Jackson, L. E. Jr, Organic sediments, Revenue Creek. Succession is formed by beds of peat, logs, organic silt with pebbly, organic-rich fluvial sand and fine...
Jackson, L. E. Jr, Thick glaciolacustrine fire sand and silt (L) overlying the terminus of a till (T) deposited during a readvance of the retreat phase of...
Jackson, L. E. Jr, Colluvial cover, Dawson Range. Tape measure is 50 cm long. Colluvium formed by the in situ physical disintegration of rock locally exceeds...
Jackson, L. E. Jr, Till deposited during the McConnell Glaciation, Crossing Creek about 30m east of the McConnell glacial limit. McConnell glacial limit, Mt....
Jackson, L. E. Jr, Frost-shuttered and ventifacted alluvial gravel and micaceous sand deposited during Reid Glaciation, headwaters, Nisling River. Clasts are...
The physical properties of the surficial deposits of that part of the Kananaskis Lakes map area within Alberta, and physical processes that shape these...
Valley margins in the Rocky Mountains are locally prone to periodic inundation by debris flows. Alluvial fans and landforms and related features may be...
The Nahanni map area was intensely glaciated during the McConnell Glaciation. At the climax of this glaciation, one or more ice centres existed over the area....
Fort Selkirk (FS) Yukon, Canada, is situated within (50 km east) of the all-time-limit of Cordilleran-ice-sheet glaciation (late Pliocene in age). Late...
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