Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska

Cover of: Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska |

Published by Dept. of the Interior, U.S. Geological Survey, [Books and Open-File Reports Section, distributor] in [Denver, Colo.?] .

Written in English

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Subjects:

  • Marine sediments -- Alaska -- Harrison Bay,
  • Sea ice -- Alaska -- Harrison Bay

Edition Notes

Includes bibliographical references (p. 69-73)

Book details

Statementby Steven A. Fischbein
SeriesOpen-file report -- 87-262, U.S. Geological Survey open-file report -- 87-262
ContributionsGeological Survey (U.S.)
The Physical Object
FormatMicroform
Pagination1 microfiche
ID Numbers
Open LibraryOL13612516M

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ANALYSIS AND INTERPRETATION OF ICE-DEFORMED SEDIMENTS FROM HARRISON BAY, ALASKA By Steven A. Fischbein1 Open-File Report This report was prepared under contract to the U.S. Geological Survey and has not been reviewed for conformity with USGS editorial standards and straligraphic by: 5. Get this from a library.

Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska. [Steven A Fischbein; Geological Survey (U.S.)]. Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska (Open-file report / Department of the Interior, U.S.

Geological Survey) [Fischbein, Steven A] on *FREE* shipping on qualifying offers. Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska (Open-file report / Department of the Interior.

Fischbein, Steven A., "Analysis and Interpretation of Ice-Deformed Sediments from Harrison Bay, Alaska" (). Papers in the Earth and Atmospheric Sciences. Ice sediment interaction has overprinted structural deformation on many of the sediments present in Harrison Bay, and has in some cases obliterated the original lithologic continuity of the Author: Steven Fischbein.

Depositional environments in Harrison Bay range from outer shelf to prodelta and delta front. Ice sediment interaction has overprinted structural deformation on many of the sediments present in Harrison Bay, and has in some cases obliterated the original lithologic continuity of the sediments.

Fischbein, S.A.,Analysis and Alaska book of ice-deformed sediments from Harrison Bay, Alaska: U.S. Geological Survey Open-File Report73 p. Publication Products Report Information.

State of Alaska Alaska / Natural Resources DNR / Geological & Geophysical Surveys DGGS / Publications Pubs / Fischbein, S.A., Fischbein, S.A., Fischbein, S.A., Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska. Buy Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska (Open-file report / Department of the Interior, U.S.

Geological Survey) by Steven A Fischbein (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Steven A Fischbein. "Analysis and Interpretation of Ice-Deformed Sediments from Harrison Ba" by Steven A. Fischbein The surficial sediments present on the continental shelf off the north coast of Alaska in the vicinity of Harrison Bay consist dominantly of fine grained sand, silt.

FISCHBEIN, Steven A. Analysis and Interpretation of Ice-Deformed Sediments from Harrison Bay, Alaska PAVLETICH, Joseph P. Amino-Acid Racemization in Siliceous Sediments from the Southern Ocean CARSON, Scott E. Liquefacation Susceptibility in the San Bernardino Valley and Vicinity, California.

In Harrison Bay, about m 3 of sediment is reworked each year by ice gouging for every square kilometer of the seafloor between water depths of 5 and 18 m. Over 50% of this sediment is moved onshore to the southeast, whereas 35% is moved alongshore to the west.

Analysis and interpretation of ice-deformed sediments from Harrison Bay, (). Analysis of pre-Pleistocene glacigenic rocks: aims and problems. Arctic sea ice as a geological agent. View Steve Fischbein’s profile on LinkedIn, the world's largest professional community.

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Analysis and interpretation of ice-deformed sediments from Harrison Bay, Alaska: Series title: Open-File Report: Series number: DOI: /ofr Edition-Year Published:   Analysis and interpretation of ice- deformed sediments from Harrison Bay, Alaska, U.S.

Geol. Surv. Open-File Rep. 73 pp. Flemming, B.W., Bartolom~i, A. (Eds.), Tidal Signatures in Modern and Ancient Sediments. Alaska book Available in the National Library of Australia collection.

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The objective of this exercise is to interpret the of a seismic data set from the northeast corner of the National Petroleum Reserve of Alaska (NPRA) just south of Harrison Bay on the coast of the Beaufort Sea.

This exercise includes a study of the geometric relationship of sequences, delta migration. Slope failure and subsequent mass movement have been identified on a slope of {degree} to {degree} on the pelagic sediment cap of Horizon Guyot, Mid-Pacific Mountains, in a zone of strong bottom-current activity.

A seismic-reflection survey and submersible investigation of this slope failure. An offset 3D seismic survey in the Harrison Bay area (southeast of the NE-NPRA 3D survey) confirms the presence of giant slides in this area, some of which are related to the well-known Fish Creek Slide (Homza, ).

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The purpose of this paper is to link information about the Shublik Formation in outcrops in and near the Arctic National Wildlife Refuge and cores from the National Petroleum Reserve in Alaska (NPRA) from Parrish et al. () with an interpretation of the sequence stratigraphy based on cores and well logs from Prudhoe Bay by Hulm ().We provide measured sections and core descriptions from.

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Carlson, Paul R., Barnes, Peter W., Hayden, Eran, and Carkin, Bradley A.,Morphology of bottom sediment of Prince William Sound along the oil spill trajectory, p. In Sediment of Prince William Sound, beach to deep fjord floor, a year after the Exxon Valdez oil spill, Paul R.

Carlson, editor, U.S. Geological Survey Open-File Report. Propagation of seismic waves is a function of impedance of the sediments, measured as the product of density and velocity.

if methane hydrate is present in sediments, the impedance is typically much higher than for non-methane hydrate–bearing sediments. impedance inversion can use calibration from well-log data to calculate bulk density, P.

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In Appendix G. BP Exploration (Alaska), Inc. Oil Discharge Pre- vention and Contingency Plan, Greater Prudhoe Bay, North Slope, Alaska. Beach sediment size analysis was performed using conventional sieving techniques at intervals and by pipet 34 analysis.

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The discussers concluded that the proposed method consistently overestimates the preconsolidation stresses for most samples taken from downtown San Francisco, and for the other two sites (North Bay and South Bay), most of the estimated values are within ± 50 % of the values determined from the consolidation tests.

OIL OEVELOPMENT IN NORTHERN ALASKA A Guide to the Effects of Gravel Placement on Wet lands and Waterbi rds by Rosa Meehan U. F ish and Wi 1 d 1 if e S e r vice Alaska Investigations Branch of Wet lands and Marine Ecology E.

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Engineering geologic maps of northern Alaska, Harrison Bay quadrangle Map and report on the surficial deposits and bedrock of the onshore part of the Harrison Bay quadrangle, Alaska.

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