Glaciers
Steven Dutch, Natural and Applied Sciences,University
of Wisconsin - Green Bay
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- What causes ice ages?
- variations in the earth's orbit
- variations in sun's heat output
- variations in sunlight reflected by the earth
- no definite cause has been conclusively proven
- Ice near the surface of a glacier exhibits ________behavior.
- brittle
- ductile
- Ice deep within a glacier exhibits________behavior.
- brittle
- ductile
- Which of the following was never an outlet of the Great Lakes
during the retreat of the glaciers?
- the Gulf via the Mississippi
- to the Atlantic via the Potomac or Susquehanna
- from Lake Erie to the Ohio River
- across Ontario to the St.
Lawrence
- The end of a glacier is located:
- where it meets an obstacle
- where the average annual temperature equals 32 degrees F.
- where snowfall plus inflow equals melting plus evaporation
- where one year's snow just melts before the next
year's snow
begins
- Most of the world's glacial ice is in:
- mountain glaciers
- the Antarctic Ice Cap
- the Greenland Ice Cap
- The Wisconsin, Illinoisan, Kansan and Nebraskan ice advances:
- account for all known Pleistocene ice advances
- account for almost all Pleistocene ice advances
- are only the last of many more Pleistocene ice advances
- The "firn line" on a glacier marks:
- the dividing line between the zones of accumulation and
ablation
- the elevation above which snow never melts
- the elevation where the average annual temperature is below
freezing
- the timber line, or elevation above which trees do not grow
- Why do continental glaciers have a dome-like profile?
- More snow falls in the interior of the glacier.
- Ice melts faster at the edges than the middle.
- Ice has lower density than rock, so the crust rises under the
glacier.
- the ice flows outward under its own weight.
- When a glacier retreats, a rock trapped within the ice
- continues to move toward the foot of the glacier
- retreats more slowly than the glacier front
- retreats as fast as the glacier front
- retreats faster than the glacial front
- Icebergs are formed by:
- freezing of sea water
- river ice which is carried out to sea
- pieces of glacial ice breaking off the glacier
- water freezing on the sea floor and floating to the surface
- During the Pleistocene, large lakes covered parts of the Western
U.S. These lakes are known as:
- crater lakes
- playas
- pluvial lakes
- flood plains
- The Pleistocene ice advances:
- are known to have ended
- are the only ones known in geologic history
- both of the above
- neither of the above
- The result of a glacier flowing into the sea:
- icebergs
- ice shelves
- both of the above
- neither of the above
- A glacier flows down a deep, slightly winding valley. After the
glacier melts, the valley will be all of these except:
- straighter
- deeper
- wider
- more winding
- Hanging valleys:
- form when a glacier in a major valley cuts deeper than the
tributary glacier
- are common locations for waterfalls
- are among the few cases of tributary valleys that do not meet
the main valley at the level of the valley floor
- all of the above
- How is it possible for a stream to have flowed on top of an
esker?
- the original stream banks are now eroded away
- there used to be a stream channel on top which has been
filled in
- the "banks" of the stream were glacial ice
- it really isn't possible
- Which of these is till?
- fine flacial lake clay
- well-sorted outwash sand
- a polished rock outcrop
- unsorted sand, gravel and clay in a moraine
- Depending on pressure, glacial ice exhibits two forms of
behavior:
- brittle and ductile
- solid and granular
- plastic and liquid
- snow and hail
- Glacial striations on an outcrop trend NE-SW. The direction of
ice movement was:
- NE to SW
- NW to SE
- SW to NE
- could be either NE or SW
- Kettle ponds formed when
- glaciers scoured deep holes
- meltwater scoured potholes
- blocks of ice melted and left depressions where the ice had
been
- large boulders rolled off the glacier and made craters
- Eskers probably form
- when the ice is advancing
- when the ice is retreating
- When a continental glacier retreats
- the entire ice front retreats smoothly
- the ice never advances again
- none of the above
- You'd use these to map the former margins of a glacier
- Eskers
- Drumlins
- Moraines
- Kames
- If you knew a glacier moved either east or west and wanted to
find out which, you'd look for
- Drumlins
- Roches Moutonees
- Either or both of these
- None of these
- Which of these would indicate the former presence of a glacial
lake?
- Varved clay
- Out wash sands
- till
- Loess
- Least likely to be a feature of mountain glaciation
- horn
- arete
- cirque
- drumlin
- As you go from lower to higher latitudes, the altitude of the
snow line should:
- increase
- stay the same
- decrease
- vary randomly
- none of these
- The zone of accumulation is characterized by:
- ablation
- the thickest development of glacial ice
- wastage
- moraines
- none of these
- A sudden movement of a glacier caused by a sudden addition of
snow on ice.
- surge
- plastic deformation
- calving
-
basal slip
- none of these
- The feature of valleys formed by glaciers which differentiates
them from valleys formed by streams is:
- the presence of kettles
- the presence of drumlines
- their characteristic V-shape
- their characteristic U-shape
- none of these
- A boulder which has been carried from its place of origin by a
glacier and later deposited on bedrock of a different nature is
called:
- a firn
- an erratic
- a kame
- an esker
- none of these
- A medial moraine is developed:
- on the side of a glacier
- at the end of the glacier
- none of these
- in the middle of two coalesced glaciers
- An esker is:
- a knife-edged ridge which separates two glacial valleys
- a smooth, elongated, asymmetric hill of till
- a depression which was caused by the melting of a block of
ice which had been buried in glacial debris
- a winding, steep-walled deposit of water-lain glacial debris
- none of these
- The following glacial feature cannot be used to determine
directions of ice movement:
- drumlins
- striation
- varves
- boulder trains
- none of these
- A glacial valley which has been left stranded above a primary
glacial valley is called:
- perched valley
- a hanging valley
- a cirque
- a truncated valley
- none of these
- Crevasses in glaciers extend down to:
- about 300 m
- the base of the glacier
- the zone of plastic flow
- variable depths depending on how thick the ice is
- the outwash layer
- If a glacier has a negative budget:
- the terminus will retreat
- its accumulation rate is greater than its wastage rate
- all flow ceases
- the glacier's length increases
- crevasses will no longer form
- There were Pleistocene mountain glaciers in Oregon at only 5000 feet
elevation, but the same elevations in Wyoming at the same latitude were
ice-free. Why?
- there was much more precipitation
in Oregon
- there really were glaciers in
Wyoming but the evidence has not yet been discovered
- there were no low-elevation glaciers
in Oregon and the evidence has been misinterpreted
- continental drift has moved Oregon
further south
- it was much warmer in Wyoming
- The bowl-shaped depression at the upper end of a glacial trough
is a(an):
- inselberg
- drumlin
- cirque
- till
- lateral moraine
- Firn is:
- freshly fallen snow
- a granular type of ice
- a valley train
- another name for the zone of wastage
- a type of glacial groove
- Pressure on ice at depth in a glacier causes it to move by:
- rock creep
- surging
- fracture
- plastic flow
- basal slip
- Rocks abraded by glaciers may develop a smooth surface that shines in reflected light.
Such a surface is called glacial:
- grooves
- striations
- polish
- till
- flour
- The most recent ice age occurred during the:
- Archean Eon
- Cambrian Period
- Pleistocene Epoch
- Tertiary Period
- Mesozoic Era
- When ice flows over a rocky knob, it creates a landform:
-
With a smooth upstream side and an irregular downstream
side
-
With a smooth downstream side and an irregular upstream
side
-
With evenly rounded sides
-
With irregular sides all over
- How weathering is thought to affect ice ages:
-
It lowers mountains and allows wind to circulate more
freely
-
It releases calcium that combines with carbon dioxide
-
It removes sulfur that otherwise might warm the
atmosphere
-
It creates methane, which cools the atmosphere
- The earth's natural Greenhouse Effect is mostly due to
- Carbon dioxide
- Methane
- Sulfur dioxide
- Water vapor
- When ice-dammed lakes drain, they usually drain
-
by evaporation
-
by seepage into the ground
-
by gradually lowering their outlets
-
by abrupt failure of the ice dam
- The number of ice advances during the Pleistocene was
most likely:
-
one
-
four
-
20-25
-
over 100
- The best record for the Pleistocene ice advances is
contained
-
In deposits on land
-
In the Antarctic ice cap
-
On the sea floor
-
In glacial lake deposits
- Marine evidence for ice advances and retreats includes
-
Alternations of warm and cold water microfossils
-
Coarse debris dropped by icebergs
-
Variations in oxygen isotopes
-
All of these
- Evidence for the "snowball earth" climate
variations is best seen in glacial deposits abruptly succeeded by:
-
warm-water limestones
-
sand dune deposits
-
coal
- volcanic ash layers
 |
Questions below refer to this diagram of a continental
glacier. |
- Melt water flowing through the crevasses at A will most likely form:
-
Eskers
- Drumlins
- Moraines
- Cirques
- The material deposited at B forms:
- Eskers
- Drumlins
- Moraines
- Cirques
- The material deposited by streams at C is termed:
-
Till
- Outwash
- Varves
- Drift
- The streams at C are most likely
-
Braided
- Meandering
- Old-Age
- Rejuvenated
-
The glacier's dome-like profile is due to:
- Ablation
- Wind erosion
- The ice spreading out under its own weight
- Greater snowfall in the interior
 |
The questions below refer to this diagram of a continental
glacier in retreat. |
- The features at A are:
- Lake deposits
- Moraines
- Drumlins
- Cirques
- The features at A indicate
- Former positions of glacial lakes
- Former margins of the glacier
- Positions of former meltwater streams
- Deposits streamlined by ice flow
- The features at B are ridges of sand and gravel. These are
- Moraines
- Drumlins
- Cirques
- Eskers
- The features at B are ridges of sand and gravel. They indicate
- Former positions of glacial lakes
- Former margins of the glacier
- Positions of former meltwater streams
- Deposits streamlined by ice flow
- The features at C are streamlined hills of till, sand and gravel. These
are:
- Moraines
- Drumlins
- Cirques
- Eskers
- The features at C are streamlined hills of till, sand and gravel. They
indicate
- Positions of former meltwater streams
- Former margins of the glacier
- Former positions of glacial lakes
- Ice-Flow Directions
- At D is a large isolated remnant of ice. When it melts it will probably
form a:
- Kettle
- Drumlin
- Moraine
- Esker
- The ice-dammed lake at E is probably depositing:
- Till
- Outwash
- Varved deposits
- Gravel
- When the ice-dammed lake at E drains, it will probably do so:
- Gradually
- By seepage into the ground
- Catastrophically and abruptly
- By evaporation
 |
The questions below refer to this diagram of a glaciated
mountain landscape |
- A cirque occurs at (letter):
-A-
-B- -C-
-D-
-E-
- A moraine occurs at (letter):
-A-
-B- -C-
-D-
-E-
- A hanging valley occurs at (letter):
-A-
-B- -C-
-D-
-E-
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Created 1/2/1997; Last Update 26 September 2003
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