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Creeps are downslope movement of particles on slopes that are covered in loose sediment, and is caused by many different types of weathering such as frost wedging and tree roots.  A landslide is when rocks and other particles are moving down a slope from abrasions.  Flows are formed by water and materials flowing down using abrasions, that causes destruction to the land in which it happened.  Slumps are formed by exfoliation that makes a part of the rock slide down the rock which creates a stair like look.  A fall is formed from abrasions and exfoliation that cause the fall to happen, in which causes a lot of destruction to the land

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An arete is a ridge between two valleys, which is caused by frost wedging, as well as abrasions, after two glaciers erode parallel valleys.  A horn is formed by a glacier erodes three or more aretes, which is formed by frost wedging, as well as effect from the glacier.   An U-shaped valley is formed by a glacier moving slowly, and creating this valley through its destructive path with the frost wedging and then melting, leaving the valley with steep sides behind.  A cirque is formed by frost wedging that then creates a semi circle valley, and is formed through frost wedging as well as abrasions that create the steep hills from the glacier. Hanging valleys are formed when two glaciers merge of different sizes, which creates the hanging valley that abruptly cuts off. A moraine is the leftover materials from when the glacier melts that uses abrasions to create new land forms.

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Caverns are formed by hydrolysis and dissolution that make the caverns into how they look, so its eroding the land to have a hole in it. Stalagmites and stalactites are formed by hydrolysis.  The water in the cavern by dissolving the calcites in the roof of that cave, then drips to make the stalactites.  The stalagmites are formed by the water from the stalactites on the ceiling piling up on the ground, and growing as more water drips.

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A sinkhole is formed by hydrolysis, which is a gradual process that uses water to break done the limestone, and the water is then displaced. After this happens to the water, underground spaces develop, and once they become too big, the ground above collapses, which creates the sinkholes.

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An Ox - Bow lake is formed by the result of a meandering stream's erosion on the bends of the stream.  When the abrasion process continues on until it has become bigger and bigger until the loops are much too big and consume too much energy, the stream finds a new path that doesn't take too much energy. After the stream stops connecting to the now lake, it forms an ox - bow lake.

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A meandering stream is formed by abrasions by creating a river that occurs in the middle or lower course. These rivers are rivers that curve, and at those curves, the river moves the fastest, which breaks done the sediments on the banks, to make the river bigger as time goes on

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A V-shaped valley is formed by frost wedging, because it is from the freeze thaw cycles that cause the valley to take the shape of a V. Also, another contributing factor of creating this are abrasions, which breaks done rock on the side of the valley to also form the sides and the dent in the middle.

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A talus slope is formed by exfoliation because it is the accumulation of the rocks at the bottom of a cliff after the layers have peeled off of that same cliff. At the bottom of the cliff, you can see all the rocks that have come off accumulated at an angle, which is where the term slope comes from.

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An arch is formed by hydrolysis, after the rocks have raised from a lower sea level, then after some erosion forces take place, the water comes in and breaks down the rocks in the middle, which creates the arch. The water mostly creates the arches by breaking off parts of the sandstone in the center.

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A pinnacle is formed by tree roots, abrasions, and hydrolysis. The plants roots make the cracks in the rock expand, which then allows the water to then get into those cracks to break down the rock even more that dissolves the sandstone a little at time. Then, the abrasions then formed the pinnacles even more to make them look like they do today.

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A hoodoo is formed by two types of weathering.  They are created by frost wedging, as well as rain also shape the Hoodoo's.  They can be ranged from 5 to 150 feet tall, depending on how much weathering has occurred.  The frost wedging broke off parts of a rock by expanding the cracks. The rain (hydrolysis) slowly dissolves the sandstone, which makes the hoodoo look more bumpy and deformed.

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Sand dunes are formed by abrasions from the winds, which broke done the rocks.  The wind blowing the rock particles forced them to rub together, which then broke done the rocks to form smaller sand particles.  The wind then carried those rocks to the location where they are now which formed the sand dunes, and the more rock that is deposited, the bigger the sand dune becomes.