Weathering

A hollow, produced by localized weathering on a steep face.

Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering (subaerial processes).

Bryce is distinctive due to geological structures called hoodoos, formed by frost weathering and stream erosion of the river and lake bed sedimentary rock.

The canyon features many formations formed by the weathering of sedimentary rock.

The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes.

The initial step in the development of Hyden Rock was the subsurface alteration by weathering of granite bedrock beneath a lateritised land surface during the Cretaceous Period between 100 and 130 million years ago.

Clay-sized hematite crystals also may occur as a secondary mineral formed by weathering processes in soil

Malachite often results from the supergene weathering and oxidation of primary sulfidic copper ores and is often found with azurite (Cu3(CO3)2(OH)2), goethite, and calcite.

A panhole or weathering pit is a depression or basin eroded into flat or gently sloping cohesive rock

Honeycomb weathering, also known as honeycombs, honeycombed sandstone, is a form of cavernous weathering that consists of regular, tightly adjoining, and commonly patterned cavities that are developed in weathered bedrock; are less than 2 cm (0.79 in) in size; and resemble a honeycombed structure

An etchplain is a plain where the bedrock has been subject to considerable "etching" or subsurface weathering

Cliffs are formed by the processes of weathering and erosion, with the effect of gravity.

Caves often form by the weathering of rock and can extend deep underground.

The blocks derive from disintegrated and weathered bedrock layers.

They are of a tumulus form of weathered granite outcrop.

They are believed to be formed by frost weathering below the surface.

Flared slopes form due to various weathering patterns that are more effective at the regolith or soil-covered base of rock walls.

Differential weathering produced the mountain/valley pattern within the Appalachian Ridge and Valley province to which Fort Valley, the Massanutten range and the adjacent Shenandoah and Page Valleys of Virginia belong.