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Cobb Asbestos Mine, Cobb Valley, Tasman Region, New Zealandi
Regional Level Types
Cobb Asbestos MineMine
Cobb ValleyValley
Tasman RegionRegion
New ZealandCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
41° 7' 26'' South , 172° 42' 0'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Riwaka986 (2011)25.5km
Motueka7,485 (2017)26.5km
Takaka1,223 (2011)31.6km
Tapawera432 (2011)32.2km
Mapua1,819 (2011)36.2km
Mindat Locality ID:
297397
Long-form identifier:
mindat:1:2:297397:8
GUID (UUID V4):
7832b164-648a-4706-b46d-271d216f5682


After Takaka Hill on State Highway 60, at Upper Takaka a road heads south to Cobb Dam. This follows the Takaka River, and requires a 4 wheel drive, if driven in winter.

The walking track to the asbestos mine leaves 2 kilometres past the powerhouse, and follows the disused mine road. The mine is a scar on the hillside, with minor rusting relics. The deposit was discovered in the 1880's. By 1917, 100 tonnes of asbestos fibre had been brought out by packhorse, but the remote location made mining unpayable.

The construction of the Cobb Dam in 1935, and resultant road, gave better access, and the Hume Company mined asbestos until 1964, producing a total of around 5000 tonnes. The mine closed due to the shortness of the asbestos fibres.

Serpentinised dunite is dominant at the mine, with abundant asbestos stock works in places. Local collectors report chrysotile, thurlite and serpentine. We are obliged to warn that asbestos fibres, even in small amounts, are highly dangerous to health, and the mine should be avoided.

A steep 30 minute walk past the mine is Asbestos Hut, which is actually made of wood. Built in 1897 by asbestos prospectors, from 1914 it was the home of Henry and Annie Chaffey for 40 years. Annie lived as a recluse, with Henry prospecting for minerals across the region, walking in supplies from the nearest town, and trying to get companies interested in mining asbestos.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


2 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 9 - Silicates
Chrysotile9..Mg3(Si2O5)(OH)4
Zoisite
var. Thulite
9.BG.10{Ca2}{Al,Mn3+3}(Si2O7)(SiO4)O(OH)
9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Unclassified
'Asbestos'-
'Serpentine Subgroup'-D3[Si2O5](OH)4

List of minerals for each chemical element

HHydrogen
H ChrysotileMg3(Si2O5)(OH)4
H Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
H Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
H Serpentine SubgroupD3[Si2O5](OH)4
OOxygen
O ChrysotileMg3(Si2O5)(OH)4
O Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
O Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
O Serpentine SubgroupD3[Si2O5](OH)4
MgMagnesium
Mg ChrysotileMg3(Si2O5)(OH)4
AlAluminium
Al Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Al Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
SiSilicon
Si ChrysotileMg3(Si2O5)(OH)4
Si Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Si Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Si Serpentine SubgroupD3[Si2O5](OH)4
CaCalcium
Ca Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Ca Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
MnManganese
Mn Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)

Other Regions, Features and Areas containing this locality

Australian PlateTectonic Plate
New Zealand

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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