Beacon Valley (77°49′S 160°39′E / 77.817°S 160.650°E) is an ice-free valley between Pyramid Mountain and Beacon Heights, in the Quartermain Mountains of Victoria Land, Antarctica. It was mapped by the British Antarctic Expedition, 1910–13, and named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) after Beacon Heights.
Beacon Valley Camp | |
|---|---|
Field Camp | |
 A helicopter prepares to land at Beacon Valley camp. | |
  Beacon Valley Camp Location of Beacon Valley in Antarctica | |
| Coordinates: 77°51′32″S 160°34′26″E / 77.859°S 160.574°E | |
| Country |  United States |
| Location in Antarctica | Beacon Valley Victoria Land Antarctica |
| Established | 2004 |
| Type | Seasonal |
| Status | Operational |
Astrobiological characteristics
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The central region of Beacon valley is considered to be one of the best terrestrial analogues for the current conditions on Mars. There is snowdrift and limited melting around the edges and occasionally in the central region, but for the most part, moisture is only found as thin films of brine around permafrost structures. It has slightly alkaline salt rich soil.[1][2]
References
edit- ^ McKay, Christopher P. (2008). "Snow recurrence sets the depth of dry permafrost at high elevations in the McMurdo Dry Valleys of Antarctica" (PDF). Antarctic Science. 21 (1): 89–94. doi:10.1017/S0954102008001508. ISSN 0954-1020. S2CID 129096753.[permanent dead link]
- ^ The Planetary and Space Sciences Research Institute, The Open University (5 December 2012). "TN2: The Catalogue of Planetary Analogues, section 1.6.3" (PDF). Under ESA contract: 4000104716/11/NL/AF.
This article incorporates public domain material from "Beacon Valley". Geographic Names Information System. United States Geological Survey.
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