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An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation.
Occurrences, Geologic record & Impact on humans
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| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Alluvial fan | is a | accumulation of sediments that fans outwards from a concentrated source of sediments | 0.90 | text |
| Alluvial fan | is a | accumulation of sediments that fans out from a concentrated source of sediments | 0.90 | text |
| cross-bedding | instance of | and sometimes show well-developed sedimentary structures | 0.80 | text |
| Alluvial fan | has impact | Alluvial | 0.60 | section |
| Alluvial fan | has impact | Many | 0.60 | section |
| Alluvial fan | has impact | Los Angeles | 0.60 | section |
| Alluvial fan | has impact | California | 0.60 | section |
| Alluvial fan | has impact | Salt Lake City | 0.60 | section |
| Alluvial fan | has impact | Utah | 0.60 | section |
| Alluvial fan | has impact | Denver | 0.60 | section |
| Alluvial fan | has impact | Colorado | 0.60 | section |
| Alluvial fan | has impact | United States | 0.60 | section |
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