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Captain John King Davis on F.I.S. Endeavour: preparing for oceanographic work in the Southern Ocean

Published online by Cambridge University Press:  28 July 2011

Anna Lucas
Affiliation:
School of Geography and Environmental Studies, University of Tasmania, Hobart, Tasmania, Australia (L.K.Kriwoken@utas.edu.au)
Lorne Kriwoken
Affiliation:
School of Geography and Environmental Studies, University of Tasmania, Hobart, Tasmania, Australia (L.K.Kriwoken@utas.edu.au)
Elizabeth Leane
Affiliation:
School of English, Journalism and European Languages, University of Tasmania, Hobart, Tasmania, Australia
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Abstract

John King Davis captained S.Y. Aurora on three voyages to Antarctica and on other sub-Antarctic cruises for Douglas Mawson's Australasian Antarctic Expedition (AAE) 1911–1914. Between the first and second Antarctic trips, he made a short return cruise in 1912 from Melbourne to Eden in southeastern Australia with the Director of Commonwealth Fisheries, on the fisheries investigation steamship, F.I.S. Endeavour. This cruise was a milestone in his continuing training for the AAE's oceanographic work. Davis went not as captain, but as an observer. His aim was to gain greater knowledge of operating techniques when using oceanographic research equipment and to apply that knowledge to observations on forthcoming voyages with Aurora. He kept abbreviated notes of the research conducted on Endeavour, and of his visit to Eden, in a small pocket notebook. These informal observations, apparently made just for his own future reference, give us a glimpse of the 28 year old Davis. He has often been portrayed in a negative light, but here his personal notes reveal an experienced seaman, temporarily freed from responsibilities of captaincy and navigation, hard working, keen to acquire new skills on board and sociable when ashore. His subsequent work on Aurora, using the skills he acquired on this trip, resulted in significant contributions to the scientific reports of the AAE, including the discovery of an extensive elevation in the sea floor south of Tasmania, now known as the South Tasman Rise.

Information

Type
Research Article
Copyright
Copyright © Cambridge University Press 2011
Figure 0

Fig. 1. Endeavour at Hobart. The After Gallows, trawling wires and sounding machine can be seen on deck. The monkey island from where bearings were taken is above the bridge. Photo: Baily. Reproduced with permission of the Maritime Museum Tasmania.

Figure 1

Fig. 2. Map of Twofold Bay, Eden, NSW, marking sites referred to in Davis's notes. Modified, with permission, from Australian Hydrographic Service Chart AUS 192 Twofold Bay. Not to be used for navigation.

Figure 2

Fig. 3. Trawling wires and Lucas sounding machine on the deck of Endeavour. Dannevig, here with ship's cat, supervised operations on board. Photo: J.K. Davis. Reproduced with permission of the State Library of Victoria.

Figure 3

Fig. 4. Dannevig with a seawater sampling bottle. Photo: J.K. Davis. Reproduced with permission of the State Library of Victoria.

Figure 4

Table 1 Early morning observations of temperatures of sea water samples at increasing depth, ESE of Green Cape, NSW, Australia, recorded by JK Davis on Endeavour on 1 October 1912. Correlation co-efficient: r = −0.968749 indicates a high correlation between depth and temperature.

Figure 5

Fig. 5. Taking a terrestrial bearing with the magnetic compass. This was mounted on the monkey island above the bridge. Note the iron compensating balls on either side of the binnacle. Photo: J.K. Davis. Reproduced with permission of the State Library of Victoria.

Figure 6

Fig. 6. The After Gallows with otter boards, chains and net, towards stern of Endeavour. Photo: J.K. Davis. Reproduced with permission of the State Library of Victoria.

Figure 7

Table 2 Afternoon observations of temperatures of sea water samples at increasing depth, using the Ekman Water Bottle fitted with a Richter Thermometer, near Green Point, NSW, Australia, recorded by JK Davis on Endeavour on 2 October 1912. Correlation co-efficient: r = −0.935081 indicates a high correlation between depth and temperature.

Figure 8

Fig. 7. Map of southeastern Australia, marking sites referred to in Davis’ notes and the South Tasman Rise discovered by Davis. Modified, with permission, from Australian Hydrographic Service Chart AUS 4601 Tasman Sea – New Zealand to South Eastern Australia. Not to be used for navigation.