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Summary
| Description | Lava flows of West Dome, one the structural highpoints of Diamond Craters, rise NE of lake-filled Malheur Maar. The shallow 2-m-deep lake occupies one of many maars (the rest of which are dry) of the Diamond Craters volcanic field. Southeastern Oregon, USA. |
| Date | |
| Source | http://www.volcano.si.edu/world/volcano.cfm?vnum=1202-17- |
| Author | Lee Siebert, Smithsonian Institution |
| Permission ( Reusing this file) |
According to Ed Venzke, webmaster of Smithsonian Institution's GVP website: All photos made by SI employees are without restriction, as they are US Government employees. Authors and source should be credited. |
| Location | Oregon |
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| This file has been identified as being free of known restrictions under copyright law, including all related and neighboring rights. | ||
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 06:06, 22 April 2007 |
| 640 × 447 (67 KB) | Seattle Skier | {{Information |Description= Lava flows of West Dome, one the structural highpoints of Diamond Craters, rise NE of lake-filled Malheur Maar. The shallow 2-m-deep lake occupies one of many maars (the rest of which are dry) of the |
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