RCAF 23-5314/15

Plate IV. Glacially striated topography. The area with crag-and-tail features, in the lower half of the
photograph, has shallow drift-cover and is underlain by Ootsa Lake Group rhyolite. The
area in the upper half is heavily drift-covered and is underlain by flat-lying Endako Group
basalt (note the indistinct shallow groves). The sharply defined gullies are meltwater channels
cut, for the most part, into bedrock and now mainly abandoned. Ice movement was from
left to right.