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Dale – Low area between hills, often with a river running through it; Defile – Narrow pass or gorge between mountains or hills; Dell – Small secluded hollow; Doab, also known as Interfluve – Land between two converging, or confluent, rivers; Draw – Terrain feature formed by two parallel ridges or spurs with low ground in between
These classifications overlap with the geological definitions of "upland" and "lowland". In geology an "upland" is generally considered to be land that is at a higher elevation than the alluvial plain or stream terrace, which are considered to be "lowlands". The term "bottomland" refers to low-lying alluvial land near a river.
Also amphidrome and tidal node. A geographical location where there is little or no tide, i.e. where the tidal amplitude is zero or nearly zero because the height of sea level does not change appreciably over time (meaning there is no high tide or low tide), and around which a tidal crest circulates once per tidal period (approximately every 12 hours). Tidal amplitude increases, though not ...
The Low Countries as seen from NASA space satellite. The Low Countries (Dutch: de Lage Landen; French: les Pays-Bas), historically also known as the Netherlands (Dutch: de Nederlanden), is a coastal lowland region in Northwestern Europe forming the lower basin of the Rhine–Meuse–Scheldt delta and consisting today of the three modern "Benelux" countries: Belgium, Luxembourg, and the ...
A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear depression may subsequently be further deepened by the forces of erosion.
Hollow: A term used regionally for a small valley surrounded by mountains or ridges. In Ireland, New England, Appalachia, and the Ozarks of Arkansas and Missouri, a hollow is a small valley or dry stream bed; often called a holler. Longitudinal valley: An elongated valley found between two nearly-parallel mountain chains.
About 60 km (35 miles) long in north–south direction and only 13 km (8 miles) wide, it is subdivided into two parts: the western "Low Shephelah", which starts at an altitude of ca. 150 metres above sea level and rises to no more than ca. 200 metres above the Coastal Plain, and the eastern "High Shephelah" rising to altitudes between 250 and ...
Satoyama is a Japanese term applied to the border zone or area between mountain foothills and arable flat land. Literally, sato means village, and yama means hill or mountain. Satoyama have been developed through centuries of small-scale agricultural and forestry use. The concept of satoyama has several definitions.