Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-27T04:31:50.152Z Has data issue: false hasContentIssue false

III.—Geological Observations in the South Shetlands, the Palmer Archipelago, and Graham Land, Antarctica

Published online by Cambridge University Press:  06 July 2012

Extract

The following observations were made during a prospecting expedition which left the Falkland Islands in the late spring of 1913 for the South Shetlands, the Palmer Archipelago, and Graham Land. The cost of the expedition was provided by Messrs Salvesen of Leith, the well-known shipping and whaling firm, who are lessees from the Colonial Office of the minerals in these remote areas. Arrangements were made to prospect as large an area as possible during the whaling season 1913–14. The steamer Hanka, a modern whaler, proved very suitable for prospecting work, owing to its light draught, small size, and fairly high speed. It could, however, owing to its small capacity, operate only within a limited radius of a supply base, and Messrs Salvesen's big whaling factory ships in King George Island; Leith Harbour, Belgica Strait, Graham Land; and Fournier Bay, Schollaert Channel, Anvers Island, formed effective bases of supply.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1922

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

List of References

(1)Gregory, J. W., “The Geological Relations of South Georgia,” Geol. Mag., 1914, pp. 6164.Google Scholar
(2)Geikie, A. Sir, “Notes on Some Specimens from the Antarctic Regions (with Petrological Notes by J. J. H. Teall),Proc, Roy. Soc. Edin., 1898, vol. xxii, pp. 6670.Google Scholar
(3)De Gerlache, A., Quinze Mois dans I' Antarctique, Paris, 1902.Google Scholar
(4)Andersson, J. G., “On the Geology of Graham Land,Bull. Geol. Inst. Upsala, 1906, vol. vi, pp. 1971.Google Scholar
(5)Pirie, J. H., “On the Graptolite-bearing Rocks of the South Orkneys,” Proc. Roy. Soc. Edin., 1905, vol. xxv, pp. 463470. (The graptolite is identified as Pleurograptus.)Google Scholar
(6)Gourdon, E., “Geographie physique, Glaciologie, Petrographie,” Exped. Antarctique Francaise, 1903–05, Paris, 1908.Google Scholar
(7)Ferguson, D., “Geological Observations in South Georgia,Trans. Roy. Soc. Edin., 1915, vol. 1, pt. iv, pp. .797816.Google Scholar
(8)Gregory, J. W., “The Geological Relations and Some Fossils of South Georgia,” Trans. Roy. Soc. Edin., 1915, vol. 1, pt. iv, pp. 817822.Google Scholar
(9)Tyrrell, G. W., “The Petrology of South Georgia,Trans. Roy. Soc. Edin., 1915, vol. 1, pt. iv, pp. 823836.Google Scholar
(10)Wordie, J. M., “The Drift of the Endurance,Geogr. Journ., 1918, vol. li, pp. 216237.CrossRefGoogle Scholar
(11)Gregory, J. W., op. cit. supra.Google Scholar
(12)Darwin, C., Geological Observations on South America, London, 1846, p. 152.Google Scholar
(13)Darwin, C., Geological Observations on South America, London, 1846, p. 190.Google Scholar
(14)Darwin, C., Geological Observations on South America, London, 1846, p. 196.Google Scholar