Beacon Valley

Beacon Valley includes several smaller geographic features, named during various scientific surveys.

• Profile Bluff (77°52′S 160°26′E), a prominent cliff (2,070 m) midway between Mount Weller and Horizon Bluff on the west side of the valley. Named in 1993 by the New Zealand Geographic Board (NZGB).[1]
• Horizon Bluff (77°54′S 160°27′E), a steep bluff at the head of the valley, rising to 2,275 metres (7,460 ft). It is west of Friedmann Valley. Named in 1993 by the NZGB.[2]
• Rector Ridge (77°54′S 160°33′E), a bold rock ridge at the head of the valley, rising to 2,105 m. It was named in 1992 by Advisory Committee on Antarctic Names (US-ACAN) after Commander Jack Rector, U.S. Navy, Commanding Officer, Antarctic Development Squadron Six (VXE-6), May 1987 to May 1988.[3]
• Vestal Ridge (77°53′S 160°38′E), a steep rock ridge in southeast Beacon Valley, rising to 2,240 m and forming the divide between Mullins Valley and Farnell Valley. It was named by US-ACAN in 1993 after J. Robie Vestal (1942–1992), a microbiologist at the University of Cincinnati whose research in Antarctica focused on adaptations of microbial ecosystems to the extreme environments.[4]

Researchers trek through Antarctica's Beacon Valley, one of the most Mars-like places on Earth. Image credit: NASA

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.[5][6]

•  This article incorporates public domain material from "Beacon Valley". Geographic Names Information System. United States Geological Survey.