Salvesen Range

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The Salvesen Range is a mountain range, also known as the Salvesen Mountains, on the southern tip of South Georgia. The range rises to a maximum height of 7,644 feet.

The main ranges of South Georgia famously crossed by Ernest Shackleton in 1916, are less rugged and precipitous than the Salvesen Mountains as they are formed from folded sandstone. These were formed from sand deposition, the sediment for which was derived from erosion of the igneous rocks and rifting continental blocks.

The range was surveyed by the South Georgia Survey, 1951-52, and named for Sir Harold Salvesen, a director of Messrs. Chr. Salvesen and Co., Leith, who gave great assistance to the SGS, 1951-52 and 1953-54.

Mountains in the range include:

Geology

Geologically the mountains are believed to have been created 127 million years ago and are made mainly from granite. The Cretaceous granite is pretruded into the Jurassic basaltic lavas and dolerite dykes. Both of which are black so they create a striking colour contrast in exposures. Both the granite and the basalt were formed from rising magma formed on the divergent plate boundary where the southern Atlantic Ocean opened.