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Tectonic stresses and erosion cause granite rock to fracture. Rockfalls later occur along these fractures

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Moraines forms along the sides of a glacier, as the glacier scrapes along, it tears off rock and soil from both sides of its path, this material is deposited as lateral moraines at the top of the glacier's edges.

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Limestone is the chief form of calcium carbonate rock, which is dissolved by water that contains carbon dioxide, forming a calcium bicarbonate solution in underground caverns. If stalagmites – the ceiling formations – grow long enough to connect with stalactites on the floor, they form a column.

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Formed by the gradual removal of slightly soluble bedrock (such as limestone) by percolating water, the collapse of a cave roof, or a lowering of the water table

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The meander stream becomes very curved, and eventually the neck of the meander becomes narrower and the river cuts through the neck during a flood, cutting off the meander and forming an oxbow lake.

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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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Formed by flowing water that streams through the area and clears out all loose objects in their path

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pile of rocks that accumulates at the base of a cliff, chute, or sloped formed by rocks sliding down a side of rock falling into a pile of other broken pieces

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Arches begin their formation as deep cracks which penetrate into a sandstone layer, then Erosion occurring within the cracks wears away exposed rock layers and enlarges the surface cracks isolating narrow sandstone walls which are called fins

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The limestone of the  Pinacles came from seashells in an earlier era that was rich in marine life. These shells were broken down into lime-rich sands that were blown inland to form high mobile dunes

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two weathering processes that continuously work together in eroding the edges of a rock formation known as a fin. The primary weathering force at Bryce Canyon (as one example) is frost wedging. The hoodoos at Bryce Canyon experience over 200 freeze/thaw cycles each year.

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The Great Sand Dunes have been formed over thousands of years, as sand deposited by moutain streams and playa lakes on the San Luis Valley floor is carried in the form of small dunes by predominant southwest winds.