Read Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks)

Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks)

W. Burleigh Harris

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Description:Published by the American Geophysical Union as part of the "Field Trip Guidebooks Series."The Atlantic Coastal Plain Province is a low-relief physiographic plain, underlain by a gently-dipping, seaward-thickening wedge of unconsolidated Mesozoic and Cenozoic sediments. The province extends from Cape Cod, Massachusetts to the northwestern extension of the Peninsular arch in Georgia and is separated into emergent and submergent parts. The emerged part, located above sea level, is called the Coastal Plain, whereas the submerged part is the continental shelf. The eastern boundary of the Coastal Plain is the Atlantic shore and the western boundary or inner margin the Fall Line. The Fall Line marks the approximate contact between the underlying igneous and metamorphic rocks of the Piedmont Province and the generally unconsolidated sediments of the Coastal Plain. Coastal Plain sediments contain a record of most of the Upper Cretaceous and Cenozoic stages. These sediments reach their maximum thickness in the Salisbury, Albermarle, and Southeast Georgia embayments, and thin appreciably over the intervening South New Jersey, Norfolk, and Cape Fear arches. This series of alternating basins and highs has produced a complex sequence of lithologic units that vary extensively on a local as well as a regional scale. Lithologic units in the Coastal Plain consist of siliciclastics and carbonates, with carbonates being more abundant in the Southeast Georgia embayment. Mild deformation related to reactivation ofearly Mesozoic grabens and half-grabens has affected various parts of the stratigraphic section.We have made it easy for you to find a PDF Ebooks without any digging. And by having access to our ebooks online or by storing it on your computer, you have convenient answers with Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks). To get started finding Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks), you are right to find our website which has a comprehensive collection of manuals listed.
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ISBN: 0875906176

Description: Published by the American Geophysical Union as part of the "Field Trip Guidebooks Series."The Atlantic Coastal Plain Province is a low-relief physiographic plain, underlain by a gently-dipping, seaward-thickening wedge of unconsolidated Mesozoic and Cenozoic sediments. The province extends from Cape Cod, Massachusetts to the northwestern extension of the Peninsular arch in Georgia and is separated into emergent and submergent parts. The emerged part, located above sea level, is called the Coastal Plain, whereas the submerged part is the continental shelf. The eastern boundary of the Coastal Plain is the Atlantic shore and the western boundary or inner margin the Fall Line. The Fall Line marks the approximate contact between the underlying igneous and metamorphic rocks of the Piedmont Province and the generally unconsolidated sediments of the Coastal Plain. Coastal Plain sediments contain a record of most of the Upper Cretaceous and Cenozoic stages. These sediments reach their maximum thickness in the Salisbury, Albermarle, and Southeast Georgia embayments, and thin appreciably over the intervening South New Jersey, Norfolk, and Cape Fear arches. This series of alternating basins and highs has produced a complex sequence of lithologic units that vary extensively on a local as well as a regional scale. Lithologic units in the Coastal Plain consist of siliciclastics and carbonates, with carbonates being more abundant in the Southeast Georgia embayment. Mild deformation related to reactivation ofearly Mesozoic grabens and half-grabens has affected various parts of the stratigraphic section.We have made it easy for you to find a PDF Ebooks without any digging. And by having access to our ebooks online or by storing it on your computer, you have convenient answers with Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks). To get started finding Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks), you are right to find our website which has a comprehensive collection of manuals listed.
Our library is the biggest of these that have literally hundreds of thousands of different products represented.

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Upper Cretaceous and Cenozoic Geology of the Southeastern Atlantic Coastal Plain: Atlanta, Georgia to Chesapeake, Virginia (Field Trip Guidebooks)

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