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Examples are mountains, hills, polar caps, and valleys, which are found on all of the terrestrial planets. The scientific study of landforms is known as geomorphology. In onomastic terminology, toponyms (geographical proper names) of individual landform objects (mountains, hills, valleys, etc.) are called oronyms. [4]
Gully – Landform created by running water and/or mass movement eroding sharply into soil; Guyot – Isolated, flat-topped underwater volcano mountain; Hanging valley – A tributary valley that meets the main valley above the valley floor; Headland – Landform extending into a body of water, often with significant height and drop
Fluvial landforms of streams; Fluvial terrace – Elongated terraces that flank the sides of floodplains and river valleys; Canyon – Deep chasm between cliffs (Gorge) Gully – Landform created by running water and/or mass movement eroding sharply into soil; Island – Piece of subcontinental land completely surrounded by water
Some geomorphic examples of fluvial landforms are alluvial fans, oxbow lakes, and fluvial terraces. Glacial processes. Features of a glacial landscape.
This category includes articles on specific landforms on all planets and similar objects. Landforms do not include geographic features, such as deserts, forests, grasslands, and impact craters. (For those, see Category:Geomorphology.) Compare to Category:Bodies of water and Category:Wetlands
The United States contains varied landforms across its territory. These include: List of beaches in the United States; List of fjords of the United States; List of glaciers in the United States; List of islands of the United States; List of lakes of the United States; List of rivers of the United States
As in the case of landforms in general, there is a lack of any commonly agreed classification or typology of ridges. They can be defined and classified on the basis of a variety of factors including either genesis, morphology, composition, statistical analysis of remote sensing data, or some combinations of these factors.
Examples of Depositional Landforms; Landform Description Image Dunes: A dune is a large pile of wind-blown material, typically sand or snow. As the pile accumulates, its larger surface area increases the rate of deposition in a positive feedback loop until the dune collapses under its own weight.