dd rpt 21 rope lake€¦ · area: rope lake report no: 2 1 010 work performed for: minnova inc....

AREA: ROPE LAKE REPORT NO: 2 1

010

WORK PERFORMED FOR: M innova Inc.

RECORDED HOLDER: S AME AS ABOVE (xx)

: OTHER

CLAIM NO.

TB 6464428 TB 646432 S TB 646433

TB 646431, TB 646433, TB 646434 S TB 646439

HOLE NO.

WL-056

WL-057

FOOTAGE

666.52m

DATE

May/88

NOTE

(D

1092.0m May-June/89 (1)

NOTES: ( 1) W8904.497, filed Dec/89

MOLE NUMBER: WL-D57HINNOVA INC.

DRILL HOLE SECORD IMPERIAL UNITS:DATE: 19-0ctober-1989

METRIC UNITS: X

MS ACT NAME: WINSTON LAKE PROJECT NUMBER: W070

DATE STARTED:DATE COMPLETED:

DATE LOGGED:

646431 , 646433 , 646434^^

PLOTTING COORDS GRID: MINE GRID EXT. NORTH: 12700.DON

EAST I 10I40.00E ELEV: 10465.00

COLLAR ASTRONCMIC AZIMUTH: 270* O 1 D"

Hay 22, 1989JLT* 20, 1989Jine 25, 1989

COLLAR SURVEY: NOMULTISHOT SURVEY: NO

ROD LOG: NO

ALTERNATE COORDS GRID:NORTH: O* O EAST: O* O ELEV: 0.00

GRID ASTRONOMIC AZIMUTH: 250' O 1 O"

PULSE EM SURVEY: YESPLUGGED: YES

HOLE SIZE: M

COLLAR DIP: -83* O' O*LENGTH OF THE HOLE: 1092.00*

START DEPTN: O.OOnFINAL DEPTH: 1092.00*

CONTRACTOR: ST. LAMBERT DRILLING LTD.CASING: 4 FT INTACT

CORE STORAGE: CLEAVER LAKE.

PURPOSE: TEST DOWN DIP OF STRONG ALTERATION AND ZN HIM IN VL-W

DIRECTIONAL DATA:

Depth Aitrononlc Dip (•) Ailnrth degreei

50.100.150.200.250.300.350.400.450.500.550.600.650.700.750.800.850.900.950.1000.1050.

25.50.100.150.200.

00 -83'000000000000000000000000000000 -000000000000 25500 24900 23900 236

-77'•76'•74'•69'•68'•64'•62'•57'•55'•SO'•48'•44'•43'

0'0'0'0'0'D'0'0'0'0'0'0'0'0'

•4V30'•40'•38'•36'•35'•34'•S3'

0' -82'0- -82'0' -78'0' -76'

00 23V 0' -72'

0'0'0'0'0'0'0'0'0'0'0'

Type ef lett

ACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDMULTISHOTMULT 1 SHOTMULTISHOTMULTISHOTMULTISHOT

FLAG Coimenu

OKOKOKOKOKOKOKOKOKOKOK FAINTOKOK FAINTOKOKOKOKOKOKOKOKOKOKOKOKOK

Depth (•)

250.00300.00350.00400.00450.00500.00550.00600.00650.00700.00750.00800.00850.00900.00950.001000.001050.001085.00

Astronomic Azimuth

230'232-233'238'244'242'24*'249'25V253'252'254'256'259'268'252'259'26V

*i.-...

0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'0'

Dip degree*

•70' 0'-67-30'•65' O 1•59' 0'•56' 0'-52' 0'•*9'30'•46-30'•44'SO'•4V 0'•39' 0'•37' 0'•37' 0'•36' 0'•36' 0--36' 0'-34' 0'•34' 0'

.

.

.

.

.

.

.

Type of lett

MULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULT I SHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOTMULTISHOT

FLAG Comwnt.

OKOKOKOKOKOKOKOKOKOKOKOKOKOK

PXOKOKOK

,HOLE NUMBER: VL-057 DRILL HOLE RECORD LOGGED IYl C. W.ENN PAAGE: 1

HOLE NUMBER: WL-057MINNOVA INC.

OR ILL HOLE RECORD DATE: 19-October-19B9

FROM TO

ROCK TYPE TEXTURE AND STRUCTURE

ANCLE TO CA ALTERATION MINERALIZATION REMARKS

0.00TO

1.70

OVERBURDEN 06.

1.70TO

412.50

PILLOWED KAF1C FLOW BMA*

Fine grained, dark green, pillowed mafic flow.Strongly foliated and locally laminated 8 .......Perterved pillow telvedge occur every 10-100cm

consisting of hornblende md quartz/feldspar bands (inn-cm tcale). Bands between pillows exhibit strong sausaerltiiation.

21.7-21.8Barren ail Iky white quarti vein.

21.25-Z1.35 FO

30.0-50.1 GR DY

36.1-36.2Conformable quart! vein (long epidote altered

pillow (clvedge.

39.5-42Broken blocky core.

{39.45-39.75} .FT.Fine (rained, pele pink brown tliceoua unit with

harp conformable contact against Mfic...........

48.6-41.8Zone of chloritic vet competent BMA (possibly healed fault?}.

55.3-55.5Epidote altered nan ive pillow cor*.

69.15-69.22Mm l ve epidote altered pillow cor*.

No hydrothermal alteration.* 3X quarti carbonate veining

conformable to the foliation. Approximately 2X quarti at li l Ice sweats * 3cm wide associated with pillow selvedges.

6.6-7.15Ceusseritized pillow selvedge.

18.35-21.25Weak pervasive tausserltisatlon of fine (rained mefic In association with abundant quartz epidote stringer* that ay locally for* vein breccia.

Incipient biotite l phlogopite alteration of felsic tuff.

Strong chlorite development associated with possible fault.

59.2inn w ide band In phlogopite

alteration.land Is conformable with laminated

pillow selvedges

69.9-70.3

Trace to locally 5X pyrite. Pyrite when present appears to be associated with pillow aelvedgec.Trace amounts of pyrrhotite.

18.45-18.6510-15X fine grained pyrite associated

with Irregular quartz vein - geochemed.

23.5Trace pyrrhotite with 2* pyrite In

conformable silica sweat.

U am teal* pyrite clou.

61.852m wide slllcs sweat with abundant fine pyrite.

MOLE NUMBER: VL-057 DRILL HOLE RECORD LOCOED lYi C. GLENN PACE;

HOLE NUMBER: VL-057MlNkOVA INC.

DRILL HOLE RECORD DATE: 19-0ctober-1989

FROM TO

ROCKt m TEXTURE AND STRUCTURE

ANGLE TO CA ALTERATION MINERALIZATION REMARKS

1M.MM.JEpidote altered, Miilve pillow core.

^12.5-117.0} .FLT ZONE*Zone consists of broken and blocky core and fault

breccia at 115.0-115.Z.fault breccia It pale green with on scale breccia

fragments In fine grained pale green tiatrlx.Faulting fi ......................................

117.0(MA becomei nore homogeneous and passive. The laminated pillow selvedges decrease and the flow

5X pale brown phlogopite associated with laminated, sausseritiied, pillow selvedge.

71.75-71.9Massive, sausseri 11led and possible brecciated pillow core.

W. 0-89.0Abundant mi-cm scale phlogopite bands associsted with laminated pillow selvedges.

85.0-85.0JIX mn scale pale yellow, glassy clou-

garnet/staurolite 1 w ith incipient phlogopite.

90.0-91.0n hematite stained hairline quartz/ feldspar atringers.

94.9-95.0Zone of epidote alteration.

Minor carbonate vein associated with faulting.

Trace - 5X leucoxene generally located within aauaserltltad pillow eoret.

K f ine to coarse anhedral to subhedral pyrite.

Trace to locally 3X fine disseminated pyrite.

93.J-93.J52X very fine grained pyrite associsted

with Intarplllow silica sweet.

107.171.2cm wide pyrite blob in silica

aweat.

110.5-110.65X very fine grained, disseminated

pyrite associated with conformable quartz vein.

Trace pyrite fnd fault breccia.

129.0

HOLE NUMBER: UL-057 DRILL NOLI KECORC LOWED IT I C. 8LENN FACE l

HOLE NUMBER: Ut-057HINNOVA INC.


menTO


becomes nore pillowed with medium grained massive causteritiied pillow cores.

141.10-141.15 Vuggy quarti/feldsper dyke.

144.3-144.35 Vuggy felsic dyke.

144.5-144.6 Broken core.

171.5-186.0 Broken and blocky - core fractures parallel to

Local rubble zones at: 175.7-176.0 176.5-178.8 179.8-180.4 181.6-181.7 185.6-185.7 2cm of chloritic fault gouge at 180.35.

{180.35} .UT.

166.0 BMA exhibit* an-cti acaU hornblende va quartz/ feldspar lamination*, lamination* occur along pillow aelvadgat and auy locally be tautierltlied.

201.5-201.6 Small acalt faulting offaettlng am tea i e

207.65-208.22 In t Dyke Medium grained, atrong foliation, light speckledgreen

{209.4-211.21} .10. At above.

218.05-218.15

ANGLE TO CA

47

50

60

TOto30

TO

ALTERATION

Locally abundant irregular quartz

None to local phlogopite at am tcalaband*.

Nona.

MINERALIZATION

Minor pyrite associated with conformable quart! vein.

174.8-175.6

pyrite.

Trace to 2X pyrite concentrated In the laminated pillow selvedge*.

Nona.t

REMARKS

HOLE NUMB. DRILL HOLE RECORD LOGGED IT: C . GLENN PAGE:

HOLE NUMBER: UL-057MINNOVA INC.

CHILL HOLE RECORD DATE: 19-0ctob*r-1989

FROM TO



As above with 1X mn ecale anhedral feldspar pheno's.

223.15-Z23.4Possible chert surrounding BHA pillow. Chert looks recrystalliied and contains 2X anhedral pink feldspar.

215.1-215.3finely laminated interpillow mafic tuff.Lamination A ............................

256.0-256.2 Broken core.

256.3-256.*Massive, aauaaerltlied pillow core; aimilar core at 256.5-256.8.

265.6-Z73Broken and blocky core; possible healed fault with fault breccia at 268.2. fault S .........................................

2T7.4-277.9Snail saueserltized pillow corn that exhibit

amygdaloidal outer tint.Amygdules are < 1am in diameter and exhibit a gradatlonal contact.

Z79-Z94.5BMA exhibits a fine grained, dark green apeckled gabbroic appearance. Strong foliations .............................. 60

290.J-J90.5Milky white quartz vein conformable with fabric.

Weak hematite staining of feldspar pheno't.

225.0Hematite staining appears within

quartz feldspar stringers and along fracture surfaces.

None.Trace amount* of leucoxene tt very

fine grained chalky white patches.

Nona.

3X fine sub-euhedral pyrite disseminated along margins and within chert.

243.12-243.253-5X fine pyrite disseminated in and

around possible recrystallited interpillow cherts.

252.1-253.21-5X fine grained pyrite disseminated

in very fir* grained aiafic flow. Pyrite also occurs as fine bands.

Z67.15Minor pyrite associated with quartz/

feldspar vein.

Trace pyrite.

Trace - U pyrite.

HOLE NUHBE' "^-057 DRILL HOLE RECORD LOCOED BY; B. CLENN PAGE) S


DRILL MOLE RECORD DATE! 19-0ctob*r-1989

FROM TO

ROCKTEXTURE AND STRUCTURE


299.2-299.65 tectonic bx Small ^ < 1 cm) fragments of (MA surrounded by

numerous quartz carbonate veins. Zone 8 ..........................................

299.82-300.5Milky white quartz vein, conformable to fabric fi Upper contact is sharp.Lower 10cm of vein contains abundant fragments of

BMA volcanics.

318.98-319.42 fD

321.0-321.7Trace to 2X magnetite associated with rims of

massive, sausseritized mafic pillow cores.

324.22-324.51Irregular quartz feldspar vein/dyke.

347.9-348.0Irregular quartz/feldspar vein.

348.3-349.5Thin amygdaloidal bands up to 2cm wide. Amyodules

look very similar to amygdule* associated with Massive, tausserltiitd pillow corts.

372.3-390Mm scale amygdule* occur sporadically (up to 2X) Amygdule! are flattened at 1.5:1 and are not associated with lausserltlzed pillow corts.

390.V5-391.10 Oti/ftp vein/dyke

Weak hematite alteration along hangingwall contact.

334.0-348Patchy w*ak phlogopite alteration of cm acale bands.

Trace - IX very fine grained pyrite.

330-333.223X disseminated pyrite as fine < lam

crystals and blot*.

S89.47-S89.T5-7X pyrite in thin band*.

394.0-394.14-5X m acale^jyrlte stringers.

394.1-394.71-2X pyrite stringers.

J94.7-395.25

HOLE NUKBf DRILL MOLE RECORD LOGGED til C . CLENN PAGE!

HOLE NUMBER: VL-057MJNNOVA INC.


FROM TO

412.50 TO

465.92

ROCK TYPE

GABBRO *GB*

TEXTURE AND STRUCTURE

395.25-396 Broken and blocky core.

39S.6-39B.8 Vein bx

406.4-406.6 Vein bx

Gabbro exhibits indistinct contact with BMA. Fine to medium grained gabbro texture becomes

apparent at 412.5 but massive, seusseritiied pillow cores persist.

427.0-432 Gabbro exhibits weak to iocally strong

magnetism in 1-3X very fine grained cub-et*idrat magnetite crystals.

427.4-427.6 INT DY

Dyke Is pale grey-white with 15X mafic clotsInn x 3am.

<437.55-437.9j .FT raft. Finely laminated (an scale) felsic tuff exhibits

fine pink layers alternating with nfic levers. Layer* may contain en acale quarti/feldepar

fragment* ? the layers drape over the top of the fragments.

Tuff ha* been strongly quarti epidote altered

440.5-440.7 DB Irregular but sharp contact.

4440.82-442.1} (OB.

Hanging wall contact sharp egalnst grained .dyke.

441.5-441.73

ANCLE TO CA

TO

20to30

30

ALTERATION

Persistent leucoxene 1-2X.

No hydrothermal alteration. Strong quarti epidote alteration associated with vein breccia.

MINERALIZATION

1-2X very fine grained pyrite stringers.

Trace pyrite.

409.5-409.6 Trace chalcopyrite end .SX pyrite

associated with quarti/feldspar vein.

Trace pyrite.

426.1 Trace chalcopyrite in quarti vein.

492.15Trace chalcopytle In quartz vein.

3X pyrite as very fine (rained cryitat aggregate* - looks remoblllied associated with vein breccia.

f

REMARKS

Gabbro looks extrusive.

MOLE NUMBER: WL-057 DRILL MOLE RECORD LOOSED IT: C. GLENN PAGE!



FROMTO

465.92TO

471.90

471.90 TO

480.20

ROCKTYPE

PILLOWEDMAFIC FLOW SMA/BSF.SIRDSHITFLOW

LAMINATED CHERT MAFICTUFF ANDINTER MEDIATESEDIMENT CRT/Win T


Granite xenolith within diabase dyke.

4449. 87-456. If *OB.Contacts S ...............,......................

{4S1.i-t53.lL Broken core - possible *FLT7*

456.45-456.52 DB

.|456. 1-464. 15f *flHA7.Possible pillowed BMA has local intrusive -

gabbro textures but alto exhibits quart: epidotealtered pillow cores. Upper contact is obscuredby dyke.

Lower contact is also dyked out.

{464. 15-465. 92f -tib*Diabase dyke exhibits amygdaloidal texture with

quartt carbonate rimmed amygdules in the middleof the dyke.

Very fine grained pillowed, dark green mafic flowexhibits < 2X feldspar glomerocryst! generally< Ion in diameter but as large as ton in diameter.Well foliated and locally laminated on mn scale.Laminations My indicate interpillow cherty seds.

Pillows are massive and exhibit quart! epidotealteration.

Mixed tone of finely laminated cherty tuffs.Mf le tuffs, flows and sediments.

471.9-473.05Finely laminated recrystsKiad and disrupted

chert and cherty felsic and Mf ic tuffs(nn-cm scale).Unit exhibits 5X (mn scale) magnetite crystals.

ANGLETO CA

52

10

63

ALTERATION

None.

470.J5-470.8VAlteration of ISF consisting of:10X cordierite15-20X biotite5-10X anthophylliteAlteration in sharp contact with trash

MflC

None.

*72.1-*T2.Z5Strong quart! epidote alteration

MINERALIZATION

Trace pyrite.

460.0-460.3IX pyrrhotite as mn scale stringers.

Trace pyrite.

466.9Trace chalcopyrite in quart! vein.

Trace -U very fine graineddisseminated pyrite.

REMARKS

HOLE NUMBER: WL-057 DRILL MOLE RECORD LOGGED BYl C. CIENN PAGE)

HOLE NUMBER: wl-057MINNOVA INC.

DRILL HOLE RECORD DATE: 19-0ctober-1v89

FROM TO


The fine laminations ney give way to more massive granular looking sediments. The magnetite may be derived from the tediment portion of this unit.

473.D5-473.2 Thin mafic flow.

Very fine grained, dark green, well foliated.

473.2-473.* Int tuff Pale brown-preen, very fine grained, locally

cherty banded on cm scale. Green cm scale bands alternating with pale brown intermediate bands up to 6cm wide. Narrow cherty lection occurs at 473.35-473.4 and

exhibits fine lamination.

473.4-473.6 Intermediate garnetiferous sediment massive, fine

grained, granular, grey-green sediment.

473. 6-473. B Ha Tuff Dark green, very fine grained, finely banded

mafic tuff. Sands are composed of quartz and feldspar material alternating with more massive, mafic bands.

Lower 3cm of mafic tuff exhibit 2X mn scale anhedral magnetite crystals-possible contamination from underlying sediment.

4473.B-476.58L *U* Flow Mafic flow with tuff/sediment flow top.

473.B-474.2 Finely laminated tuffaceous sediment -

massive from 473.B-474.0 with cm scale

474.2-474.5

ANCLE TO CA

W

62

70

69to 5556

62

ALTERATION

creates pervasive pale green colour.

None.

None.

5X cm scale garnets. 2-5X * mm scale magnetite crystals.

tt f ine phlogopite is thin wisps and mm scale ragged clots.

473.8-474.0 3X cm tcale garnets related to sedimentary component in flow top.

MINERAL RATION

None.

None.

None.

Trace pyrite.

REMARKS

HOLE NUMBER: UL-057 DRILL MOLE RECORD LOGGED IVt G. GLENN PAGE: 9

HOLE NUMBER: WL-057HINNOVA INC.

DRILL MOLE RECORD DATE: 19-0ctober-1989

FROM TO



Very fine grained, dark green mafic flow that exhibits cubhedrat amphibole phenocryst*. This flow ends abruptly at another tuffaceous sediment flow top as described above, and grades Into massive mafic flow. Lower flow exhibits a possible pillow core adjacent to the lower contact. Core is quarti epidote altered.Lower contact fi ..........................,......

476.56-477.53 Felsic TuffVery fine grained, white to green, felsic

matrix locally supporting fine m scale mafic clots.

4477.53-460.2* *MA* flow Dark green, very fine grained moderately foliated mafic flow. Flow exhibits local garnet and chlorite (retrograded from garnet)

4460.2-482.3} *Alt FT*Sharp upper contact to felsic S .................Upper .Tim exhibits weak to moderate alteration with fine grained granular texture. Lower portion of unit Is intensely altered.Colour varies from pale grey white to blue brown.Strong foliations .....................,........Unit exhibits fine lamination at 480.1.Lamination tn scale fi ...........................

karren white quartz veins at:480.3-460.35460.4-460.4J4tO.76-4BO.82

70

None. Trace pyrite.

Trace - IX very fine grained, disseminated phlog.

478.8-479.53-5X garnet 2-Jmm in diameter,

euhedral. 2-SX chlorite - retrograded from

garnet. Chlorite exhibits euhedralshape of garnets.

480.2-480.95Weak to moderate alteration consisting

of fine grained:cordierite 5Xblotite/phlogoplte 7X

460.95-482.3Intense alteration consisting ef:

cordierite 10-15Xbiotlte/phlogopite 15-20*staurolite 5X

Trace * IX very fine grained disseminated pyrite.

Trace pyrite.

480.20TO

(95.62

GABBRO CB. Dark green to medium grained, massive to weakly

foliated mafic intrusive with fine grained chiliad contact 8 ........................................

Gabbro exhibits amphibole porphyritic texture and locally exhibits cm scale quartz/feldspar

78

None.

None.

None.

Nona.

HOLE NUMBER: UL-057 DRILL HOLE RECORD LOGGED BY! G. GLENN PAGE) 1 0

HOLE NUMBER: Wt-057HINNOVA INC.


FROMTO

495.62TO

501.90

501.90TO

530.95

COCKTYPE

TRANSITIONZONE T2*

GABBRO*GB.


Clots - look similar to "Bird thlt" In BSf.fluartz/feldspar clots make up 2X and are very

faint.

Transition lone marked by appearance of 3-5Xphlogopite as wisps and w i spy blotches. The tileof the amphibole crystals increases to 2-3ffro indiameter.

The grain site then increases to 2-lam. Lowercontact is marked by blotches of quartz/feldsparbetween 501.S-501.55. The transition lone thenbecomes very fine grained and exhibits a granulartexture and weak magnetism.

Fine to medium grained, moderately well foliated.Dark green, speckled mafic intrusive. Locally mylook pillowed with massive quartz epidote atter'nOverall gabbro is homogeneous.

510.6-511.11cm wide quartz-carbonate vein running parallel

to CA.

^521. 0-530.9} *CLR Raft*

521.0-522.6Mixed clotted rhyolite and fine grained gabbro.

Contacts are indistinct.

521.0-521.2 Mafic tuff/CLRQuartz veins marking contact between lau i ve

mafic tuff and finely laminated intermediate tuff.

521. 20-521. JIntermediate tuff exhibits fine m acale

ANGLETO CA

71

n59

ALTERATION

Trace - 1X leucoxene.

Trace phlogoplte/biotlte (relativelyunaltered)*

MINERALIZATION

Trace pyrite.

Trace pyrite.

None.

3-5X medium grained euhedral pyrite -predominantly atsociated with quartzvein. 1-2X very fine grainedinterfollal pyrite.

REMARKS

MOLE NUMBER: WL-05T DRILL HOLE RECORD LOGGED (Y: G. GLENN PAGE! 11



FROM TO



521.3-521.95More massive mafic tuff/clotted rhyolite, very fine grained, dark brown green. Lower contact with gabbro is sharp 8 ..........

Trace - 2X very fine grained phlogoplte/blotlte of the mafic layers.

None - trace biotlte/phlogopite.

521.95-522.65 GBFine to medium, dark green speckled gabbro. Lower

contact with massive, clotted rhyolite is indistinct over 20cm.

522.65-530.95 CLRIntermediate felsic clotted unit consisting of

very fine grained pale white grey quartz/feldspar matrix with 10-60X mafic clots < 1mm in size.Unit is moderately foliated S ...................

No hydrothermal alteration.

69

2-3X very fine grained bedded pyrite.

2-4X fine to medium grained pyrite associated with 2-3cm wide blue quartz vein.1-2X very fine grained disseminated

pyrite.

Trace pyrite.

526.7-526.910X coerce euhedral pyrite associated

with 2 milky white quartz veins.

530.95TO

904.00

GABBRO GB* As above. Locally magnetic contact with clotted

rhyolite is aharp but irregular 8 ...............

5*3.35-5*3.9 MD

60

565.75-566.4Milky white quartz vein.

579.1-586.62 Up phyrlcGabbro with 20* im acale feldspar phenc's. Local pale green phlogopite occurs in wisp* and increases to 2-3X downhole.Zone ends abruptly at fault zone.

581.15-581.25

581.65-581.8

GR DY

GR DY

585.92-586.1* Felcic Dyke

{586.62-589.6} *FLT ZONE*Strong fabric developed In gabbro leading up to 10cm chlorite fault gouge at 587.8-587.9.2cm of chloritic fault gouge at 589.3.

65Strong chlorite developed associated

with fault lone.

Trace pyrite.

565.75-565.15Chalcocite In quartz vein.Est: 2* Cu l 0 .40m

Locally the gabbro any exhibit extrusive textures - massive quartz epidote altered pillow cores.Intrusive is possibly partially

extrusive.

Possible t rant It ion sane T

Trace pyrite.

HOLE NUHBEft: W.-057 ORlli HOLE RECORD LOGGED BY I G. GLENN PAGE l 12

HOCE NUMBER: WL-057MINNOVA INC.


FROH TO

ROCK TrPE TEXTURE AND STRUCTURE

ANCLE TO CA ALTERATION MINERALIZATION REMARKS

588.2-594.5Locally weakly banded and mgnetlc gabbro bands are * 2mm in diameter and are quartz/feldspar in composit ion.Banding G .......................,..............

592.25-593.35 Mo fsp

623.1-633.15 Milky white qv.

634.6-63A.68 Mi Iky white qv.

636.05-636.2Quart! epidote bleached tone.

650.02-650.43Gabbro contains 1-2X feldspar glomerocryst* that range from 20mm x 3om to 25mm x 25mm

655.62-655.9Gabbro exhibits 2im wide quartz and quart i l feldspar bands. Banding doesn't look like veining.Ouartt gabbro composition is also exhibited at

660.0-660.2.

655.9-656.2 DB

{671.15-672.25f *FD.Light pink, massive, homogeneous felsic dyke with 5cm intrusive breccia on upper contact.Contacts sharp G ................................

73

42

ei672.42-672.62 As above.

FD

{674.65-675.9} .FO. As above.

Gabbro still exhibits 3X very fine grained leucoxene as fine ufsps.

613-61430X quartz epidote veining parallel to

CA.Locally strong hematite associated

with veining creates a red green hue

1-2X very fine grained leucoxene.

661.25-661.353-5X mn (cale phlogopite witpe.

672.8-673.23t phlogopite as an scale wisps in

fresh looking gabbro. Similar phlogopite rich tones it: 673.6-674.65 (SX)

Trace pyrite.

None.

624.5Pyrite associated with quartz vein

minor hematite staining.

3X fine euhedral pyrite associated with quartz vein.

2X pyrite associated with qv.

Glomerocrvsts support for partly extensive nature to gabbro ?

Trace - 1X disseminated pyrite. 4671.15-675.9} .felsic dyke (warn 7.

HOLE NUMBER: Wl-057 DRILL MOLE RECORD LOGGED IT: G. GLENN PAGE: 13

HOLE NUMBER: WL-057HINNOVA INC.

DRILL HOLE RECORD DATE: 19-0etober-1989

fROHto


{675.9-680.451 *PX. Meta pyroxenite displaying dark green - black

colour, medium grained size, granular texture and strong magnetism.

from 678.4-676.7 and broken core at 679.2-679.5.

{680. 45-681 .05} *T2. Transition tone displaying strong phlogopite

alteration, medium grain site, and granular texture. Colour is dark brownish green.

685. 82-656. 0 KD

691.8-692.7 Strong foliated gabbro. Foliation Increases in intensity towards centre of the lone.

698.4-733.7 Gabbro starts to display pseudo banded appearance with bands < t "m wide composed of quartz/feldspar. Locally the quartz/feldspar forms ntrix (up to

SO*) and m scale amphibole crystal*. Banding 8 .......................................

712.5-713.4 GR DY

4728.6-730.6f -OB. Diabase dyke has sharp irregular contacts that run tubparatlel to the CA.

73J.7-744.5 Gabbro displays medium to coarse grain ill*

with feldspar crystals up to 4mn In diameter. ftp has a rolled appearance and have been localized Into bands.

744.5 Typical gabbro texture and appearance returns.

ANGLE TO CA

BOBS

73

10 15

ei

ALTERATION

682.2-682.5 690.0-690.S

2-3*. pervasive chlorite alteration of met* PX.

10X phlogopite as pervasive wisps surrounding amphibole crystals

Trace phlogopite.

Trace - 1X leucoxene.

713.4-713.6 2X phlogopite as wisps.

MINERALIZATION

None.

None.

None.

712.4 1mm wide band of magnetite (SOU) and pyrite (50X).

center of the band and nay encapsulate an acale monetite crystals

j

REMARKS

HOLE NUMBER: Ut-057 DRILL HOLE RECORD LOGGED IY: C. GLENN fACE l 14

HOLE NUMBER: Wl-057M1NNOVA 1MC.


FROM10

904.00TO

910.15

ROCKTin

QUARTZFELDSPARPHYSIC FLOW.OFF.CAMP FLOW


^45. 5-7*7. Of *GR DY.

7*8.95-749.45 GR DY

756.4-757.0 GR DY

775. 92-776. e MDFeldspar phyric.

BOS. 5Blue quarti vein - barren.

812,85-813.5 MD

852.9-653.0 GR DY

Sharp but Irregular contact against gabbro S ,...OFF ranges from blue grey to grey white In colour

fine grained and massive to weakly foliatedfoliation B .............

904.0-906.4

ANGLETO CA

30

30

30

47

as

ALTERATION

755.9-756.15Silicified gabbro with 3-5X phlogopite

as patches.

758.75-759.11-2X phlogopite as wisps.

Weak quarti epidote bleachingassociated with abundant stringers.

827.55-827.65Ouarti epidote bleached zone.

862.4-863.935-7X quarti carbonate stringers at

various angle*.

866.0-866.t85-10X quarti carbonate stringers.

872.2-872.4Silicified gabbro.

873.4-873.5euarti epidote bleached gabbro.

MINERALIZATION

751.9Minor pyrite associated with irregular

quarti/feldspar vein.

755.9-756.153X very fine grained disseminated

pyrite.

Minor pyrite associated with uppercontact of granite dyke.

None.

809.4Minor pyrite associated quarti epidote

vefning.

866.0-866.185X pyrite associated with quarti

carbonate stringers.

Hone - trace pyrite.

f

REMARKS

MOLE NUMBER! VL-057 DRILL HOLE RECORD LOGGED IT l 6 . GLENN PAGE l IS



FROM TO



OFF it fine grained, dark blue grey and looks weakly altered.

906.4OFF le pale grey white with little to no mafic content.Locally it exhibits a very fine grained sugary

texture.

^912.8-913. U \ vCRT/MTxVery fine grained, dark green, bedded cherty

mafic tuff. Thick mafic beds seperate thin cherty felsic bands.Unit is disrupted and may represent flow bottom breccia to OFF.

From 91J.16-913.26Fault with fault breccia disrupts the bedding.Fault S .......,.................................

913.26-9U.1 Ma FlowDark green, very fine grained, mafic flow with

moderate foliation fi .............................Lower contact with OFF is sharp fi ...............

920.5-923.0 Intermediate phase?Fine grained granular, grey brown lone

exhibiting strong foliation fi ....................Contacts with pale grey white OFF are indistinct

over 20cm.

922-930.75 Patchy alteredOFF ranges from fine grained sugary, pale grey -

white relatively unaltered OFF to coarse granular strongly altered OFF.

Lower contact with gabbro as (harp 8 ............

89

90

Alteration consists of 5X biotite/ phlogopite as im em scale wisps/bands. Trace -U sillimanite it 905.9-906.2.

Incipient biotlte/phlogoplte.

929.2-929.5 MD

None.

5-10X biotite. Trace sillimanite

Local strong alteration consisting of:biotite/phlogoplte 20-30Xchlorite 10*quart! 5XZona* of strong (Iteration occur it:925.7-925.6926.9-927.tZ928.6-926.79J0.65-9J1.15

909.0Trace chalcopyrite.

913.16-913.265-7X pyrite, very fine to fine grained

disseminated and bedded in matrix of brown silica ?

Trace - IX very fine grained diseminated pyrite.

Trace pyrite.

Trace sphalerite in quartz vein (t 929.6-929.7.

MOLE NUMBER: WL-057 DRILL HOLE RECORD LOGGED til 6. GLENN PAGE: 16


DRIU HOLE RECORD BATE: 19-0ctober-1989

FI! OH TO

930.15 TO

937.70

937.70 TO

939.65

939.65 TO

977.85

977.85 TO

981. W

981. M TO

982 75

982.75 TO

984.85

ROCK TYPE

GABBRO tcGB*

TRANSITION ZONE *T2*

META-

PYROXEKITE PX*

TRANSITION ZONE*TZ*

ALTERED QUARTZ PHYRICRHYOLITE FLOW

CAMP FLOU

MAFIC FIOU MA/MO? )* LADDER FLOU OR DYKE?


Dark green, fine to medium grained, massive, speckled differentiated mafic intrusive. Upper contact displays 15cm chilled margin and

is quartz bearing. Lower contact with transition lone it faulted.

^37.7f .FIT. Dark green, chloritic, weakly magnetic fine

grained unit.

Dark green-blue, massive, homogeneous unit exhibiting strong magnetism - 15-20}. mn scale magnetite crystals.

{940. 8t -f LI. 1cm chloritic fault gouge.

Dark green, fine grained, equigranular transition tone exhibiting minor pervasive chlorite as matrix to dark green amphibole phenos. Only trace feldspar present. Upper contact is marked by disappearance of

magnetism exhibited by PX and the development of chlorite.

Moderate altered OFF exhibiting, moderate to

Fine to medium grained and grey-blue-brown

Dark green, fine grained, weakly bedded moderately foliated mafic flow.

982.4-983.1 Possible flow top exhibiting weak bedding -

ANCLE TO CA

76

80

ALTERATION

None.

Moderate pervasive chlorite alteration and minor carbonate veins.

Minor quartz carbonate vefning.

Minor pervasive chlorite.

Weak to moderate pervasive biotite S-10Xcordierite < 3X

Moderate to strong brickwork style

biotite 20-SOXcordierite 20-50X

over 10cm.

None.

MINERALIZATION

None.

None.

None,

None.

Trace pyrite.

REMARKS

HOLE NUMBER: WL-057 DRILL HOLE RECORD LOGGED Ifl G. GLENN PAGE: 17

HOLE NUMBER: WL-057MINNOVA IHC.

DRILL HOLE RECORD DATE: 19-0etober-1989

FROM TO

9M.65 TO

998.00

998.00 TO

1016. Z5

1016.25 10

1023.75

ROCK TYPE

ALTERED QUARTZ (FELDSPAR) PORPHYRY

ALTERED MAIN OFF-

OUARTZ FELDSPAR PORPHYRY nOFP* MAIM Off

HIKED ALTERED SILICEOUS AND TUFFACEOUS


possible chert layers 7 Chert ? layers tp to aim thick are milky uMte.

983.1-98A.e5 Mafic flow 7 It dark green, homogeneous and weak

feldspar pnyric -feldspars < Inn In tile.

Grey brown, fine grained, locally granular, quartz phyric felsic unit. Unit exhibits thin discontinuous (mf ic-chloritlc

Quart! occurs as fine grained groundmass exhibiting a mosaic appearance.

4990.35-992.B} *OR DY. Granite /pegmatite dyke with 15X coarse euhedral

biotite.

Pile grey, massive, homogeneous, very siliceous quartz feldspar porphyry. Quartz eyes make up 20-50* in very fine grained siliceous matrix, feldspar makes up < 1W as very fine grained white subhedral pnenocryste.

{998.0- 1001. 35} *GR DY. As above.

1005.3-1005.45 GR DY As above.

1005.6-1005.9 GR DY At above.

1006.1-1006.5 GR DY As above.

1016.25-1019. 45 Massive, altered siliceous sediments prey - green

In colour, moderately foliated end weakly

ANGLE TO CA

06

ALTERATION

Weak alteration consisting of * 5X biotite associated with mafic tuffaceous layers.

fine silky wisps to 2-SX Trace garnet

Weak pervasive biotite alteration Trace garnet. Locally strong, brickwork style

alteration with biotite and cordierite.

10W.O-10M.5 SX garnet and retrograde garnet -

chlorite with silica rims.

Pervasive moderate to strong Iteration consisting of trice garnet, 1C* cordierite, S-10X biotite (In fine

MINERALIZATION

Trace pyrite.

Trace pyrite.

Trace pyrite. '

REMARKS

Tuffaceous arenite 7

Clastic/reworked sediment component dominates with tuff c securing as minor conponont i

MOLE NUMBER: VL-057 DRILL MOLE RECORD LOGGED (YI G. GLENN PAGE t IB



FROM TO

ROCK WE TEXTURE AND STRUCTURE


SEDIMENTS MIXED ALT SEDS* PICK LAKE SEDIMENTS

Upper contact (harp 8

1019.45-1019.85Well laminated distal wacke.

grained silceous matrix) Garnet increases to 5-7X between 1019. -1019.45

None - incipient biotite. Trace pyrite.

Bedding 8 ....................................Cm acale alternating beds of mixed felsic and

mafic aiateriaU

1019.85-1021.12Massive, altered siliceous sediment as above.Lower contact t ...,,....,.,.......,..........

1020.12-1020.45 GR DY

1021.12-1022.BWell laminated distal wacke.Alternating felsic and mafic material.

Bedding 8

1022.8-1023.75Massive to weakly layered, green - grey altered aediment/tuff exhibits weak to moderate (to locally strong) alteration.Bedding when present is defined by sausterltlzed felsic layers.Bedding fi .......................................

69

87

80

78

No to very minor cherty component hence clastic sediments.

1020.022X pyrite associated with 2cm wide

milky white quart! vein.

Hematite stained.

None - incipient biotite.

Weak pervasive 5-7X biotite locally (1026.1-1026.6)Biotite increases to JO-40* with trace

cord!trite, anthophyllite and < 5X chlorite.

None - trace.

1023.75TO

1039.1C

MIXED ALTERED FELSIC VOLCANI CLASTIC ANDTUFFACEOUS SEDIMENTS tCLR/SEDS*

This wit is defined by the appearance of a cherty component to the well laminated zones

Unit varies from massive grey-green to well laminated grey-white felsic layers alternating with hornblende-rich layers.

1023.75-1026.6Mixed altered intermediate tuff and CRT. Zone Is fine grained to very fine grained and grey to grey brown In colour. The cherty component exhibits layering 8 ....................................... 78

Variable.Ranges from moderate pervasive with

brickwork style overprint consisting of biotite and cordierite, minor staurolite and sillimanite.

Alteration varies tuffaceous zones exhibit S-10X biotite, up to 10* waxy green cordierite.Cherty tuff zones:

None to trace pyrite.

None.

HOLE NUMBER: WL-057 DRILL DOLE RECORD LOGGED (Y: G. GLENN f Mf: 1 9

HOLE NUMBER: Ut-057M1NNOVA INC.


FROM TO



The nore tuffaceous tones are massive.

1026.6-1027.15 CRT/ITWell layered cherty Intermediate tuff.layering is mm - cm scale, sub-parallel to CA

Lower contact is possibly faulted - now healed 8.

1027.15-1028.45Well laminated CRT - as above.Bedding t . ......................................

1026.45-1028.95 MTDark preen, weakly layered, very fine grained

mafic tuff.Layering S .....................................Lower contact occupied by 4cm wide barren white

quart! vein S ........,..........................Small fault offsetting bedding running parallel

to CA.

1028.95-1033.4 Mixed CRT/1T/MT. tedding a .......

1011.4-1015.8 FTMassive to weakly layered grey felsic tuff.

41033.8-1034.8f *CR DV*

1035.4S-1035.88 GR DY

1034.8-1039.1well laminated CRT/sediments.Laminations li on HID scale.Unit exhibits a layered grey-black and white colour with pervasive light grey overprint and exhibits tp to SK m scale, euhedral, magnetite crystals.

65

78

80

5X biotite, < 3X cordierite.

Biotite and cordierite alteration developed In nore mafic layers.

None.

1028.35-1028.45Minor carbonate veining.

Alteration varies with the felsic to Intermediate units virtually unaltered but the mafic exhibiting weak-moderate biotite, cordierite, trace garnet alteration

Trace biotite as fine clots.

Hematite stained.

Hematite stained.

None - fresh.

None.

Trace - IX pyrite associated with carbonate veins.

Trace very fine grained disseminated pyrite.

None - trace pyrite.

Trace - U very fine grained disseminated pyrite.

Trace pyrite. Magnetite occurs disseminated throughout well banded units Indicating sedimentary component.

HOLE NUMB' DRILL HOLE RECORD LOGGED IT: C. CLENM PAGE t 20

HOLE NUMBED: Ut-057MINNOVA IHC.

DRILL HOLE RECORD DME: 19-0etober-1989

FROM TD



1016.6-1036.75 MDDark green black feldspar phyric mafic dyke.

MIXED ALTERED CHERTY TUFF xCLR*

{1039.1-1044.4 J .CRT.Very well laminated, alternating black and white layers.This CRT appears to be cleaner than the above

unit.Bedding S .......................................

1044.4-1059.12Weakly altered intermediate tuff and siliceous clotted volcaniclastic*.Intermediate tuff generally fine grained, medium

to dark grey, crass i ve to weakly layered.

Siliceous clotted volcaniclastic generally white with < IX mm scale mafic clots.

1057.75-1057.90 GR DY

{1057.90-1059.12f *GB DY*

1041.0-1041.25 MD Feldspar phyric.

41M2.6-1MJ.6l. *OB.

1044. 4-1059.12Typical CLR exhibiting minor local changes in

composition from intermediate to felsic siliceous matrix. Colour is grey white supporting mn scale mafic clots - locally up to 10X.

{1047.351; *FLT.

{1057.92-1059.121} *GB DY*Park green, medium to fine grained at contacts

mafic dyke.Lower contact B ...............................

Weak patchy biotite grading into locally strong brickwork alteration consisting of cordierite, biotite.

Weak pervaiive biotite. Locally in more Intermediate sections (1046.0- 1049.0) alteration Is 10X biotite and trace cordierite.

1055.0-1055.0Waak pervasive hematite staining of

siliceous clotted rhyolite.

10S4.5-1054.TPossible sillimanite K as very fine silky wisps.

Trace pyrite.

None.

Lack of disseminated magnetite indicates cleaner tuffaceous origin.Minor magnetite occurs on lamination surface.

1051.0Trace molybdenite in 5cm wide milky

white quartz vein.

NOLE NUMBER: UL-057 DRILL MOLE RECORD LOGGED (Y: G. GLENN FACE: 21

HOLE NUMBER: Wl-057M1NNOVA INC.

DRILL HOLE RECORD DATE: 19-0ctober-1v89

FROM TO

1066.2270

1072.00

ROW TYPE

GRANITE•GR.

E. O.K.


1059.12-1066.22 Patchy altered siliceous clotted votcanfclaitfc. Characterized by very tiliceous CLR windows in hazy contact with nediim grey, mast i ve biotite altered patches.

LocaKy, strong brick work style alteration overprints medium pervasive biotite.

White to pale pink massive to weakly foliated. Granite exhibiting both quart* and feldspar •m scale anhedral crystals. Fine to mediun grained, contains < 5X wispy

hornblende.

{1068.7-1071.31f rfO* Feldspar phyrlc.

1071.8-1072.3 MD

^075. *-1076. K \ *ti*

1089.9-1090.0 MD

End of Mole.

ANGLE TO CA

75

ALTERATION

Clotted rhyolite windows exhibit weak biotite alteration of mafic clots and trace - U sillimanite as white wftps sometimes within the mafic clots. The massive grey sediment exhibits incipient very fine grained biotite, trace cordierite and locally strong brickwork alteration consisting of cordierite in biotite matrix, ie: 1059.6-1059.75

Hematite staining.

MINERALIZATION

Trace very fine grained disseminated pyrite.

1064.95 Trace molybdenite In brickwork altered

sediment.

None.

REMARKS

HOLE NUMBER: UL-057 PRILL HOLE RECORD LOGGED IT l G. CLENN PAGE! 12

of ' Report rOOCUMbNI NONoj.he.Dcve.op.en,

pf

Ontario

Name! Address of Recorded Holder

[NOVA

SUITE 3970 - P. O. BOX 91, COMMERCE COURT WEST, TORONTO, ONTARIO MSL 1C7Summary of Work Performance and Distribution of CreditsTotal Work Days Cr. claimed

. 70for Performance of the following .vork, (Check one only)

Manual Work

rjshatl Sinking Drifting or other Lateral Work,

FJ Compressed Air, other Power driven or mechanical equip.

FJj Power Stripping

KjDiamond or other Core drilling BQ

FJl.and Survey

All the work was performed on Mining cialmls): TB 646428, 646431, 646432, 646433, 646434, 646439:

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) additional claims

WORK PERFORMED BY t ST. LAMBERT DRILLING CO. LTD., P. O. BOX 473,

DURING THE PERIOD: May lith, 1989 to

D. D. H. WL-56 - May lith - 22nd, 1989CRfbtTS /)v*/*-} S"?C /. 76

s f~.[.t o**~e*Cffb/f* tfff&t 0737. f j. —*-* A ,i f** t "70 no

C-Afb/T *4*rh *D. D. H. WL-57 - May

Total footage dril!1,758.52 Meters x

QNXAfl'O GEOLOGICAL22nd, rT(.. JvWQ ,t2Qwir-i

OFFICE:

DEC2V 198ed' 2 8 ff E' u ET V^

To be used for this Bnumrssion- ,~3

PgnHfil fir— fvitMrf submission ___ 8.

June 20th, 1989

Claim TB 646428 168 M.

646432 412 M.

646433 86.52 Mpth ,of- Hole ———— 666.52 M.

L98.9Claiii TB 646431 225 M

646433 221 M

^ 646434 483 M

646439 163 M

J^^-J /r, ^ 1,092 M7759 D lys/Feet94 Days/Eae eate of R8port

VALLEY FI ELD, QUEBECJ6S 4V7

*B

CC' 666.52 M.ro :.: -lir.: : : r: , ,ro ., ~; MCO ' "* Cj O

-1 rn i-~^5 *~ nl^ -?^092 - 0 M-

5 JL^w^*^^^^^ ^~*Total —1,758.52 M

•T

Recor64d Holder or Agent (Signature*

tfl^/t/s t ~ sCertification Verifying Report of Work

1 hereby certify that 1 have e penonal end Intimate knowledge of the facts set forth In the deport of Work annexed hereto, having porfomind the work or witnessed lame during and/or after its completion and the annexed report Is true.

Name and Postal Address of Penon Certifying

IAN R. MORRISON C/O MINNOVA Inc. 2606 VICTORIA AVENUE, EAST, THUNDER BAY,Certified by (Signature)

ONTARIO P7C 1E7Table of Information/Attachments Required by the Mining Recorder

Date Certified

7 V AJf^ S 7 7Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

Specific Information per type

Nil

Type of equipment

Type of equipment end amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.

Signed core log Ihowing; footage, diameter of core, number end angles of holes.

Nemo and address of Ontario land surveyor.

Other Information (Common to 2 or more types)

Names and addresses of mon who performed manual work /operated equipment, together with dates and hours of employment.

Names and addresses of owner or operator together with dates when drilling/stripping done.

Nil

Attachments

Work Sketch: thoso are required to show the location and extent of work in relation to the nearest claim post.

Work Sketch (as above) in duplicate

Nil

W (85/12)

300

DICKISON LAKE G-3187 0 I5'

49 U 07 30 —

Green hedge

Lake

1103020 H0302I

wm l * -n , TB

1103005 i 1103006 l1103002 l "03003 | 1103004

NortMtne LaJte

103000 11081436 11081439 i IOW442

1103012 ; 103013 l H030IBJ.——-A--

l 646 4d748J6467^ j^ _ J

565714 f! Co At S1565664 .556216

___ | _"

814469(814474 |8I4 493 ' \,'8144~~~'"*""~'

1814487 181 - - -l- - - -t- - -

654420 654421 646583 l 64 6566j646 5.87 -|— —-"- ——^- " ^ - -J - -L^d^^ K646585 '646588 1646589814484 814485----- ———— L.---—— - r

654422 1646584 ion i l814453 .814454 - — — -l — -

Y n - .y—646436 |8464pO

~ ~ ~ ~ ~ ~ l646733 16^6736,646737 _ '6 ^b^4 t 645306 '645307 .645308

07J 38,6806 '6464381646435 ,64643! 64642 9 '646728- —Jl—————— J— — ~ J 7" — — - H- — — -(-^r-s.^ -j— — —— i- — — — -^ 646 4 |B '646-H9 '64 64 20

8 386805 ^646439*^64643^^6464321646428 [646414 j646 415^6^5416 [646417 j,. ,- , ,.J^ l " "l l ~" fTB3i46 674264

49 0 07 30

N-

CDl

OLLJ

OCO<to <O<DC LU Q. Q.

49 0 00 49 0 00'

870 30' 870 I5'

PAYS PLAT LAKE G-606

REFERENCES

LEGENDH l r, HW A-v ,", \" ' : -J

OTHf'u RfjAP'"

TRAILS

SURVLYEO LINES:TOWNSHIPS, BASF L 'NFS, ETC LOTS. Mirj'NG ( l A l VS PA H 1.1 i S \

UNSURVt""- ( ' INbS.LOT LINLbPARCEL BOUNDARYMINING CI AIMS ETt.

RAILWAY AND RtGHl Of WAY

UTILITY LINtS

NONPtRfcNNIAl STReAM

FLOODING UR l l OODING RIGHTS

SUBDIVISION uR ( I.IMPOM l Ir PL AN

RESERVAT IONS

ORIGINAL SHOHH iNfc

MAR^H OR MUSKEG

MINbS

TRAVtRSE- MONUMFN l

DISPOSITION OF CROWN LANDS

OF DOCUMENT SYMBOL

PATENT. SURFACE 8t MINING RIGHTS *

.SURFACE RIGHTS ON L Y . . . . ©

.MINING RIGHTS ONLY O

LEASE, SURFACE 8, MINING RIGHTS H

SURFACE RIGHTS ON L Y . H

" MINING RIGHTS ONLY . y

LICENCE OF OCCUPATION . .... ... .

ORDER IN COUNCIL ...... . .

RESERVATION ... . ... . ...

CANCELLED ...... .. ®

SAND fi. GRAVEL ..... . ... . (f)

NOTE; M INING R IGHTS IN PARCELS P ATENTED PRIOR TO MAV 6 .1913, VESTED I N ORIGINAL P ATENTEE B V THE PUBLIC LANDS A CT R SO 1970 CHAP 380, S F C 63. SU8SEC 1

SCALE 1 INCH = 40 CHAINS

O lOOO i?OOO 60 OO

WE T RI ',10OO

i l K M?000

(2 KM i

AREA

ROPE LAKEM.N.R. ADMINISTRATIVE DISTRICT

TERRACE BAYMINING DIVISION * G-***^-r*"

THUNDER BAYLAND T ITLES/ REGISTRY DIVISION

THUNDER BAY

Ministry ofNaturalResources

Land

Management

BranchOntario

Oate F EB. 17,1982 Number

G-609

42Efl3SW8ai03 21 ROPE LAKE 200

dd rpt 21 rope lake€¦ · area: rope lake report no: 2 1 010 work performed for: minnova inc....

Documents