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A landform is a feature on the solid surface of the Earth or other . They may be natural or may be anthropogenic

(2025). 9789048130573 .
(2025). 9783319543314, Springer International Publishing.
(caused or influenced by human activity). Landforms together make up a given , and their arrangement in the is known as . Landforms include , , , and , as well as features such as , , and , including submerged features such as , , and the great .


Physical characteristics
Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure , rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as , , , , , , , , , and numerous other structural and size-scaled (e.g. vs. , vs. ) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Hills, mountains, , and are the four major types of landforms on Earth. Minor landforms include basins, , canyons, and valleys. Tectonic plate movements under Earth's crust can create landforms by pushing up hills and mountains.


Hierarchy of classes
+ Landforms by order
and
, , , and
, , , , and etc.

and exemplify the highest-order landforms. Landform elements are parts of a high-order landforms that can be further identified and systematically given a cohesive definition such as hill-tops, shoulders, saddles, foreslopes and backslopes.

Some generic landform elements including: pits, peaks, channels, ridges, passes, pools and plains.

(or relief) is the third or vertical dimension of land surface. is the study of terrain, although the word is often used as a synonym for relief itself. When relief is described , the term is used. In , many different techniques are used to describe relief, including and triangulated irregular networks.

Elementary landforms (segments, facets, relief units) are the smallest homogeneous divisions of the land surface, at the given scale/resolution. These are areas with relatively homogeneous properties, bounded by lines of discontinuity. A plateau or a hill can be observed at various scales, ranging from a few hundred meters to hundreds of kilometers. Hence, the spatial distribution of landforms is often scale-dependent, as is the case for soils and geological strata. A number of factors, ranging from to and deposition (also due to human activity), can generate and affect landforms. factors can also influence landforms—for example, note the role of in the development of systems and , and the work of and in the formation of .

Landforms do not include several man-made features, such as , and many ; and geographic features, such as , , and . Many of the terms are not restricted to refer to features of the planet , and can be used to describe surface features of other planets and similar objects in the . 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 .

In terminology, (geographical proper names) of individual landform objects (mountains, hills, valleys, etc.) are called .


Recent developments
Landforms may be extracted from a digital elevation model (DEM) using some automated techniques where the data has been gathered by modern satellites and aerial surveillance cameras. Until recently, compiling the data found in such data sets required time consuming and expensive techniques involving many man-hours. The most detailed DEMs available are measured directly using techniques.


See also
  • , to prevent coastal erosion and creation of beach
    • (CERF)


Sources


Further reading
  • Hargitai et al. (2015). " Classification and Characterization of Planetary Landforms". In: Hargitai H. (ed.). Encyclopedia of Planetary Landforms. Springer. DOI 10.1007/978-1-4614-3134-3
  • Page D. (2015). "The Geology of Planetary Landforms". In: Hargitai H. (ed.). Encyclopedia of Planetary Landforms. Springer.


External links

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