File:Wiki diagram.jpg
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| 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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I, the copyright holder of this work, hereby publish it under the following license:
This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
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- to share – to copy, distribute and transmit the work
- to remix – to adapt the work
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- attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 08:11, 8 November 2012 | | 640 × 480 (59 KB) | Onavo1 (talk | contribs) | User created page with UploadWizard |
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