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Summary
| Description |
Orogenic collapse can occur under different circumstances. If the tectonic forces which thickened the crust are still active, then it is considered a fixed-boundary collapse, where the brittle upper crust breaks down. If the tectonic forces have been released, then it is considered a free-boundary collapse, where the upper and lower crust extend together. |
| Date | |
| Source | Own work |
| Author | CrunchyRocks |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 05:37, 29 January 2022 | | 800 × 600 (19 KB) | CrunchyRocks | Misaligned arrow |
| 04:17, 29 January 2022 |  | 800 × 600 (19 KB) | CrunchyRocks | Uploaded own work with UploadWizard |
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