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Summary
| Description |
English: A cryoconite hole on top of Taylor Glacier. Cryoconite holes are a water-filled cylindrical melt-holes on glacial ice surfaces. They are formed when dark-colored material such as dirt is deposited on the ice surface. The material absorbs solar radiation and causes the ice to melt, eventually forming a hole. Cryoconite holes are home to small ecosystems with living microorganisms. |
| Date | |
| Source | https://photolibrary.usap.gov/PhotoDetails.aspx?filename=taylor-glacier-blood-falls-cryoconite2.JPG |
| Author | Peter Rejcek, NSF |
Licensing
|
This image is a work of a National Science Foundation employee, taken or made as part of that person's official duties. As a work of the U.S. federal government, the image is in the public domain. |  |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:45, 12 October 2024 | | 6,000 × 4,000 (7.52 MB) | Hubert Kororo | Uploaded a work by Peter Rejcek, NSF from https://photolibrary.usap.gov/PhotoDetails.aspx?filename=taylor-glacier-blood-falls-cryoconite2.JPG with UploadWizard |
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