File:Wiki diagram.jpg
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Summary
| Description |
English: The development of an alluvial fan is a result of the amount of tectonic activity present. If there is more tectonic activity than about of sediment being deposited, then the alluvial fan forms closer to the mountain range. If there is little to no tectonic activity present, the alluvial fan forms in a more horizontal manner. |
| Date | |
| Source | Own work |
| Author | Onavo1 |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 08:11, 8 November 2012 | | 640 × 480 (59 KB) | Onavo1 | User created page with UploadWizard |
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