Notes on glaciation in central Yukon Territory
- 1 January 1966
- report
- Published by Natural Resources Canada/CMSS/Information Management
Abstract
Two clearly defined series of glacial limit features, readily correlated and traced from place to place are inferred to mark the limits of the last glacial advance in central Yukon. These are the McConnell Moraine and an earlier advance, the Reid Moraine. In addition, older glacial drift, till, erratics and modified landforms have been found beyond the clearly marked limits and perhaps record two earlier glaciations. These earlier features are referred to as the Klaza Drift (the younger) and the Nansen Drift (the older).Keywords
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