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  • Data  (6)
  • 1960-1964  (6)
Collection
Keywords
Publisher
Years
Year
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Straczek, J A; Horen, Arthur; Ross, Malcolm; Warshaw, Charlotte M (1960): Studies of the manganese oxides. IV. Todorokite. American Mineralogist, 45, 1174-1184, http://www.minsocam.org/ammin/AM45/AM45_1174.pdf
    Publication Date: 2023-08-28
    Description: Todorokite is a very abundant manganese oxide mineral in many deposits in Cuba and has been noted from other localities. Six new analyses are givenl they lead to the approximate formula (Na, Ca, K, Mn+2)(Mn+4, Mn+2, Mg)6O12.3H2O. Electron diffraction data show the mineral to be orthorhombic, or monoclinic with beta near 90°. The x-ray powder pattern is indexed on a cell with a=0.75A, b=2.849A, c=9.59A, beta=90°. A differential thermal analysis curve is given.
    Keywords: Aluminium oxide; Barium oxide; Calcium oxide; Charco_Redondo_S; Cobalt oxide; Colorimetry; Copper(II) oxide; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Flame photometry; Guanaba_S; Iron oxide, Fe2O3; Latitude of event; Longitude of event; Magnesium oxide; Manganese dioxide; Manganese oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Oxygen; Polarograph; Ponupo_S; Potassium oxide; Quinto_S; Sample ID; Silicon dioxide; Sodium oxide; Specific gravity; Strontium oxide; Taratana_S; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-08-28
    Keywords: Atlantic Ocean; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Event label; File name; Identification; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Substrate type; Uniform resource locator/link to image; V19; V19-1; V19-10; V19-100; V19-103; V19-105; V19-106; V19-109; V19-10C; V19-111; V19-112; V19-115; V19-117; V19-118; V19-119C; V19-11RD; V19-12; V19-121; V19-121C; V19-122C; V19-123; V19-124C; V19-125C; V19-126C; V19-128C; V19-13; V19-130; V19-130C; V19-131; V19-134; V19-136; V19-138; V19-14; V19-141C; V19-144C; V19-145C; V19-15; V19-150; V19-151; V19-152; V19-154; V19-155; V19-157; V19-158; V19-159; V19-161; V19-162C; V19-163; V19-164; V19-165; V19-166; V19-166C; V19-167; V19-168; V19-168C; V19-169; V19-170; V19-171; V19-172; V19-172C; V19-179C; V19-18; V19-182; V19-184; V19-186; V19-192C; V19-198C; V19-1C; V19-1RD; V19-20; V19-201C; V19-205; V19-209; V19-21; V19-210; V19-211; V19-213; V19-214; V19-216; V19-217; V19-22; V19-220C; V19-223; V19-224C; V19-226; V19-228; V19-23; V19-230; V19-231; V19-232; V19-239; V19-242; V19-244; V19-247; V19-248C; V19-254C; V19-255C; V19-269; V19-272; V19-276; V19-280; V19-281; V19-282; V19-28C; V19-295; V19-296; V19-29C; V19-2C; V19-2RD; V19-305; V19-307; V19-312; V19-38; V19-3C; V19-4; V19-43; V19-44; V19-45; V19-5; V19-52; V19-53; V19-54; V19-55; V19-58; V19-59C; V19-5C; V19-6; V19-60; V19-61C; V19-64C; V19-66; V19-67; V19-68; V19-68C; V19-69; V19-69C; V19-7; V19-70; V19-71; V19-72; V19-74C; V19-75; V19-75C; V19-76; V19-78; V19-79; V19-8; V19-80; V19-81; V19-82; V19-83; V19-84; V19-85; V19-87; V19-88; V19-8C; V19-9; V19-91; V19-93; V19-94; V19-96; V19-97; V19-99; V19-9C; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 3057 data points
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Kaneps, A; Lair, C; Morgenstein, M (1964): R/V Robert Conrad Cruise 8 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 208
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the Robert Conrad Cruise 8 from November 1963 until August 1964 by the Lamont Geological Observatory, Columbia University from the R/V Robert Conrad. A total of 140 cores and dredges were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; RC08; RC08-100; RC08-102; RC08-103; RC08-106; RC08-107; RC08-109; RC08-11; RC08-110; RC08-112; RC08-113; RC08-114; RC08-116; RC08-12; RC08-120; RC08-125; RC08-126; RC08-128; RC08-129; RC08-12RD; RC08-130; RC08-135; RC08-137; RC08-14; RC08-140; RC08-141; RC08-143; RC08-144; RC08-145; RC08-147; RC08-148; RC08-15; RC08-16; RC08-19; RC08-20; RC08-21; RC08-25; RC08-26; RC08-27; RC08-31; RC08-32; RC08-34; RC08-35; RC08-36; RC08-37; RC08-38; RC08-39; RC08-42; RC08-43; RC08-44; RC08-45; RC08-48; RC08-49; RC08-4RD; RC08-5; RC08-50; RC08-53; RC08-55; RC08-6; RC08-63; RC08-67; RC08-69; RC08-70; RC08-71; RC08-72; RC08-73; RC08-75; RC08-7RD; RC08-8; RC08-80; RC08-81; RC08-82; RC08-83; RC08-84; RC08-85; RC08-86; RC08-87; RC08-88; RC08-89; RC08-8RD; RC08-90; RC08-94; RC08-97; RC08-98; RC08-99; RC08-9RD; Robert Conrad; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 1616 data points
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Pratt, Richard M (1962): The Ocean Bottom. Science, 138(3539), 492-495, https://doi.org/10.1126/science.138.3539.492
    Publication Date: 2023-08-28
    Description: Photography has become an integral part of submarine geological and biological investigations of the ocean bottom. The underwater cameras used to make these photographs were designed by Harold Edgerton. The pictures were taken from 1960 to 1962, from ships of the Woods Hole Oceanographic Institution. They show that life occurs even in the deepest trenches, and that sedimentary and biological processes in deep water do not differ in kind from those in shallow water.
    Keywords: AT260; AT260-7C; AT26601; AT266-18C; Atlantic Ocean; Atlantis (1931); Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 17 data points
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  • 5
    Publication Date: 2023-11-14
    Description: Reports on ATLANTIS Cruises 280 and 281 to the New England Seamount Chain are combined here. . A continuous bathymetric survey was run on both cruises, with profiles across several seamounts. A series of dredge and camera stations were made. They are dicussed in this report. Also included are photographs representative of each camera lowering and photographs of dredged material.
    Keywords: AT28001; AT280-01; AT280-01C; AT280-03; AT280-04; AT280-04C; AT280-05; AT280-05C; AT280-06C; AT280-09; AT280-10; AT280-12; AT280-13; AT280-14; AT280-15; AT280-16; Atlantic Ocean; Atlantis (1931); Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sediment type; Size; Substrate type; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 131 data points
    Location Call Number Expected Availability
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bramlette, M (1961): Pelagic sediments. in: Invited Lectures Presented at the International Oceanographic Congress Held in New York, 31 August-12 September 1959. Presented at the International Oceanographic Congress, 1959, American Association for the Advancement of Science, New York, U.S.A., 345-366, https://archive.org/details/oceanographyinvi00inte
    Publication Date: 2023-08-28
    Description: The vast extent of pelagic deposits, covering about 70 per cent of the ocean floor, thus about half of the earth, makes them of obvious importance to all Earth Science. All the pelagic (eupelagic) sediments, whether largely of plankton remains or fine inorganic particles, have certain distinctive characteristics to reflect their environment of accumulation. The great segregation of manganese in pelagic sediments presents many problems. It is hypothesized that in the formation of present day nodules a relatively slow accumulation in order to permit deposition of more of the manganese as large nodules, rather than as the disseminated micronodules that are in larger proportion in the Tertiary.
    Keywords: CHUB01BD; CHUB01BD-017G; CHUB-17; CHUBASCO; Comment; Core; CORE; Elevation of event; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Sample ID; Spencer F. Baird; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
    Location Call Number Expected Availability
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