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File Created: 25-Jun-1986 by Larry Jones (LDJ)
Last Edit:  09-Mar-1989 by Laura L. Duffett (LLD)

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NMI 103B11 Sds1
Name HOTSPRING ISLAND Mining Division Skeena
BCGS Map 103B053
Status Showing NTS Map 103B11W
Latitude 052º 34' 34'' UTM 09 (NAD 83)
Longitude 131º 26' 36'' Northing 5827922
Easting 334439
Commodities Hotspring, Sodium Sulphate Deposit Types T02 : Geothermal spring
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The hot mineral spring is located at a 9-metre elevation on the west shore of Hotspring Island which lies 26 kilometres south of Lyell Island.

Analysis of the spring was taken in 1901.

The wallrock consists of a volcanic hypabyssal porphyry plug of the Tertiary Masset Formation, intruding siltstone and greywacke of the Lower Cretaceous Longarm Formation. These rocks are cut by quartz veins up to several centimetres wide.

The hotspring issues from several fissures within agglomerates at a rate of about 0.06 cubic metres per minute. The issuing temperature is 72 degrees celsius and the pH at 23 degrees celsius is 8.1. An analysis of the water gave 28.5 grains per litre of chlorides and 1.2 grains per litre of sulphates. Elemental content of the water, in parts per million, is as follows: Si - 46, Ca - 61, Na - 784, K - 48, Cl - 1742, SO4 - 199 and HCO3 - 24.

The hotspring may be a saline spring recirculating warmed meteoric waters with added seawater.

Bibliography
EMPR AR *1901-1001,1002
EMPR BULL 54, Fig. 34
GSC MAP 1385A
GSC P 73-18, pp. 230,238; 86-20; 88-1E, pp. 221-227; 89-1H; 90-10; 91-1A, pp. 383-391
McDonald, J.J., (1978): Hotsprings of Western Canada, A Complete Guide; Labrador Tea Company, Vancouver, pp. 106-108

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