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External Forces Shaping the Earth
External Forces Shaping the Earth

... For erosion to occur, a transporting agent, such as water or wind must be present. When a river enters the ocean, the sediment is deposited in a fan like landform called a delta. ...
Guided Notes on Erosion and Deposition—Section 7
Guided Notes on Erosion and Deposition—Section 7

... dropped in one location. 3. Gravity influences the erosional and depositional process because it causes materials to move downslope or down stream. When gravity stops acting on weathered materials, they become deposited. 4. There are 4 major agents of erosion: (1) Glaciers (2) Wind (3) Running water ...
Document
Document

... – slip circle failures in moderately thick soil layers, – plane failures in rock slopes, – wedge failures in rock slopes, – undercutting (erosion) of embankments and talus slopes, – hillcreep on steep slopes, and in addition, – significant erosion gulleys occurred along some of the preferential drai ...
Weathering, Erosion, Deposition: Effects on the Texas
Weathering, Erosion, Deposition: Effects on the Texas

... Which station models this erosion of the limestone cliffs? ...
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Determining Top or Crown of a Bank

... If a landowner disagrees with an SWCD delineation of the top of bank for a public water, it may be necessary for the SWCD to review surveyed cross sections of the bank and buffer strip area along the public water in the area of disagreement to verify or clarify the top of bank location. Surveyed cro ...
Erosion is the process by which the surface of the Earth gets worn
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page 39 - Egypt Vocabulary - 6
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... Definition Powerful Egyptian Pharaoh from the New Kingdom period area formed by soil deposits at the mouth of a river name for a powerful ruler line of rulers from a single family that holds power for a long time A major river system in northeastern Africa that is considered the longest single river ...
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River bank failure



River bank failure can be caused when the gravitational forces acting on a bank exceed the forces which hold the sediment together. Failure depends on sediment type, layering, and moisture content.All river banks experience erosion, but failure is dependent on the location and the rate at which erosion is occurring.River bank failure may be caused by house placement, water saturation, weight on the river bank, vegetation, and/or tectonic activity. When structures are built too close to the bank of the river, their weight may exceed the weight which the bank can hold and cause slumping, or accelerate slumping that may already be active. Adding to these stresses can be increased saturation caused by irrigation and septics, which reduce the soil’s strength. While deep rooted vegetation can increase the strength of river banks, replacement with grass and shallower rooted vegetation can actually weaken the soil. Presence of lawns and concrete driveways concentrates runoff onto the riverbank, weakening it further. Foundations and structures further increase stress. Although each mode of failure is clearly defined, investigation into soil types, bank composition, and environment must be clearly defined in order to establish the mode of failure, of which multiple types may be present on the same area at different times. Once failure has been classified, steps may be taken in order to prevent further erosion. If tectonic failure is at fault, research into its effects may aid in the understanding of alluvial systems and their responses to different stresses.
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