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• W2343908258 abstract "years BP. The loess was likely derived from the floodplain of the Yukon River during periods of low flow. Turf in growth position and organic matter in the silt similar to that of loessal grasslands near Kluane Lake suggest a grassland environment for the area during McConnell glaciation. A mummified carcass in the silts indicates that some of these sediments have been frozen since shortly after deposition. Ice wedges are commonly found in the upper portion of the silt, but these wedges rarely extend into the overlying organic material. Separate, smaller ice wedges are found in the Holocene unit. Radiocarbon dates indicate that peat growth began at the start of the Mohxne, as in sther unglaciated portions sf Yukon, when the climte became abruptly wetter." @default.
• W2343908258 created "2016-06-24" @default.
• W2343908258 creator A5022817700 @default.
• W2343908258 date "1997-01-01" @default.
• W2343908258 modified "2023-09-27" @default.
• W2343908258 title "On the nature and origin of iSmyck§5 deposits in the Klondike areas Yukon Territory" @default.
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• W2343908258 hasPublicationYear "1997" @default.
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