2 edition of Geology and tectonic history of the lower Cape Fear River Valley, southeastern North Carolina found in the catalog.
Geology and tectonic history of the lower Cape Fear River Valley, southeastern North Carolina
D. R. Soller
1988 by U.S. G.P.O., For sale by the Books and Open-File Reports Section, U.S. Geological Survey in Washington, D.C, Denver, CO .
Written in English
|Statement||by David R. Soller.|
|Series||Surface and shallow subsurface geological studies of the Carolina coastal plains, U.S. Geological Survey professional paper ;, 1466-A|
|LC Classifications||QE148.C35 S65 1988|
|The Physical Object|
|Pagination||iv, 60 p. :|
|Number of Pages||60|
|LC Control Number||88600245|
Cape Fear - HUC ; Cape Fear - HUC ; South Atlantic-Gulf - HUC Online USGS Watershed Information For: Links to Projects, Publications and Information for Cataloging Unit - Lower Cape Fear Acid-precipitation Stations in North Carolina - Links to Projects, Publications and Information for Accounting Unit - Cape Fear. Relief shown by hachures. Depths shown by soundings. Oriented with north toward the upper left. Includes "Tide Scale at Smithville." Available also through the Library of Congress Web site as a raster image. LC copy imperfect: Discoloration and staining on bottom of all sheets. Torn along edges with minor losses. to determine nitrogen (N) speciation and loading to the Cape Fear River Estuary (CFRE), Southeastern North Carolina, and to ascertain why NH4 + concentrations in the estuary have more than doubled in the past 8 years. River fluxes are the primary source of N into the estuary, contributing >90% of TN : Leslie C. Bradshaw.
On the various contrivances by which British and foreign orchids are fertilized by insects
Van Dean Theory Workbook
Progress in 1965-66 at the Bureau of Commercial Fisheries Biological Laboratory, Honolulu
Contrast Sensitivity of the Human Eye and Its Effects on Image Quality (SPIE Press Monograph Vol. PM72)
Weapons system fundamentals.
What research says about early childhood education.
Forgettings no excuse
Great recipes from great restaurants.
Toxicity of pulp and paper mill effluent
The development of modern France, 1870-1939
GEOLOGY AND TECTONIC HISTORY OF THE LOWER CAPE FEAR RIVER VALLEY, SOUTHEASTERN NORTH CAROLINA By DAVID R. SOLLER ABSTRACT The Cape Fear River is a major Piedmont-draining river system that flows across the Atlantic Coastal Plain in North Carolina. A detailed study of stratigraphy, mineralogy, and geomorphology wasCited by: Get this from a library.
Geology and tectonic history of the lower Cape Fear River Valley, southeastern North Carolina. [D R Soller; Geological Survey (U.S.)]. General Information. Title: Geology and tectonic history of the lower Southeastern North Carolina book Fear River valley, southeastern North Carolina Author(s): Soller, D.R.
Publishing Organization: U.S. Geological Survey Series and Number: Professional Paper A Larger Work: Surface and shallow subsurface geologic studies of the Carolina coastal plains Publication Date: The Cape Fear River is a major Piedmont-draining river system that flows across the Atlantic Coastal Plain in North Carolina.
A detailed study of stratigraphy, mineralogy, and geomorphology was undertaken to assess the geology and tectonic history of the valley and the implications for late Cenozoic tectonism in the region.
PP A / Soller, D. / GEOLOGY AND TECTONIC HISTORY OF THE LOWER CAPE FEAR RIVER VALLEY SOUTHEASTERN NORTH CAROLINA,pb, 80 pages, 1 plate (in pocket), 28 figs., 4 tables, new, uncirculated condition, $ Cape Fear River, river in central and southeastern North Carolina, U.S., formed by the confluence of the Deep and Haw rivers along the boundary between Chatham and Lee counties.
It flows generally southeast past Fayetteville, Elizabethtown, and Wilmington and enters the Atlantic Ocean at Southport, opposite Smith Island, after a course of about miles ( km). D.R. SollerGeology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina U.S.
Geological Survey professional paper (No. A) ()Cited by: Welcome to the Digital Archive for Southeastern Geology Geology and tectonic history of the lower Cape Fear River Valley Heron, founding editor of Southeastern Geology. Hosted by Belk Library and Information Commons and the Department of Geological and Environmental Sciences at Appalachian State University, Boone, NC.
Soller, D.Geology and tectonic history of the Lower Cape Fear River Valley, southeastern North Carolina, U.S. Geological Survey Professional Paper A, p, A Google Scholar 44Cited by: Cape Fear River transect: the Upper Cretaceous Cape Fear, Black Creek and Peedee Formations of southeastern North Carolina and overlying.
North Carolina's long and often turbulent geologic history reveals the effects of both plate tectonics and weather. The earth's crust is essentially a crude patchwork of continually shifting plates that collide with one another as new crust is generated.
Geology and tectonic history of the lower Cape Fear River valley, southeastern (). Geology of the Coastal Plain of North Carolina.
The American Philosophical Society. New Series. R o b e r t s,D. L.,K a r k a n a s,P.,J a c o b s,Z.,M a r e a n,C. Land of the Golden River: Historical Events and Stories of Southeastern North Carolina and the Lower Cape Fear, Volume One: Old Times on the Seacoast to [Hall, Lewis Philip] on *FREE* shipping on qualifying offers.
Land of the Golden River: Historical Events and Stories of Southeastern North Carolina and the Lower Cape FearAuthor: Lewis Philip Hall. Wilmington, located on the east bank of the river near the fork in its branches, quickly replaced Brunswick Town as the center of commerce for Lower Cape Fear and as the seat for New Hanover County.
By the outbreak of the American Revolution, the younger town was vying to become the leading municipality in the province, whereas Brunswick would soon be taken over. Most inland eolian dunes associated with rivers on the Georgia Coastal Plain probably date to glacial periods.
Direct dating of the dune sand by optically stimulated luminescence dating, combined with limiting ages from radiocarbon dating, shows that dunes formed during isotope stage 2, stage 3, the transition between stages 4 and 5, and isotope stage 6 or earlier.
North Carolina Rivers Shown on the Map: Black River, Broad River, Cape Fear River, Catawba River, Chowan River, Deep River, Don River, French Broad River, Haw River, Lumber River, Neuse River, Northeast Cape Fear River, Pee Dee River, Roanoke River, Rocky River, South River, Tar River and Yadkin River.
North Carolina Lakes Shown on the Map: B. Everett. Download Citation | Fluvial terraces of the little river valley, atlantic coastal plain, North Carolina | An optically-stimulated luminescence (OSL) and radiocarbon chronology is presented for. Northeast CAPE FEAR Estuary, North Carolina USGS Water-Supply Paper E $ Geology and Tectonic History of the Lower CAPE FEAR RIVER Valley, Southeastern North Carolina - USGS Professional Paper A $ The Black Creek-Peedee Formational Contact (Upper Cretaceous) in the CAPE FEAR RIVER Region of North Carolina - USGS.
/ MINERAL RESOURCES OF THE CHARLOTTE 1X2 QUADRANGLE, NORTH CAROLINA AND SOUTH CAROLINA,pb, pages, 1 plate (in pocket), 49 figs., 13 tables, $ 30 PP A / Soller, D. / GEOLOGY AND TECTONIC HISTORY OF THE LOWER CAPE FEAR RIVER VALLEY SOUTHEASTERN NORTH CAROLINA,pb, 80 pages, 1 plate (in pocket), 28.
METHODISM in the Upper Cape Fear Valley [C. Franklin Grill] on *FREE* shipping on qualifying offers. METHODISM in the Upper Cape Fear ValleyAuthor: C. Franklin Grill. The Cape Fear River basin, which occupies much of North Carolina’s southeastern quadrant, is the largest.
The Roanoke River drains the state’s northeastern corner, flowing southeast from Virginia into the ocean at Albermarle Sound. Bisecting North Carolina from north to south is the Yadkin–Pee Dee River.
The lower strata consist of numerous laterally persistent units of gravelly sand grading up to sand and muddy sand exposed along the Cape Fear River and other areas near Fayetteville, North Carolina. They suggested that the term “Cape Fear Formation” be applied to these strata, following nomenclature proposed by Stephenson(,).
At Wilmington, it receives the Northeast Cape Fear River and Brunswick River, turns south, widening as an estuary and entering the Atlantic approximately 3 miles (5 km) west of Cape Fear. During the colonial era, the river provided a principal transportation route to the interior of North Carolina.⁃ location: North Carolina.
The eastern quarter of Tweesdside was cut off by the course of Dunfield Creek which empties into the Cape Fear River about 4 miles to the south. A map drawn by Dan MacMillan of Fayetteville housed at the NC Department of Archives and History shows Dunfield Creek closely paralleling the River Road through this eastern quarter of Tweedside.
The North Carolina Dept. of Environment, Health, and Natural Resources, Division of Land Resources, NC Geological Survey, in cooperation with the NC Center for Geographic Information and Analysis, (updated ), Geology - North Carolina (,), coverage data file. Chronicles of the Cape Fear river, Date: | Identifier: FC2 S68 Original held by New Hanover County Public Library, Wilmington, N.C.
more. distribution on terraces in the Cape Fear River Valley of North Carolina, in an Geology and Tectonic History of Lower Cape Fear River Valley, Southeastern North Carolina, U.S.
Geological Survey Professional Paper A, 60 pp Soller, D.R. Hackney C.T., Avery G.B., Leonard L.A., Posey M., Alphin T. () Biological, Chemical, and Physical Characteristics of Tidal Freshwater Swamp Forests of the Lower Cape Fear River/Estuary, North Carolina.
In: Ecology of Tidal Freshwater Forested Wetlands of the Southeastern United States. Springer, DordrechtCited by: David R.
Soller. Geologist, U.S. Geological Survey. Current position Chief, National Geologic Map Database project -- Development and management of science databases for support of societal decisionmaking and scientific research are critical and widely recognized needs.
Little River (Cape Fear River tributary) Little River (Eno River tributary) Little River (French Broad River tributary) Little River (Horry County, South Carolina) Little River (Jacob Fork) Little River (Neuse River tributary) Little River (North Carolina-Virginia) Little River (Pee Dee River tributary) Little River (Roanoke River tributary).
Special programs and rotating exhibits on unique chapters of Cape Fear history may also be available. USS North Carolina Battleship. Anchored along the Cape Fear Riverfront, the massive USS North Carolina is a historic battleship that had an impressive run in World War II.
Put into service inand earning 15 battle stars during its tenure. Game lands users should identify posted signs on the ground as well as refer to the current North Carolina Inland Fishing, Hunting, & Trapping Regulations Digest for regulatory information.
For questions or comments, email [email protected] Black Creek Cretaceous deposits along the Cape Fear River, North Carolina: Black Creek Fomation: UNC at Chapel Hill: Master thesis: Tectonic history of the Blue Ridge and Brevard zone near Old Fort, North Carolina: Black Mountain, Montreat, Old Fort Geology of the southeastern quarter of the Marion Minute Quadrangle, North Carolina.
The Cape Fear River (CFR) is a low discharge river, which drains the largest area of any rivers fully contained within North Carolina.
The river is formed in the Piedmont by the convergence of the Haw and Deep Rivers and then flows southeast through the state terminating into Long Bay in the Atlantic by: 1. The Cape Fear River basin is the largest in North Carolina.
Which statement BEST describes a river basin. A) River basins are tributaries that drain into a much larger water shed. B) A river basin is a large channel of water that is always flowing down a slope.
C) It contains a major river and all the streams and creeks that flow into that river. Soller, D.R.,Geology and tectonic history of lower Cape Fear River valley, southeastern North Carolina, U.S. Geological Survey Professional Paper A, 60 p Swezey, et al, ; Eolian Dunes Of Late Quaternary Age On The Floodplain Of The Savannah River, Jasper County, South Carolina, GSA Abstracts with Programs, Vol.
44, No. 4, p. The oldest of these river terraces that is present in the Cape Fear River Valley is approximately million years old, which is in the Pliocene Epoch.
Therefore it is inferred that the Lower Cape Fear River drainage system, though evolving, has been present since that time. The Big Book of the Cape Fear River Editor’s Note. This is a truly remarkable work, a shining example of tax dollars well spent.
I first came across this report on the places where history happened on the Cape Fear River in the office of Mary Strickland at the North Carolina Maritime Museum in Southport a few years ago. THE BLACK CREEK-PEEDEE FORMATIONAL CONTACT (UPPER CRETACEOUS) IN THE CAPE FEAR RIVER REGION OF NORTH CAROLINA By NORMAN F.
SOHL and RAYMOND A. CHRISTOPHER1 ABSTRACT Stratigraphic and paleontologic data from six sections exposed along the Cape Fear River, N.C., suggest that the contact between theCited by: Americae Sive Novi Orbis Nova Descriptio.
Reference: Philip D. Burden, The Mapping of North America: A list of printed maps Herts, England: Raleigh Publications, Map Repository: Outer Banks History Center (call number MCo). "Geology mapped in " Includes text, bibliography, index map, 2 ancillary maps, 1 columnar section, and 7 col.
cross sections. Related Work Cape Fear region, Florence 1 x 2 quadrangle, and northern half of the Georgetown 1 x 2 quadrangle, North and South Carolina. Sometimes called the “East Branch,” the Northeast Cape Fear River flows from a point 2 miles south of Mount Olive in Duplin County, past Albertson and Chinquapin in Pender County.
It joins the main channel of the Cape Fear at Point Peter, just north of downtown Wilmington. Its course covers some miles, passing along .The following quote is from a paper entitled Geology and Tectonic History of the Lower Cape Fear River Valley, Southeastern North Carolina; Surface And Shallow Subsurface Geologic Studies Of The Carolina Coastal Plains, U.S.
Geological Survey Professional Paper A, By David R. Soller. AN ESTIMATE OF THE AGES OF DUNES AND CAROLINA BAYS.