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  • 1960-1964  (438,949)
  • 1950-1954  (228,318)
  • 1945-1949  (130,850)
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Year
  • 1
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    Annotated record of the detailed examination of Mn deposits from the Swedish Deep Sea Expedition (1951)
    PANGAEA
    In:  Supplement to: Nybelin, Orvar (1951): Introduction and Station List. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume II. Swedish Natural Science Research Council Stockholm 23 - Sweden, 1-28
    Details
    Publication Date: 2024-06-26
    Description: The cores and dredges described in this report were taken during the Swedish Deep Sea Expedition from July 1947 until October 1948 aboard the S/S Albatross (Boström). A total of 370 cores and trawls during this World circumnavigation.
    Keywords: Albatross IV (1963); Comment; Core; CORE; core_43; core_44; core_45; core_46; core_47; core_48; core_50A; core_51; core_52; core_53; core_56; core_57; core_69; core_70; core_72; core_76; core_80; core_81; core_82; core_87; core_89; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; 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; NODC-0418; North Pacific Ocean; Position; Quantity of deposit; Sample ID; SDSE_065; SDSE_066; SDSE_068; SDSE_069; SDSE_070; SDSE_073; SDSE_076; SDSE_078; SDSE_079; SDSE_081; SDSE_086; SDSE_087; SDSE_102; SDSE_104; SDSE_105-2; SDSE_114-2; SDSE_125-2; SDSE_127-2; SDSE_128; SDSE_136-2; SDSE_139-2; SDSE_373-2; Sediment type; Size; South Atlantic Ocean; South Pacific Ocean; Substrate type; SwedishDeepSeaExpedition; TRAWL; Trawl net; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
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  • 2
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    (Table, page 742) Radium concentration in a manganese nodule found buried in a red clay core from the Central Pacific Ocean (1953)
    PANGAEA
    In:  Supplement to: Kröll, Victor (1953): Vertical Distribution of Radium in Deep-Sea Sediments. Nature, 171(4356), 742-742, https://doi.org/10.1038/171742a0
    Details
    Publication Date: 2024-06-26
    Description: The surprisingly high content of radium in certain deep-sea sediments discovered nearly fifty years ago by J. Joly remained unexplained until 1937, when H. Pettersson suggested an ocean-wide precipitation of ionium from sea water on to the ocean bottom as its origin. Extensive radium measurements on deep-sea cores raised by the Swedish Deep-Sea Expedition carried out in this institute by Pettersson, T. Bernert and me did not confirm the regular vertical distribution of radium reported by other workers. An expected rise in radium content from moderate values in the uppermost surface layers to a maximum corresponding to a radioactive equilibrium between precipitated ionium and ionium-supported radium generally occurred; but the maximum was not followed by the theoretical exponential decline downwards governed by the rate of decay of ionium, to 50 per cent in 83,000 years, to 25 per cent in 166,000 years, etc. Instead, a number of secondary maxima of radium content separated by equally pronounced minima were observed (see graph), which could not well be explained as due to intervening changes in the rate of total sedimentation. Another explanation offered was that ionium and radium are not in radioactive equilibrium; that is, the assumption underlying the use of measurements of radium as indicating the concentration in the same layer of its mother element is unjustified.
    Keywords: Albatross IV (1963); Core; CORE; core_87; Deposit type; DEPTH, sediment/rock; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North Pacific Ocean; Radium; SDSE_136-2; SwedishDeepSeaExpedition
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 3
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    (Appendix Table 1) Physical oceanography during the Swedish Deep Sea Expedition with R/V Albatross in 1947-1948 (1951)
    PANGAEA
    Details
    Publication Date: 2024-06-26
    Keywords: Albatross IV (1963); Alboran Sea; Arabian Sea; Canarias Sea; CTD, handheld; Date/Time of event; Density, sigma, in situ; DEPTH, water; Eastern Basin; Elevation of event; Event label; Flores Sea; Gases, dissolved; Gulf of Aden; hCTD; Indian Ocean; Lakshadweep Sea; Latitude of event; Longitude of event; NODC-0418; North Pacific Ocean; Number; Pacific Ocean; pH; Philippine Sea; Phosphate; Red Sea; Salinity; SDSE_043CTD; SDSE_045CTD; SDSE_047CTD; SDSE_048CTD; SDSE_049CTD; SDSE_052CTD; SDSE_055CTD; SDSE_058CTD; SDSE_059CTD; SDSE_060CTD; SDSE_062CTD; SDSE_063CTD; SDSE_065CTD; SDSE_067CTD; SDSE_069CTD; SDSE_070CTD; SDSE_072CTD; SDSE_074CTD; SDSE_076CTD; SDSE_077CTD; SDSE_078CTD; SDSE_079CTD; SDSE_080CTD; SDSE_081CTD; SDSE_082CTD; SDSE_084CTD; SDSE_085CTD; SDSE_086CTD; SDSE_087CTD; SDSE_088CTD; SDSE_089CTD; SDSE_090CTD; SDSE_091CTD; SDSE_093CTD; SDSE_094CTD; SDSE_102CTD; SDSE_105CTD; SDSE_108CTD; SDSE_111CTD; SDSE_113CTD; SDSE_115CTD; SDSE_116CTD; SDSE_119CTD; SDSE_121CTD; SDSE_122CTD; SDSE_123CTD; SDSE_126CTD; SDSE_128CTD; SDSE_129CTD; SDSE_130CTD; SDSE_131CTD; SDSE_133CTD; SDSE_135CTD; SDSE_137CTD; SDSE_138CTD; SDSE_143CTD; SDSE_150CTD; SDSE_157CTD; SDSE_162CTD; SDSE_173CTD; SDSE_183-184CTD; SDSE_190CTD; SDSE_196CTD; SDSE_200CTD; SDSE_202CTD; SDSE_204CTD; SDSE_205CTD; SDSE_206CTD; SDSE_207CTD; SDSE_208CTD; SDSE_211CTD; SDSE_213CTD; SDSE_216CTD; SDSE_220CTD; SDSE_223CTD; SDSE_225CTD; SDSE_227CTD; SDSE_228CTD; SDSE_232CTD; SDSE_235CTD; SDSE_240CTD; SDSE_243CTD; SDSE_244CTD; SDSE_246CTD; SDSE_247CTD; SDSE_248CTD; SDSE_251CTD; SDSE_254CTD; SDSE_261CTD; SDSE_262CTD; SDSE_263CTD; SDSE_266CTD; SDSE_267CTD; SDSE_268CTD; SDSE_269CTD; SDSE_270CTD; SDSE_271CTD; SDSE_272CTD; SDSE_285CTD; SDSE_301CTD; SDSE_306CTD; SDSE_307CTD; SDSE_308CTD; SDSE_309CTD; SDSE_314CTD; SDSE_319CTD; SDSE_321CTD; SDSE_322CTD; SDSE_323CTD; SDSE_325CTD; SDSE_326CTD; SDSE_327CTD; SDSE_328CTD; SDSE_330CTD; SDSE_332CTD; SDSE_333CTD; SDSE_335CTD; SDSE_336CTD; SDSE_337CTD; SDSE_340CTD; SDSE_342CTD; SDSE_343CTD; SDSE_344CTD; SDSE_345CTD; SDSE_347CTD; SDSE_349CTD; SDSE_351CTD; SDSE_353CTD; SDSE_354CTD; SDSE_357CTD; SDSE_360CTD; SDSE_362CTD; SDSE_367CTD; SDSE_371CTD; SDSE_373CTD; SDSE_384CTD; SDSE_387CTD; SDSE_400CTD; Silicate; South Atlantic Ocean; South Pacific Ocean; Strait of Gibraltar; SwedishDeepSeaExpedition; Temperature, water; Western Basin
    Type: Dataset
    Format: text/tab-separated-values, 15537 data points
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  • 4
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    (Table 1, page 1376) Chemical analyses of manganese nodules and crusts from the Pacific Ocean (1961)
    PANGAEA
    In:  Supplement to: Mero, John L (1961): Sea floor manganese nodules. Unpublished report to the Daniel C. Jackling Award Fellowship Committee; American Institute of Mining, Metallurgical, and Petroleum Engineers (AIME), https://www.ngdc.noaa.gov/mgg/geology/data/1599/15995009/15995009.pdf
    Details
    Publication Date: 2024-06-26
    Description: A compilation of chemical analyses of Pacific Ocean nodules using an x-ray fluorescence technique. The equipment used was a General Electric XRD-5 with a tungsten tube. Lithium fluoride was used as the diffraction element in assaying for all elements above calcium in the atomic table and EDDT was used in conjunction with a helium path for all elements with an atomic number less than calcium. Flow counters were used in conjunction with a pulse height analyzer to eliminate x-ray lines of different but integral orders in gathering count data. The stability of the equipment was found to be excellent by the author. The equipment was calibrated by the use of standard ores made from pure oxide forms of the elements in the nodules and carefully mixed in proportion to the amounts of these elements generally found in the manganese nodules. Chemically analyzed standards of the nodules themselves were also used. As a final check, a known amount of the element in question was added to selected samples of the nodules and careful counts were taken on these samples before and after the addition of the extra amount of the element. The method involved the determination and subsequent use of absorption and activation factors for the lines of the various elements. All the absorption and activation factors were carefully determined using the standard ores. The chemically analyzed samples of the nodules by these methods yielded an accuracy to at least three significant figures.
    Keywords: 248; Acapulco Trench, Pacific ocean; ALB-13; ALB-173; ALB-2; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; Albatross IV (1963); ALBTR-13; ALBTR-173; ALBTR-2; ALBTR-31; ALBTR-4622; ALBTR-4656; ALBTR-4658; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; Aluminium; Argo; B1 VS-78; Barium; Calcium; Calculated from weight loss after ignition at 450 °C; CAP-50BG-1; CAPB01BD-050BG-01; CAPRICORN-B; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-248; CHA-252; CHA-276; CHA-285; CHA-289; CHA-299; CHA-302; Challenger1872; CHUB01BD; CHUB01BD-001G; CHUB01BD-002G; CHUB01BD-003G; CHUB01BD-009G; CHUB01BD-017G; CHUB01BD-019G; CHUB01BD-039G; CHUB-1; CHUB-11G; CHUB-17; CHUB-19; CHUB-2; CHUB-3; CHUB-39; CHUB5; CHUB-7G; CHUB-9; CHUBASCO; Cobalt; Copper; Core; CORE; core_48; CRU9121; CUSP1954; CUSP8P; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-054G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD7; DWBG147B; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG54; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHH4; Epce; Event label; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Henderson Seamount, Pacific Ocean; Horizon; Identification; Iron; Lead; Loss on ignition; Manganese; MDPC01HO-005-02; MDPC02HO-032; MDPC02HO-MP-025F-2; MDPC02HO-MP-026A-3; MDPC02HO-MP-033K; MDPC02HO-MP-037A; MDPC03HO-MP-043D; MIDPAC; Molybdenum; Monegasque Trawl; MONS01AR-MONS08AR; MONS08AR-139D; MONSOON; MPC-25F-2; MPC-26A-3; MPC-32; MPC-33K; MPC-37A; MPC-43D; MPC-5-2; MSN-07G; MSN-10G; MSN-11G; MSN-139D; MSN-17G; MSN-18G; MSN G; MSNK; MSN Q; MSN S; MTRW; NEL-HEND; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North-East Pacific Ocean; Northern_Holiday; North Pacific Ocean; Northwest Pacific Ocean; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Page(s); PAS-19121; Phosphorus; Potassium; Sample code/label; SDSE_073; Sediment type; Silicon; Size; SOB; SOB-005D; SOB-010D; SOB-013D; SOB-020D; SOB-022D; SOB-025D; SOB-027D; SOBO03BD-005D; SOBO03BD-010D; SOBO03BD-013D; SOBO04BD-020D; SOBO04BD-022D; SOBO04BD-025D; SOBO04BD-027D; Southern Borderland; Specific gravity; Spencer F. Baird; Strontium; SwedishDeepSeaExpedition; Titanium; TRANS_14C; TRANS_14D; TRAWL; Trawl net; UNK_BH2; UNK_MS; VERMILION_SEA; Vermilion Sea, Pacific Ocean; Vityaz (ex-Mars); Vityaz-29; VITYAZ4191-TR; VITYAZ4199-TR; VITYAZ4217-TR; VITYAZ4221-TR; VS BII-35; VSS35D; VSS78D; Water in rock; WIG-6; WIGWAM; Wired profile sonde; WP; X-ray fluorescence (XRF); Zinc
    Type: Dataset
    Format: text/tab-separated-values, 2243 data points
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  • 5
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    Annotated record of the detailed examination of Mn deposits from JOIDES Preliminary Cruise with M/V Caldrill I on the Blake Plateau (1964)
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    Details
    Publication Date: 2024-06-26
    Description: In May 1964 the Institute of Marine Science (University of Miami), Scripps Institution of Oceanography (University of California), Woods Hole Oceanographic Institution, and Lamont Geological Observatory (Columbia University) joined in the establishment of the JOINT OCEANOGRAPHIC INSTITUTIONS DEEP EARTH SAMPLING (JOIDES) program. The long range purpose of this organization is to obtain continuous core samples of the entire sedimentary column from the floors of the oceans. It was decided that initial efforts would be limited to water depths of less than 1000 fathoms (6000 feet), and tentative locations were selected for drilling operations off the eastern, western and Gulf coasts of the United States. Near the end of December 1964 it was found that the M/V Caldrill I, a drilling vessel capable of working to depths of 6000 feet, was to engage in drilling operations on the Grand Banks of Newfoundland during the summer of 1965 for the Pan American Petroleum Corporation. Thus it was agreed to organize a drilling program along the track of Caldrill between California and the Grand Banks. Selection was made of an area on the continental shelf and the Blake Plateau off Jacksonville, Florida. Based upon many previous geological and geophysical investigations by the participating laboratories, a considerable body of knowledge had been gained about this region of the continental-oceanic border. For this initial program of JOIDES, the Lamont Geological Observatory was chosen as the operating institution with J. L. Worzel as principal investigator, and C. L. Drake and H. A. Gibbon as program planners.
    Keywords: Blake Plateau, Atlantic Ocean; Caldrill I; Comment; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; JOID-6; JOIDES_prelim; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample code/label; Sample ID; Sediment type; Size; Substrate type
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 6
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    Annotated record of the detailed examination of Mn deposits from TETHYS Expedition stations (1960)
    PANGAEA
    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
    Details
    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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  • 7
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    Results of isotopic analysis of planktonic foraminifera from sediment core 189 of the Swedish Deep-Sea Expedition (Table I) (1954)
    PANGAEA
    In:  Supplement to: Emiliani, Cesare (1954): Pleistocene temperature variations in the Mediterranean. Quarternaria, 2, 87-97
    Details
    Publication Date: 2024-06-26
    Description: For temperature investigations, a core in the Mediterranean Sea (No 189 of the Swedish Deep-Sea Expedition 1947-1948) was sampled at approximately 10 m intervals. Globigerina dubia, G. inflata and Globigerinoides rubra were seperated from each sample and their test were investigated for stable oxygen isotopic measurement. Oxygen isotopic analysis showed the following: 1) Ten stages are indicated. 2) The temperature minimum of stage 2 corresponds to a racliocarbon age of 17,200 years. 3) Temperature maxima of odd stages are about equal to the modern August mean, except that of stage 5 which is considerably higher and, probably reflects the influx of ice melt water. 4) Temperature minima of even stages are all very low, especially that of stage 2, and reflect conditions similar to those now prevailing around Newfoundland. 5) The temperature record indicates that during most of the time covered by the core, the Mediterranean was cooler than at present and that conditions similar to the present occurred only during comparatively short intervals. 6) Minor temperature fluctuations occur, especially in the warmer stages, which are of doubtful significance. 7) An average rate of sedimentation of 4.3 cm/1000 years is indicated for the whole core.
    Keywords: Albatross IV (1963); core_189; DEPTH, sediment/rock; Globigerina dubia, δ18O; Globigerina inflata, δ18O; Globigerinoides rubra, δ18O; NODC-0418; PC; Piston corer; SDSE_276; South Levantine Basin; SwedishDeepSeaExpedition
    Type: Dataset
    Format: text/tab-separated-values, 121 data points
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  • 8
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    Composition of Pacific sea-floor manganese nodules (1964)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Description: This collection of data on manganese nodules on the floor of the Pacific Ocean represents all the information that was available to the authors in May, 1964. It is compiled from both published references and original data. No attempt is made here to generalize or to speculate on the origin of the manganese or associated elements further discussion of these aspects of the subject may be had by reference to the literature.
    Keywords: ALB-13; ALB-173; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-31; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-299; CHA-302; Challenger1872; CHIN02BD; CHIN02BD-016G; CHINOOK; CHNK-16G; CHUB01BD; CHUB01BD-002G; CHUB01BD-034G; CHUB-2; CHUB-34; CHUB5; CHUBASCO; Core; CORE; DNWB0ABD; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBG147B; DWBG16; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHG34; DWHH4; DWHH92; Eastern Basin, Pacific Ocean; Epce; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; MDPC02HO-MP-025F-1; MDPC02HO-MP-033D; MDPC03HO-MP-043A; MIDPAC; MPC-25F-1; MPC-33D; MPC-43A; NAGA; NAGA8C; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; SIO-DX-1; Spencer F. Baird; Stranger; TRAWL; Trawl net; V15; V15-126; Vema; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; VITYAZ4289-TR
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    Chemical analyses of manganese nodules and crusts from the Pacific Ocean using atomic emission spectroscopy (1964)
    PANGAEA
    Details
    Publication Date: 2024-06-25
    Keywords: ALB-13; ALB-173; ALB-31; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-31; ALBTR-4660; ALBTR-4662; ALBTR-4676; ALBTR-4681; ALBTR-4685; ALBTR-4701; ALBTR-4711; ALBTR-4721; Aluminium; Atomic emission spectroscopy (AES); Barium; Bismuth; Boron; Cadmium; Calcium; Calculated from mass/volume; Calculated from weight loss after ignition at 450 °C; CARN_Revelle_46; CARN_Revelle_78; CARN7-150; CARN7-86; CARN-Cruise7; Carnegie; CASC-5D; CASCADIA; CHA-299; CHA-302; Challenger1872; CHIN02BD; CHIN02BD-016G; CHINOOK; CHNK-16G; Chromium; CHUB01BD; CHUB01BD-002G; CHUB01BD-034G; CHUB-2; CHUB-34; CHUB5; CHUBASCO; Cobalt; Copper; Core; CORE; DEPTH, sediment/rock; Description; DNWB0ABD; DNWB0ABD-016G; DNWB0ABD-017G; DNWB0ABD-019G; DNWB0BBD; DNWB0BBD-037G; DNWB0BBD-040G; DNWB0BBD-043G; DNWB0BBD-048G; DNWB0BBD-052G; DNWB0BBD-054G; DNWB0BBD-055G; DNWB0BBD-056G; DNWB0DBD; DNWB0DBD-147GB; DNWH0AHO-004H; DNWH0BHO-034G; DNWH0DHO-092H; DOWNWIND-B1; DOWNWIND-B2; DOWNWIND-B4; DOWNWIND-H; Dredge; Dredge, rock; DRG; DRG_R; DWBD1; DWBD2; DWBD4; DWBD5; DWBD7; DWBG147B; DWBG16; DWBG17; DWBG19; DWBG37; DWBG40; DWBG43; DWBG48; DWBG52; DWBG54; DWBG55; DWBG56; DWBG78; DWHD15; DWHD16; DWHD47; DWHD55; DWHD72; DWHG34; DWHH4; DWHH92; Eastern Basin, Pacific Ocean; Epce; Event label; Gallium; GC; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Horizon; Identification; Iron; Lanthanum; Lead; Loss on ignition; Magnesium; Manganese; MDPC02HO-MP-025F-1; MDPC02HO-MP-033D; MDPC03HO-MP-043A; MIDPAC; Molybdenum; MPC-25F-1; MPC-33D; MPC-43A; NAGA; NAGA8C; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North-East Pacific Ocean; Pacific Ocean; Page(s); Phosphorus; Potassium; Sample code/label; Scandium; Sediment type; Shape; Silicon; Silver; SIO-DX-1; Size; Sodium; Spencer F. Baird; Stranger; Strontium; Thallium; Thorium; Titanium; TRAWL; Trawl net; Uranium; Vanadium; Vityaz (ex-Mars); Vityaz-29; VITYAZ4239-TR; VITYAZ4289-TR; Water content, wet mass; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 1930 data points
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  • 10
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    Statistical grain size parameter of surface samples from Kiel Bay (1961)
    PANGAEA
    In:  Supplement to: Seibold, Eugen; Dill, Robert F; Walger, Eckart (1961): Tauchbeobachtungen und petrographische Untersuchungen zur Sedimentumlagerung in der Kieler Außenförde. Meyniana, 11, 82-96, https://doi.org/10.2312/meyniana.1961.11.82
    Details
    Publication Date: 2024-06-10
    Description: Geological observations, using "free-diving" techniques (Figure I) were made in September, 1960 and March 1961 along two continuous profiles in the outer Kiel Harbor, Germany and at several other spot locations in the Western Baltic Sea. A distinct terrace, cut in Pleistocene glacial till, was found that was covered with varying amounts and types of recent deposits. Hand samples were taken of the sea-floor sediments and grainsize distribution determined for both the sediment as a whole and for its heavy mineral fraction. From the Laboratory and Field observations it was possible to recognize two distinct types of sand; Type I, Sand resulting from transportation over a long period of time and distance and Type 11, Sand resulting from little transportation and found today near to xvhere it was formed. Several criterea related to the agent of movement could be used to classify the nature of the sediment; (1) undisturbed (the sediment Cover of the Pleistocene Terrace is essentially undisturbed), (2) mixed by organisms, (3) transported by water movements (sediment found with ripple marks, etc., and (4) "Scoured" (the movement of individual particles of sediment from around larger boulders causes a slow downward movement or "Creeping" which is due to both the force of gravity and bottom currents. These observations and laboratory studies are discussed concerning their relationship to the formation of residual sediments, the direction of sand transportation, and the intensive erosion on the outer edge of the wave-cut platform found in this part of the Baltic Sea.
    Keywords: buelk; Calculated; Comment; Depth, bathymetric; DEPTH, sediment/rock; DIVER; ECHO; Echosounder; Heavy minerals; off Leuchtturm Bülk, Kieler Bucht, Baltic Sea; Profile ID; Sample ID; Sampling by diver; Sand; Size fraction, statistical value; Smear slide analysis
    Type: Dataset
    Format: text/tab-separated-values, 790 data points
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