Soil
Mass movement/weathering
Fluvial landforms
Water in the lithosphere
Slopes and streams
100

The four components that make up soil

Minerals, organic matter, water, and air

100

Three types of weathering

Mechanical, chemical, biological

100

Natural deposits that run on both sides of the channel preventing future floods

Levees

100

The complete system of the trunk and its tributaries forming a network that occupies a region

Drainage basin

100

Drainage networks seen on flat-lying sedimentary rocks

Dendritic
200

The "P" in the soil forming "ClORPT" equation

Parent material
200

The slowest type of mass movement

Soil creep

200

Type of channel formed when the river needs to carry a lot of large sized sediments

Braided channels

200

The natural phenomena when water trapped in between rocks freezes

Frost action

200

The primary mechanisms by which streams shape landscapes

Erosion, transport, and deposition of sediment

300

The region you will most likely find Gelisol soils

The poles (cold, high latitude)

300

Two factors that affect what type of mass movement we see

Speed of motion & amount of water

300

What happens to stream discharge if cross sectional area of a stream increases

Stream discharge also increases
300

Sediment accumulation which fills the river's valley and raises the bed level

Aggradation 

300

The two aspects of stream power equilibrium

Energy available, sediment to be carried

400

The term that describes the light color associated with soil "E" horizons

Eluvatiation

400

The likelihood for mass movement on a shallow slope compared to a steep slope

Low

400

The __ shaped deposit where a mountain stream emerges on to a plain (or name of the deposit)

Alluvial fan

400

Downward erosion of streams lowering the level of the bed

Incision

400

The type of energy streams generate as they flow downstream

Kinetic energy

500

Soil texture associated with high water content but low plant available water

Clays

500

Location you are most likely to find chemical weathering occurring 

Tropical regions (high temperatures, greater rainfall)

500

The area of deposition on the inside bend of a meandering stream

Point Bar

500

The formula to measure the discharge of a stream

Q = velocity x cross sectional area

500

If stream water appears to be very muddy, what type of sediment does it likely have a lot of

Suspended load

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