The 'Estuary Last Test Ch 18,19, 20' assesses knowledge on glacial processes and formations, including glacier flow mechanisms, types, and moraines. It evaluates understanding of Pleistocene glacial episodes and features shaped by glaciers, crucial for students of Earth and environmental sciences.
Kettle
Ground
Terminal
Medial
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Frost heaving
Crevassal Slip
Morainal Sliding
Basal Slip (Sliding)
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Kansan
Indianan
Wisconsinan
Dakotan
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Drumlins
Cirques
Moraines
Eskers
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Valley and mountain
Continental and polar
Valley (alpine) and continental
Polar and mountain
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“U” shaped
“V” shaped
“S” shaped
“A” shaped
None of the above
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H. Goering
Louis Agassiz
M. Milankovich
H. Marcee
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Kettle
Esker
Cirque
Moraine
None of the above
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Iceland
Siberia
Antarctica
Greenland
None of the above
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Steppes
Tundras
Sundras
Sabkhas
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Precipitation totals are low; dew points are lower in the summer than winter.
Evaporation potential exceeds actual precipitation.
Storms are infrequent and rainfall amounts are highly variable.
Wind is the dominant agent of erosion and sediment transport.
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Wash
Playa
Rivulet
Rill
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5 and 10
20 and 30
40 and 50
0 and 5
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Cool, dry air aloft is descending; surface winds are blowing toward the equator.
Warm, humid air aloft is descending; surface winds blow away from the equator
Warm, humid air is rising; surface winds are calm.
Cool, dry air at the surface is rising, causing winds to blow away from the equator.
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Cross beds
Dunes
Till
Loess
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Wind speed
Barometric pressure
Temperatures
Latitude and longitude
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Is increasingly becoming a problem
Is a natural process
Is exacerbated by human processes
Results in droughts and famine
All of the above
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Blowing wind removes fine-size particles; coarser particles abrades to sand size
Intense chemical weathering removes the sand and silt particles, leaving coarse rock debris covering the land surface
Running water deposits gravel and sand over finer sized particles.
Deflation and sheet wash remove fine sized particles leaving coarse weathered rock fragments concentrated at the surface.
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Longitudinal
Transverse
Star
Parabolic
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Flood
Rip
Drift
Ebb
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It has fallen about 10 inches per century
It has remained about the same
It has risen about 10 centimeters per century
None of the above
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Emergent
Submergent
Stable
Retreating
None of the above
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Causes mass movement of sediment downshore
Creates a loss of sediment from some beaches
Creates an increase in sediment on some beaches
Can be stabilized by groins and jetties
All of the above
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Relaxing
Reflection
Refraction
Refluxing
Recalcitrating
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Sea spit
Sea stack
Sea rampart
Sea span
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Breakwaters
Groins
Seawalls
Jetties
Tombolos
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Pennsylvanian period
Miocene epoch
Mesozoic era
Pleistocene epoch
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Lateral moraine
Terminal moraine
Ground moraine
Recessional moraine
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Boundary between parts of the glacier moving by basal sliding and crevassal slip
Boundary between the basal sliding and external flowage zones
Bottom of the basal sliding zone
Top of the internal deformation and flowage zone
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Lake in a cirque
Valley before it was glaciated
Drowned glacial trough
Period of the Ice Age
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Composed of outwash
Ridges formed on top of a glacier
Formed in the zone of fracture
Not found singly, but in clusters
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The internal, flowage zone
The snout zone
The surface, brittle zone
The basal, sliding zone
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Refers only to alpine glaciers
Refers only to moraines
Is synonymous with the term "till"
means any sediments of glacial origin
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Esker
Yazoo ridge
Valley plain
Kettle
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Kaming
Calving
Surging
Drowning
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Tarn
Paternoster
Kame
Kettle
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Terminal moraine
Outwash blanket
Kame sheet
Ground moraine
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Kame terrace
esker
Outwash plain
Ground moraine
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Desert landscapes are monotonous, relatively flat areas covered to various depths with sand
Deserts and dry lands are concentrated in areas of ascending air masses and relatively low atmospheric pressures
Despite infrequent rainfalls, erosional and depositional features of running water are important in desert landscapes
Rainshadow deserts occur where air masses descend after first having risen to cross a mountain range
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Rivulet
Playa
Rill
Wash
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was once glacial outwash deposits
is in the form of transverse dunes
Is uniformly thick
had its source in desert regions
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10%
66%
30%
3%
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Balda
Bajada
Bahia
Baja
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Insulated icebergs floating in a hot spring
Blowouts cut from bedrock in mountainous areas
lithified rock formed by cementation of wind-deposited, dune sands
bedrock hills in a highly eroded desert landscape
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Spring
Ebb
Neap
None of these
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Spring
Ebb
Neap
None of these
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Right
Left
West
East
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Right
Left
West
East
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