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The rocks, soils, sand, regoith move down slope. It’s effected by water being constant
Mudflows topples falls each with different characteristics
With the slopes

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Gypsum overlain. The weakest stops are where gypsum form

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Formed by erosion of limestone in solutions

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Steep and unstable

Water is flowing at a higher pressure when the fastest and deeper

Weathering

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U shaped bend

When the bend gets large enough it will cut off to its own body off water and forms the oxbow lakes

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1. Curved shape

2. Resembles a part of a oxbow

3. Also known as billabong

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When a meander stream is cut off, its creating its own body of water

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Creeps

Landslides

Flows

Slump

Falls

Mudslides

Water can decrease or increase the depth of the slope

These can be thick

There has to be enough water but not to little and not to much for it not to cause these events

Triggers

Earthquakes

Increases soil moisture

Reduction of roots holding the soil to bedrock

Weathering

Bioturbation

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Horns

Arêtes

Cirques

Glacial troughs

Hanging valleys

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Point bar and a cut bank within the curves

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Produced by a stream or river as it erodes the sediment is press into one another making a outer layer

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Stream

River swinging from side to side

Floods acrossed  the flood plane

Moves with the valley

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Curves

Benda

Loops

Turns

Windings

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Down cut

Landslides

Rockfalls

These make the valley wider

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Ice and water

Forces of gravity

Some hang most are hollow

Water winds come toward the sea it can create a natural twist in the land to make different valley types

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Shaped like a v or u

Steepnessof the side

Mountain valleys

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When debris is added to the slope it increases the slope or angle

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Ice within the mountains

The temperature has to drop to a certain point for this to happen

The water Can freeze and expand

These can happen during the spring and fall

When the ice melts the water will be free

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Physical and chemical weathering causes a talus slope

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Mountain cliffs

Volcano

Valley shoulders

Landforms are called talus deposits

Upwards form to it

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Also known as a Scree

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Creeps

Slides

Flows

Topples

Falls

Happens over time

Downslope

Gravity

Effected by water

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Ice sheets and different layers of rocks and minerals

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Compaction and recrystallization

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Continental glaciers two. These have sandstone layers

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Down hill from gravity. Formed by wind and water. Moraines

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Forms by water and frost wedging. Contains sandstones, limestones or basalt.

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There often replaced with v shaped caverns

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Hoodoos don’t last that long

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Starts with high plateaus to finning then the window last hoodoos

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Creeps down slope. Grain flows is with dry material with sand dunes on a steep slope.

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Wind blown sand dunes above the glacial moraines

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The dripzone  is where the limestone dissolves and drips down and it will create peeks that form above and below the cave underground

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The cave contains limestone the water makes it dissolve and can make a drip stone

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In limestone caves they’re stalactites that form from calcium and other minerals.