Zobrazeno 1 - 10
of 56
pro vyhledávání: '"Harley J. Knebel"'
Publikováno v:
Marine Geology. 155:277-318
Four categories of modern seafloor sedimentary environments have been identified and mapped across the large, glaciated, topographically complex Long Island Sound estuary by means of an extensive regional set of sidescan sonographs, bottom samples, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::424b961bcbad2ba0d094e208b207777d
https://doi.org/10.1016/s0025-3227(98)00129-7
https://doi.org/10.1016/s0025-3227(98)00129-7
Publikováno v:
Marine Geology. 133:11-33
Cape Cod Bay is a glacial, semi-enclosed embayment that has a patchy distribution of modern seafloor sedimentary environments of erosion or nondeposition, deposition, and sediment reworking. Sidescan-sonar records and supplemental bathymetric, sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8e02d545281f88514fb2daf20ccfc38
https://doi.org/10.1016/0025-3227(96)00014-x
https://doi.org/10.1016/0025-3227(96)00014-x
Publikováno v:
Geomorphology. 9:301-309
Streamlined, oval-shaped, oriented topographic highs in Massachusetts Bay are identified as the erosional remnants of drumlins. The topographic highs correlate with outlines of lag gravel deposits on the sea floor and both the highs and lag gravel se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80892a3f0d9d8b1f2a2251b82ce0ab42
https://doi.org/10.1016/0169-555x(94)90051-5
https://doi.org/10.1016/0169-555x(94)90051-5
Autor:
Harley J. Knebel
Publikováno v:
Marine Geology. 110:7-30
Three modern sedimentary environments have been identified and mapped across the glaciated Boston Harbor estuary and adjacent inner shelf of Massachusetts Bay by means of an extensive set of sidescan sonar records and supplemental bathymetric, sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72d6795649252d043fa0ceff3721f25d
https://doi.org/10.1016/0025-3227(93)90102-2
https://doi.org/10.1016/0025-3227(93)90102-2
Publikováno v:
Marine Geology. 103:165-183
The Holocene transgression of the Delaware Bay estuary and adjacent Atlantic coast results from the combined effect of regional crustal subsidence and eustasy. Together, the estuary and ocean coast constitute a small sedimentary basin whose principal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::573821ef976249d6f57980f4781ff87d
https://doi.org/10.1016/0025-3227(92)90014-9
https://doi.org/10.1016/0025-3227(92)90014-9
Publikováno v:
Geological Society of America Bulletin. 102:283-297
Modern facies-distribution patterns, extensive core data, and chronostratigraphic cross sections provide a detailed history of Holocene inundation within the Delaware Bay estuary and sedimentation in adjacent coastal environments. Flooding of the est
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5ada6b54f62d9ca7614a55dc71ad695
https://doi.org/10.1130/0016-7606(1990)102<0283:heoaec>2.3.co
https://doi.org/10.1130/0016-7606(1990)102<0283:heoaec>2.3.co
The U.S. Geological Survey has produced detailed geologic maps of the sea floor in Long Island Sound, a major East Coast estuary surrounded by the most densely populated region of the United States. These studies have built upon cooperative research
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d1c433172e095ccfc84b42c427c6703
https://doi.org/10.3133/i2736
https://doi.org/10.3133/i2736
