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A floodplain or flood plain is an area of land adjacent to a stream or river which stretches from the banks of its channel to the base of the enclosing valley walls and which experiences flooding during periods of high discharge.

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A horn results when glaciers erode three or more arêtes, usually forming a sharp-edged peak. Cirques are concave, circular basins carved by the base of a glacier as it erodes the landscape. the rubble from the creation will deposit down to the base of the mountain and weathering will smoothen out the sharp edges. An arête is a thin, crest of rock left after two adjacent glaciers have worn a steep ridge into the rock.The top if the mountain is the horn.

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Both are pointy formations also found in limestone caves. A Stalactite is like an icicle which hangs from the ceiling and a Stalagmite is like a ground icicle which is on the ground and points up.

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Transport of sediment across riverine flood plains contributes a significant but poorly constrained fraction of the total chemical weathering fluxes from rapidly eroding mountain belts which has important implications for chemical fluxes to the oceans and the impact of orogens on long term climate.

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A kettle is a shallow, sediment-filled body of water formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of ice calving from glaciers and becoming submerged in the sediment on the outwash plain

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They are formed by chemical weathering.First the water dissolves then the calcite's in the rock of a cave roof and the calcite is deposited as a strange structure below

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Stalagmites form as calcium carbonate then water drips from the ceiling of a cave which form icicle looking rocks

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Floodplains are made by a meander eroding sideways as it travels downstream. When a river breaks its banks, it leaves behind layers of alluvium silt. These gradually build up to create the floor of the plain.

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Same thing goes to erosion

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An erosional floodplain is created as a stream cuts deeper into its channel and laterally into its banks.

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Kettles are depressions left behind after partially-buried ice blocks melt. Many are filled with water.

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A kettle lake occurs where a chunk of ice was left behind in the till of a retreating glacier.