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Alluvial plain

An alluvial plain is a plain (an essentially flat landform) created by the deposition of sediment over a long period by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular time. In contrast, the alluvial plain is the larger…

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Alluvial plains by continent

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Alluvial plains by continent

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Alluvial plain

Nodes95
Edges94
Triples11
Avg. degree1.98
Density0.021053
Components1

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Alluvial plain

Top relations

related to North America · 9
Alluvial plain → California, Costa Rica, Laguna, San Jose, Santa Rosa, United StatesMississippi Alluvial Plain, United StatesOxnard Plain, United StatesSanta Clara Valley, United StatesTempisque River Plain
is a · 2
Alluvial plain → larger area representing the region over which the floodplains have shifted over geological time.As the highlands erode due to weathering and water flow, plain

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Important terminology

alluvial plain plains flood time water floodplain lower river new delta north landform sediment rivers soil area larger region flow

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Alluvial plainis aplain0.90text
Alluvial plainis alarger area representing the region over which the floodplains have shifted over geological time.As the highlands erode due to weathering and water flow0.90text
Alluvial plainrelated to North AmericaLaguna0.60section
Alluvial plainrelated to North AmericaSanta Rosa0.60section
Alluvial plainrelated to North AmericaUnited StatesMississippi Alluvial Plain0.60section
Alluvial plainrelated to North AmericaUnited StatesOxnard Plain0.60section
Alluvial plainrelated to North AmericaUnited StatesSanta Clara Valley0.60section
Alluvial plainrelated to North AmericaSan Jose0.60section
Alluvial plainrelated to North AmericaCalifornia0.60section
Alluvial plainrelated to North AmericaUnited StatesTempisque River Plain0.60section
Alluvial plainrelated to North AmericaCosta Rica0.60section

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