River basins have typical features, these include: Tributary – a smaller river or stream flowing into a larger river. Their rate of sediment delivery is equivalent to an average lowering of the lands by 30 centimetres (12 inches) in 9,000 years, a rate that is sufficient to remove all the existing continental relief in 25,000,000 years. The tributary that started the farthest distance from the river's end would be considered the source, or headwaters.
About one-quarter of all suspended load is estimated to come down the Ganges-Brahmaputra and the Huang He (Yellow River), which together deliver some 4,500,000,000 tons a year; the Yangtze (Chang Jiang), Indus, Amazon, and Mississippi deliver quantities ranging from about 500,000,000 to approximately 350,000,000 tons a year.
Aerial view of the Amazon River in Brazil.
Generally speaking, except in high latitudes and on steep coasts, little or no coarse bed load ever reaches the sea. A stream or river that feeds into a larger watercourse. The wearing away, in this case by water and rocks constantly rubbing.
Arroyo and (dry) wash connote ephemeral streams or their resultant channels. Usually rain water that has a roof into a gutter, or run - off sloping ground into a channel or pond. A drowned river valley in a coastal lowland area. Most rivers flow out into the sea, and this is where they end their journey. A B C D E F G H I J K L M N O P Q R S T U V W X Modern usage includes rivers that are multichanneled, intermittent, or ephemeral in flow and channels that are practically bankless. Materials that are not supposed to be in the river make it dirty. Lakes hold less than 0.5 percent of all fresh water, soil moisture accounts for about 0.05 percent, and water in river channels for roughly half as much, 0.025 percent, which represents only about one four-thousandth of the Earth’s total fresh water. Announcing our NEW encyclopedia for Kids! This often happens on the inside of meanders, because the water is flowing slowly. Cliffs reated by rivers are called river cliffs. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. Rivers carry sediment (fine rock particles) that abrade the banks and bed of the river channel. Rivers always flow downhill because of gravity. A river lays down or drops the sediment or material that it is carrying such as sand, mud, and small stones or sticks. The contribution of direct precipitation on the water surface is usually minute, except where much of a catchment area is occupied by lakes.
The meander continually changes shape as the fast flowing current of water erodes the outside bank of the meander bend and deposition occurs in the slack water of the inside of the bend. The amount of water in river systems at any time is but a tiny fraction of the Earth’s total water; 97 percent of all water is contained in the oceans and about three-quarters of fresh water is stored as land ice; nearly all the remainder occurs as groundwater. The name given to material that has been carried by rivers or the sea and then deposited. Opposite to the currents flow - towards the source of the river. In one sense, such geomorphic features belong to the same series as deltas, estuary fills, and the terrestrial sediments of many inland basins. The concept of channeled surface flow, however, remains central to the definition.
Water is constantly cycled through the systems of land ice, soil, lakes, groundwater (in part), and river channels, however. Below the water table the soil or rock is saturated. The wearing away of particles of rock as they bounce along the riverbed or knock against each other and wear away becoming more rounded. Water that has from something. The Three Gorges Dam spanning the Yangtze River (Chang Jiang) near Yichang, Hubei province, China. A pool at the foot of a small water-fall in a river.
Learn vocabulary, terms, and more with flashcards, games, and other study tools. Mudflats are large area of mud that the tide washes over twice each day. The word stream (derived ultimately from the Indo-European root srou-) emphasizes the fact of flow; as a noun, it is synonymous with river and is often preferred in technical writing. Oxbows are only found on river floodplains. Many rivers, including the Rhone in Western Europe, begin as streams in mountains or hills.
The discharge of rivers to the oceans delivers to these systems the equivalent of the water vapour that is blown overland and then consequently precipitated as rain or snow—i.e., some 7 percent of mean annual precipitation on the globe and 30 percent of precipitation on land areas. Least is known about dissolved load, which at coastal outlets is added to oceanic salt. Gorges are created over thousands of years.
(Silt is tiny material carried by running water).
The force of the water wears away the river bank from underneath. In areas where there is not much rainfall, farmers irrigate the land, by diverting water from rivers to their fields, in channels, ditches or pipes. River water losses result from seepage and percolation into shallow or deep aquifers (permeable rock layers that readily transmit water) and particularly from evaporation.
Rivers are nourished by precipitation, by direct overland runoff, through springs and seepages, or from meltwater at the edges of snowfields and glaciers.
A general term for all forms of water particles  rain, snow, sleet, dew, hail etc. This process causes attrition, and adds to the silt and sediment in the river.
A valley is a long trough in the landscape that has been eroded by a river or a combination of river and glacier action. A bend in a river - usually in the middle or lower course.
High ground that surrounds a drainage basin. The effect is much the same as using sandpaper. A cliff is any steep slope that has been formed by natural processes. The pool is deep because the water plunging into it has eroded the river bed. are formed when the river flows over a relatively tough band of rock overlying less resistant rock. Well over half of suspended load is deposited at river mouths as deltaic and estuarine sediment. This article concentrates on the distribution, drainage patterns, and geometry of river systems; its coverage of the latter includes a discussion of channel patterns and such related features as waterfalls.
Our editors will review what you’ve submitted and determine whether to revise the article. What is a river basin? The supply of water to farmland so that crops can grow in areas wherewater supplies are scarce or unreliable.
See more. the shape of the channel and how rough the bed and banks are are.... model that shows how rivers change as they go downstream, velocity and discharge are highest at these stages, velocity and discharge are lowest at these stages due to friction so loss of energy, shows the shape of the channel and the valley, an area from which water drains into a particular drainage basin, small circular depressions in the river carved out of solid rock, these are formed when rock fragments drill into holes and cavities by turbulent whisking actions of the river, causing holes to form in the rock below.
Considerable attention is also given to fluvial landforms and to the processes involved in their formation. A river is a naturally winding watercourse that drains surplus water from a drainage basin.
The area of land that is drained by a river and its tributaries. The river cuts this deep valley by erosion.
River . Rates of erosion and transportation, and comparative amounts of solid and dissolved load, vary widely from river to river. A fjord is a deep, narrow flooded inlet of the sea that was formed during the last Ice Age. The rivers of Tennessee drain directly into the Pacific Ocean. River basin definition, the area of land drained by a river and its branches. Tiny streams or channels are referred to as rills or runnels. Rapids are fast-flowing stretches of water formed where the river surface breaks up into waves because rocks are near to the surface.
A ridge of land that extends partly across a valley.
A fan-shaped area of sediment built up at the mouth of a river.
0.001, 0.01, 0.1, 1.0, 10, 100 (Hjulstrom Curve), a graph that shows the rivers gradient from the source to the mouth, lowest point the river can erode to (long profile graph), this is influenced by the gradiet, the discharge and the channel characteristics, cross sectional area of river / wetter perimeter, the part of the bed/bank touched by water.
A large area of nearly flat land which does not have any significant hills. Occurs near or at the mouth of a river, where the tide meets the current and the fresh and salt waters mix. A place for vessels to load and unload cargo or to be repaired. Omissions? Y Z. Abrasion is a form of erosion caused by rubbing of fine particles against an object. Water that has from something. Get exclusive access to content from our 1768 First Edition with your subscription.
A river is a flowing, moving stream of water. Please select which sections you would like to print: Corrections? The boundary of a river basin. The trenches in which rivers flow for most of the year.
For information concerning the plant and animal forms that inhabit the riverine environment, see inland water ecosystem. The riverbed is the ground at the bottom of the river - often made up of sand and stones. A barrier forming a temporary dam that may be erected quickly or permanently alongside a river to protect a flood-prone area.
Sediment may be called alluvium if it deposited on the bed or a river, it may be called a beach when deposited by waves.
where the river flows over a varitey of different rock types which erode at different times, and often erode into irregular shapes. Cliffs are formed when rivers cut swiftly into the land. The place where a ship or boat is docked (or tied up). A small arc-shaped lake formed when a meander is sealed off by deposition. The amount of water flowing in a river per second. The water table is the natural level of water in a soil or rock. Rivers often get their water from many tributaries, or smaller streams, that join together.
The place where a river begins is called its source.River sources are also called headwaters. River Keywords and definitions.
The name for any material deposited by a river. Start studying geography river definitions. The Rio Grande flowing through the desert at the foot of the Chisos Mountains in Big Bend National Park, Texas. A gorge is a steep-sided river valley which is very narrow and deep. Its concentration in tropical rivers is not necessarily high, although very high discharges can move large amounts; the dissolved load of the lowermost Amazon averages about 40 parts per million, whereas the Elbe and the Rio Grande, by contrast, average more than 800 parts per million. Extraordinarily high rates have been recorded for some lesser rivers: for instance, 1,060 tons per square kilometre per year on the Jing and 1,080 tons per square kilometre per year on the Luo, both of which are Loess Plateau tributaries of the Huang He. Flooding happens when a river has too much water in its channel. Rock debris enters fluvial systems either as fragments eroded from rocky channels or in dissolved form.
Small natural watercourses are sometimes called rivulets, but a variety of names—including branch, brook, burn, and creek—are more common, occurring regionally to nationally in place-names. Usually rain water that has a roof into a gutter, or run - off sloping ground into a channel or pond. The boundary of a river basin is called the watershed. Find out more with Bitesize KS2 Geography. The direction that the river flows, towards the mouth of the river. A reservoir is an artificial lake created by building a dam across a river. Senior Editor, Earth Sciences. Additional information about the action of flowing water on Earth’s surface is provided in the article valley. A river is a naturally winding watercourse that drains surplus water from a drainage basin. Kids learn about world rivers. The floodplain is usually found in the lower course of a river. Runoff .
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