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  2. Laurentide ice sheet - Wikipedia

    en.wikipedia.org/wiki/Laurentide_ice_sheet

    The Cordilleran ice sheet covered up to 1,500,000 square kilometres (580,000 sq mi) at the Last Glacial Maximum. [11] The eastern edge abutted the Laurentide ice sheet. The sheet was anchored in the Coast Mountains of British Columbia and Alberta, south into the Cascade Range of Washington. That is one and a half times the water held in the ...

  3. Wisconsin glaciation - Wikipedia

    en.wikipedia.org/wiki/Wisconsin_glaciation

    Table III Laurentide Ice Sheet; Glacial lobes and sublobes of the southern Laurentide Ice Sheet during the late Wisconsin Glaciation. [6] Major Lobes Minor Lobes Des Moines Grantsburg St. Louis Rainey Lake Superior [7] Wadena Chippewa [7] Wisconsin Valley [7] Langlade [7] Green Bay [7] Lake Michigan [7] Delavan Harvard-Princeton Peoria Decatur

  4. Lake Agassiz - Wikipedia

    en.wikipedia.org/wiki/Lake_Agassiz

    The Laurentide Ice Sheet continued to recede. Continued warming shrank the ice front towards present day Hudson Bay. Here, the Lake Agassiz northward outlet drained into the Tyrrell Sea. This breach dropped the water level below the eastern Kinojevis outlet. The drainage was followed by the disintegration of the adjacent ice front at about ...

  5. Deglaciation - Wikipedia

    en.wikipedia.org/wiki/Deglaciation

    Mapped extent of the Laurentide Ice Sheet during deglaciation has been prepared by Dyke et al. [21] Cycles of deglaciation are driven by various factors, with the main driver being changes in incoming summer solar radiation, or insolation, in the Northern Hemisphere. But, as not all of the rises in insolation throughout time caused deglaciation ...

  6. Proglacial lakes of Minnesota - Wikipedia

    en.wikipedia.org/wiki/Proglacial_lakes_of_Minnesota

    As the Laurentide Ice Sheet decayed at the end of the Wisconsin glaciation, lakes were created in depressions or behind moraines left by the glaciers. Evidence for these lakes is provided by low relief topography and glaciolacustrine sedimentary deposits. [1]

  7. Foothills Erratics Train - Wikipedia

    en.wikipedia.org/wiki/Foothills_Erratics_Train

    In addition, the atypically linear string of glacial erratics that comprise the Foothills Erratics Train was created by the parallel, non-turbulent flowage of two very large ice masses—the Cordilleran Ice Sheet to the west, and the Laurentide Ice Sheet to the east—that occurred at the boundary between them.

  8. Colorado snow forecast: Multiple feet expected in the Rockies ...

    www.aol.com/colorado-snow-forecast-multiple-feet...

    Editor's note: Follow USA TODAY's Wednesday coverage of the Thanksgiving 2024 weather forecast and travel updates.. Heavy snow showers of 1 to 2 feet are expected to blanket in the Colorado ...

  9. Cordilleran ice sheet - Wikipedia

    en.wikipedia.org/wiki/Cordilleran_ice_sheet

    Unlike the Laurentide Ice Sheet, which may have taken as many as eleven thousand years to fully melt, [3] the Cordilleran ice sheet melted very quickly, probably in four thousand years or less. [4] This rapid melting caused floods such as the overflow of Lake Missoula and shaped the topography of the fertile Inland Empire of Eastern Washington. [5]