Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1747
Seismic-reflection data from R/V FARNELLA cruises FRNL82-7, FRNL85-1, FRNL85-2, and FRNL85-3A in the U.S. Gulf of Mexico EEZ Seismic-reflection data from R/V FARNELLA cruises FRNL82-7, FRNL85-1, FRNL85-2, and FRNL85-3A in the U.S. Gulf of Mexico EEZ
During the winter of 1982 and the summer and early fall of 1985, the U.S. Geological Survey (USGS) in cooperation with the Institute of Oceanographic Sciences of the United Kingdom collected approximately 30,508 line kilometers of seismic-reflection data in the U.S. Gulf of Mexico Exclusive Economic Zone (EEZ) as part of a USGS program to map the EEZ. In water depths exceeding 3,000 m...
Authors
D.C. Twichell, B.A. McGregor, D.J. Lubinski
Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies
No abstract available.
Authors
Paul Huddlestun, Vernon J. Henry, Judith A. Commeau, Jana Da Silva, F.T. Manheim, Peter Popenoe, James R. Herring
Chemical composition of ferromanganese crusts in the world ocean: a review and comprehensive database Chemical composition of ferromanganese crusts in the world ocean: a review and comprehensive database
A comprehensive database of chemical and mineralogical properties for ferromanganese crusts collected throughout the Atlantic, Pacific, and Indian Oceans, and has been assembled from published and unpublished sources which provide collection and analytical information for these samples. These crusts, their chemical compositions and natural distribution, have been a topic of interest to...
Authors
Frank T. Manheim, Candice M. Lane-Bostwick
Flow separation of currents in shallow water Flow separation of currents in shallow water
Flow separation of currents in shallow coastal areas is investigated using a boundary layer model for two-dimensional (depth-averaged) tidal flow past an elliptic headland. If the shoaling region near the coast is narrow compared to the scale of the headland, bottom friction causes the flow to separate just downstream of the point where the pressure gradient switches from favoring to...
Authors
Richard P. Signell
The Blake Plateau Basin and Carolina Trough The Blake Plateau Basin and Carolina Trough
Presently, the continental margin of the southeastern United States (Fig. 1) forms a zone of transition between the actively building, steep-fronted carbonate platform of the Bahamas and the typical eastern North American terrigenous clastic-dominated, drowned, shelf-slope-rise configuration. This region of the continental margin is underlain by two major sedimentary basins—the Blake...
Authors
William P. Dillon, Peter Popenoe
Cobalt in ferromanganese crusts as a monitor of hydrothermal discharge on the Pacific sea floor Cobalt in ferromanganese crusts as a monitor of hydrothermal discharge on the Pacific sea floor
Ferromanganese oxide crusts, which accumulate on unsedimented surfaces in the open ocean1–6, derive most of their metal content from dissolved and particulate matter in ambient bottom water7,8, in proportions modified by the variable scavenging efficiency of the oxide phase for susceptible ions9. They differ in this respect from abyssal nodules, much of whose metals are remobilized from...
Authors
F.T. Manheim, C.M. Lane-Bostwick
Mineral resources of the U.S. Atlantic continental margin Mineral resources of the U.S. Atlantic continental margin
Most geologic materials may be usable resources in some form and at some time, whether it be for general land fill and aggregate, beach replenishment, construction material, or as a source of metals and fuels. Thus, most natural materials occurring within the Atlantic continental margin are resources, defined as “materials, including those only surmised to exist, that have present or...
Authors
Stanley R. Riggs, Frank T. Manheim
A geologic overview of Cape Cod; a field trip guide A geologic overview of Cape Cod; a field trip guide
No abstract available.
Authors
R. N. Oldale
Late Pleistocene drainage systems beneath Delaware Bay Late Pleistocene drainage systems beneath Delaware Bay
Analyses of an extensive grid of seismic-reflection profiles, along with previously published sedimentary data and geologic information from surrounding coastal areas, outline the ancestral drainage systems of the Delaware River beneath lower Delaware Bay. Major paleovalleys within these systems have southeast trends, relief of 10-35 m, widths of 1-8 km, and axial depths of 31-57 m below...
Authors
H.J. Knebel, R.C. Circe
Late Wisconsinan-Holocene paleogeography of Delaware Bay; a large coastal plain estuary Late Wisconsinan-Holocene paleogeography of Delaware Bay; a large coastal plain estuary
Analyses of an extensive grid of seismic reflection profiles along with previously published core data and modern sedimentary environment information from surrounding coastal areas permit an outline of the paleogeography of the large Delaware Bay estuary during the last transgression of sea level. During late Wisconsinan times, the Delaware River system eroded a dendritic drainage...
Authors
H.J. Knebel, C.H. Fletcher, J.C. Kraft
Options for radioactive and other hazardous waste siting within the U. S. Exclusive Economic Zone Options for radioactive and other hazardous waste siting within the U. S. Exclusive Economic Zone
Some areas of the E.E.Z. (Exclusive Economic Zone) offer technical, political and economic options that may complement existing approaches to hazardous waste storage and disposal.
Authors
Frank T. Manheim, Allyn Vine
Elephant teeth from the western Gulf of Maine and their implications Elephant teeth from the western Gulf of Maine and their implications
No abstract available.
Authors
R. N. Oldale, F.C. Whitmore, J.R. Grimes