weathering, erosion, deposition, and landscapes Flashcards
pysical weathering
the breakdown of rock without changing its chemical composition
frost action
when water freezes its expands, so when water freezes and a crack in a rock gets bigger, this is how pot holes form.
biological action
animals and plantroots break rock apart
abrasion
when sediments in a river bump into each other causing sediments to be round smooth
chemical weathering
the breakdown of rock while changing the chemical composition
oxidation
when iron minerals in a rock interact with the oxygen in the air it often causes rust
hydration
when minerals in a rock interact with the hydrosphere sometimes mineral can dissolve forming caves, caverns, or sink holes
mineral composition
harder minerals weather slower than softer minerals
particle size
the smaller the particles the faster they weather
climate
temperature: warmer temperatures cause a faster weathering rate.
chemical weathering
occurs more in warm, humid climates
A horizon
topsoil-high organic content and weathered bedrock
B horizon
-partially weathered bedrock with some organic material
C horizon
partially/slightly weathered rock
bedrock
parent material-the solid rock under the soil
the two components of soil
weathered bedrock and organic material (humus)
the difference between transported soil and residual soil
residual soil forms from the rocks below
transported soil was brought throughout the area by an agent of erosion
erosion
the removal of sediment
the four natural agents of erosion are:
water, glaciers, wind, gravity
gravity causes
mass movements (pulling rocks and sediments downhill)
examples of mass movements include:
landslides, soil creep, mud flows and mudslides, rock falls, debris falls, avalanches
rocks eroded by gravity appear
jagged and broken
deflation occurs when
wind carries away loose sediments and lowers the earth’s surface (this is a problem on farmland)
sandblasting
occurs when winds blow sand or silt against other rocks causing the surface of the rock to appear pitted.
as a glacier moves over land…
loose rocks and sediments freeze within the ice.
rocks within a glacier help the glacier to scratch and carve out the land below producing …
glacial grooves and parrallel scratches on the rocks called striations.
Glacial grooves show…
the direction that the glacier moved.