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  • Data  (28)
  • 1985-1989
  • 1960-1964  (26)
  • 1930-1934  (2)
  • 1963  (18)
  • 1960  (8)
  • 1932  (2)
Collection
Keywords
Publisher
Years
  • 1985-1989
  • 1960-1964  (26)
  • 1930-1934  (2)
Year
  • 1
    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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  • 2
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    In:  Supplement to: Pachadzhanov, D N; Bandurkin, G A; Migdisov, Areg A; Girin, Yury P (1963): Data on the geochemistry of manganese nodules from the Indian Ocean. Geokhimiya, 5, 493-499, hdl:10013/epic.46169.d001
    Publication Date: 2023-08-28
    Description: Analyses are given for the core and outer colliform shell of a manganese nodule collected at a depth of 5000 m in the Indian Ocean, and for the red clay that encloses the nodules. Trace elements determined include rare earths, Nb, Ta, Th, and V. The cores of the nodules were once composed of basaltic rock, but now are phillipsite and nontronite. The outer shell is composed of manganite, with admixed quartz, phillipsite, and some geothite. The correlations established between the redox potentials and the concentration coefficients for 12 elements indicate that Eh plays a greater role in the formation of the manganiferous shells than coprecipitation properties.
    Keywords: GC; Gravity corer; Indian Ocean; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Vityaz (ex-Mars); Vityaz-31; VITYAZ4575
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the R/V Robert Conrad Cruise 02 from 26 until 28 January 1963 by the Lamont Geological Observatory, Columbia University. A total of 5 cores 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; 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; RC02; RC0201; RC02-1; RC02-2; RC02-4; RC02-5; Robert Conrad; Sample ID; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 75 data points
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  • 4
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the R/V Robert Conrad Cruise 05 from March until April 1963 by the Lamont Geological Observatory, Columbia University. A total of 13 cores 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; RC05; RC05-1; RC05-10; RC05-11; RC05-12; RC05-13; RC05-14; RC05-1RD; RC05-7; RC05-8; RC05-9; Robert Conrad; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 306 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Burckle, Lloyd H; Hekinian, Roger; Lair, C (1963): Robert Conrad Cruise 04 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 13 pp
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the R/V Robert Conrad Cruise 04 in March 1963 by the Lamont Geological Observatory, Columbia University. A total of 9 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Core; CORE; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; 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; RC04; RC04-1; RC04-2; RC04-3; RC04-4; RC04-7CC; RC04-8; Robert Conrad; Sample ID; Sediment type
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Lamont-Doherty Earth Observatory (1963): Robert Conrad Cruise 06 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 9 pp
    Publication Date: 2023-08-28
    Description: The cores described in this report were taken during the R/V Robert Conrad Cruise 06 from May until June 1963 by the Lamont Geological Observatory, Columbia University. A total of 5 cores were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; 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; RC06; RC06-1; RC06-2; RC06-3; Robert Conrad; Sample ID; Sediment type; Size
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Anderson, N D; Burckle, Lloyd H; Baker, R (1963): R/V Robert Conrad Cruise 7 - Preliminary Megascopic Descriptions of Split Cores. Lamont Geological Observatory, Columbia University, New York, unpublished, 48 pp
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the Robert Conrad Cruise 7 from July until October 1963 by the Lamont Geological Observatory, Columbia University from the R/V Robert Conrad . A total of 29 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; RC07; RC0701-RC0708; RC07-1; RC07-10; RC07-12; RC07-13; RC07-15; RC07-16; RC07-17; RC07-1RD; RC07-20; RC07-21; RC07-25; RC07-26; RC07-28; RC07-29; RC07-3; RC07-30; RC07-4; RC07-5; RC07-6; RC07-7; Robert Conrad; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 353 data points
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  • 8
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Event label; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; Position; Quantity of deposit; Size; Substrate type; TRAWL; Trawl net; Visual description; VITYAZ; Vityaz (ex-Mars); VITYAZ3782-TR; VITYAZ3996-TR
    Type: Dataset
    Format: text/tab-separated-values, 13 data points
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  • 9
    Publication Date: 2023-08-28
    Keywords: Calcium; DEPTH, sediment/rock; Description; Emanescence radiometry; Event label; Gas chromatography; Identification; Insoluble residue; Iron; Loss on ignition; Luminescent analysis; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; Phosphorus; Radium; Silicon; Thorium; Thorium-230; TRAWL; Trawl net; Uranium; VITYAZ; Vityaz (ex-Mars); VITYAZ3782-TR; VITYAZ3996-TR; Wet chemistry; X-ray radiometry
    Type: Dataset
    Format: text/tab-separated-values, 142 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Nikolayev, D S; Yefimova, E I (1963): On the age of iron-manganese concretions from the Indian and Pacific Oceans. Geochemistry, 7, 703-714, hdl:10013/epic.47397.d001
    Publication Date: 2023-08-28
    Description: Uranium, radium, thorium and ionium were determined directly on seven concretions from three stations in the Indian Ocean, and on two concretions and a manganese-rich crust from two stations in the Pacific Ocean. The uranium content averages 3 to 5 gamma/g and the thorium content varies only slightly, but the Th/U ratio in the concretions is typically 2 to 5 in the Indian Ocean and 5 to 15.5 in the Pacific. The ionium content ranges from 1.0 x 10-9 to 3.6 10**-9 g/g in concretions from both oceans. Radium is more abundant in specimens from the Pacific Ocean (Ra = 3 - 12.7 x 10**-11 g/g) than from the Indian Ocean (1.5 - 5.2 x 10**-11 g/g). Analyses for Ca, Mn, Fe, Si, Ni, P, and ignition loss are also given. Radioactive equilibria between uranium, ionium, and radium are strongly disturbed throughout the concretions, and the RA/U and lo/U ratios generally exceed equilibrium ratios. Migration of radium from interior layers was established, so that neither determination of the ages of the concretions nor of their rates of growth can be considered reliable. The age of the concretions cannot exceed 800,000 years, and all grew within relatively short periods of time; there may have been "dormant" periods during growth. Estimates of growth rates are calculated from the radium and ionium contents; they show marked discordance.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northwestern Basin, Pacific Ocean; TRAWL; Trawl net; VITYAZ; Vityaz (ex-Mars); VITYAZ3782-TR; VITYAZ3996-TR
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 11
    Publication Date: 2023-08-28
    Keywords: Deposit type; DEPTH, sediment/rock; Description; Elevation of event; GC; Gravity corer; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Vityaz (ex-Mars); Vityaz-31; VITYAZ4575
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 12
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    PANGAEA
    In:  Supplement to: SCRIPPS Institution of Oceanography (1963): LUSIAD Expedition, May 1962-August 1963, List of sediment cores and dredge hawls, R/V Argo and R/V Horizon. Scripps Institution of Oceanography, UC San Diego, unpublished, 29 pp, https://www.ngdc.noaa.gov/mgg/curator/data/argo/lusiad/lusiad_expedition_report.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on the LUSIAD Expedition from May 1962 until August 1963 by the Scripps Institution of Oceanography from both the R/V Argo and the R/V Horizon. A total of 310 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Argo; Atlantic Ocean; Comment; Coral Sea; D2; D3; D4; D5; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Horizon; Indian Ocean; Java Sea; Latitude of event; Longitude of event; LSDA; LSDA-013D; LSDA-102G; LSDA-119G; LSDA-121G; LSDA-122G; LSDA-123G; LSDA-124G; LSDA-125G; LSDA-126G; LSDA-131G; LSDA-132P; LSDA-132PG; LSDA-134P; LSDA-138G; LSDA-138V; LSDA-139GB; LSDA-140G; LSDA-145PB; LSDA-145PGA; LSDA-145PGB; LSDA-147PG; LSDA-148G; LSDA-155V; LSDA-157V; LSDA-162G; LSDA-179D; LSDA-194G; LSDA-199D; LSDA-219D; LSDA-222D; LSDH; LSDH-022G; LSDH-022V; LSDH-023G; LSDH-034V; LSDH-035V; LSDH-036V; LSDH-038G; LSDH-042V; LSDH-045G; LSDH-046V; LSDH-053G; LSDH-054G; LSDH-055V; LSDH-063G; LSDH-078P; LSDH-085G; LSDH-086G; LSDH-087P; LSDH-089PG; LSDH-089V; LSDH-090P; LSDH-090PG; LSDH-093P; LSDH-093PG; LSDH-093V; LSDH-095G; LSDH-099G; LSDH-100G; LSDH-100V; LSDH-102G; LUSIAD-A; LUSIAD-H; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Piston corer; Position; Quantity of deposit; Sample ID; Sediment type; Size; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 633 data points
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  • 13
    Publication Date: 2023-08-28
    Keywords: Aluminium oxide; Calcium oxide; Carbon, organic, total; DEPTH, sediment/rock; Description; GC; Gravity corer; Indian Ocean; Iron oxide, Fe2O3; Iron oxide, FeO; Magnesium oxide; Manganese oxide; Niobium (V) oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus pentoxide; Potassium oxide; Sample ID; Silicon dioxide; Sodium oxide; Tantalum (V) oxide; Thorium; Titanium dioxide; Vanadium; Vityaz (ex-Mars); Vityaz-31; VITYAZ4575; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 14
    Publication Date: 2023-07-10
    Keywords: Aptenodytes forsteri; Catharacta skua; Chionis alba; Comment; Daption capensis; DATE/TIME; Diomedea exulans exulans; Eudyptes chrysolophus; Fulmarus glacialoides; Halobaena caerulea; Larus dominicanus; LATITUDE; LONGITUDE; Macronectes giganteus; Oceanites oceanicus; Pachyptila desolata; Pagodroma nivea; Phalacrocorax atriceps; Pygoscelis adeliae; Pygoscelis antarctica; Pygoscelis papua; Sterna vittata; Thalassoica antarctica; Visual observation; Weddell_Sea_Region; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 859 data points
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  • 15
    Publication Date: 2023-07-10
    Keywords: Aptenodytes forsteri; Catharacta skua; Chionis alba; Daption capensis; DATE/TIME; Diomedea chrysostoma; Diomedea exulans exulans; Diomedea melanophris; Fulmarus glacialoides; Halobaena caerulea; LATITUDE; LONGITUDE; Macronectes giganteus; Oceanites oceanicus; Pachyptila desolata; Pagodroma nivea; Phoebetria fusca; Phoebetria palpebrata; Pterodroma macroptera macroptera; Pygoscelis adeliae; Pygoscelis antarctica; Thalassoica antarctica; Visual observation; Weddell_Sea_Region; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 456 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Hewett, DF; Fleischer, Michael; Conklin, Nancy (1963): Deposits of the manganese oxides; supplement. Economic Geology, 58(1), 1-51, https://doi.org/10.2113/gsecongeo.58.1.1
    Publication Date: 2024-07-01
    Description: In an earlier paper by two of the authors the conclusion was reached that the 33 recognized species of oxides of Mn could be separated into 3 groups: 1) those which appeared to be persistently supergene in origin, 2) those which appeared to be persistently hypogene, and 3) those which were supergene in some localities and hypogene in other localities. When that paper was written, there were available about 250 X-ray diffraction analyses of mineral specimens, also 35 complete and about 150 partial chemical analyses. The conclusions of that paper were based upon the interpretation of the geologic conditions under which these specimens occurred. Late in the preparation of that paper, it seemed worthwhile to make numerous semiquantitative analyses of specimens, largely from 9 western [U.S.A] states, selected carefully from 5 groups of geologic environments, in the hope that the frequency and percentages of some elements might be distinctive of the several geologic groups. For this purpose, 95 specimens were selected from the 5 groups, as follows: 19 specimens interpreted as supergene oxides by the geologists who collected them, 35 specimens of hypogene vein oxides, 22 specimens of Mn-bearing hot spring aprons, 9 specimens of stratified oxides, and 10 specimens of deep-sea nodules. The spectrographic analyses here recorded indicate that a group of elements - W, Ba, Sr, Be, As, Sb, Tl, and Ge - are present more commonly, and largely in higher percentages, in the hypogene oxide than in the supergene oxides and thus serve to indicate different sources of the Mn. Also, the frequency and percentages of some of these elements indicate a genetic relation of the manganese oxides in hypogene veins, hot spring aprons, and stratified deposits. The analyses indicate a declining percentage of some elements from depth to the surface in these 3 related groups and increasing percentages of some other elements. It is concluded that some of the elements in deep-sea nodules indicate that sources other than rocks decomposed on the continents, probably vulcanism on the floors of the seas, have contributed to their formation.
    Keywords: ALB-13; ALB-173; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-4662; Aluminium; Barium; Beryllium; Bismuth; Boron; Calcium; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWBD1; DWHD47; Elevation of event; Event label; FANB01BD; FANBD-25D; FANFARE-B; Horizon; Indian Ocean; Iron; Lanthanum; Latitude of event; Lead; LGO-BT-57 or VM14 SBT57 (SIO); Longitude of event; Magnesium; MDPC02HO-MP-025F-2; MDPC02HO-MP-033K; MIDPAC; Molybdenum; MPC-25F-2; MPC-33K; NAGA; NAGA10C; Neodymium; Nickel; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Photo/Video; Potassium; PV; Sample ID; Scandium; Silicon; Sodium; Spectrographic analysis; Spencer F. Baird; Stranger; Strontium; Thallium; Titanium; V14; V14-57RD; Vanadium; Vema; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 296 data points
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  • 17
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    In:  Supplement to: Arrhenius, Gustaf (1963): Pelagic sediments. In: Hill, M.N. (Ed.) The Earth Beneath the Sea, History, The Sea - Ideas and Observations on Progress in the Study of the Seas, Wiley J, New York, U.S.A., 3, 655-727, hdl:10013/epic.46253.d001
    Publication Date: 2024-07-01
    Description: Attempts to classify pelagic sediments have been based either on appearance and composition, or on the ultimate origin of the components. In particular it appears feasible to distinguish minerals which crystallized in sea-water from those which formed in magmas, in hydrothermal solution, or by weathering under acidic conditions. It is the case of iron and manganese oxide mineral aggregates which constitute one of the major types of rock encountered on the ocean floor; according to Menard (unpublished) about 10% of the pelagic area of the Pacific is covered by such nodules. The nodules consist of intimately intergrown crystallites of different minerals among those identified, besides detrital minerals and organic matter, are opal, goethite, rutile, anatase, barite, nontronite, and at least three manganese oxide minerals of major importance. Arrhenius and Korkisch (1959) have attempted to separate from each other the different minerals constituting the nodules, in order to establish the details of their structure and the localization of the heavy metal ions. The results demonstrate (Table II) that copper and nickel are concentrated in the manganese oxide phases concentrated in the reducible fraction. Cobalt, part of the nickel and most of the chromium are distributed between these and the acid-soluble group of the non-manganese minerals, dominated by goethite and disordered FeOOH.
    Keywords: Acid soluble, total; ALB-13; ALB-2; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-2; ALBTR-4711; ALBTR-4721; Barium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD4; DWHD72; Event label; Horizon; Identification; Iron; Lanthanum; Lead; Manganese; Molybdenum; Nickel; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Optical spectrographic analysis; Pacific Ocean; Reducible total; Residual; Scandium; Spencer F. Baird; Strontium; Thorium; Titanium; Wired profile sonde; WP; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 386 data points
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  • 18
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    In:  Supplement to: Arrhenius, Gustaf; Bonatti, Enrico (1963): Neptunism and vulcanism in the ocean. Progress in Oceanography, 3, 7-22, https://doi.org/10.1016/0079-6611(65)90005-4
    Publication Date: 2024-07-01
    Description: The origin of authigenic minerals on the ocean floor has been extensively discussed in the past with emphasis on two major processes; precipitation from solutions originating from submarine eruptions, and slow precipitation from sea water of dissolved elements, originating from weathering of continental rocks. It is concluded that in several marine authigenic mineral systems these processes overlap. A diagnostic principle is suggested, permitting a qualitative or semiquantitative discrimination between marine authigenic minerals crystallized from dissolved species, which have spent a long time in solution on the one hand, and the same minerals generated from solutions, near their source on the other. Extensive data are available for the manganese and iron oxide minerals forming manganese nodules. It is indicated on the basis of their composition and structure that many of the nodules found in the vicinity of the continents are made up essentially of manganese derived from continental weathering. In contrast to this group, all of the nodules found in the Pacific area of submarine vulcanism display the criteria for rapid precipitation near the source of solution. The distribution of barium minerals over the deep ocean floor is discussed.The same diagnostic principle is suggested for application to these solids, in order to discriminate between baryte and harmotome crystallized near the source of barium- rich, acidic vulcanites, and the same minerals formed from continental solution with passage through the biosphere. In the case of the authigenic aluminosilicates it is found that many of the framework elements (Si and particularly Al) have low passage time through solution, and the major fraction of these elements is consequently removed from solution in the vicinity of the eruptive source materials. Extensive modification of the crystal structures, however, takes place over long periods of time, adding particularly cations from sea water, and probably to some extent silica from siliceous fossils, which on their decay on the ocean floor appear to contribute to the silicate framework of growing zeolites. The marked fractionation of the rare earth ions between coexisting phases is pointed out, with discussion of the potential use of this phenomenon to indicate the processes of formation. The use of the hafnium/zirconium ratio as a tracer for the igneous source type is suggested, and the application of ideally imperfect tracers to establish the varying relative importance of volcanic versus halmeic source of marine minerals is discussed in general.
    Keywords: ALB-13; ALB-2; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-2; ALBTR-4711; ALBTR-4721; Chromium; Cobalt; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD4; DWHD72; Event label; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Spencer F. Baird
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 19
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    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
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  • 20
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    In:  Supplement to: Frondel, C; Marvin, U B; Ito, J (1960): New occurrences of todorokite. American Mineralogist, 45(11-12), 1167-1173, http://www.minsocam.org/ammin/AM45/AM45_1167.pdf
    Publication Date: 2023-08-28
    Description: Chemical, x-ray and other data are given for todorokite, (Mn, Mg, Ca, Ba, Na, K)2.Mn5O12.3H2O, from Charco Redondo, Cuba, Farragudo, Portugal, and Hüttenberg, Austria. Additional localities at Romanèche, France, Saipan Island, Bahia, Brazil and Sterling Hill, New Jersey, are noted. Delatorreite of Simon and Straczek (1958) is identical with todorokite.
    Keywords: Austria; Barium oxide; Calcium oxide; Charco_Redondo_S; Cobalt oxide; Copper(II) oxide; Cuba; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; Farragudo_F; Huttenberg_F; Iron oxide, Fe2O3; Latitude of event; Lead oxide; Lithium oxide; Longitude of event; Magnesium oxide; Manganese dioxide; Manganese oxide; Nickel oxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Portugal; Potassium oxide; Sample ID; Silicon dioxide; Sodium oxide; Strontium oxide; Sulfur trioxide; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 58 data points
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  • 21
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1960): Southern Borlerland (SOB) Expedition, Core List, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 4 pp, https://www.ngdc.noaa.gov/mgg/curator/data/spencer_f._baird/sob/15995008.pdf
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken on the Southern Borderland (SOB) Expedition in February-March 1960 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 34 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; SOB; SOB-005D; SOB-006D; SOB-007D; SOB-008G; SOB-010D; SOB-013D; SOB-020D; SOB-022D; SOB-025D; SOB-027D; SOB-030D; SOB-031GA; SOB-033D; SOBO03BD-005D; SOBO03BD-006D; SOBO03BD-010D; SOBO03BD-013D; SOBO04BD-020D; SOBO04BD-022D; SOBO04BD-025D; SOBO04BD-027D; SOBO04BD-030D; SOBO04BD-033D; Southern Borderland; Spencer F. Baird; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 153 data points
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  • 22
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1960): Physical and Chemical Data Vermilion Sea Expedition 13 April - 29 May 1959, (R/V Spencer F. Baird). SIO Reference, 60-51, 26 pp, https://escholarship.org/uc/item/2jg3k3d0
    Publication Date: 2023-08-28
    Description: On Vermilion Sea Expedition two research vessels among which the R/V Spencer F. Baird conducted a geological and geophysical exploration of the Gulf of California from February to May, 1959. Support was obtained from the Office of Naval Research and the Bureau of Ships of the U. S. Navy and from a grant of the American Petroleum Institute. Study of the canyons was one feature of the first part of the expedition. Submarine canyon studies were directed by Francis P. Shepard, Professor of Submarine Geology, aboard the research vessel Spencer F. Baird. The expedition found that the narrow channel between Angel de la Guarda Island, toward the head of the Gulf, and the peninsula is scoured almost free of sediments by strong currents. On the other side of Angel de la Guarda Island, between it and the mainland, one of the dredge hauls brought up a manganese nodule. It came from a depth of approximately 1500 feet. This is the shallowest water in which the nodules have been found. Studies have been under way some time on the feasibility of mining such nodules from the sea floor. They contain cobalt, nickel, copper and other valuable metals. (also in, Scripps Institution of Oceanography Vermilion Sea Expedition to the Gulf of California, http://library.ucsd.edu/dc/object/bb34484017)
    Keywords: B1 VS-78; Comment; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Photo/Video; Position; PV; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Station 17-L2502; Station 17-L2503; Station 17-L2504; Station 17-L2505; Station 17-L2506; Station 19-L2507; Station 19-L2508; Substrate type; TRAWL; Trawl net; Uniform resource locator/link to image; VERMILION_SEA; Vermilion Sea, Pacific Ocean; VS BII-35; VSS17PH-L2502; VSS17PH-L2503; VSS17PH-L2504; VSS17PH-L2505; VSS17PH-L2506; VSS19PH-L2507; VSS19PH-L2508; VSS35D; VSS78D
    Type: Dataset
    Format: text/tab-separated-values, 89 data points
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  • 23
    Publication Date: 2023-08-28
    Description: The cores and dredges described in this report were taken during the Vema 16 Expedition from October 1959 until September 1960 by the Lamont Geological Observatory, Columbia University from the R/V Vema. An approximate total of 300 cores, dredges and camera stations were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; Identification; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TRAWL; Trawl net; Uniform resource locator/link to image; V16; V16-100; V16-103; V16-104; V16-105; V16-106; V16-108; V16-10C; V16-11; V16-119; V16-121; V16-126; V16-127; V16-128; V16-129; V16-130; V16-131; V16-132; V16-133; V16-134; V16-136; V16-137; V16-139; V16-15; V16-17SBT; V16-18; V16-187; V16-188; V16-189; V16-19; V16-190; V16-192; V16-197; V16-198; V16-199; V16-19SBT; V16-20; V16-202; V16-207; V16-208; V16-209; V16-20SBT; V16-211; V16-218; V16-22; V16-222; V16-22SBT; V16-23; V16-233; V16-242; V16-25C; V16-26; V16-27; V16-27C; V16-29SBT; V16-31; V16-34SBT; V16-35SBT; V16-38; V16-3PD; V16-3SBT; V16-4; V16-41; V16-41C; V16-41SBT; V16-42; V16-42SBT; V16-44; V16-45; V16-47; V16-53; V16-54; V16-55; V16-57; V16-59; V16-60; V16-61; V16-67; V16-69; V16-70; V16-71; V16-77; V16-78; V16-80; V16-81; V16-83; V16-87; V16-88; V16-8SBT; V16-90; V16-91; V16-97; V16-98; V16-9C; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 2368 data points
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  • 24
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    In:  Supplement to: Woods Hole Oceanographic Institution (1960): R/V Atlantis Cruise 260 - Descriptions of cores. unpublished, https://www.dla.whoi.edu/catalog/rv-atlantis-ketch-cruise-260-1960-10-29-1960-11-07
    Publication Date: 2023-08-28
    Description: The cores described here were taken during the R/V Atlantis Cruise 260 from October until November 1960 by the Woods Hole Oceanographic Institution at the Muir Seamount. A total of 27 cores and dredges were recovered and are available at Woods Hole Oceanographic Institution for sampling and study.
    Keywords: AT260; AT260-7D; AT260-8D; AT260-9D; Atlantis (1931); Bermuda Rise; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 25
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    In:  Supplement to: Needleman, Stanley M (1960): Soil science studies at Centrum Sø, northeast Greenland, 1960. Polarforschung, 30(1/2), 33-41, hdl:10013/epic.29211.d001
    Publication Date: 2024-06-10
    Description: During the period May to August 1960, an Air Force scientific field party conducted earth science studies and tested a raised sand terrace, located about 224 km south of Station Nord, Northeast Greenland. The operation staged from Thule Air Force Base was climaxed by successful test Iandings on the terrace by C-119 and C-130 aircraft. Significant data were obtained from related investigations on a typical arctic lake, ice-free soils, meteorology, engineering geology, geomorphology, and electrical resistivity of soils.
    Keywords: 20S-15N; California bearing ratio; Centrum Sø, notheast Greenland; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Geological profile sampling; GEOPRO; Profile ID; Temperature, soil; Thickness; Water content, dry mass
    Type: Dataset
    Format: text/tab-separated-values, 119 data points
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  • 26
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    In:  Supplement to: SCRIPPS Institution of Oceanography (1960): TETHYS (1960) Expedition, June-July 1960, List of core and dredge samples, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 7 pp, https://www.ngdc.noaa.gov/mgg/curator/data/spencer_f._baird/tethys/15005002.pdf
    Publication Date: 2024-06-26
    Description: The cores and dredges described in this report were taken on the TETHYS Expedition from June 1960 until July 1960 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 124 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Position; Quantity of deposit; Sample ID; Sediment type; Size; Spencer F. Baird; Substrate type; TET_27G-B; TET-10G; TET-21G; TET-22G; TET-24G; TET-28G; TET-54G; TETH01BD; TETH01BD-010G; TETH02BD; TETH02BD-021G; TETH02BD-022G; TETH02BD-024G; TETH02BD-027G-B; TETH02BD-028G; TETH02BD-054G; TETHYS_1; TETHYS_2
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 27
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    In:  Supplement to: Kindle, Edward Martin (1932): Lacustrine concretions of manganese. American Journal of Science, 5(24), 496-504, https://doi.org/10.2475/ajs.s5-24.144.496
    Publication Date: 2023-08-28
    Description: A pancake-shaped concretion from Ship Harbour Lake, a small freshwater lake in eastern Nova Scotia (now named Lake Charlotte) is part of collection sent to the National Museum of Canada by Mr. R. A. Logan, of the Pan American Airvays. These concretions are of similar to the well-known marine concretions with a composition similar to wad. These are known only from abyssmal depths of the sea in the red clay deposits, while the present concretions occur in very shallow lake waters. They should be of interest to geologists, who may be concerned with the rather difficult problem which some concretions raise of distinguishing between concretions of syngenitic and epigenetic origin.
    Keywords: Aluminium oxide; Calcium oxide; Canada; Carbon dioxide; Event label; Grab; GRAB; Heavy metals; Iron oxide, Fe2O3; Iron oxide, FeO; Lake_Charlotte-S; Latitude of event; Longitude of event; Magnesium oxide; Manganese dioxide; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample elevation; Silicon dioxide; Water in rock; Wet chemistry
    Type: Dataset
    Format: text/tab-separated-values, 11 data points
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  • 28
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    In:  Supplement to: Chumley, James (1932): Report on the deposit-samples collected during the "Michael Sars" North Atlantic Deep-Sea Expedition 1910. In: Report on the scientific results of the "Michael Sars" north Atlantic deep-sea expedition 1910, carried out under the auspices of the Norwegian government and the superintendence of Sir John Murray, K.C.B., and Dr. Johan Hjort. The Trustees of the Bergen museum, Bergen. Volume 1, 12 pp, https://doi.org/10.5962/bhl.title.11322
    Publication Date: 2023-08-28
    Description: The deposit-samples and rock specimens brought home by the "Michael Sars" were received in the Challenger Office shortly after the return of the expedition, and upon examination the rock specimens proved to be so numerous and to offer so many points of interest that Dr. B. N. Peach, F. R. S., was requested to report upon them. A brief note on his results appeared in "The Depths of the Ocean" (London, Macmillan, 1912), pp. 202-209, and his detailed report was published in the Proc. Roy. Soc. Edin., vol. XXXII., pp. 262—291, 1912. When the author met Dr. Hjort in London in May 1914 he desired me to prepare, for publication in the series of Reports on the scientific Results of the "Michael Sars" North Atlantic Expedition, descriptions of the deposit samples, including for each station a brief summary of Dr. Peach's observations on the rock-specimens obtained. The accompanying Report shows that the "Michael Sars" expedition has made a notable contribution to our knowledge regarding the materials covering the floor of the North Atlantic Ocean.
    Keywords: Date/Time of event; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; Elevation of event; Event label; Latitude of event; Longitude of event; Michael Sars (1900); MS1910; MSARS-48; MSARS-58; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Size; South Atlantic Ocean; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 14 data points
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