The Ice occurrence is located at an elevation of approximately 800 metres on a gentle northeast-facing slope, approximately 4 kilometres south-southeast of Endako.

The area is underlain primarily by intermediate to felsic intrusions of the Upper Jurassic Francois Lake Intrusive Suite.

The Ice showing consists of molybdenite associated with granite, alaskite and diorite.

Work History

In 1971, Endako Mines Ltd. completed a program of soil sampling on the area immediately west of the occurrence as the Pat 97 group of claims.

In 2018, Thompson Creek Metals Co. Inc. completed a 17.5 line-kilometre induced polarization survey on several areas of the Endako property including the area southwest of the Ice occurrence.