GEO 200 Ch 19

25 July 2022
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question
At its maximum extent, ice covered almost ________ of the Earth's land surface.
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1/3
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Hills rounded and sheared off by glacial erosion are called ________.
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roche moutonnees
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Unsorted debris from ice sheets, after deposition, is known as ________.
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till
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The shape of a(n) ________ can be likened to an amphitheater.
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cirque
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The maximum extent of a glacier is marked by a ________.
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terminal moraine
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________ is granular snow which is beginning to coalesce into glacial ice.
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Neve
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The most significant erosive work of glaciers is accomplished by ________.
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plucking
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The main sediment type carried by streams in glacial regions is ________.
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glacial flour
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Antarctica's ice sheet encompasses about ________ percent of the world's total land ice.
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85
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At its maximum extent, continental glacial ice in North America extended as far south as ________.
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The Ohio River
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The approximate maximum thickness of contemporary glacial ice is ________ meters.
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4,000
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A nunatak is a rocky pinnacle poking through a(n) ________.
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ice field
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A huge boulder resting on a completely different type of bedrock in glacial zones is a(n) ________.
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erratic
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The movement of a glacier along its bottom, lubricated by meltwater, is known as ________.
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basal slip
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The movement of a glacier is normally measured in ________ per day.
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centimeters
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The glacial scouring by bedrock embedded in ice is erosion by ________.
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abrasion
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A dark band of rock debris down the middle of a glacier from the union of two adjacent glaciers is a(n) ________.
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medial morraine
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A(n) ________ is created by a group of cirques eroding into a mountain peak.
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horn
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Long sinuous ridges of stratified drift are termed ________.
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eskers
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Glaciers often polish rock to form grooves and smaller, similar features called ________.
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striations
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A glacier grows when the accumulation zone grows faster than the ablation zone.
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True
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Most sediment in glacial regions consists of glacial flour.
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True
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Glacial erosion invariably produces smooth valley slopes.
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False
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Cirques are located at elevations high above sea level.
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True
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Hanging valleys occur where the mouths of tributary valleys are perched high along the sides of the major stream valleys.
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True
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The valley train is the same thing as an outwash plain.
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False
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The Great Lakes of the U.S./Canadian border are classic examples of paternoster lakes
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False
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Fjords are glacial features found only in the Southern Hemisphere.
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False
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U-shaped stream valleys are indicators that a stream valley has been glaciated.
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True
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Alaska was completely covered by a Pleistocene ice sheet.
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False
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Morainal surfaces containing a number of mounds and depressions are called ________ topography.
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kame-and-kettle
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he Finger Lakes district of upstate New York is a prime example of the glacial feature called ________.
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U-shaped troughs
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A ________ is an irregularly undulating surface of broad, low rises and shallow depressions. It is composed of unsorted glacially-deposited materials which can cover the landscape to the extent that the preglacial shape is obliterated.
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till plain
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A ________ is a lengthy deposit of glaciofluvial alluvial confined to a valley bottom and found beyond the outwash plain.
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valley train
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________ are relatively steep-sided mounds or conical hills of stratified drift made from meltwater deposition in a region of stagnant ice.
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Kames
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Name and discuss two of the three (3) types of glacial movement.
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Plastic Flow of Ice - When a mass of ice attains a thickness of about 50 meters, the plastic flow of ice begins in response to the overlying weight. The entire mass does not move universally, rather, there is an oozing outward from around the edge of an ice sheet or downvalley from the end of an alpine glacier. Basal Slip - the entire mass slides over its bed on a lubricating film of water. The glacier mold itself to the shape of the terrain it's riding over.
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The basic landform feature in glaciated mountains is the cirque - what is it?
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A cirque is a broad amphitheater hollowed out at the upper-most head of a glacial valley. It has steep, often perpendicular, head and side walls and floor that is either flat, gently sloping or even gouged enough to form a basin. It marks the place where an alpine glacier originated.