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Whangairorohea Hot Pool SNA 560 ± 0508 WILDNZ www.wildlands.co.nz Legend Rivers and Streams Roads Site Boundary Tracks 1:50,000 0 1,000 2,000 500 Meters ± ± 1:400,000 0 5 10 2.5 Kilometers 1:5,000 0 50 100 25 Meters Legend Rivers and Streams Roads Site Boundary Tracks Vegetation Type Boundary

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Whangairorohea Hot PoolSNA 560

±

0508 WILDNZ www.wildlands.co.nz

Legend

Rivers and StreamsRoads

Site BoundaryTracks

1:50,0000 1,000 2,000500

Meters

±±

1:400,0000 5 102.5

Kilometers

1:5,0000 50 10025

Meters

Legend

Rivers and StreamsRoads

Site BoundaryTracks

Vegetation Type Boundary

Contract Report No. 2049 Page 314 © 2009

Whangairorohea Hot Pool Site Number: SNA560 Ecological District: Atiamuri Source of Information: Shaw and Beadel (1998); Spring-Rice (Unpublished) Digital Scale: 1:5,000 Data Source: WRAPS 2007 Regional Council: Waikato 1998 Site Number: NHS No. 560 Current Tenure: Unprotected Site Area: 0.1 ha Altitude Range: 300 m Bioclimatic Zone: Lowland Grid Reference: NZTM E1882988, N5733149

VEGETATION LANDFORM EXTENT

CODE TYPE 1 Radiata pine, blackberry, open water. Alluvial valley terrace in

rolling hills (Cody 2007) <0.1 ha

Indigenous Flora: Not known.

Fauna: Not known.

Notes on Overall Condition:

Not known. There appears to be an unplanted buffer around the site following recent post-harvest replanting of plantation forest estate.

Change Relative to Shaw and Beadel (1998):

Not known.

Threats/Modification/ Vulnerability:

Damage by stock or vandalism are the greatest threats (Spring-Rice Unpublished).

Risk Assessment:

Not known.

Significance Level:

Local (Appendix 5 - Table 1 - Criteria 5; Table 2 - Factor S)

Significance Justification:

This site is of local significance as it contains geothermal habitat, an uncommon habitat type prior to human settlement. Cody (2007) ranked the geothermal feature of this site as being of national significance.

Fieldwork Required:

No fieldwork required to assess significance, but fieldwork required to update biodiversity and management information.

Notes: 5 m above a stream bed. The spring water has a pH of 7.0 at 40 C and produces no sinter deposits. This spring has never been studied, and is a unique feature of high scientific interest owing to both its location and structure (Cody 1995).

Cody (2007) indicates that this pool was only discovered to science in the 1980s and ranked this geological feature as being of national significance.

This site is used by local people for bathing (Cody 2007).

References: Spring-Rice (Unpublished); Cody (1995 & 2007).