File:Sulis 20180921123112.jpg
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Summary
| Description |
English: The basement rock of Lost City is primarily uplifted peridotite and gabbro, allowing serpentinization to occur where olivine is present. However, some cracks and striations do not suggest intense serpentinization, such as these cracks which do not have carbonate precipitates. |
| Date | |
| Source | Cruise media archive. |
| Author | “Susan Lang, U. of SC. / NSF / ROV Jason / 2018 © Woods Hole Oceanographic Institution.” |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 14:36, 24 September 2019 | | 5,968 × 3,352 (1.88 MB) | Wünderbrot | User created page with UploadWizard |
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