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- W183838540 abstract "Montana is unique in hosting multiple Pleistocene examples of all glacier types including continental ice sheets, large mountain ice caps, small mountain ice caps and transection glaciers. The chapter reviews that uncounted valley, cirque, and niche glaciers also existed in more than 60 distinct mountain ranges. The distribution of these glaciers, with equilibrium-line altitudes rising from north-west to south-east, is consistent with control by moist air masses entering the north-western comer of the state. Prevailing winter westerly winds immediately south of the Cordilleran Ice Sheet at the glacial maximum are indicated. Mapped extents of Pleistocene glaciers in the mountains of western Montana were achieved from topographic map and aerial photographic interpretation, with limited field verification. Nowhere in Montana are the ages of glacial episodes well-constrained. Most Last-glacial moraines are correlated with the Pinedale glaciation elsewhere in the Rocky Mountains, rather than dated directly. Radiocarbon dates in the Yellowstone region and south of Glacier National Park and occurrences of Glacier Peak volcanic ash in the Flathead region show massive retreat or disintegration of the major ice caps prior to the Younger Dryas Chronozone. It is assumed that similar ages apply to the many mountain glaciers as well." @default.
- W183838540 created "2016-06-24" @default.
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- W183838540 date "2004-01-01" @default.
- W183838540 modified "2023-10-18" @default.
- W183838540 title "Pleistocene mountain glaciation in Montana, USA" @default.
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- W183838540 doi "https://doi.org/10.1016/s1571-0866(04)80193-3" @default.
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