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Summary
| Description |
English: In structural geology, a syncline is a fold with younger rock layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. Illustrated are a folded sequence of rock layers, being old at the bottom and young at the top forming a syncline and two anticlines with corresponding axes (or here rather axial planes) marking their centers. |
| Date | |
| Source | Own work |
| Author | Fabio Crameri |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 08:36, 6 October 2023 | | 2,616 × 949 (1.71 MB) | FCrameri | Uploaded own work with UploadWizard |
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