Wastage exceeds accumulation
Accumulation exceeds wastage
Accumulation and wastage are about equal
None of the above.
Kettle
Ground
Terminal
Medial
Frost heaving
Crevassal Slip
Morainal Sliding
Basal Slip (Sliding)
Kansan
Indianan
Wisconsinan
Dakotan
Drumlins
Cirques
Moraines
Eskers
Valley and mountain
Continental and polar
Valley (alpine) and continental
Polar and mountain
“U” shaped
“V” shaped
“S” shaped
“A” shaped
None of the above
H. Goering
Louis Agassiz
M. Milankovich
H. Marcee
Kettle
Esker
Cirque
Moraine
None of the above
Iceland
Siberia
Antarctica
Greenland
None of the above
Steppes
Tundras
Sundras
Sabkhas
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.
Wash
Playa
Rivulet
Rill
5 and 10
20 and 30
40 and 50
0 and 5
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.
Cross beds
Dunes
Till
Loess
Wind speed
Barometric pressure
Temperatures
Latitude and longitude
Is increasingly becoming a problem
Is a natural process
Is exacerbated by human processes
Results in droughts and famine
All of the above
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.
Longitudinal
Transverse
Star
Parabolic
Flood
Rip
Drift
Ebb
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
Emergent
Submergent
Stable
Retreating
None of the above
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
Relaxing
Reflection
Refraction
Refluxing
Recalcitrating
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