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Cambria Mine, Thames, Thames-Coromandel District, Waikato Region, New Zealandi
Regional Level Types
Cambria Mine- not defined -
ThamesTown
Thames-Coromandel DistrictDistrict
Waikato RegionRegion
New ZealandCountry

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Latitude & Longitude (WGS84):
37° 7' 34'' South , 175° 32' 33'' East
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Thames7,136 (2014)1.4km
Ngatea1,151 (2011)17.9km
Kerepehi537 (2011)19.3km
Paeroa3,994 (2011)28.9km
Whangamata4,253 (2011)29.9km
Mindat Locality ID:
301673
Long-form identifier:
mindat:1:2:301673:5
GUID (UUID V4):
0


Historic gold mine. Located immediately south of the Non Pareil Mine, on the northern side of Waiotahi Stream.

The Cambria Gold Mining Company was formed in 1884 and soon found rich gold as a bonanza at 234-294 feet below the surface, accessed by the Cambria shaft. The bonanza was 20 feet below the No. 3 level, occurring where the reef intersected a cross-vein one foot wide, and clay filled fissure. The reef here carried rich ore 4-10 feet wide, with specimen stone within this 2-3 feet wide.

During a month in 1885, 5599 ounces of gold was recovered. 4160 ounces and 2574 ounces are mentioned as fortnightly results across late 1885 to early 1886. The Cambria Mine was the ninth largest producer on the goldfield at 59 151 ounces of gold from 30 915 tonnes of ore. The company is said to have lasted until 1897, when it was incorporated into other leases, but little information was found in the 1890's for it as a separate mine.

Peter Johnstone (52) was killed in the mine in 1888, although the reason is not mentioned. In 1898, John Cameron (58) committed suicide by throwing himself down the Cambria shaft.

The mine is mentioned briefly 1909 to 1914 as the New Cambria.

The Cambria Reef is sometimes called the Waiotahi-Cambria, reflecting it is the same reef but thrown by the major Moanataiari Fault which cuts the reef in half. The reef trends north-east to south-west, showing complex forking (anastromising?), and numerous blows of quartz. Economic ore was found confined to the Hanging Wall, with small auriferous quartz veins across the rest of the reef. Below the No. 4 level, gold grades rapidly diminished.

The quartz contained pyrite, crystallised stibnite, and ruby silver coloured pyrargyrite.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Stibnite2.DB.05Sb2S3
Pyrite2.EB.05aFeS2
Pyrargyrite2.GA.05Ag3SbS3
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S PyrargyriteAg3SbS3
S PyriteFeS2
S StibniteSb2S3
FeIron
Fe PyriteFeS2
AgSilver
Ag PyrargyriteAg3SbS3
SbAntimony
Sb PyrargyriteAg3SbS3
Sb StibniteSb2S3
AuGold
Au Native GoldAu

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.

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