Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1757
Offshore and onshore sediment resource delineation and usage for coastal erosion control in Louisiana: The Isles Dernieres and Plaquemines barrier systems Offshore and onshore sediment resource delineation and usage for coastal erosion control in Louisiana: The Isles Dernieres and Plaquemines barrier systems
No abstract available.
Authors
S. Penland, J. Mossa, R.A. McBride, K. Ramsey, J.R. Suter, C.G. Groat, S.J. Williamson
Recent geophysical and geological research in Antarctica related to the assessment of petroleum resources and potential environmental hazards to their development Recent geophysical and geological research in Antarctica related to the assessment of petroleum resources and potential environmental hazards to their development
During the 6-year negotiation of and adoption of the Convention on the Regulation of Antarctic Mineral Resources Activities on June 2, 1988, various countries have increased their attention to the possibility of exploitation of Antarctica's petroleum resources, which are covered by this treaty. However, there are no known petroleum resources in Antarctica, and scientific information is...
Authors
John C. Behrendt
A dolomitized shelf edge hardground in the northern Gulf of Mexico - Reply A dolomitized shelf edge hardground in the northern Gulf of Mexico - Reply
We (Poppe et al., 1990) agree with Gerald Friedman that the anaerobic oxidation of methane is important to the early diagenetic cementation by carbonates, but we feel that a few points need clarification.
Authors
Lawrence J. Poppe, Ronald C. Circe, April K. Vuletich
Major off-axis hydrothermal activity on the northern Gorda Ridge Major off-axis hydrothermal activity on the northern Gorda Ridge
The first hydrothermal field on the northern Gorda Ridge, the Sea Cliff hydrothermal field, was discovered and geologic controls of hydrothermal activity in the rift valley were investigated on a dive series using the DSV Sea Cliff. The Sea Cliff hydrothermal field was discovered where predicted at the intersection of axis-oblique and axis-parallel faults at the south end of a linear...
Authors
Peter A. Rona, Roger P. Denlinger, M. R. Fisk, K. J. Howard, G. L. Taghon, Kim D. Klitgord, James S. McClain, G. R. McMurray, J. C. Wiltshire
Iberian plate kinematics: A jumping plate boundary between Eurasia and Africa Iberian plate kinematics: A jumping plate boundary between Eurasia and Africa
THE rotation of Iberia and its relation to the formation of the Pyrenees has been difficult to decipher because of the lack of detailed sea-floor spreading data, although several models have been proposed1-7. Here we use detailed aeromagnetic measurements from the sea floor offshore of the Grand Banks of Newfoundland to show that Iberia moved as part of the African plate from late...
Authors
S.P. Srivastava, Hans Schouten, W.R. Roest, Kim D. Klitgord, L.C. Kovacs, J. Verhoef, R. Macnab
Origin of Florida Canyon and the role of spring sapping on the formation of submarine box canyons Origin of Florida Canyon and the role of spring sapping on the formation of submarine box canyons
Florida Canyon, one of a series of major submarine canyons on the southwestern edge of the Florida Platform, was surveyed using GLORIA, SeaBeam, and Deep-Tow technologies, and it was directly observed during three DSRV Alvin dives. Florida Canyon exhibits two distinct morphologies: a broad V-shaped upper canyon and a deeply entrenched, flat-floored, U-shaped lower canyon. The flat-...
Authors
Charles K. Paull, Fred N. Spiess, Joseph R. Curray, David C. Twichell
Sediment movement along the U.S. east coast continental shelf-I. Estimates of bottom stress using the Grant-Madsen model and near-bottom wave and current measurements Sediment movement along the U.S. east coast continental shelf-I. Estimates of bottom stress using the Grant-Madsen model and near-bottom wave and current measurements
Bottom stress is calculated for several long-term time-series observations, made on the U.S. east coast continental shelf during winter, using the wave-current interaction and moveable bed models of Grant and Madsen (1979, Journal of Geophysical Research, 84, 1797-1808; 1982, Journal of Geophysical Research, 87, 469-482). The wave and current measurements were obtained by means of a...
Authors
V.D. Lyne, B. Butman, W.D. Grant
United States Geological Survey Yearbook, fiscal year 1989 United States Geological Survey Yearbook, fiscal year 1989
The fiscal year 1989 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.
Authors
Dallas L. Peck, John A. Kelmelis, Charles W. Boning, Richard Z. Poore, Eugene C. Napier, Ernest B. Brunson, K. Lea Ginnodo, G. Gray Tappan, Dean J. Tyler, Donald G. Moore, C.R. Baskin, Charlotte H. Goodson, Wendy R. Hassibe, Betty B. Brodes
Holocene paleoclimatic evidence and sedimentation rates from a core in southwestern Lake Michigan Holocene paleoclimatic evidence and sedimentation rates from a core in southwestern Lake Michigan
Preliminary results of a multidisciplinary study of cores in southwestern Lake Michigan suggest that the materials in these cores can be interpreted in terms of both isostatically and climatically induced changes in lake level. Ostracodes and mollusks are well preserved in the Holocene sediments, and they provide paleolimnologic and paleoclimatic data, as well as biogenic carbonate for...
Authors
Steven M. Colman, Glenn A. Jones, R. M. Forester, D. S. Foster
Effect of wave-current interaction on wind-driven circulation in narrow, shallow embayments Effect of wave-current interaction on wind-driven circulation in narrow, shallow embayments
The effect of wind waves on the steady wind-driven circulation in a narrow, shallow bay is investigated with a two-dimensional (y, z) circulation model and the Grant and Madsen [1979] bottom-boundary layer model, which includes wave-current interaction. A constant wind stress is applied in the along-channel x direction to a channel with a constant cross-sectional profile h(y). The wind...
Authors
Richard P. Signell, Robert C. Beardsley, H. C. Graber, A. Capotondi