Fluvial landforms of streams

Fluvial landforms of streams


The fluvial landforms of streams, stream beds, and river valleys have various landforms.

Classification

There are five generic classifications:
  • Consequent streams are streams whose course is a direct consequence of the original slope of the surface[1][2] upon which it developed, i.e., streams that follow slope of the land over which they originally formed.
  • Subsequent streams are streams whose course has been determined by selective headward erosion along weak strata. These streams have generally developed after the original stream. Subsequent streams developed independently of the original relief of the land and generally follow paths determined by the weak rock belts.[3]
  • Resequent streams are streams whose course follows the original relief, but at a lower level than the original slope (e.g., flows down a course determined by the underlying strata in the same direction). These streams develop later and are generally a tributary to a subsequent stream.
  • Obsequent streams are streams flowing in the opposite direction of the consequent drainage.
  • Insequent streams have an almost random drainage often forming dendritic patterns. These are typically tributaries and have developed by a headward erosion on a horizontally stratified belt or on homogeneous rocks. These streams follow courses that apparently were not controlled by the original slope of the surface, its structure or the type of rock.

See also

References

  • Marie Morisawa, "Classification of Rivers," in Rhodes W. Fairbridge (ed.), The Encyclopedia of Geomorphology, New York: Reinhold Book Corporation, 1968, pp. 956–957.
  1. ^ "consequent stream - Definitions from Dictionary.com". Dictionary.com. http://dictionary.reference.com/browse/consequent%20stream. Retrieved 2008-04-24. 
  2. ^ "Stream Erosion and Landscape Development". Water: Science and Issues. http://www.waterencyclopedia.com/St-Ts/Stream-Erosion-and-Landscape-Development.html. Retrieved 2008-04-24. 
  3. ^ "Stream Erosion and Landscape Development". Water: Science and Issues. http://www.waterencyclopedia.com/St-Ts/Stream-Erosion-and-Landscape-Development.html. Retrieved 2008-04-24. 

Wikimedia Foundation. 2010.

Игры ⚽ Нужен реферат?

Look at other dictionaries:

  • Fluvial — is used in geography and earth science to refer to the deposits and landforms created by the action of rivers or streams and the processes associated with them. When the stream or rivers are associated with glaciers, ice sheets, or ice caps, the… …   Wikipedia

  • Geomorphology — (from Greek: γη, ge , earth ; μορφή, morfé , form ; and λόγος, logos , knowledge ) is the study of landforms and the processes that shape them. Geomorphologists seek to understand why landscapes look the way they do: to understand landform… …   Wikipedia

  • Headward erosion — is a fluvial process of erosion that lengthens a stream, a valley or a gully at its head and also enlarges its drainage basin. The stream erodes away at the rock and soil at its headwaters in the opposite direction that it flows. Once a stream… …   Wikipedia

  • Debouch — The port and city are the southern terminus of the Suez Canal that transits through Egypt and debouches into the Mediterranean Sea near Port Said. Debouch is a term used in river and stream geography, and the military. Contents 1 G …   Wikipedia

  • River delta — Nile River delta, as seen from Earth orbit. The Nile is an example of a wave dominated delta that has the classic Greek delta (Δ) shape after which river deltas were named. A delta is a landform that is formed at the mouth of a river where that… …   Wikipedia

  • Channel (geography) — This article is about a geographical feature. For other uses, see channel. Wooden pilings mark the navigable channel for vessels entering Lake George from the St. Johns River in Florida …   Wikipedia

  • Degradation (geology) — In geology, degradation refers to the lowering of a fluvial surface, such as a stream bed or floodplain, through erosional processes.[1][2] It is the opposite of aggradation. Degradation is characteristic of channel networks in which either… …   Wikipedia

  • Mouth bar — A mouth bar is a bar in a river that is typically created in the middle of a channel in a river delta.[1] It is created by a positive feedback between mid channel deposition and flow divergence. As the flow diverges near the ocean, sediment… …   Wikipedia

  • Behavioral modeling in hydrology — In hydrology, behavioral modeling is a modeling approach that focuses on the modeling of the behavior of hydrological systems.The behavioral modeling approach makes the main assumption that every system, given its environment, has a most probable …   Wikipedia

  • alluvial plain —     a) A large assemblage of fluvial landforms (braided streams, terraces, etc.,) that form low gradient, regional ramps along the flanks of mountains and extend great distances from their sources (e.g., High Plains of North America.    SW.… …   Glossary of landform and geologic terms

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”