Soils And Geomorphology Flashcards
Define geomorphology
The scientific study of landscapes and land forms on the earth’s surface and the processes is acting on them
Characteristics of the Active layer in a permafrost environment
The surface layer characterized by freezing and thawing on a seasonal basis
Define aggradation
Filling in a stream channel with sediment usually associated with low discharges and or heaving sediment loads
Scouring and downcutting of a stream channel usually associated with high discharges
Degradation
Erodibility
The relative susceptibility of a soil to erosion
The k-factor
US soil conservation service term for a value used in the universal soil loss equation representing relative erodibility
Erosion
The removal of rock debris through moving water, wind, or glaciers.
Geomorphic system
A physical system comprised of an assemblage of landforms linked together by Geomorphic processes
What is a hard pan soil layer and how is it formed
A cemented layer in the soil usually 2 to 4 feet under the surface. Formed chemically by lime, iron, or silicate materials deposited at the same level and cementing the soil particles together.
Define mass wasting
The movement of rock and soil down slope under the influence of gravity. Examples include rockfalls, slumps, debris flows.
What events can cause mass wasting
Can be caused by rain fall, seismic activity
How is a moraine Landform formed
Comprised of material left behind by a moving glacier usually soil and rock
Soil types from smallest to largest
Clay (0.002 mm or smaller)
Silt (0.002 - 0.05)
Sand (2 - 0.05)
Describes the soil changes from soil to semisolid to plastic to liquid as water is added to dry soil
Atterberg limits
Moisture content in the soil at the threshold between semi solid and plastic
Plastic limit
Moisture content in the soil at the threshold between plastic and liquid.
Liquid limit
Moisture content in the soil at the threshold between solid and semisolid
Shrinkage limit
Symptoms of compacted soils
Poor aeration, reduced infiltration. Caused by the space between soil particles being greatly reduced or eliminated