File:X-ray of core 2.jpg
X-ray_of_core_2.jpg (646 × 514 pixels, file size: 65 KB, MIME type: image/jpeg)
Summary edit
Concentration of gravel particles (>2 mm diameter) assessed from X-radiographs (inset shows example from core D20) are inferred to be dominantly ice-rafted. Cores with low concentrations represent areas overwhelmed by fine-grained sediments delivered from the sandur.
Licensing edit
| Description |
Concentration of gravel particles (>2 mm diameter) assessed from X-radiographs (inset shows example from core D20) are inferred to be dominantly ice-rafted. |
|---|---|
| Source |
The image appears on a website entitled, "Glacimarine sedimentation in Kangerdluk (Disko Fjord), West Greenland, in response to a surging glacier" at url=http://geog.queensu.ca/gilbert/surge%20paper.PDF. |
| Date |
9 September 2000 |
| Author |
Robert Gilbert, Niels Nielsen, Henrik Möller, Joseph R. Desloges, and Morten Rasch |
| Rationale |
No free use or Public Domain image known to show concentration of gravel particles (>2 mm diameter) assessed from X-radiographs (inset shows example from core D20) inferred to be dominantly ice-rafted. |
| Permission |
Fair Use |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:13, 25 September 2014 | | 646 × 514 (65 KB) | Marshallsumter (discuss | contribs) | Concentration of gravel particles (>2 mm diameter) assessed from X-radiographs (inset shows example from core D20) are inferred to be dominantly ice-rafted. Cores with low concentrations represent areas overwhelmed by fine-grained sediments delivered f... |
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