-02

Lohijärvi 1 9256/1 89.09 2011-05-02

Lohijärvi 2 9256/1 87.03 2011-05-02

Lohijärvi 3 9256/1 100.00 2011-05-02

Lohijärvi 4 9256/1 97.29 2011-05-02

Lohijärvi 5 9256/1 100.00 2011-05-02

Lohijärvi 6 9256/1 100.00 2011-05-02

Lohijärvi 7 9256/1 100.00 2011-05-02

Lohijärvi 8 9256/1 17.83 2011-05-02

Lohijärvi 9 9256/1 93.03 2011-05-02

Lohijärvi 10 9256/1 99.82 2011-05-02

Lohijärvi 11 9256/1 100.00 2011-05-02

Lohijärvi 12 9256/1 100.00 2011-05-02

Lohijärvi 13 9256/1 82.89 2011-05-02

Lohijärvi 14 9256/1 96.78 2011-05-02

Lohijärvi 15 9256/1 100.00 2011-05-02

Lohijärvi 16 9256/1 49.79 2011-05-02

Lohijärvi 17 9256/1 100.00 2011-05-02

Lohijärvi 18 9256/1 61.50 2011-05-02

Lohijärvi 19 9256/1 100.00 2011-05-02

Lohijärvi 20 9256/1 91.03 2011-05-02

Lohijärvi 21 9256/1 94.42 2011-05-02

Lohijärvi 22 9256/1 87.86 2011-05-02

Lohijärvi 23 9256/1 100.00 2011-05-02

Lohijärvi 24 9256/1 94.42 2011-05-02

Lohijärvi 25 9256/1 74.92 2011-05-02

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Lohijärvi 26 9256/1 98.89 2011-05-02

Lohijärvi 27 9256/1 100.00 2011-05-02

Lohijärvi 28 9256/1 100.00 2011-05-02

Lohijärvi 29 9256/1 63.71 2011-05-02

Lohijärvi 30 9256/1 6.37 2011-05-02

Lohijärvi 31 9256/1 95.86 2011-05-02

Lohijärvi 32 9256/1 100.00 2011-05-02

Lohijärvi 33 9256/1 100.00 2011-05-02

Lohijärvi 34 9256/1 98.82 2011-05-02

Lohijärvi 35 9256/1 100.00 2011-05-02

Lohijärvi 36 9256/1 100.00 2011-05-02

Lohijärvi 37 9256/1 100.00 2011-05-02

Lohijärvi 38 9256/1 100.00 2011-05-02

Lohijärvi 39 9256/1 100.00 2011-05-02

Lohivaara 1 9256/1 83.38 2011-05-02

Lohivaara 2 9256/1 44.22 2011-05-02

Lohivaara 3 9256/1 97.93 2011-05-02

Lohivaara 4 9256/1 84.48 2011-05-02

Lohivaara 5 9256/1 67.03 2011-05-02

Lohivaara 6 9256/1 100.00 2011-05-02

Lohivaara 7 9256/1 100.00 2011-05-02

Lohivaara 8 9256/1 77.39 2011-05-02

Lohivaara 9 9256/1 92.85 2011-05-02

Lohivaara 10 9256/1 32.66 2011-05-02

Lohivaara 11 9256/1 100.00 2011-05-02

Lohivaara 12 9256/1 98.01 2011-05-02

Lohivaara 13 9256/1 44.16 2011-05-02

Lohivaara 14 9256/1 100.00 2011-05-02

Lohivaara 15 9256/1 100.00 2011-05-02

Lohivaara 16 9256/1 99.54 2011-05-02

Lohivaara 17 9256/1 99.85 2011-05-02

Lohivaara 18 9256/1 100.00 2011-05-02

Lohivaara 19 9256/1 100.00 2011-05-02

Lohivaara 20 9256/1 100.00 2011-05-02

Lohivaara 21 9256/1 100.00 2011-05-02

Lohivaara 22 9256/1 98.10 2011-05-02

Lohivaara 23 9256/1 46.76 2011-05-02

Lohivaara 24 9256/1 100.00 2011-05-02

Lohivaara 25 9256/1 100.00 2011-05-02

Lohivaara 26 9256/1 100.00 2011-05-02

Lohivaara 27 9256/1 100.00 2011-05-02

Lohivaara 28 9256/1 100.00 2011-05-02

Lohivaara 29 9256/1 91.03 2011-05-02

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Lohivaara 30 9256/1 93.09 2011-05-02

Lohivaara 31 9256/1 42.31 2011-05-02

Lohivaara 32 9256/1 98.93 2011-05-02

Lohivaara 33 9256/1 62.22 2011-05-02

Lohivaara 34 9256/1 100.00 2011-05-02

Lohivaara 35 9256/1 26.55 2011-05-02

Lohivaara 36 9256/1 79.46 2011-05-02

Lohivaara 37 9256/1 84.65 2011-05-02

Lohivaara 38 9256/1 50.08 2011-05-02

Lohivaara 39 9256/1 100.00 2011-05-02

Lohivaara 40 9256/1 100.00 2011-05-02

Louejoki 1 9256/1 100.00 2011-05-02

Louejoki 2 9256/1 100.00 2011-05-02

Louejoki 3 9256/1 100.00 2011-05-02

Louejoki 4 9256/1 100.00 2011-05-02

Louejoki 5 9256/1 100.00 2011-05-02

Louejoki 6 9256/1 100.00 2011-05-02

Louejoki 7 9256/1 100.00 2011-05-02

Louejoki 8 9256/1 100.00 2011-05-02

Louejoki 9 9256/1 87.78 2011-05-02

Louejoki 10 9256/1 100.00 2011-05-02

Louejoki 11 9256/1 100.00 2011-05-02

Louejoki 12 9256/1 95.05 2011-05-02

Louejoki 13 9256/1 100.00 2011-05-02

Louejoki 14 9256/1 100.00 2011-05-02

Louejoki 15 9256/1 85.46 2011-05-02

Louejoki 16 9256/1 67.60 2011-05-02

Louejoki 17 9256/1 99.97 2011-05-02

Louejoki 18 9256/1 95.11 2011-05-02

Louejoki 19 9256/1 97.05 2011-05-02

Louejoki 20 9256/1 100.00 2011-05-02

Louejoki 21 9256/1 100.00 2011-05-02

Louejoki 22 9256/1 70.79 2011-05-02

Louejoki 23 9256/1 98.74 2011-05-02

Louejoki 24 9256/1 99.82 2011-05-02

Louejoki 25 9256/1 99.13 2011-05-02

Louejoki 26 9256/1 60.87 2011-05-02

Louejoki 27 9256/1 100.00 2011-05-02

Louejoki 28 9256/1 95.12 2011-05-02

Louejoki 29 9256/1 100.00 2011-05-02

Louejoki 30 9256/1 92.67 2011-05-02

Louejoki 31 9256/1 77.15 2011-05-02

Louejoki 32 9256/1 45.22 2011-05-02

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Louejoki 33 9256/1 79.23 2011-05-02

Louejoki 34 9256/1 72.45 2011-05-02

Mellajoki 1 9256/1 100.00 2011-05-02

Mellajoki 2 9256/1 100.00 2011-05-02

Mellajoki 3 9256/1 100.00 2011-05-02

Mellajoki 4 9256/1 100.00 2011-05-02

Mellajoki 5 9256/1 93.12 2011-05-02

Mellajoki 6 9256/1 100.00 2011-05-02

Mellajoki 7 9256/1 100.00 2011-05-02

Mellajoki 8 9256/1 100.00 2011-05-02

Mellajoki 9 9256/1 100.00 2011-05-02

Mellajoki 10 9256/1 100.00 2011-05-02

Mellajoki 11 9256/1 100.00 2011-05-02

Mellajoki 12 9256/1 100.00 2011-05-02

Mellajoki 13 9256/1 100.00 2011-05-02

Mellajoki 14 9256/1 100.00 2011-05-02

Mellajoki 15 9256/1 100.00 2011-05-02

Mellajoki 16 9256/1 100.00 2011-05-02

Mellajoki 17 9256/1 84.76 2011-05-02

Mellajoki 18 9256/1 92.64 2011-05-02

Mellajoki 19 9256/1 100.00 2011-05-02

Mellajoki 20 9256/1 91.69 2011-05-02

Mellajoki 21 9256/1 100.00 2011-05-02

Mellajoki 22 9256/1 100.00 2011-05-02

Mellajoki 23 9256/1 100.00 2011-05-02

Mellajoki 24 9256/1 100.00 2011-05-02

Mellajoki 25 9256/1 100.00 2011-05-02

Mellajoki 26 9256/1 100.00 2011-05-02

Mellajoki 27 9256/1 65.96 2011-05-02

Mellajoki 28 9256/1 62.16 2011-05-02

Mellajoki 29 9256/1 51.90 2011-05-02

Mellajoki 30 9256/1 100.00 2011-05-02

Mellajoki 31 9256/1 100.00 2011-05-02

Mellajoki 32 9256/1 100.00 2011-05-02

Mellajoki 33 9256/1 100.00 2011-05-02

Mellajoki 34 9256/1 100.00 2011-05-02

Mellajoki 35 9256/1 100.00 2011-05-02

Mellajoki 36 9256/1 100.00 2011-05-02

Mellajoki 37 9256/1 100.00 2011-05-02

Mellajoki 38 9256/1 99.92 2011-05-02

Mellajoki 39 9256/1 73.88 2011-05-02

Mellajoki 40 9256/1 100.00 2011-05-02

Mellajoki 41 9256/1 100.00 2011-05-02

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Mellajoki 42 9256/1 99.84 2011-05-02

Mellajoki 43 9256/1 87.34 2011-05-02

Mellajoki 44 9256/1 7.84 2011-05-02

Mellajoki 45 9256/1 83.46 2011-05-02

Mellajoki 46 9256/1 98.08 2011-05-02

Mellajoki 47 9256/1 100.00 2011-05-02

Mellajoki 48 9256/1 100.00 2011-05-02

Mellajoki 49 9256/1 100.00 2011-05-02

Mellajoki 50 9256/1 100.00 2011-05-02

Mellajoki 51 9256/1 100.00 2011-05-02

Mellajoki 52 9256/1 100.00 2011-05-02

Mellajoki 53 9256/1 100.00 2011-05-02

Mellajoki 54 9256/1 100.00 2011-05-02

Mellajoki 55 9256/1 100.00 2011-05-02

Mellajoki 56 9256/1 100.00 2011-05-02

Mellajoki 57 9256/1 100.00 2011-05-02

Mellajoki 58 9256/1 100.00 2011-05-02

Mellajoki 59 9256/1 100.00 2011-05-02

Mellajoki 60 9256/1 100.00 2011-05-02

Mellajoki 61 9256/1 100.00 2011-05-02

Mellajoki 62 9256/1 100.00 2011-05-02

Mellajoki 63 9256/1 100.00 2011-05-02

Mellajoki 64 9256/1 100.00 2011-05-02

Mellajoki 65 9256/1 100.00 2011-05-02

Mellajoki 66 9256/1 100.00 2011-05-02

Mellajoki 67 9256/1 100.00 2011-05-02

Mellajoki 68 9256/1 100.00 2011-05-02

Mellajoki 69 9256/1 100.00 2011-05-02

Mellajoki 70 9256/1 100.00 2011-05-02

Mellajoki 71 9256/1 100.00 2011-05-02

Mellajoki 72 9256/1 100.00 2011-05-02

Mellajoki 73 9256/1 100.00 2011-05-02

Mellajoki 74 9256/1 100.00 2011-05-02

Mellajoki 75 9256/1 100.00 2011-05-02

Mellajoki 76 9256/1 100.00 2011-05-02

Mellajoki 77 9256/1 100.00 2011-05-02

Mellajoki 78 9256/1 100.00 2011-05-02

Mellajärvi 1 9256/1 100.00 2011-05-02

Mellajärvi 2 9256/1 100.00 2011-05-02

Mellajärvi 3 9256/1 70.65 2011-05-02

Mellajärvi 4 9256/1 100.00 2011-05-02

Mellajärvi 5 9256/1 100.00 2011-05-02

Mellajärvi 6 9256/1 80.06 2011-05-02

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Mellajärvi 7 9256/1 27.10 2011-05-02

Mellajärvi 8 9256/1 67.41 2011-05-02

Mellajärvi 9 9256/1 95.80 2011-05-02

Mellajärvi 10 9256/1 96.56 2011-05-02

Mellajärvi 11 9256/1 84.01 2011-05-02

Mellajärvi 12 9256/1 49.66 2011-05-02

Mellajärvi 13 9256/1 68.79 2011-05-02

Mellajärvi 14 9256/1 25.15 2011-05-02

Mellajärvi 15 9256/1 99.18 2011-05-02

Mellajärvi 16 9256/1 100.00 2011-05-02

Mellajärvi 17 9256/1 65.93 2011-05-02

Mellajärvi 18 9256/1 53.60 2011-05-02

Mellajärvi 19 9256/1 58.71 2011-05-02

Mellajärvi 20 9256/1 85.11 2011-05-02

Mellajärvi 21 9256/1 64.54 2011-05-02

Mellajärvi 22 9256/1 66.78 2011-05-02

Mellajärvi 23 9256/1 100.00 2011-05-02

Mellajärvi 24 9256/1 100.00 2011-05-02

Mellajärvi 25 9256/1 90.99 2011-05-02

Mellajärvi 26 9256/1 100.00 2011-05-02

Mellajärvi 27 9256/1 100.00 2011-05-02

Mellajärvi 28 9256/1 100.00 2011-05-02

Mellajärvi 29 9256/1 100.00 2011-05-02

Mellajärvi 30 9256/1 100.00 2011-05-02

Mellajärvi 31 9256/1 99.95 2011-05-02

Mellajärvi 32 9256/1 100.00 2011-05-02

Mellajärvi 33 9256/1 100.00 2011-05-02

Mellajärvi 34 9256/1 100.00 2011-05-02

Mellajärvi 35 9256/1 99.76 2011-05-02

Mellajärvi 36 9256/1 100.00 2011-05-02

Mellajärvi 37 9256/1 100.00 2011-05-02

Mellajärvi 38 9256/1 100.00 2011-05-02

Mellajärvi 39 9256/1 100.00 2011-05-02

Mellajärvi 40 9256/1 100.00 2011-05-02

Mellajärvi 41 9256/1 100.00 2011-05-02

Mellajärvi 42 9256/1 100.00 2011-05-02

Mellajärvi 43 9256/1 100.00 2011-05-02

Mellajärvi 44 9256/1 100.00 2011-05-02

Mellajärvi 45 9256/1 100.00 2011-05-02

Mellajärvi 46 9256/1 100.00 2011-05-02

Mellajärvi 47 9256/1 100.00 2011-05-02

Mellajärvi 48 9256/1 100.00 2011-05-02

Mellajärvi 49 9256/1 100.00 2011-05-02

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Mellajärvi 50 9256/1 19.87 2011-05-02

Mellajärvi 51 9256/1 43.32 2011-05-02

Mellajärvi 52 9256/1 100.00 2011-05-02

Mellajärvi 53 9256/1 100.00 2011-05-02

Mellajärvi 54 9256/1 100.00 2011-05-02

Mellajärvi 55 9256/1 100.00 2011-05-02

Mellajärvi 56 9256/1 100.00 2011-05-02

Mellajärvi 57 9256/1 100.00 2011-05-02

Mellajärvi 58 9256/1 94.97 2011-05-02

Mellajärvi 59 9256/1 59.91 2011-05-02

Mellajärvi 60 9256/1 80.03 2011-05-02

Mellajärvi 61 9256/1 44.98 2011-05-02

Mellakoski 1 9256/1 69.71 2011-05-02

Mellakoski 2 9256/1 68.25 2011-05-02

Mellakoski 3 9256/1 77.64 2011-05-02

Mellakoski 4 9256/1 40.05 2011-05-02

Mellakoski 5 9256/1 100.00 2011-05-02

Mellakoski 6 9256/1 100.00 2011-05-02

Mellakoski 7 9256/1 99.83 2011-05-02

Mellakoski 8 9256/1 97.27 2011-05-02

Mellakoski 9 9256/1 100.00 2011-05-02

Mellakoski 10 9256/1 93.26 2011-05-02

Mellakoski 11 9256/1 98.35 2011-05-02

Mellakoski 12 9256/1 100.00 2011-05-02

Mellakoski 13 9256/1 100.00 2011-05-02

Mellakoski 14 9256/1 96.04 2011-05-02

Mellakoski 15 9256/1 100.00 2011-05-02

Mellakoski 16 9256/1 100.00 2011-05-02

Mellakoski 17 9256/1 71.78 2011-05-02

Mellakoski 18 9256/1 100.00 2011-05-02

Mellakoski 19 9256/1 100.00 2011-05-02

Mellakoski 20 9256/1 96.29 2011-05-02

Mellakoski 21 9256/1 95.21 2011-05-02

Mellakoski 22 9256/1 97.88 2011-05-02

Mellakoski 23 9256/1 80.20 2011-05-02

Mellakoski 24 9256/1 71.44 2011-05-02

Mellakoski 25 9256/1 92.52 2011-05-02

Mellakoski 26 9256/1 57.91 2011-05-02

Mellakoski 27 9256/1 99.31 2011-05-02

Mellakoski 28 9256/1 100.00 2011-05-02

Mellakoski 29 9256/1 49.26 2011-05-02

Mellakoski 30 9256/1 36.71 2011-05-02

Mellakoski 31 9256/1 90.23 2011-05-02

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Mellakoski 32 9256/1 84.61 2011-05-02

Mellakoski 33 9256/1 97.53 2011-05-02

Mellakoski 34 9256/1 75.71 2011-05-02

Mellakoski 35 9256/1 9.85 2011-05-02

Mellakoski 36 9256/1 75.66 2011-05-02

Mellakoski 37 9256/1 86.39 2011-05-02

Mellakoski 38 9256/1 89.02 2011-05-02

Mellakoski 39 9256/1 100.00 2011-05-02

Mellakoski 40 9256/1 100.00 2011-05-02

Mellakoski 41 9256/1 95.34 2011-05-02

Mellakoski 42 9256/1 21.74 2011-05-02

Mellakoski 43 9256/1 95.14 2011-05-02

Mellakoski 44 9256/1 75.17 2011-05-02

Mellakoski 45 9256/1 23.62 2011-05-02

Mellakoski 46 9256/1 100.00 2011-05-02

Mellakoski 47 9256/1 48.42 2011-05-02

Mellakoski 48 9256/1 87.71 2011-05-02

Mellakoski 49 9256/1 100.00 2011-05-02

Mellakoski 50 9256/1 59.92 2011-05-02

Mellakoski 51 9256/1 100.00 2011-05-02

Mellakoski 52 9256/1 97.75 2011-05-02

Mellakoski 53 9256/1 100.00 2011-05-02

Mellakoski 54 9256/1 100.00 2011-05-02

Mellakoski 55 9256/1 100.00 2011-05-02

Mellakoski 56 9256/1 95.21 2011-05-02

Mellakoski 57 9256/1 100.00 2011-05-02

Mellakoski 58 9256/1 100.00 2011-05-02

Mustiaapa 1 9256/1 50.00 2011-05-02

Mustiaapa 2 9256/1 100.00 2011-05-02

Mustiaapa 3 9256/1 50.00 2011-05-02

Mustiaapa 4 9256/1 100.00 2011-05-02

Mustiaapa 5 9256/1 100.00 2011-05-02

Mustiaapa 6 9256/1 50.00 2011-05-02

Mustiaapa 7 9256/1 65.10 2011-05-02

Mustiaapa 8 9256/1 99.29 2011-05-02

Mustiaapa 9 9256/1 100.00 2011-05-02

Mustiaapa 10 9256/1 100.00 2011-05-02

Mustiaapa 15 9256/1 50.00 2011-05-02

Mustiaapa 11 9256/1 29.08 2011-05-02

Mustiaapa 12 9256/1 92.58 2011-05-02

Mustiaapa 13 9256/1 100.00 2011-05-02

Mustiaapa 16 9256/1 100.00 2011-05-02

Mustiaapa 17 9256/1 100.00 2011-05-02

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Mustiaapa 18 9256/1 100.00 2011-05-02

Mustiaapa 19 9256/1 100.00 2011-05-02

Mustiaapa 26 9256/1 100.00 2011-05-02

Mustiaapa 27 9256/1 100.00 2011-05-02

Mustiaapa 28 9256/1 100.00 2011-05-02

Mustiaapa 29 9256/1 100.00 2011-05-02

Mustiaapa 14 9256/1 69.16 2011-05-02

Mustiaapa 20 9256/1 99.36 2011-05-02

Mustiaapa 21 9256/1 100.00 2011-05-02

Mustiaapa 22 9256/1 100.00 2011-05-02

Mustiaapa 23 9256/1 100.00 2011-05-02

Mustiaapa 30 9256/1 100.00 2011-05-02

Mustiaapa 31 9256/1 100.00 2011-05-02

Mustiaapa 32 9256/1 100.00 2011-05-02

Mustiaapa 33 9256/1 100.00 2011-05-02

Mustiaapa 24 9256/1 72.31 2011-05-02

Mustiaapa 25 9256/1 93.46 2011-05-02

Mustiaapa 34 9256/1 81.82 2011-05-02

Mustiaapa 35 9256/1 98.54 2011-05-02

Mustijoki 1 9256/1 29.19 2011-05-02

Mustijoki 2 9256/1 97.54 2011-05-02

Mustijoki 3 9256/1 100.00 2011-05-02

Mustijoki 4 9256/1 100.00 2011-05-02

Mustijoki 5 9256/1 99.85 2011-05-02

Mustijoki 6 9256/1 100.00 2011-05-02

Mustijoki 7 9256/1 100.00 2011-05-02

Mustijoki 8 9256/1 100.00 2011-05-02

Mustijoki 9 9256/1 100.00 2011-05-02

Mustijoki 10 9256/1 100.00 2011-05-02

Mustijoki 11 9256/1 100.00 2011-05-02

Mustijoki 12 9256/1 100.00 2011-05-02

Mustijoki 13 9256/1 95.93 2011-05-02

Mustijoki 14 9256/1 100.00 2011-05-02

Mustijoki 15 9256/1 100.00 2011-05-02

Mustijoki 16 9256/1 100.00 2011-05-02

Mustijoki 17 9256/1 99.64 2011-05-02

Mustijoki 18 9256/1 90.19 2011-05-02

Mustijoki 19 9256/1 81.63 2011-05-02

Mustijoki 20 9256/1 94.78 2011-05-02

Mustijoki 21 9256/1 96.85 2011-05-02

Mustijoki 22 9256/1 65.69 2011-05-02

Mustijoki 23 9256/1 100.00 2011-05-02

Mustijoki 24 9256/1 83.66 2011-05-02

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Mustijoki 25 9256/1 99.98 2011-05-02

Mustijoki 26 9256/1 74.55 2011-05-02

Mustijoki 27 9256/1 80.73 2011-05-02

Mustijoki 28 9256/1 100.00 2011-05-02

Mustijoki 29 9256/1 99.68 2011-05-02

Rajakirakka 1 9256/1 100.00 2011-05-02

Rajakirakka 2 9256/1 89.55 2011-05-02

Rajakirakka 3 9256/1 61.26 2011-05-02

Rajakirakka 4 9256/1 100.00 2011-05-02

Rajakirakka 5 9256/1 49.08 2011-05-02

Rajakirakka 6 9256/1 100.00 2011-05-02

Rajakirakka 7 9256/1 100.00 2011-05-02

Rajakirakka 8 9256/1 100.00 2011-05-02

Rajakirakka 9 9256/1 100.00 2011-05-02

Rajakirakka 10 9256/1 50.00 2011-05-02

Rajakirakka 11 9256/1 100.00 2011-05-02

Rajakirakka 12 9256/1 100.00 2011-05-02

Rajakirakka 13 9256/1 100.00 2011-05-02

Rajakirakka 14 9256/1 100.00 2011-05-02

Rajakirakka 15 9256/1 100.00 2011-05-02

Rajakirakka 16 9256/1 100.00 2011-05-02

Rajakirakka 17 9256/1 93.53 2011-05-02

Rajakirakka 18 9256/1 62.22 2011-05-02

Rajakirakka 19 9256/1 32.17 2011-05-02

Rajakirakka 20 9256/1 38.31 2011-05-02

Rajakirakka 21 9256/1 74.72 2011-05-02

Rajakirakka 22 9256/1 50.00 2011-05-02

Rajakirakka 23 9256/1 96.17 2011-05-02

Rajakirakka 24 9256/1 100.00 2011-05-02

Rajakirakka 25 9256/1 100.00 2011-05-02

Rajakirakka 26 9256/1 100.00 2011-05-02

Ristiaapa 1 9256/1 100.00 2011-05-02

Ristiaapa 2 9256/1 100.00 2011-05-02

Ristiaapa 3 9256/1 100.00 2011-05-02

Ristiaapa 4 9256/1 100.00 2011-05-02

Ristiaapa 5 9256/1 100.00 2011-05-02

Ristiaapa 6 9256/1 100.00 2011-05-02

Ristiaapa 7 9256/1 100.00 2011-05-02

Ristiaapa 8 9256/1 100.00 2011-05-02

Ristiaapa 9 9256/1 75.16 2011-05-02

Ristiaapa 10 9256/1 100.00 2011-05-02

Ristiaapa 11 9256/1 100.00 2011-05-02

Ristiaapa 12 9256/1 86.39 2011-05-02

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Ristiaapa 13 9256/1 100.00 2011-05-02

Ristiaapa 14 9256/1 100.00 2011-05-02

Ristiaapa 15 9256/1 100.00 2011-05-02

Ristiaapa 16 9256/1 100.00 2011-05-02

Ristiaapa 17 9256/1 100.00 2011-05-02

Ristiaapa 18 9256/1 100.00 2011-05-02

Ristiaapa 19 9256/1 100.00 2011-05-02

Ristiaapa 20 9256/1 100.00 2011-05-02

Ristiaapa 21 9256/1 100.00 2011-05-02

Ristiaapa 22 9256/1 100.00 2011-05-02

Ristiaapa 23 9256/1 100.00 2011-05-02

Ristiaapa 24 9256/1 100.00 2011-05-02

Ristiaapa 25 9256/1 100.00 2011-05-02

Ristiaapa 26 9256/1 100.00 2011-05-02

Ristiaapa 27 9256/1 100.00 2011-05-02

Ristiaapa 28 9256/1 100.00 2011-05-02

Ristiaapa 29 9256/1 100.00 2011-05-02

Ristiaapa 30 9256/1 100.00 2011-05-02

Ristiaapa 31 9256/1 100.00 2011-05-02

Ristiaapa 32 9256/1 100.00 2011-05-02

Ristiaapa 33 9256/1 100.00 2011-05-02

Ristiaapa 34 9256/1 100.00 2011-05-02

Ristiaapa 35 9256/1 100.00 2011-05-02

Ristiaapa 36 9256/1 100.00 2011-05-02

Ristiaapa 37 9256/1 100.00 2011-05-02

Ristijärvi 1 9256/1 53.43 2011-05-02

Ristijärvi 2 9256/1 99.15 2011-05-02

Ristijärvi 3 9256/1 58.23 2011-05-02

Ristijärvi 4 9256/1 51.95 2011-05-02

Ristijärvi 6 9256/1 40.85 2011-05-02

Ristijärvi 5 9256/1 86.48 2011-05-02

Ristijärvi 7 9256/1 14.53 2011-05-02

Ristijärvi 8 9256/1 100.00 2011-05-02

Ristijärvi 9 9256/1 91.57 2011-05-02

Ristijärvi 10 9256/1 28.97 2011-05-02

Ristijärvi 11 9256/1 100.00 2011-05-02

Ristijärvi 12 9256/1 100.00 2011-05-02

Ristijärvi 13 9256/1 83.37 2011-05-02

Ristijärvi 14 9256/1 74.95 2011-05-02

Ristijärvi 15 9256/1 100.00 2011-05-02

Ristijärvi 16 9256/1 92.14 2011-05-02

Ristijärvi 17 9256/1 100.00 2011-05-02

Ristijärvi 18 9256/1 100.00 2011-05-02

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Ristijärvi 19 9256/1 100.00 2011-05-02

Ristijärvi 20 9256/1 100.00 2011-05-02

Ristijärvi 21 9256/1 100.00 2011-05-02

Ristijärvi 22 9256/1 100.00 2011-05-02

Ristijärvi 23 9256/1 100.00 2011-05-02

Ristijärvi 24 9256/1 100.00 2011-05-02

Ristijärvi 25 9256/1 83.93 2011-05-02

Ristijärvi 26 9256/1 100.00 2011-05-02

Ristijärvi 27 9256/1 100.00 2011-05-02

Ristijärvi 28 9256/1 44.53 2011-05-02

Ristijärvi 29 9256/1 91.82 2011-05-02

Ristijärvi 30 9256/1 100.00 2011-05-02

Ristijärvi 31 9256/1 94.73 2011-05-02

Ristijärvi 32 9256/1 96.34 2011-05-02

Ristijärvi 33 9256/1 96.19 2011-05-02

Ristijärvi 34 9256/1 100.00 2011-05-02

Ristijärvi 35 9256/1 100.00 2011-05-02

Ristijärvi 36 9256/1 32.82 2011-05-02

Ristijärvi 37 9256/1 98.85 2011-05-02

Ristijärvi 38 9256/1 100.00 2011-05-02

Ristijärvi 39 9256/1 30.16 2011-05-02

Ristijärvi 40 9256/1 76.93 2011-05-02

Ristijärvi 41 9256/1 100.00 2011-05-02

Ristijärvi 42 9256/1 96.75 2011-05-02

Ristijärvi 43 9256/1 100.00 2011-05-02

Ristijärvi 44 9256/1 100.00 2011-05-02

Ristijärvi 45 9256/1 100.00 2011-05-02

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Granted Reservations New Act

Reservation Mining registry Area in Date of Date granted Date of

name number/reservation hectares application expiry

Mustavaara VA2012:0193-01 12140 12/12/2012 10/7/2013 12/12/2014

Granted Exploration Permits New Act

Claim application Mining registry Area in Date of

name number/Claim hectares application

Identification

Kairamaat 2-3 ML2013:0041-01H 1462 7/19/2013

Applied Exploration Permits New Act

Claim application Mining registry Area in Date of

name number/Claim hectares application

identification

Kairamaat 1 263 7/19/2013

Kultamaat,Hirvimaa ML2014:0033-01H 4202 4/15/2014

Raja 890 7/21/2014

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Appendix 2: List of Drill Holes Collars Drilled by Mawson to Date at Rompas

Prospect Name HoleID Prospect Easting Northing TotalDepth (m) Dip AzimUTM

Kaita KD0001 ROM 3401928 7372824 59.4 -49.4 250

Kaita KD0002 ROM 3401942 7372829 58.7 -49.7 250

Kaita KD0003 ROM 3401928 7372834 59.4 -50.2 250

Kaita KD0004 ROM 3401980 7372932 59.5 -49.8 250

Kaita KD0005 ROM 3401858 7373000 60 -49.6 250

Kaita KD0006 ROM 3401877 7373007 59.6 -49.1 250

Kaita KD0007 ROM 3401808 7373173 59.6 -49.4 250

Kaita KD0008 ROM 3401803 7373123 62.2 -49.9 250

Kaita KD0009 ROM 3401825 7373131 62 -48.7 250

Kaita KD0010 ROM 3401843 7373117 59.4 -50.8 250

Kaita KD0011 ROM 3401821 7373109 59 -51.4 250

Kaita KD0012 ROM 3401844 7373061 60.7 -49.8 250

Kaita KD0013 ROM 3401869 7373070 64.7 -49.4 250

Hirvimaa LD0001 RAJ 3409740 7374505 5.4 -90.0 0

Hirvimaa LD0002 RAJ 3409726 7374520 7 -90.0 0

Hirvimaa LD0003 RAJ 3409716 7374531 5.8 -90.0 0

Hirvimaa LD0004 RAJ 3409700 7374542 6.1 -90.0 0

Hirvimaa LD0005 RAJ 3409684 7374551 6.4 -90.0 0

Hirvimaa LD0006 RAJ 3409666 7374566 7.6 -90.0 0

Hirvimaa LD0007 RAJ 3409647 7374577 5.6 -90.0 0

Hirvimaa LD0008 RAJ 3409672 7374559 182 -90.0 0

Hirvimaa LD0009 RAJ 3409635 7374591 6.9 -90.0 0

Hirvimaa LD0010 RAJ 3409620 7374602 5.9 -90.0

Hirvimaa LD0011 RAJ 3409600 7374616 6 -90.0 0

Hirvimaa LD0012 RAJ 3409580 7374471 6.2 -90.0 0

Hirvimaa LD0013 RAJ 3409567 7374476 5 -90.0 0

Hirvimaa LD0014 RAJ 3409549 7374491 5 -90.0 0

Hirvimaa LD0015 RAJ 3409532 7374506 5 -90.0 0

Hirvimaa LD0016 RAJ 3409509 7374517 5 -90.0 0

Hirvimaa LD0017 RAJ 3409497 7374526 6.6 -90.0 0

Hirvimaa LD0018 RAJ 3409484 7374540 5 -90.0 0

Hirvimaa LD0019 RAJ 3409466 7374554 7.1 -90.0 0

Hirvimaa LD0020 RAJ 3409434 7374577 6.1 -90.0 0

Hirvimaa LD0021 RAJ 3409395 7374601 6.1 -90.0 0

Hirvimaa LD0022 RAJ 3409370 7374627 4.8 -90.0 0

Hirvimaa LD0023 RAJ 3409343 7374553 9.4 -90.0 0

Hirvimaa LD0024 RAJ 3409326 7374566 8 -90.0 0

Hirvimaa LD0025 RAJ 3409351 7374545 4.8 -90.0 0

Hirvimaa LD0026 RAJ 3409306 7374578 8 -90.0 0

Hirvimaa LD0027 RAJ 3409286 7374586 6 -90.0 0

Hirvimaa LD0028 RAJ 3409353 7374637 6.5 -90.0 0

Hirvimaa LD0029 RAJ 3409335 7374654 8.1 -90.0 0

Hirvimaa LD0030 RAJ 3409315 7374664 5 -90.0 0

Hirvimaa LD0031 RAJ 3409300 7374676 7 -90.0 0

Hirvimaa LD0032 RAJ 3409198 7374699 7 -90.0 0

Hirvimaa LD0033 RAJ 3409181 7374713 6 -90.0 0

Hirvimaa LD0034 RAJ 3409166 7374722 5 -90.0 0

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Hirvimaa LD0035 RAJ 3409147 7374736 6 -90.0 0

Hirvimaa LD0036 RAJ 3408934 7374691 6 -90.0 0

Hirvimaa LD0037 RAJ 3408946 7374677 7.2 -90.0 0

Hirvimaa LD0038 RAJ 3408959 7374664 6.9 -90.0 0

Hirvimaa LD0039 RAJ 3408717 7374710 10.5 -90.0 0

Hirvimaa LD0040 RAJ 3408709 7374727 3.9 -90.0 0

Hirvimaa LD0041 RAJ 3408699 7374746 5.4 -90.0 0

Hirvimaa LD0042 RAJ 3408691 7374763 4.1 -90.0 0

Hirvimaa LD0043 RAJ 3408678 7374777 4.9 -90.0 0

Hirvimaa LD0044 RAJ 3408673 7374795 5 -90.0 0

Hirvimaa LD0045 RAJ 3410705 7374721 7.1 -90.0 0

Hirvimaa LD0046 RAJ 3410704 7374680 6.8 -90.0 0

Hirvimaa LD0047 RAJ 3410701 7374634 8 -90.0 0

Hirvimaa LD0048 RAJ 3410704 7374596 8.5 -90.0 0

Hirvimaa LD0049 RAJ 3411200 7374316 8.5 -90.0 0

Hirvimaa LD0050 RAJ 3411200 7374359 7.7 -90.0 0

Hirvimaa LD0051 RAJ 3411195 7374398 4.4 -90.0 0

Hirvimaa LD0052 RAJ 3411185 7374434 7.2 -90.0 0

Hirvimaa LD0053 RAJ 3411194 7374479 6.5 -90.0 0

Hirvimaa LD0054 RAJ 3411195 7374516 8 -90.0 0

Hirvimaa LD0055 RAJ 3411193 7374608 8.8 -90.0 0

Hirvimaa LD0056 RAJ 3411205 7374640 4 -90.0 0

Hirvimaa LD0057 RAJ 3411198 7374684 10.2 -90.0 0

Hirvimaa LD0058 RAJ 3411195 7374716 7 -90.0 0

Hirvimaa LD0059 RAJ 3411199 7374763 7 -90.0 0

Hirvimaa LD0060 RAJ 3411262 7374834 10.1 -90.0 0

Hirvimaa LD0061 RAJ 3409252 7374164 7.8 -90.0 0

Hirvimaa LD0062 RAJ 3409237 7374179 11.4 -90.0 0

Hirvimaa LD0063 RAJ 3409223 7374193 11.3 -90.0 0

Hirvimaa LD0064 RAJ 3409211 7374206 10.2 -90.0 0

Hirvimaa LD0065 RAJ 3409198 7374220 8 -90.0 0

Hirvimaa LD0066 RAJ 3409220 7374198 13.3 -90.0 0

Hirvimaa LD0067 RAJ 3409232 7374185 9.8 -90.0 0

Hirvimaa LD0068 RAJ 3409181 7374230 10.4 -90.0 0

Hirvimaa LD0069 RAJ 3409168 7374242 9 -90.0 0

Hirvimaa LD0070 RAJ 3409147 7374263 9 -90.0 0

Hirvimaa LD0071 RAJ 3409148 7374416 8.2 -90.0 0

Hirvimaa LD0072 RAJ 3409176 7374391 6.9 -90.0 0

Hirvimaa LD0073 RAJ 3409207 7374365 7.1 -90.0 0

Hirvimaa LD0074 RAJ 3409237 7374341 8.7 -90.0 0

Hirvimaa LD0075 RAJ 3409251 7374327 8.3 -90.0 0

Hirvimaa LD0076 RAJ 3409267 7374312 5.8 -90.0 0

Hirvimaa LD0077 RAJ 3409279 7374300 4.5 -90.0 0

Hirvimaa LD0078 RAJ 3409298 7374287 7.5 -90.0 0

Hirvimaa LD0079 RAJ 3409318 7374273 6.7 -90.0 0

Hirvimaa LD0080 RAJ 3409330 7374262 5.5 -90.0 0

Hirvimaa LD0081 RAJ 3409341 7374248 7 -90.0 0

Hirvimaa LD0082 RAJ 3409374 7374225 8.7 -90.0 0

Hirvimaa LD0083 RAJ 3409411 7374204 9.5 -90.0 0

Hirvimaa LD0084 RAJ 3409438 7374197 7.5 -90.0 0

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Hirvimaa LD0085 RAJ 3409426 7374202 10.5 -90.0 0

Hirvimaa LD0086 RAJ 3409451 7374187 8 -90.0 0

Hirvimaa LD0087 RAJ 3409433 7374169 9.5 -90.0 0

Hirvimaa LD0088 RAJ 3409465 7374144 8.1 -90.0 0

Hirvimaa LD0089 RAJ 3409489 7374118 7.4 -90.0 0

Hirvimaa LD0090 RAJ 3409688 7374128 4.5 -90.0 0

Hirvimaa LD0091 RAJ 3409702 7374117 4 -90.0 0

Hirvimaa LD0092 RAJ 3409806 7374204 6.5 -90.0 0

Hirvimaa LD0093 RAJ 3409792 7374212 4.8 -90.0 0

Hirvimaa LD0094 RAJ 3409498 7374313 6 -90.0 0

Hirvimaa LD0095 RAJ 3409446 7374349 4.1 -90.0 0

Hirvimaa LD0096 RAJ 3409432 7374365 5 -90.0 0

Hirvimaa LD0097 RAJ 3409414 7374379 6 -90.0 0

Hirvimaa LD0098 RAJ 3409404 7374387 7 -90.0 0

Hirvimaa LD0099 RAJ 3409397 7374392 5.8 -90.0 0

Hirvimaa LD0100 RAJ 3409377 7374405 6 -90.0 0

Hirvimaa LD0101 RAJ 3409370 7374410 8.1 -90.0 0

Hirvimaa LD0102 RAJ 3409353 7374421 8 -90.0 0

Hirvimaa LD0103 RAJ 3409337 7374433 7.5 -90.0 0

Hirvimaa LD0104 RAJ 3409170 7374459 10 -90.0 0

Hirvimaa LD0105 RAJ 3409151 7374467 8.6 -90.0 0

Hirvimaa LD0106 RAJ 3409096 7374384 7 -90.0 0

Hirvimaa LD0107 RAJ 3409055 7374402 7.5 -90.0 0

Hirvimaa LD0108 RAJ 3409023 7374411 5.8 -90.0 0

Hirvimaa LD0109 RAJ 3408986 7374435 7.6 -90.0 0

Hirvimaa LD0110 RAJ 3408951 7374448 7.3 -90.0 0

Hirvimaa LD0111 RAJ 3408917 7374468 10 -90.0 0

Hirvimaa LD0112 RAJ 3409414 7374183 11.5 -90.0 0

Hirvimaa LD0113 RAJ 3409405 7374189 11.2 -90.0 0

Hirvimaa LD0114 RAJ 3409409 7374185 9.1 -90.0 0

Hirvimaa LD0115 RAJ 3409418 7374179 9.9 -90.0 0

Hirvimaa LD0116 RAJ 3409407 7374176 12.7 -90.0 0

Hirvimaa LD0117 RAJ 3409396 7374176 9.4 -90.0 0

Hirvimaa LD0118 RAJ 3409368 7374154 9.1 -90.0 0

Hirvimaa LD0119 RAJ 3409334 7374166 8.5 -90.0 0

Hirvimaa LD0120 RAJ 3409380 7374190 9.7 -90.0 0

Shallow North Rompas NROM001 ROM 3399475 7378557 4.95 90.0 0

Shallow North Rompas NROM002 ROM 3399456 7378551 6 -90.0

Shallow North Rompas NROM003 ROM 3399433 7378557 5.9 -90.0

Shallow North Rompas NROM004 ROM 3399411 7378566 8.3 -90.0 0

Shallow North Rompas NROM005 ROM 3399396 7378575 8 -90.0 0

Shallow North Rompas NROM006 ROM 3399374 7378566 5.55 -90.0 0

Shallow North Rompas NROM007 ROM 3399356 7373793 3.9 -90.0 0

Shallow North Rompas NROM008 ROM 3399336 7378552 3 -90.0 0

Shallow North Rompas NROM009 ROM 3399314 7378543 6.7 -90.0 0

Shallow North Rompas NROM010 ROM 3399295 7378538 2.9 -90.0 0

Shallow North Rompas NROM011 ROM 3399282 7378538 3.4 -90.0 0

Shallow North Rompas NROM012 ROM 3399266 7378525 3.7 -90.0 0

Shallow North Rompas NROM013 ROM 3399255 7378509 4.35 -90.0 0

Shallow North Rompas NROM014 ROM 3399256 7378491 3.85 -90.0 0

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Shallow North Rompas NROM015 ROM 3399248 7378474 3.9 -90.0 0

Shallow North Rompas NROM016 ROM 3399243 7378434 5.8 -90.0 0

Shallow North Rompas NROM017 ROM 3399222 7378397 9.5 -90.0 0

Shallow North Rompas NROM018 ROM 3399212 7378353 6 -90.0 0

Shallow North Rompas NROM019 ROM 3399491 7378572 3.95 -90.0 0

Shallow North Rompas NROM020 ROM 3399509 7378588 5.65 -90.0 0

Shallow North Rompas NROM021 ROM 3399522 7378598 6.9 -90.0 0

Shallow North Rompas NROM022 ROM 3399536 7378614 6.85 -90.0 0

Shallow North Rompas NROM023 ROM 3399242 7378714 5.6 -90.0 0

Shallow North Rompas NROM024 ROM 3399295 7378714 4.15 -90.0 0

Shallow North Rompas NROM025 ROM 3399184 7378675 8.3 -90.0 0

Shallow North Rompas NROM026 ROM 3399549 7378638 5.9 -90.0 0

Shallow North Rompas NROM027 ROM 3399571 7378629 6.75 -90.0 0

Shallow North Rompas NROM028 ROM 3399680 7378658 6.9 -90.0 0

PAL PAL0001 RAJ 3408871 7374467 110.95 -45.2 135

PAL PAL0002 RAJ 3408912 7374424 98.75 -45.8 135

PAL PAL0003 RAJ 3409829 7374326 14.05 -45.0 150

PAL PAL0003B RAJ 3409832 7374326 160.5 -44.8 150

PAL PAL0004 RAJ 3409865 7374269 121.5 -44.6 150

PAL PAL0005 RAJ 3409944 7374362 51.55 -45.0 150

PAL PAL0006 RAJ 3409977 7374300 95.5 -43.8 150

PAL PAL0007 RAJ 3411300 7374683 104.3 -44.5 150

Rajapalot Regional PRAJ0001 RAJ 3408254 7375081 3.54 60.0 358

Rajapalot Regional PRAJ0002 RAJ 3408254 7375081 6.95 60.0 358

Palokas PRAJ0003 RAJ 3408688 7373822 20.19 -60.0 118

Palokas PRAJ0004 RAJ 3408681 7373826 19.63 60.0 116

Palokas PRAJ0005 RAJ 3408673 7373830 19.26 60.0 116

Palokas PRAJ0006 RAJ 3408686 7373839 29.03 -60.0 116

Palokas PRAJ0007 RAJ 3408705 7373831 5 60.0 116

Palokas PRAJ0008 RAJ 3408696 7373836 13.3 60.0 116

Palokas PRAJ0009 RAJ 3408711 7373854 34.95 60.0 116

Palokas PRAJ0010 RAJ 3408709 7373859 13.02 60.0 116

Palokas PRAJ0011 RAJ 3408753 7373879 4.3 60.0 140

Palokas PRAJ0012 RAJ 3408730 7373906 3.36 60.0 140

Palokas PRAJ0013 RAJ 3408736 7373899 2.3 60.0 140

Palokas PRAJ0014 RAJ 3408743 7373891 7.28 60.0 140

Palokas PRAJ0015 RAJ 3408729 7373862 12.67 60.0 116

Palokas PRAJ0016 RAJ 3408686 7373802 28.37 60.0 116

Palokas PRAJ0017 RAJ 3408686 7373776 23 60.0 116

Palokas PRAJ0018 RAJ 3408677 7373765 20.75 60.0 116

Palokas PRAJ0019 RAJ 3408666 7373787 4.5 60.0 116

Palokas PRAJ0020 RAJ 3408673 7373808 31.2 60.0 116

Palokas PRAJ0021 RAJ 3408695 7373819 19.94 60.0 116

Palokas PRAJ0022 RAJ 3408677 7373842 37.5 60.0 116

Palokas PRAJ0023 RAJ 3408684 7373863 28.52 76.5 116

Palokas PRAJ0024 RAJ 3408673 7373868 37.02 76.5 116

Palokas PRAJ0025 RAJ 3408697 7373878 40.25 76.5 116

Palokas PRAJ0026 RAJ 3408693 7373856 35.2 75.5 296

Palokas PRAJ0027 RAJ 3408795 7373932 12.46 76.5 140

Palokas PRAJ0028 RAJ 3408784 7373942 22.34 76.5 140

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Palokas PRAJ0029 RAJ 3408770 7373958 20.55 77.0 140

Palokas PRAJ0030 RAJ 3408756 7373974 27.85 77.0 140

Rajapalot Regional PRAJ0031 RAJ 3409623 7375180 6.74 -60.0 135

Rajapalot Regional PRAJ0032 RAJ 3409642 7375161 13.8 -60.0 132

Rajapalot Regional PRAJ0033 RAJ 3409659 7375143 11.55 -60.0 135

Rajapalot Regional PRAJ0034 RAJ 3409611 7375201 7.8 -60.0 135

Rajapalot Regional PRAJ0035 RAJ 3409562 7374969 9.35 -60.0 224

Rajapalot Regional PRAJ0036 RAJ 3409205 7374181 6.1 -60.0 224

Rajapalot Regional PRAJ0037 RAJ 3409200 7374191 19.25 -60.0 224

Rajapalot Regional PRAJ0038 RAJ 3409178 7374214 13.55 -60.0 224

Rajapalot Regional PRAJ0039 RAJ 3409483 7374210 11.6 -60.0 135

Rajapalot Regional PRAJ0040 RAJ 3409472 7374214 12.45 -60.0 135

Rajapalot Regional PRAJ0041 RAJ 3409467 7374235 10.05 -61.0 135

Rajapalot Regional PRAJ0042 RAJ 3409456 7374248 11.1 -60.0 138

Rajapalot Regional PRAJ0043 RAJ 3409444 7374264 8.8 -60.0 132

Rajapalot Regional PRAJ0044 RAJ 3409424 7374272 13.35 -60.0 135

Rajapalot Regional PRAJ0045 RAJ 3409412 7374290 5.6 -60.0 135

Rajapalot Regional PRAJ0046 RAJ 3409402 7374306 6.85 -60.0 135

Rajapalot Regional PRAJ0047 RAJ 3410301 7373140 31.85 -58.0 155

Rajapalot Regional PRAJ0048 RAJ 3410294 7373151 34.1 -60.0 155

Rajapalot Regional PRAJ0049 RAJ 3410280 7373160 31.25 -60.0 155

Rajapalot Regional PRAJ0050 RAJ 3410478 7373137 28.35 -60.0 155

Rajapalot Regional PRAJ0051 RAJ 3410433 7373156 7.5 -60.0 110

Rajapalot Regional PRAJ0052 RAJ 3410413 7373164 15.8 -85.0 115

Rajapalot Regional PRAJ0053 RAJ 3410354 7373192 17.3 -60.0 110

Rajapalot Regional PRAJ0054 RAJ 3410298 7373206 9.65 -60.0 110

Rajapalot Regional PRAJ0055 RAJ 3410880 7372767 21.75 -60.0 123

Rajapalot Regional PRAJ0056 RAJ 3410600 7372701 26.4 -60.0 134

Rajapalot Regional PRAJ0057 RAJ 3409451 7372108 26.7 -60.0 148

Rajapalot Regional PRAJ0058 RAJ 3409562 7372099 9 -60.0 152

Rajapalot Regional PRAJ0059 RAJ 3409572 7372082 8 -60.0 147

Rajapalot Regional PRAJ0060 RAJ 3409593 7372045 8.6 -60.0 153

Rajapalot Regional PRAJ0061 RAJ 3409554 7372042 9.5 -60.0 153

Rajapalot Regional PRAJ0062 RAJ 3409514 7371997 3 60.0 149

Rajapalot Regional PRAJ0063 RAJ 3409514 7371997 8 90.0

Rajapalot Regional PRAJ0064 RAJ 3409647 7372161 6.15 86.0 152

Rajapalot Regional PRAJ0065 RAJ 3410054 7372039 18.85 61.0 150

Rajapalot Regional PRAJ0068 RAJ 3410473 7373367 10.25 60.0 150

Rajapalot Regional PRAJ0069 RAJ 3410195 7373026 15.35 60.0 152

Kaita Shallow PROM0001 ROM 3401849 7372989 15.03 -60.0 90

Kaita Shallow PROM0002 ROM 3401831 7372990 6 -60.0 90

Kaita Shallow PROM0003 ROM 3401860 7372991 15.28 -60.0 90

Kaita Shallow PROM0004 ROM 3401820 7372988 15.65 -60.0 90

Kaita Shallow PROM0005 ROM 3401812 7372992 16.41 -60.0 90

Kaita Shallow PROM0006 ROM 3401872 7372991 15.47 -60.0 90

Kaita Shallow PROM0007 ROM 3401892 7372986 9.46 -60.0 270

Kaita Shallow PROM0008 ROM 3401973 7372930 10.3 -62.0 270

Kaita Shallow PROM0009 ROM 3401983 7372929 5.35 -60.0 270

Kaita Shallow PROM0010 ROM 3401994 7372927 19.21 -60.0 270

Kaita Shallow PROM0011 ROM 3402006 7372931 6.57 -60.0 270

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Kaita Shallow PROM0012 ROM 3402039 7372930 19.71 -60.0 270

Kaita Shallow PROM0013 ROM 3401940 7372933 9.72 -60.0 270

Kaita Shallow PROM0014 ROM 3401909 7372819 20.68 -60.0 245

Kaita Shallow PROM0015 ROM 3401915 7372819 15.67 -60.0 238

Kaita Shallow PROM0016 ROM 3401916 7372820 30 -60.0 143

Kaita Shallow PROM0017 ROM 3401920 7372823 17.32 -60.0 234

Kaita Shallow PROM0018 ROM 3401935 7372835 19.95 -60.0 234

Kaita Shallow PROM0019 ROM 3402390 7372695 14.53 60.0 110

Kaita Shallow PROM0020 ROM 3402340 7372708 5.5 60.0 110

Kaita Shallow PROM0021 ROM 3402356 7372700 9.91 61.0 110

Kaita Shallow PROM0022 ROM 3402301 7372721 9.53 60.0 110

Kaita Shallow PROM0023 ROM 3402103 7372784 9.77 60.0 110

Kaita Shallow PROM0024 ROM 3402049 7372802 6.88 60.0 290

Kaita Shallow PROM0025 ROM 3402010 7372801 7 60.0 290

Kaita Shallow PROM0026 ROM 3401960 7372821 8 60.0 290

Kaita Shallow PROM0027 ROM 3401920 7372935 8.68 69.0 270

Kaita Shallow PROM0028 ROM 3401903 7372938 9.77 69.0 270

Kaita Shallow PROM0029 ROM 3401874 7372937 15.58 69.0 270

Kaita Shallow PROM0030 ROM 3401855 7372937 14.79 69.0 270

Kaita Shallow PROM0031 ROM 3401828 7372932 7.71 70.0 270

Kaita Shallow PROM0032 ROM 3401817 7372934 10.47 75.0 270

Kaita Shallow PROM0033 ROM 3401789 7372933 10.08 70.0 270

Kaita Shallow PROM0034 ROM 3401758 7372929 12.54 70.0 270

Kaita Shallow PROM0035 ROM 3401732 7372930 12.34 72.0 270

Kaita Shallow PROM0036 ROM 3401785 7373119 10.69 60.0 68

Kaita Shallow PROM0037 ROM 3401777 7373119 12.31 60.0 68

South Rompas ROM0001 ROM 3401495 7373295 82.9 -44.3 88

South Rompas ROM0002 ROM 3401498 7373315 100.6 -43.6 78

South Rompas ROM0003 ROM 3401488 7373275 109.6 -43.8 77

South Rompas ROM0004 ROM 3401483 7373255 103.7 -43.6 83

South Rompas ROM0005 ROM 3401455 7373293 82.76 -43.6 82

South Rompas ROM0006 ROM 3401460 7373316 85.4 -43.4 88

South Rompas ROM0007 ROM 3401444 7373255 109.8 -44.3 83

South Rompas ROM0008 ROM 3401395 7373254 106.6 -43.1 9

South Rompas ROM0009 ROM 3401366 7373766 86.05 -44.7 78

South Rompas ROM0010 ROM 3401323 7373759 93.1 -44.9 79

South Rompas ROM0011 ROM 3401341 7373794 151.4 -45.4 80

South Rompas ROM0012 ROM 3401333 7373815 100.55 -44.4 77

South Rompas ROM0013 ROM 3401392 7373771 75.4 -44.8 268

South Rompas ROM0014 ROM 3401308 7373788 161.8 -44.6 81

South Rompas ROM0015 ROM 3401308 7373756 97 -44.5 266

South Rompas ROM0016 ROM 3401345 7373254 91.6 -45.0 89

South Rompas ROM0017 ROM 3401302 7373757 62.4 -60.0 77

South Rompas ROM0018 ROM 3401320 7373717 131.95 -44.8 242

South Rompas ROM0019 ROM 3401295 7373254 98.2 -45.0 91

South Rompas ROM0020 ROM 3401331 7373686 135 -44.7 263

South Rompas ROM0021 ROM 3401244 7373254 93.9 -44.3 79

South Rompas ROM0022 ROM 3401381 7373739 181.1 -44.7 256

South Rompas ROM0023 ROM 3401200 7373257 95.3 -44.2 87

South Rompas ROM0024 ROM 3401156 7373257 87.95 -44.2 93

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South Rompas ROM0025 ROM 3401354 7373851 115.5 -45.3 261

South Rompas ROM0026 ROM 3401098 7373269 106.6 -49.3 90

South Rompas ROM0027 ROM 3401263 7373295 84.95 -49.2 88

South Rompas ROM0028 ROM 3401375 7373807 172 -45.3 200

South Rompas ROM0029 ROM 3401447 7373219 89.1 -45.2 84

South Rompas ROM0030 ROM 3401465 7373176 95 -44.2 103

South Rompas ROM0031 ROM 3401510 7373173 91.9 -45.0 85

South Rompas ROM0032 ROM 3401477 7373124 100.8 -44.8 78

South Rompas ROM0033 ROM 3401483 7373076 95.2 -44.4 77

South Rompas ROM0034 ROM 3401433 7373079 152.7 -44.5 73

South Rompas ROM0035 ROM 3401335 7373686 98 -44.4 79

South Rompas ROM0036 ROM 3401334 7373686 102 -69.8 77

South Rompas ROM0037 ROM 3401350 7373779 92.3 -49.7 78

South Rompas ROM0038 ROM 3401539 7373293 143 -44.6 88

South Rompas ROM0039 ROM 3401612 7373293 124.7 -45.0 82

North Rompas ROM0040 ROM 3399439 7378411 65.4 -48.0 57

North Rompas ROM0041 ROM 3399452 7378394 50.55 -49.9 58

North Rompas ROM0042 ROM 3399423 7378401 107.5 -45.4 57

North Rompas ROM0043 ROM 3399419 7378430 90.2 -50.9 60

North Rompas ROM0044 ROM 3399430 7378378 95.45 -43.8 63

North Rompas ROM0045 ROM 3399429 7378440 60.1 -45.1 57

North Rompas ROM0046 ROM 3399417 7378456 66 -49.4 57

North Rompas ROM0047 ROM 3399408 7378450 87 -58.5 57

North Rompas ROM0048 ROM 3399393 7378440 102 -61.3 61

North Rompas ROM0049 ROM 3399470 7378377 39 -54.7 61

North Rompas ROM0050 ROM 3399461 7378374 88.7 -63.5 61

North Rompas ROM0051 ROM 3399486 7378355 59.4 -63.0 61

North Rompas ROM0052 ROM 3399503 7378370 89.3 -45.1 237

North Rompas ROM0053 ROM 3399488 7378388 115.4 -44.7 239

North Rompas ROM0054 ROM 3399477 7378408 92 -45.1 240

North Rompas ROM0055 ROM 3399463 7378434 106.55 -45.0 239

North Rompas ROM0056 ROM 3399456 7378454 102.45 -45.3 239

North Rompas ROM0057 ROM 3399333 7378478 100.4 -44.2 57

North Rompas ROM0058 ROM 3399388 7378517 91.5 -45.2 57

North Rompas ROM0059 ROM 3399290 7378455 22.2 -45.0 237

North Rompas ROM0060 ROM 3399294 7378457 81.1 -45.6 57

North Rompas ROM0061 ROM 3399297 7378552 98 -45.6 58

North Rompas ROM0062 ROM 3399345 7378578 88.8 -45.1 59

North Rompas ROM0063 ROM 3399279 7378699 94.8 -44.8 57

North Rompas ROM0064 ROM 3399358 7378390 101.2 -45.0 60

North Rompas ROM0065 ROM 3399328 7378342 103.7 -45.5 57

North Rompas ROM0066 ROM 3399289 7378314 100.3 -45.6 57

North Rompas ROM0067 ROM 3399367 7378365 103.6 -45.9 57

North Rompas ROM0068 ROM 3399352 7378303 60.5 -45.0 57

South Rompas ROM0069 ROM 3401331 7373815 71.35 -65.5 77

South Rompas ROM0070 ROM 3401351 7373817 59.7 -49.9 257

South Rompas ROM0071 ROM 3401340 7373795 37.2 -55.2 80

South Rompas ROM0072 ROM 3401340 7373794 50.2 -68.3 80

South Rompas ROM0073 ROM 3401355 7373795 25.8 -45.2 260

South Rompas ROM0074 ROM 3401356 7373795 38.1 -65.6 260

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South Rompas ROM0075 ROM 3401371 7373770 44.8 -64.1 260

South Rompas ROM0076 ROM 3401371 7373770 53.3 -45.5 260

South Rompas ROM0077 ROM 3401368 7373781 41.3 -45.4 260

South Rompas ROM0078 ROM 3401378 7373782 65.1 -50.0 260

South Rompas ROM0079 ROM 3401360 7373810 53.35 -45.3 260

South Rompas ROM0080 ROM 3401370 7373811 58.6 -44.9 260

South Rompas ROM0081 ROM 3401370 7373811 62.9 -60.4 260

South Rompas ROM0082 ROM 3401375 7373832 92.5 -59.0 260

South Rompas ROM0083 ROM 3401350 7373813 88.1 -44.6 190

South Rompas ROM0084 ROM 3401354 7373836 119.4 -44.6 190