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.