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Oxbow lake – U-shaped lake or pool left by an ancient river meander; Panhole – Depression or basin eroded into flat or gently sloping cohesive rock; Pothole – Natural bowl-shaped hollow carved into a streambed; Plunge pool – Depression at the base of a waterfall; Pond – Relatively small body of standing water
The most common type of fluvial lake is a crescent-shaped lake called an oxbow lake due to the distinctive curved shape. They can form in river valleys as a result of meandering. The slow-moving river forms a sinuous shape as the outer side of bends are eroded away more rapidly than the inner side.
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 ...
Terrain – Dimension and shape of land surfaces; Geomorphologist – Person who studies landforms; Geomorphosite – Landform of scientific or social value; Beach erosion and accretion – Area of loose particles at the edge of the sea or other body of water Beach evolution – Changes to a shoreline by accretion and erosion
Oxbow lake: a U-shaped lake formed when a wide meander from the mainstem of a river is cut off to create a lake. Phytotelma: a small, discrete body of water held by some plants. Plunge pool: a depression at the base of a waterfall. Pool: various small bodies of water such as a swimming pool, reflecting pool, pond, or puddle. Pond
An oxbow lake is a U-shaped lake or pool that forms when a wide meander of a river is cut off, creating a free-standing body of water. The word "oxbow" can also refer to a U-shaped bend in a river or stream, whether or not it is cut off from the main stream. [1] [2] It takes its name from an oxbow which is part of a harness for oxen to pull a ...
Flat-lying duricrusts and volcanic rocks also form the caprock of various tablelands. In case of duricrusts, e.g. laterite or silcrete , the formation of tablelands involves a three-stage process. First, the formation of a thick indurated surface layer duricrust by deep weathering beneath a relatively flat surface.
The village of Santarfa in Ethiopia is established on a structural flat along a 1000-metre-high escarpment. A flat is a relatively level surface of land within a region of greater relief, such as hills or mountains, usually used in the plural.