Exam 17: Glacial and Periglacial Processes and Landforms
Worldwide, alpine glaciers are presently increasing in size and number.
False
The transformation of snow into glacial ice in Antarctica takes ________ than in midlatitude alpine glaciers because ________.
D
Describe the importance of periglacial processes.
Periglacial regions occupy over 20% of the Earth's land surface and are dominated by the geomorphological processes related to the freezing of water. Periglacial conditions occur at high latitudes, with a near permanent ice cover, at high elevations in lower latitudes, with areas that are seasonally snow free. They tend to correspond to subarctic and polar climate zones, in particular the tundra climate.
In areas where the soil, sediment, or rock is below freezing for at least two years, permafrost forms. Where permafrost is not covered by a glacier, it is considered periglacial. Large portions of Alaska, Canada, China, Scandinavia, Greenland, and Antarctica have permafrost. Permafrost may be divided into continuous and discontinuous zones and are exactly as the names suggest.
These periglacial environments are subject to freeze/thaw actions and the landforms that result, such as ice wedges, hummocks, patterned ground, solifluction, and gelifluction. Humans have also settled periglacial regions. Due to the freeze/thaw processes, humans must learn to properly adapt structures to the environment.
If a glacier does not have debris embedded in its base, it is not a very effective agent of abrasion.
Unfrozen ground in a region of discontinuous permafrost is known as
Solifluction is the downslope movement of soil particles resulting from freeze/thaw cycles.
Alpine glaciers eroding parallel valleys may produce thin, sharp ridge forms known as arête.
The zone of seasonally frozen ground that exists between the subsurface permafrost layer and the ground surface is called the
A class of landforms formed by the accumulation of glacial till are known as
Which of the following is not correct regarding the Pleistocene?
Vertical and horizontal movement caused by the expansion of freezing water are called
Most glaciers are stationary, moving at no more than several millimeters per year.
If two glaciers with lateral moraines join, a medial moraine may form.
Many western states rely heavily on snowmelt for their municipal water supplies.
A glacier confined in a bowl-shaped recess is known as a(n)
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