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  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(529-H)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, H-39 S. + 5 pl.
    Series Statement: U.S. Geological Survey professional paper 529-H
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(529-B)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: IV, B-44 S. + 1 pl.
    Series Statement: U.S. Geological Survey professional paper 529-B
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
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    PANGAEA
    In:  Supplement to: Pratt, Richard M (1968): Atlantic continental shelf and slope of the United States - Physiography and sediments of the deep-sea basin. U.S. Geological Survey Professional Paper, 529-B, 50 pp, https://pubs.usgs.gov/publication/pp529B
    Publication Date: 2023-08-28
    Description: The major topographic features, or provinces, beyond the continental slope off the Atlantic coast of the United States are (1) Sohm Plain, (2) Hatteras Plain, (3) Nares Plain, (4) Blake Basin, (5) Blake Plateau-Bahama Banks, and (6) Bermuda Rise. The whole of the described area is commonly referred to as the North American Basin. This basin is bounded on the north by Newfoundland Ridge and on the south by Puerto Rico Trench. Topographic features of note within the basin are the divide and the area of depressions between Sohm and Hatteras Plains, the sharply crested Blake Ridge, and the Puerto Rico Ridge. Recently accumulated data on deep-sea oores has given good evidence that the silt and sand covering the abyssal plains are displaced continental sediments in a virtually quartz-free oceanic environment. These sediments were deposited on a primary volcanic bottom. The primary or volcanic bottom is characterized by abyssal hills and seamounts, and the sediment bottom is characterized by abyssal plains, which extend seaward from the continental margins. On the Blake Plateau, bottom photographs and dredge hauls in the axis of the stream show that locally sediment has been removed and the bottom is paved with crusts and nodules of manganese. Photographs and dredged samples from the outer part of the New England Seamount, Chain and Caryn Peak also indicate extensive encrustations of manganese oxide which acts as a binding agent in areas of ooze or other organic debris and thus helps to stabilize the bottom.
    Keywords: AT260; AT260-7D; AT26601; AT266-15C; AT28001; AT280-05C; Atlantic Ocean; Atlantis (1931); Bermuda Rise; 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; Substrate type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Kulm, LaVerne D; von Huene, Roland; Duncan, John R; Ingle, James C; Kling, S A; Musich, L F; Piper, David J W; Pratt, Richard M; Schrader, Hans-Jürgen; Weser, Oscar E; Wise, Sherwood W (1973): Site 172. In: Kulm, L.D.; von Huene, R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVIII, 15-30, https://doi.org/10.2973/dsdp.proc.18.103.1973
    Publication Date: 2023-08-28
    Description: Site 172 was continuously cored to a depth of 24 meters in a sediment pond 140 kilometers south of the Murray fracture zone. The upper 9 meters consist of a moderate brown pelagic clay which changes to a zeolite-rich brown clay, brown clay zeolitite and zeolitite in the lower 9 to 24 meters. An Early Oligocene (35 to 38 my) nannofossil horizon occurs near an extrusive basalt encountered at 24 meters. These sediments are older than the 29 my age indicated by a recent identification of magnetic anomaly 8 in the "disturbed" zone. The age discrepancy suggests that the magnetic anomalies in the "disturbed" zone are still not identified correctly.
    Keywords: 18-172; Comment; Deep Sea Drilling Project; Deposit type; DEPTH, sediment/rock; Description; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Identification; Leg18; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; North Pacific; Position; Quantity of deposit; Sample code/label; Sediment type; Size; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Manheim, Frank T; Pratt, Richard M; McFarlin, P F (1980): Composition and origin of phosphorite deposits of the Blake Plateau. In: Bentor, Y.K. (Ed.), Marine Phosphorites - Geochemistry, Occurrence, Genesis, Society of Economic Paleontologists and Mineralogists, Special Publication, 29, 117-137, https://download.pangaea.de/reference/80812/attachments/Manheim-etal_1980.pdf
    Publication Date: 2023-08-28
    Description: An area of about 22,000 km² on the northern Blake Plateau, off the coast of South Carolina, contains an estimated 2 billion metric tons of phosphorite concretions, and about 1.2 billion metric tons of mixed ferromanganese-phosphorite pavement. Other offshore phosphorites occur between the Blake Plateau and known continental deposits, buried under variable thicknesses of sediments. The phosphorite resembles other marine phosphorites in composition, consisting primarily of carbonate-fluorapatite, some calcite, minor quartz and other minerals. The apatite is optically pseudo-isotropic and contains about 6% [CO3]**2- replacing [PO4]**3- in its structure. JOIDES drillings and other evidence show that the phosphorite is a lag deposit derived from Miocene strata correlatable with phosphatic Middle Tertiary sediments on the continent. It has undergone variable cycles of erosion, reworking, partial dissolution and reprecipitation. Its present form varies from phosphatized carbonate debris, loose pellets, and pebbles, to continuous pavements, plates, and conglomeratic boulders weighing hundreds of kilograms. No primary phosphatization is currently taking place on the Blake Plateau. The primary phosphate-depositing environment involved reducing conditions and required at least temporary absence of the powerful Gulf Stream current that now sweeps the bottom of the Blake Plateau and has eroded away the bulk of the Hawthorne-equivalent sediments with which the phosphorites were once associated.
    Keywords: NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Pratt, Richard M (1967): Photography of seamounts (Chapter 13). In: Hersey, JB (Ed.): Deep Sea Photography, The Johns Hopkins Oceanographic Studies. John Hopkins University Press, 145-148, https://www.vliz.be/en/imis?module=ref&refid=11063
    Publication Date: 2023-08-28
    Description: Seamounts are very effectively studied by deep-sea photography. Each photograph can be considered as a sample point when used in connection with bathymetric surveys, dredge samples, and cores, thus making it possible to delineate and map geologic and biologic zones on a seamount. Seamounts transcend through a great depth range and are characterized by minimal sedimentation which results in exciting and photogenic differences of environment over a short distance, as typified by our studies of Great Meteor and the New England Seamounts.
    Keywords: AT260-8D; Bermuda Rise; Deposit type; DEPTH, sediment/rock; Description; Dredge; DRG; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Position; Quantity of deposit; Sample ID; Sediment type; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 7
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    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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  • 8
    Publication Date: 2023-08-28
    Keywords: AT26601; AT266-05; AT266-18; AT266-21C; Atlantic Ocean; Atlantis (1931); Comment; 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; 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, 21 data points
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  • 9
    Publication Date: 2023-08-28
    Keywords: AT26601; AT266-05; Atlantic Ocean; Atlantis (1931); Cerium; Date/Time of event; DEPTH, sediment/rock; Description; Dredge; DRG; Dysprosium; Elevation of event; Emission spectrometry; Europium; High oxygen indicators; Lanthanum; Latitude of event; Longitude of event; Lutetium; Neodymium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Proustite; Samarium; Sample ID; Terbium; Thulium; Ytterbium; Yttrium
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
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  • 10
    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
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