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Falls- The dense, erosion resistant metamorphic rock that makes up the fall line.

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Creeps- The movement of a slope by stretching outwards, this cause avalanches and moves all tree roots up, masses out, and hills sloped at an angle.

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Slumps- A form of mass wasting that occurs when a coherent mass of loosely consolidated materials or rock layers moves a short distance down a slope. Movement is characterized by sliding along a concave-upward on a planar surface.

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Flows- Debris flows are geological phenomena in which water-laden masses of soil and fragmented rock rush down mountainsides, funnel into stream channels, entrain objects in their paths, and form thick, muddy deposits on valley floors.

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Landslides- Movement occur when gravitational and other types of shear stresses within a slope exceed the shear strength of the materials that form the slope.

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Moraines- A medial moraine consists of a long, narrow line or zone of debris formed when lateral moraines join at the intersection of two ice streams.

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Hanging Valley- Such valleys generally form when glacier ice deeply erodes a main or trunk valley, leaving tributary valleys literally hanging far above the main valley floor.

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Cirque-Exposed rock walls and separates the stationary from the moving ice; in early summer it opens, exposing the rock at its base to diurnal changes of temperature. Frost action then causes rapid disintegration of lower rock, which causes the upper rock to avalanche and produce an almost vertical head wall. Resulting rock material is embedded in the glacier and scours a concave floor. This forms a cirque.

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U-Shaped Valley- A glaciated valley that has a u shape, formed by a glacier with less angles and more curvature that run through a mountain range, erode the rocks down and eventually melts or moves away.

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Horn- Horn, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Formed by glaciers concentrating at one point or two tectonic plates that collide and the top is a horn.

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Arête- It is typically formed when two glaciers erode parallel U-shaped valleys. Also can be formed by when glaciers head on towards each other.

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Pillar- A column is simply a stalagmite and a stalagmite that have grown enough to meet in the middle.

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Stalagmites-  They form through deposition of calcium carbonate and other minerals, which is precipitated from mineralized water solutions. Also, just simply stated, it is the accumulation of certain materials on a surface.

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Stalactites- Any meltable material, or a material that can turn into liquid, drops from a ceiling or roof and forms a stalactites.

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Sinkhole- Sediments spall into an underground cavity, spalling continues and cohesively sediments form an arch, the cavity migrates upwards and forms a roof, and the cavity breaches the surface and cause a dramatic and sudden sinkhole.

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Ox-Bow Lake- Erosion narrows the neck of a river, during a period of flooding, water takes the shortest way and that forms a straighter route. Later, the area that was part of the original river gets cut off and forms an ox-bow lake.

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Meandering Stream- A meandering stream forms when moving water in a stream erodes the outer banks and widens its valley, and the inner part of the river has less energy and deposits silt.

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V-Shaped Valley- A river erodes away some part of a location, then the upper area of the valley break apart and get carried away by other erosion forces and leaves a V.

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Talus Slope- Rocks that accumulate on the side of a cliff and some of these rocks are here from storm winds and regular winds, like sand dunes except not grains, genuine rocks.

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Arch- Abrasion is the main cause of worldwide arches. Although, the arches in Arches National Park are formed because they are on top of a salt bed, or evaporite layer.

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Pinnacles- Seashells from past marine lives breakdown get blown inland, and form highly mobile dunes. They can also be formed off vents from volcanoes.

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Hoodoo- The rock’s resistance to erosion cause hoodoos. Frost wedging also breaks apart the rocks even more and cause huge gaps in between rocks.

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Sand Dunes- The Sand Dunes are caused by storm winds, winds that breeze west to east. The grains accumulate, in the picture below's situation because of the mountains.