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19.2: Geologic Work of Glaciers

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    Glacial erosion

    Glaciers themselves do relatively little significant erosion because ice is so soft. Under the weight of an ice sheet thousands of feet thick continental glaciers detach material from the surface by crushing the underlying bedrock. Once the material is loosened from the surface, ice can quarry (also known as plucking) the rock by freezing around and into fractures, then lifting it from the surface. The rock embedded in the ice gouges and smoothes bedrock surfaces by abrasion. Striations are fine scratches left in bedrock by abrasion. At a larger scale, linear grooves are ground into the bedrock in the direction of ice movement. Chipping of bedrock leaves crescent-shaped marks called chatter marks gouged into the bedrock. The constant abrasion of exposed rock also creates polished bedrock.

    First slide
    Figure \(\PageIndex{1}\): Chatter marks in bedrock, Kilarney Provincial Park, Canada. Sun glasses for scale. (Image Courtesy: Michael Ritter)
    Second slide, polished bedrock
    Figure \(\PageIndex{2}\): Polished bedrock. Kilarney Provincial Park, Canada (Image Courtesy: Michael Ritter)
    Third slide, glacial striations
    Figure \(\PageIndex{3}\): Glacial Striations. Camera Lense cap for scale. (Image Courtesy USGS)
    Fouth slide, grooves at Kellys Island
    Figure \(\PageIndex{4}\): Glacial Grooves. Grooves in granite bedrock, Kelly Island, Ohio. (Federal Highway Administration)

    Glacier Transport and Deposition

    Glacial drift deposited directly by a glacier is called till. Unlike sediment deposited by running water, till is not sorted by sediment size. Till looks like a jumbled mixture of fine and coarse textured material as shown in Figure \(\PageIndex{5}\). Fragments of rock encased in ice tend to retain their angular shape, though occasionally the edges are knocked off when rubbing against the bedrock beneath. Rocks that tumble and roll through a stream are more rounded from striking the bed of a stream channel.

    51dc7cebe4b097e4d3838cb1_535.jpg
    Figure \(\PageIndex{5}\): Glacial till in moraine in Whiteshell Park, Canada. (Source: USGS)

    Erratics are boulders whose composition does not match the local bedrock where they are found. Glaciers transported erratics great distances, then deposited them in their current locations as the glaciers retreated.

    37897c78-99b7-42a3-bb9b-13e26df42909Original_535px.jpg
    Figure \(\PageIndex{6}\): Giant erratic in Yellowstone National Park

    Water melting from a glacier carries sediment with it. Outwash is stratified drift laid down by water issuing off a glacier. The velocity slows as meltwater runs across the surface causing sediment in the water to deposit. The varying water velocity sorts and layers the drift. Streams running off the edge of the glacier overburdened with sediment form braided streams in outwash deposits.

    DSC_0322_535px.jpg
    Figure \(\PageIndex{7}\): Sands and fine gravels in stratified glacial outwash near Houghton Lake, Michigan. (Courtesy of Randall Schaetzl, Michgan State University)

    Video: "Basal Till and Strations" (Courtesy of UBC Virtual Soil Learning Resources)

    Loess is principally wind-deposited silt, much of which was eroded from Pleistocene glacial sediments. Vast deposits of loess are spread across the upper Midwest United States, with significant deposits along major rivers like the Mississippi. The sediment is deposited by glacial meltwater then eroded by strong winds. The Loess Hills of Iowa and Loess Plateau of China are two well-known examples of loess topography.

    loess_pierre_marquette.jpg
    Figure \(\PageIndex{8}\): CLoess deposit in Pierre Marquette State Park, Illinois (Source: Michael Ritter)

    This page titled 19.2: Geologic Work of Glaciers is shared under a CC BY-SA 4.0 license and was authored, remixed, and/or curated by Michael E. Ritter (The Physical Environment) via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.

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