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The Bellingshausen-Palmer meeting

Published online by Cambridge University Press:  02 June 2015

Rip Bulkeley*
Affiliation:
38 Lonsdale Road, Oxford, OX2 7EW (rip@igy50.net)
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Abstract

The celebrated meeting between Captain Bellingshausen of the Imperial Russian Navy and the American sealing skipper Nathaniel Brown Palmer, off the South Shetland Islands in February 1821, has often been described by following just one or other of the two men's divergent and in some respects irreconcilable accounts. The most contentious issue is whether or not Palmer told Bellingshausen about the existence of a body of land to the south of the South Shetlands, known today as the Antarctic Peninsula. This note attempts to reach a balanced assessment of the matter by examining evidence from both sides, including several previously unconsidered items. It concludes that, although the truth will never be known with absolute certainty, the basic American account is more plausible, by the narrowest of narrow margins, than the Russian.

Information

Type
Research Article
Copyright
Copyright © Cambridge University Press 2015 
Figure 0

Fig. 1. Part of Bellingshausen's track chart at the South Shetland Islands, with north to the left. Smith Island at the bottom left is followed by Snow, Livingston, Deception, Greenwich, Robert, Nelson and King George Islands in ascending order, with few details of the straits between them. The entry for the meeting with Palmer near Livingston Island is picked out in bold (Belov, 1963: Sheet 14, detail).

Figure 1

Fig. 2. Track of Palmer's first reconnaissance of the south side of Bransfield Strait in November 1820, from Bertrand (1971: 62).

Figure 2

Fig. 3. The Palmer-Bellingshausen meeting, as imagined in Fanning (1833: 45). The foreground probably represents Neptune's Bellows, the channel leading into the caldera on Deception Island.

Figure 3

Figs. 4a, 4b. A sketch map attributed to Nathaniel Palmer (left) shows Deception Island at the bottom, followed by parts of Livingston Island, McFarlane Strait and Greenwich Island in ascending order with magnetic north at the top (Martin 1940: 533). The corresponding part of a map published by Bellingshausen (right) has been oriented to a similar alignment (Bellingshausen 1831, Atlas, Sheet 62, detail).