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  • PANGAEA
  • MDPI Publishing
  • 1940-1944  (3)
  • 1942  (3)
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  • 1940-1944  (3)
Year
  • 1
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    PANGAEA
    In:  EPIC3Records of observations, Scripps Institution of Oceanography, University of California Press, Berkley and Los Angeles, Bremerhaven, PANGAEA, 1(1), pp. 1-64
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/pdf
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-11-08
    Keywords: Accession number; Aerial photography; AERP; Area/locality; Bildflug_I; Bildflug_II; Bildflug_III; Bildflug_IV; Bildflug_V; Bildflug_VI; Bildflug_VII; DAE3_1938/39; DATE/TIME; Deutsche Antarktische Expedition 1938/39; Directory of research expeditions of Germany; Dronning Maud Land, Antarctica; Event label; EXP_GER; Figure; File name; Image number/name; LATITUDE; LONGITUDE; ORDINAL NUMBER; Schwabenland; Uniform resource locator/link to image; View
    Type: Dataset
    Format: text/tab-separated-values, 3277 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Bramlette, M; Bradley, Wilmot Hyde (1942): Geology and biology of North Atlantic deep-sea cores between Newfoundland and Ireland - Part 1. Lithology and geologic interpretations. In: United States Geological Survey, Professional Paper, 196-A, 222 pp, https://pubs.usgs.gov/publication/pp196
    Publication Date: 2023-08-28
    Description: In May and June 1936 Dr. C. S. Piggot of the Geophysical Laboratory, Carnegie Institution of Washington, took a series of 11 deep-sea cores in the North Atlantic Ocean between the Newfoundland banks and the banks off the Irish coast. These cores were taken from the Western Union Telegraph Co.'s cable ship Lord Kelvin with the explosive type of sounding device which Dr. Piggot designed. All but two of these cores (Nos. 8 and 11) are more than 2.43 meters (8 feet) long, and all contain ample material for study. Of the two short cores, No. 8 was taken from the top of the Faraday Hills, as that part of the mid-Atlantic ridge is known, where the material is closely packed and more sandy and consequently more resistant; No. 11 came from a locality where the apparatus apparently landed on volcanic rock that may be part of a submarine lava flow.
    Keywords: Atlantic Ocean; Comment; Core; CORE; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Latitude of event; LK-11; LK-13; LK-8; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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