abrasion | The grinding away of rock by friction and impact during transportation.
(See page(s) 401)
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alluvial fan | Large fan-shaped pile of sediment that usually forms where a stream’s velocity decreases as it emerges from a narrow canyon onto a flat plain at the foot of a mountain range.
(See page(s) 412)
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bar | A ridge of sediment, usually sand or gravel, that has been deposited in the middle or along the banks of a stream by a decrease in stream velocity.
(See page(s) 403)
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base level | A theoretical downward limit for stream erosion of Earth’s surface.
(See page(s) 419)
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bed load | Heavy or large sediment particles in a stream that travel near or on the stream bed.
(See page(s) 402)
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braided stream | A stream that flows in a network of many interconnected rivulets around numerous bars.
(See page(s) 406)
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delta | A body of sediment deposited at the mouth of a river when the river velocity decreases as it flows into a standing body of water.
(See page(s) 409)
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dendritic pattern | Drainage pattern of a river and its tributaries, which resembles the branches of a tree or veins in a leaf.
(See page(s) 397)
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discharge | In a stream, the volume of water that flows past a given point in a unit of time.
(See page(s) 400)
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dissolved load | The portion of the total sediment load in a stream that is carried in solution.
(See page(s) 402)
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distributary | Small shifting river channel that carries water away from the main river channel and distributes it over a delta’s surface.
(See page(s) 409)
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divide | Line dividing one drainage basin from another.
(See page(s) 396)
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downcutting | A valley-deepening process caused by erosion of a stream bed.
(See page(s) 419)
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drainage basin | Total area drained by a stream and its tributaries.
(See page(s) 396)
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drainage pattern | The arrangement in map view of a river and its tributaries.
(See page(s) 397)
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flood plain | A broad strip of land built up by sedimentation on either side of a stream channel.
(See page(s) 409)
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graded stream | A single bed with coarse grains at the bottom of the bed and progressively finer grains toward the top of the bed.
(See page(s) 419)
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headward erosion | The lengthening of a valley in an uphill direction above its original source by gullying, mass wasting, and sheet erosion.
(See page(s) 422)
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hydraulic action | The ability of water to pick up and move rock and sediment.
(See page(s) 401)
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hydrologic cycle | The movement of water and water vapor from the sea to the atmosphere, to the land, and back to the sea and atmosphere again.
(See page(s) 395)
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incised meander | A meander that retains its sinuous curves as it cuts vertically downward below the level at which it originally formed.
(See page(s) 424)
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lateral erosion | Erosion and undercutting of stream banks caused by a stream swinging from side to side across its valley floor.
(See page(s) 423)
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meander | A pronounced sinuous curve along a stream’s course.
(See page(s) 407)
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meander cutoff | A new, shorter channel across the narrow neck of a meander.
(See page(s) 407)
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natural levee | Low ridges of flood-deposited sediment formed on either side of a stream channel, which thin away from the channel.
(See page(s) 409)
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oxbow lake | A crescent-shaped lake occupying the abandoned channel of a stream meander that is isolated from the present channel by a meander cutoff and sedimentation.
(See page(s) 409)
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point bar | A stream bar (see definition) deposited on the inside of a curve in the stream, where the water velocity is low.
(See page(s) 407)
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pothole | Depression eroded into the hard rock of a stream bed by the abrasive action of the stream’s sediment load.
(See page(s) 401)
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radial pattern | A drainage pattern in which streams diverge outward like spokes of a wheel.
(See page(s) 397)
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rectangular pattern | A drainage pattern in which tributaries of a river change direction and join one another at right angles.
(See page(s) 397)
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saltation | A mode of transport that carries sediment downcurrent in a series of short leaps or bounces.
(See page(s) 402)
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sheetwash | Water flowing down a slope in a layer.
(See page(s) 396)
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solution | Usually slow but effective process of weathering and erosion in which rocks are dissolved by water.
(See page(s) 401)
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stream | A moving body of water, confined in a channel and running downhill under the influence of gravity.
(See page(s) 395)
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stream channel | A long, narrow depression, shaped and more or less filled by a stream.
(See page(s) 396)
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stream gradient | Downhill slope of a stream’s bed or the water surface, if the stream is very large.
(See page(s) 399)
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stream terrace | Steplike landform found above a stream and its flood plain.
(See page(s) 423)
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stream velocity | The speed at which water in a stream travels.
(See page(s) 398)
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superposed stream | A river let down onto a buried geologic structure by erosion of overlying layers.
(See page(s) 424)
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suspended load | Sediment in a stream that is light enough in weight to remain lifted indefinitely above the bottom by water turbulence.
(See page(s) 402)
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traction | Movement by rolling, sliding, or dragging of sediment fragments along a stream bottom.
(See page(s) 402)
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trellis pattern | A drainage pattern consisting of parallel main streams with short tributaries meeting them at right angles.
(See page(s) 397)
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tributary | a small stream flowing into a larger one.
(See page(s) 396)
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