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Oodaaq Ø and other short-lived islets north of Greenland

Published online by Cambridge University Press:  08 July 2019

Ole Bennike Open the ORCID record for Ole Bennike [Opens in a new window]  and
Jeff Shea
Ole Bennike*
Affiliation:
Geological Survey of Denmark and Greenland (GEUS), C.F. Møllers Allé 8, DK-800 Aarhus C, Denmark
Jeff Shea
Affiliation:
World Parks, Inc., 2785 Goodrick Avenue, Richmond, CA 94801USA
*
Author for correspondence: Ole Bennike, E-mail: obe@geus.dk
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Abstract

In 1978, a small island was discovered north of Kaffeklubben Ø, until then considered the most northern island on Earth. This island was named Oodaaq Ø. It was visited again in 1979, and in 1980 it was seen from Kaffeklubben Ø by members of the Sirius sledge patrol. Sirius searched for Oodaaq Ø again from 1981 to 1984 but did not find it. During the period from 1996 to 2008, the region was visited regularly and a number of new islets were discovered: the 1996 ATOW Island, KMS Island, 2001 RTOW Island, 83-42 Island, Stray Dog West Island and the 2008 Island. The islets are composed of gravel. We believe the area with islets is shallow, being a continuation of a coastal plain to the south. We suggest that the sea floor in the area is irregular and that the islets form by floes of sea ice that bulldoze material from the sea floor up above sea level. In some cases, perhaps all, the islets disappear when sea ice floes bulldoze sediment back below sea level. Alternatively, the so-called islets are just accumulations of gravel on sea ice.

Keywords

Oodaaq ØGreenlandKaffeklubben ØKap Morris Jesup
Type
Research Article
Information
Polar Record , Volume 55 , Issue 1 , January 2019 , pp. 14 - 24
Copyright
© Cambridge University Press 2019 

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References

Andersson, H., Funder, S., & Hjort, C. (1980). På verdens nordligste landjord. Naturens Verden, 1980, 314–322.Google Scholar
Baker, T. (2003). New Islands, New Northernmost Point of Land on Earth Discovered off Northern Coast of Greenland. Retrieved from http://archive.li/vWT9n (10 March, 2019).Google Scholar
Bennike, O., Funder, S., & Hjort, C. (1986). Notes on the Holocene marine fauna of eastern North Greenland. Bulletin of the Geological Society of Denmark, 35, 71–74.Google Scholar
Boertmann, D., Olsen, K., & Gilg, O. (2010). Ivory Gulls breeding on ice. Polar Record, 46(236), 86–88. doi: 10.1017/S0032247409008626 CrossRefGoogle Scholar
Borup, G. (1911). A Tenderfoot with Peary. New York, NY: Frederick A. Stokes Co.Google Scholar
Burress, C. (2004). Romancing the North. Berkeley Explorer may have Stepped on Ancient Thule. San Francisco Chronicle 17 June 2004. Retrieved from https://www.sfgate.com/bayarea/article/BERKELEY-Romancing-the-north-Berkeley-2748730.php (9 March, 2019).Google Scholar
Danish Meteorological Institute (2018). Ice Charts of Greenland Waters. Retrieved from http://ocean.dmi.dk/arctic/icecharts_gl_1.php (10 March, 2019).Google Scholar
Davies, W. E. (1964). Glacial geology of northern Greenland. Polarforschung, 5, 94–103.Google Scholar
Davies, W. E. (1972). Landscape of northern Greenland. Cold Regions Research and Engineering Laboratory Special Report, 164, 67 pp.Google Scholar
Dawes, P.R. (1986). Glacial erratics on the Arctic Ocean margin of North Greenland: implications for an extensive ice-shelf. Bulletin of the Geological Society of Denmark, 35, 59–69.Google Scholar
Dawes, P. R. (2003). Udforskningen af Peary Land gennem 4000 år. In Martens, G., Jensen, J. F., Meldgaard, M., and Meltofte, H. (Eds.), Peary Land (59–137). Nuuk: Forlaget Atuagkat.Google Scholar
Dawes, P. R., & Lautrup, J. (2017). A Symphony of Scenic Beauty. Avannaarsua: Greenland’s Farthest North. Copenhagen: Geological Survey of Denmark and Greenland.Google Scholar
England, J., Atkinson, N., Bednarski, J., Dyke, A. S., Hodgson, D. A., O Cofaigh, C. (2006). The Innuitian Ice Sheet: configuration, dynamics and chronology. Quaternary Science Reviews, 25, 689–703. doi: 10.1016/j.quascirev.2005.08.007 CrossRefGoogle Scholar
Funder, S. (1980). Feltdagbogfra Nordgrønland, Sommeren 1979, 91 pp. Unpublished field notes, GEUS Report file no. 22886.Google Scholar
Funder, S. (1982). C14-Dating of samples collected during the 1979 expedition to North Greenland. Rapport Grønlands Geologiske Undersøgelse, 110, 9–14.Google Scholar
Funder, S., & Hjort, C. (1980). A reconnaissance of the Quaternary geology of eastern North Greenland. Rapport Grønlands geologiske Undersøgelse, 99, 99–105.Google Scholar
Funder, S., & Larsen, O. (1982). Implications of volcanic erratic in Quaternary deposits of North Greenland. Bulletin of the Geological Society of Denmark, 31, 57–61.Google Scholar
Garboe, A. (1961). Geologiens Historie I Danmark II, Forskere og Resultater. Copenhagen: C. A. Reitzels Forlag.Google Scholar
Gardiner, S. (2003). Return to the top of the World. In Richardson, J. M. (Ed.) Under the Midnight Sun. The Ascent of John Denver Peak and the Search for the Northern Most Point of Land on Earth (97–107). Greenwood Village, CO: Stars End Creations.Google Scholar
Glagow, S. (2008). NDR Team entdeckt Insel im arktischen Eis. Retrieved from https://www.ndr.de/der_ndr/ultimathule100.html (10 March, 2019).Google Scholar
Hansen, K. Q., Adamsen, N., Olsen, S., & Amstrup, B. (2005). Ice and Metocean Conditions off the Northeast Coast of Greenland (Report). Copenhagen: Danish Meteorological Institute. Retrieved from https://www.govmin.gl/images/stories/petroleum/environmental_reports/DMI_2008_Iceand_metocean_conditions_NE_Greenland.pdf (March, 2019).Google Scholar
Hequette, A., Desrosiers, M., & Barnes, P. W. (1995). Sea ice scouring on the inner shelf of the southeastern Canadian Beaufort Sea. Marine Geology, 128, 201–209. doi: 10.1016/0025-3227(95)00095-G CrossRefGoogle Scholar
Hultén, E. (1962). Plants of the floating ice-island ‘Arlis II’. Svensk Botanisk Tidsskrift, 56, 362–363.Google Scholar
Ives, P. C., Levin, B., Robinson, R. D., & Rubin, M. (1964). U.S. Geological Survey radiocarbon dates VII. Radiocarbon, 6, 37–76.CrossRefGoogle Scholar
Jakobsson, M., Mayer, L.A., Coakley, B., Dowdeswell, J. A., Forbes, S., Fridman, B., Hodnesdal, H., Noormets, R., Pedersen, R., Rebesco, M., Schenke, H.-W., Zarayskaya, A. Y., Accettella, D., Armstrong, A., Anderson, R. M., Bienhoff, P., Camerlenghi, A., Church, I., Edwards, M., Gardner, J. V., Hall, J. K., Hell, B., Hestvik, O. B., Kristoffersen, Y., Marcussen, C., Mohammad, R., Mosher, D., Nghiem, S. V., Pedrosa, M. T., Travaglini, P. G., & Weatherall, P. (2012). The international bathymetric chart of the Arctic Ocean (IBCAO) version 3.0. Geophysical Research Letters, 39, L12609. doi: 10.1029/2012GL052219 CrossRefGoogle Scholar
Jancik, J. (2004). Jensenland, historical timeline of the search for the northernmost point of land on Earth. American Alpine Journal, 2004, 250–251.Google Scholar
Jancik, J. A., & Zerbst, K. L. (1997). The 1996 American Top of the World Expedition achieves world exploration history on July 10, 1996. Unpublished report, 1 page. Available at Polarbiblioteket [The Polar Library], Copenhagen.Google Scholar
Johnson, G. W. (2011). Beyond the edge, the search for Ultima Thule, the northern most land on Earth. Minneapolis, MN: Bascom Hill Publishing Group.Google Scholar
Knies, J., Köseoglu, D., Rise, L., Baeten, N., Bellec, V. K., Bøe, R., Klug, M., Panieri, G., Jernas, P. E., & Belt, S. T. (2018). Nordic Seas polynyas and their role in preconditioning marine productivity during the Last Glacial Maximum. Nature Communications 9, 3859. doi: 10.1038/s41467-018-06252-8 CrossRefGoogle ScholarPubMed
Knuth, E. (1960) Unpublished diary in Dronningens Håndbibliotek, Copenhagen, 282 pp.Google Scholar
Koch, L. (1926). Report on the Danish Bicentenary Jubilee Expedition North of Greenland 1920–23. Meddelelser om Grønland, 70(1), 232.Google Scholar
Laberg, J. S., Forwick, M., & Husum, K. (2017). New geophysical evidence for a revised maximum position of part of the NE sector of the Greenland ice sheet during the last glacial maximum. Arktos, 3, 2–9. doi: 10.1007/s41063-017-0029-4 CrossRefGoogle Scholar
Larsen, N. K., Kjær, K. H., Funder, S., Möller, P., vander Meer, J. J. M., Schomacker, A., Linge, H., & Darby, D. A. (2010). Late Quaternary glaciations history of northernmost Greenland – evidence of shelf-based ice. Quaternary Science Reviews, 29, 3399–3414. doi: 10.1016/j.quascirev.2010.07.027 CrossRefGoogle Scholar
Larsen, N. K., Funder, S., Linge, H., Möller, P., Schomacker, A., Fabel, D., Xu, S., & Kjær, K. H. (2016). A Younger Dryas re-advance of local glaciers in north Greenland. Quaternary Science Reviews, 147, 47–58. doi: 10.1016/j.quascirev.2015.10.036 CrossRefGoogle Scholar
Lillestrand, R. L., & Johnson, G. W. (1971). Cartography of North Greenland. Surveying and Mapping, 30, 223–250.Google Scholar
Lillestrand, R. L., Roots, E. F., Niblett, E. R., & Weber, J. R. (1970). Position of Kaffeklubben Island. Canadian Surveyor, 24, 142–146.Google Scholar
Petersen, M.-L. D. (1986). Hvad indad tabes skal udad vindes:om verdens nordligste ø, som blev opkaldt efter nordpolsfareren Oodaaq . Tidsskriftet Grønland, 34, 317–320.Google Scholar
Rasmussen, L. B. (1988). En jordisk krønnike. Træk af DGU’s historie 1888–1988. Copenhagen: Danmarks Geologiske Undersøgelse.Google Scholar
Reimnitz, E., & Barnes, P. W. (1987). Sea-ice influence on Arctic coastal retreat. In Kraus, N. C. (Ed.) CoastalSediments 87, Vol. 2, 1578–1591.Google Scholar
Richardson, J. H. (2007). Journey to the end of the Earth. Esquire, 206-217, 238, 241–242.Google Scholar
Riise-Jensen, C., & Vestergaard Olesen, A. (2008). Feltrapport fra basispunktinspektion i nordlige Peary Land 1. August 2008. Unpublished report, DTU Space, 3 pp.Google Scholar
Rowell, G. (1997). The (very) top of the world. Life, 20, 94–100.Google Scholar
Schmitt, D. (1997). North America, Greenland, Stjernebannertinde, ascent, and exploration of Kaffeklubben and Oodaap Islands. American Alpine Journal, 1997, 215.Google Scholar
Schmitt, D. (2004). North America, Greenland, the far north, Jensenland, explorations of most northerly land. American Alpine Journal, 2004, 248.Google Scholar
Shea, J. (2012). Greenland– Discovery of New Northernmost Point of Land. Retrieved from http://jeffshea.org/greenland-stray-dog-west-expedition/ (9 March, 2019).Google Scholar
Skafte, P. (2005a). Searching for ‘Ultima Thule’: part two. The Polar Times, 3(6), 22–23.Google Scholar
Skafte, P. (2005b). Searching for ‘Ultima Thule’: part three. The Polar Times, 3(7), 18–19.Google Scholar
Svendsen, J. I., Astakhov, V. I., Bolshiyanov, Yu, D., Demidov, I., Dowdeswell, J. A., Gataullin, V., Hjort, C., Hubberten, H. W., Larsen, E., Mangerud, J., Melles, M., Moller, P., Saarnisto, M., & Siegert, M. J. (1999). Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian. Boreas, 28, 234–242. doi: 10.1111/j.1502-3885.1999.tb00217.x CrossRefGoogle Scholar
Wake, L. M., Lecavalier, B. S., & Bevis, M. (2016). Glacial isostatic adjustment (GI) in Greenland: A review. Current Climate Change Reports, 2, 101–111. doi: 10.1007/s40641-016-0040-z CrossRefGoogle Scholar
Wikipedia (2018). Ultima Thule 2008. Retrieved from https://de.wikipedia.org/wiki/Ultima_Thule_2008#cite_note-3 (March 9, 2019).Google Scholar