Unit symbol: | Qs |
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Age range | Quaternary (1.806 to 0 Ma) |
Lithology: | Unconsolidated |
Group name: | Unconsolidated and poorly consolidated surficial deposits |
Source map | Patton, W.W., Jr., Wilson, F.H., Labay, K.A., and Shew, Nora, 2009, Geologic map of the Yukon-Koyukuk basin, Alaska: U.S. Geological Survey Scientific Investigations Map SIM-2909, 26 p., 2 sheets, scale 1:500,000. |
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Symbol | QTgl |
Unit name | Glacial and glaciolacustrine deposits. |
Description | Includes unsorted to poorly sorted till, outwash sand and gravel, alluvium, and eolian deposits. Along the southern edge of Brooks Range, unit is characterized by little-modified middle and late Pleistocene drift including prominent morainal ridges (shown by hachured lines), ice-contact features, and glaciolacustrine deposits. Further south, in Bettles, Hughes, Shungnak, and Selawik quadrangles, unit is composed of discontinuous areas of highly modified drift of Pliocene(?) and early Pleistocene age interspersed with alluvium and eolian deposits. Glacial erratics occur in hilly parts of the central Shungnak and Hughes quadrangles to an elevation of 600 meters. In the Bettles quadrangle the southern margin of the unit consists chiefly of lacustrine sediments deposited from a large proglacial lake. Glacial drift deposits bordering the southern edge of the Brooks Range and extending to the southern edge of the Selawik, Shungnak, Hughes, and Bettles quadrangles. Also includes drift from small Pleistocene alpine glaciers in the Melozitna, Tanana, and Medfra quadrangles |
Lithology | Unconsolidated |
Label | Qm |
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Description | Glacial deposits, undivided, of Holocene and/or Pleistocene age |
Geologic age | Pleistocene to Holocene |
Geologic setting | Unconsolidated |
Lithology | Form | Importance |
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Gravel < Coarse-detrital < Unconsolidated | Glacial | Major |
Sand < Coarse-detrital < Unconsolidated | Glacial | Major |
Silt < Fine-detrital < Unconsolidated | Glacial | Indeterminate, major |
Boulders < Coarse-detrital < Unconsolidated | Glacial | Minor |