Cape Hatteras National Seashore Geologic Resources Inventory Report
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WASTEWATER MANAGEMENT in COASTAL NORTH CAROLINA The
WASTEWATER MANAGEMENT IN COASTAL NORTH CAROLINA The University of North Carolina at Chapel Hill Raymond J. Nierstedt Daniel A. Okun Charles R. OIMelia Jabbar K. Sherwani Department of Environmental Sciences and Engineering School of Public Health Milton S. Heath, Jr. Warren Jake Wicker Institute of Government and North Carolina State University Larry D. King Department of Soil Science December 1980 The investigation on which this publication is based was supported through The University of North Carolina Water Resources Research Institute by the Division of Environmental Management of the NC Department of Natural Resources and Community Development, and the US Environmental Protection Agency. Project No. 50020 TABLE OF CONTENTS Page Abstract xii Acknowledgments CHAPTER I: INTRODUCTION Options for Water Quality Management Study Areas Population Distribution and Growth Northern Area Southern Area Sewerage Computer Program Wastewater Disposal Inland Coastal Sounds Ocean Disposal Land Application Wet land Application Water Reuse Costs Interceptor Sewer System - Gravity Sewers Pump Stations Force Mains Treatment Costs Ocean Discharge Land Application CHAPTER 11: WASTEWATER MANAGEMENT IN THE NORTHERN (DARE COUNTY) COASTAL AREA Area Description Economy and Major Employment-Generating Activities Land Use Precipitation and Flood Control Water Supply in the Northern Area Water Resources in the Northern Area Wastewater Treatment Water Quality Wastewater Flows Disposal Options Coastal Sounds Ocean Discharge Land Application for Roanoke Island Land -
1 the Outer Banks Brogue Overview North Carolina's Outer Banks Is
The Outer Banks Brogue “We’re losing our heritage basically. I mean…we’re going from a fishing community to more like a tourism community…And you don’t realize it, but you slowly adapt to a new way of life. And it ain’t nothing negative, but it ain’t nothing positive.” –Bubby Boos, resident of Ocracoke Island Overview North Carolina’s Outer Banks is one of the most geographically, historically, and culturally distinct areas in the state and along the entire Atlantic Seaboard. In this lesson, students will explore one of the more distinctive aspects that makes the North Carolina coastal area so culturally rich – its dialect. For several centuries, the small villages dotting the barrier islands of North Carolina and the adjacent coastal mainland harbored one of the most distinctive varieties of English in the United States, the so-called “Outer Banks Brogue.” Through reading, discussion, and interaction with audio and visual clips, students will not only have the chance to hear the Brogue, but also begin to think about how the history and geography of North Carolina resulted in such diverse language qualities. Students will culminate their exploration by experimenting with a long-time Outer Banks tradition – storytelling – in which they practice integrating some of the unique words and pronunciations of the region. Grade 8 NC Essential Standards • 8.H.3.2 - Explain how changes brought about by technology and other innovations affected individuals and groups in North Carolina and the United States. • 8.H.3.4 - Compare historical and contemporary issues to understand continuity and change in the development of North Carolina and the United States. -
Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches Tiffany Roberts University of South Florida, [email protected]
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School January 2012 Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches Tiffany Roberts University of South Florida, [email protected] Follow this and additional works at: http://scholarcommons.usf.edu/etd Part of the American Studies Commons, Geology Commons, and the Geomorphology Commons Scholar Commons Citation Roberts, Tiffany, "Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches" (2012). Graduate Theses and Dissertations. http://scholarcommons.usf.edu/etd/4216 This Dissertation is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Natural and Anthropogenic Influences on the Morphodynamics of Sandy and Mixed Sand and Gravel Beaches by Tiffany M. Roberts A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Geology College of Arts and Sciences University of South Florida Major Professor: Ping Wang, Ph.D. Bogdan P. Onac, Ph.D. Nathaniel Plant, Ph.D. Jack A. Puleo, Ph.D. Julie D. Rosati, Ph.D. Date of Approval: July 12, 2012 Keywords: barrier island beaches, beach morphodynamics, beach nourishment, longshore sediment transport, cross-shore sediment transport. Copyright © 2012, Tiffany M. Roberts Dedication To my eternally supportive mother, Darlene, my brother and sister, Trey and Amber, my aunt Pat, and the friends who have been by my side through every challenge and triumph. -
Open-File Report 88-480 Prepared in Cooperation with the Raleigh, North
BIBLIOGRAPHY OF HYDROLOGIC AND WATER-QUALITY INVESTIGATIONS CONDUCTED IN OR NEAR THE ALBEMARLE-PAMLICO SOUNDS REGION, NORTH CAROLINA By Jerad D. Bales and Thomas M. Nelson U.S. GEOLOGICAL SURVEY Open-File Report 88-480 Prepared in cooperation with the ALBEMARLE-PAMLICO ESTUARINE STUDY, NORTH CAROLINA DEPARTMENT OF NATURAL RESOURCES AND COH1UNITY DEVELOPMENT Raleigh, North Carolina 1988 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Books and Open-File Reports Post Office Box 2857 Box 25425, Federal Center Raleigh, North Carolina 27602 Denver, Colorado 80225 CONTENTS Page Abstract ................................ 1 Introduction .............................. 1 Purpose and scope ......................... 1 Previous bibliographies ...................... 3 Acknowledgments .......................... 3 Description of bibliography. ...................... 3 References cited ............................ 4 Bibliography .............................. 5 Index by study location. ........................ 125 Index by primary topic ......................... 137 ILLUSTRATIONS Page Figure 1. Map showing the Albemarle-Pamlico Sounds region ....... 2 TABLES Page Table 1. Study site locations used in location index. ......... 4 2. Primary investigation topics used in topic index ....... 4 n i ABSTRACT A bibliography containing 1,100 In order to consolidate and ana citations is presented. The cited lyze existing hydrologic and water- works are primarily reports of quality data from ATbemarle and investigations of the effects of land Pamlico Sounds and the surrounding use and land-use change on water area, the APES Project Office, located quality, artificial drainage, hydro within the North Carolina Department logy and hydrodynamics, and water of Natural Resources and Community quality in the Albemarle-Pamlico Development (NRCD), and the U.S. -
Stratigraphic Studies of a Late Quaternary Barrier-Type Coastal Complex, Mustang Island-Corpus Christi Bay Area, South Texas Gulf Coast
Stratigraphic Studies of a Late Quaternary Barrier-Type Coastal Complex, Mustang Island-Corpus Christi Bay Area, South Texas Gulf Coast U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1328 COVER: Landsat image showing a regional view of the South Texas coastal zone. IUR~AtJ Of ... lt~f<ARY I. liBRARY tPotC Af•a .VAStf. , . ' U. S. BUREAU eF MINES Western Field Operation Center FEB 1919S7 East 360 3rd Ave. IJ.tA~t tETUI~· Spokane, Washington .99~02. m UIIM» S.tratigraphic Studies of a Late Quaternary Barrier-Type Coastal Complex, Mustang Island Corpus Christi Bay Area, South Texas Gulf Coast Edited by GERALD L. SHIDELER A. Stratigraphic Studies of a Late Quaternary Coastal Complex, South Texas-Introduction and Geologic Framework, by Gerald L. Shideler B. Seismic and Physical Stratigraphy of Late Quaternary Deposits, South Texas Coastal Complex, by Gerald L. Shideler · C. Ostracodes from Late Quaternary Deposits, South Texas Coastal Complex, by Thomas M. Cronin D. Petrology and Diagenesis of Late Quaternary Sands, South Texas Coastal Complex, by Romeo M. Flores and C. William Keighin E. Geochemistry and Mineralogy of Late Quaternary Fine-grained Sediments, South Texas Coastal Complex, by Romeo M. Flores and Gerald L. Shideler U.S. G E 0 L 0 G I CAL SURVEY P R 0 FE S S I 0 N A L p·A PER I 3 2 8 UNrfED S~fA~fES GOVERNMENT PRINTING ·OFFICE, WASHINGTON: 1986 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging-in-Publication Data Main entry under title: Stratigraphic studies of a late Quaternary barrier-type coastal complex, Mustang Island-Corpus Christi Bay area, South Texas Gulf Coast. -
Supplemental Article to Where Is the Lost Colony?
Challenges to living by the sea A supplement to the serial story, Where is The Lost Colony? written by Sandy Semans, editor, Outer Banks Sentinel The thin ribbon of sand that forms the chain of islands known as the Outer Banks is bounded on the east by the Atlantic Ocean and on the west by the sounds. The shapes of the islands and the inlets that run between them continue to be altered by hurricanes, nor’easters and other weather events. Inlets that often proved to be moving targets created access to the ocean and the sounds. Inlets were formed and then later filled with sand and disappeared. Maps of the coastline show many places named “New Inlet,” although currently there is no inlet there. The one exception has been Ocracoke Inlet between Ocracoke and Portsmouth islands. Marine geologists estimate that the existing inlet — with some minor changes — has been in place for at least 2500 years. During the English exploration of the 1500’s, most likely the ships came through this inlet, making it a long sail to Roanoke Island. At that time, there was a small shallow inlet between Hatteras and Ocracoke islands, but the shallow inlet probably was avoided for fear of going aground. By the early 1700s, this inlet had filled in, and the two became just one long island. But in 1846, a hurricane created two major inlets. One, now called Oregon Inlet, sliced through the sand, leaving today’s Pea Island to the south and Bodie Island to the north. And a second inlet, now known as Hatteras Inlet, once again separated Hatteras Island from Ocracoke Island. -
Coral Reefs, Unintentionally Delivering Bermuda’S E-Mail: [email protected] fi Rst Colonists
Introduction to Bermuda: Geology, Oceanography and Climate 1 0 Kathryn A. Coates , James W. Fourqurean , W. Judson Kenworthy , Alan Logan , Sarah A. Manuel , and Struan R. Smith Geographic Location and Setting Located at 32.4°N and 64.8°W, Bermuda lies in the northwest of the Sargasso Sea. It is isolated by distance, deep Bermuda is a subtropical island group in the western North water and major ocean currents from North America, sitting Atlantic (Fig. 10.1a ). A peripheral annular reef tract surrounds 1,060 km ESE from Cape Hatteras, and 1,330 km NE from the islands forming a mostly submerged 26 by 52 km ellipse the Bahamas. Bermuda is one of nine ecoregions in the at the seaward rim of the eroded platform (the Bermuda Tropical Northwestern Atlantic (TNA) province (Spalding Platform) of an extinct Meso-Cenozoic volcanic peak et al. 2007 ) . (Fig. 10.1b ). The reef tract and the Bermuda islands enclose Bermuda’s national waters include pelagic environments a relatively shallow central lagoon so that Bermuda is atoll- and deep seamounts, in addition to the Bermuda Platform. like. The islands lie to the southeast and are primarily derived The Bermuda Exclusive Economic Zone (EEZ) extends from sand dune formations. The extinct volcano is drowned approx. 370 km (200 nautical miles) from the coastline of the and covered by a thin (15–100 m), primarily carbonate, cap islands. Within the EEZ, the Territorial Sea extends ~22 km (Vogt and Jung 2007 ; Prognon et al. 2011 ) . This cap is very (12 nautical miles) and the Contiguous Zone ~44.5 km (24 complex, consisting of several sets of carbonate dunes (aeo- nautical miles) from the same baseline, both also extending lianites) and paleosols laid down in the last million years well beyond the Bermuda Platform. -
An Historical Overviw of the Beaufort Inlet Cape Lookout Area of North
by June 21, 1982 You can stand on Cape Point at Hatteras on a stormy day and watch two oceans come together in an awesome display of savage fury; for there at the Point the northbound Gulf Stream and the cold currents coming down from the Arctic run head- on into each other, tossing their spumy spray a hundred feet or better into the air and dropping sand and shells and sea life at the point of impact. Thus is formed the dreaded Diamond Shoals, its fang-like shifting sand bars pushing seaward to snare the unwary mariner. Seafaring men call it the Graveyard of the Atlantic. Actually, the Graveyard extends along the whole of the North Carolina coast, northward past Chicamacomico, Bodie Island, and Nags Head to Currituck Beach, and southward in gently curving arcs to the points of Cape Lookout and Cape Fear. The bareribbed skeletons of countless ships are buried there; some covered only by water, with a lone spar or funnel or rusting winch showing above the surface; others burrowed deep in the sands, their final resting place known only to the men who went down with them. From the days of the earliest New World explorations, mariners have known the Graveyard of the Atlantic, have held it in understandable awe, yet have persisted in risking their vessels and their lives in its treacherous waters. Actually, they had no choice in the matter, for a combination of currents, winds, geography, and economics have conspired to force many of them to sail along the North Carolina coast if they wanted to sail at all!¹ Thus begins David Stick’s Graveyard of the Atlantic (1952), a thoroughly researched, comprehensive, and finely-crafted history of shipwrecks along the entire coast of North Carolina. -
Foundation Document Cape Lookout National Seashore North Carolina October 2012 Foundation Document
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Cape Lookout National Seashore North Carolina October 2012 Foundation Document To Nags Head OCRACOKE Natural areas within Water depths 12 Cape Lookout NS Ocracoke D Lighthouse N y Maritime forest 0-6 feet Ranger station Drinking water r A r L e S (0-2 meters) I F r Picnic area Parking e Cape Hatteras Beach and More than 6 feet g Permit required n (more than 2meters) e National grassland s Picnic shelter Showers s HYDE COUNTY a Seashore P Marshland CARTERET COUNTY E Restrooms Sanitary disposal station Beacon I K O C A North Rock R Tidal flat Toll ferry Lodging Gas station C Shell Castle O Life-Saving Service Station (Historic) PORTSMOUTH VILLAGE (Historic) Casey Ocracoke Open seasonally Island Inlet Babb-Dixon Cemetery There are no roads within Some land within the park National Ocean Survey Methodist Church the national seashore; a remains private property; charts are indispensable Community Cemetery 4-wheel-drive vehicle is please respect the owner's for safe navigation in Schoolhouse highly recommended for rights. these waters. driving on the beach. Sheep Island Tidal flats may flood quickly at high tide— depending upon winds North 0 5 Kilometers and seasons. ) y r y r r e 0 5 Miles F r e e PORTSMOUTH FLATS F t a t e S l c a i n i h l e o r V a C h t r o N ( PAMLICO SOUND PAMLICO COUNTY Mullet Shoal CARTERET COUNTY Pilontary Islands Wainwright I Shell Island Harbor Island Chain Shot Island Cricket Hog Island Island Cedar Island y r Point of Grass a d C n eda -
Cape Fear Sail & Power Squadron
Cape Fear Sail & Power Squadron We are America’s Boating Club® NORTH CAROLINA OCEAN INLETS Listed in order of location north to south Oregon Inlet Outer Banks. Northern-most ocean inlet in NC. Located at the north end of New Topsail Inlet Near ICW Mile 270. As of July Hatteras Island. Provides access to Pamlico Sound. 7, ’20, the inlet was routinely passable by medium Federally maintained.* See Corps of Engineers and small vessels at higher states of the tide. survey1 However, buoys were removed in 2017 due to shoaling, so the channel is currently unmarked. See Hatteras Inlet Outer Banks. Located between Corps of Engineers survey Hatteras and Ocracoke Islands. Provides access to Pamlico Sound. Once inside the inlet itself, the Little Topsail Inlet Located ½ N.M. SW of New passage of a lengthy inshore channel is required to Topsail Inlet. Not normally passable and does not access the harbor or navigable portions of Pamlico currently connect to navigable channels inshore. Sound. Rich Inlet Located between Topsail and Figure 8 Ocracoke Inlet Outer Banks. Located at S end Islands near ICW Mile 275. of Ocracoke Is. Provides access to Pamlico Sound. Once inside the inlet itself, the passage of a shifting Mason Inlet Located between Figure 8 Island and inshore channel named Teaches Hole is required to Wrightsville Beach island near ICW Mile 280. access the harbor or navigable portions of Pamlico Dredged in 2019 but not buoyed as of July 31, ’20. Sound. Buoyed & lighted as of June 29, ’19. See Corps of Engineers surveys1 (for the inlet) and (for Masonboro Inlet Located between Wrightsville Teaches Hole). -
Historic and Architectural Resources of Currituck County 1790-1958
NPS Form 10-900-a OMB No. 1024-0018 (8-86) United States Department of the Interior National Park Service NATIONAL REGISTER OF HISTORIC PLACES CONTINUATION SHEET Historic and Architectural Resources of Currituck County, 1790-1958 Section __E___ Page __1 =================================================================================== Introduction “When Nature came to design the topography of eastern North Carolina,” wrote North Carolina historian Charles Christopher Crittenden in 1936, “she almost persuaded herself to create a great maritime center.”1 The interplay between water and land in Currituck is key to understanding the history and evolution of the county. Although one of the oldest in the state of North Carolina, the county has also been one of the most overlooked. Piecing together the history of the county is difficult. Many of the records pertaining to the early history of Currituck have been lost or destroyed. A courthouse fire in 1842, for example, destroyed a substantial body of records, including marriage records. As a consequence, much of the county’s past lives on as oral history; written accounts tend to be either personal reminiscences or a recounting of events that have been passed orally through the different generations of a family. The history of the county remains to be written. A Geographical Overview of the County The most northeasterly of the one hundred North Carolina counties, Currituck is a peninsula: the land is long and narrow, low and even. The county consists of a mainland 1 Charles Christoper Crittenden, The Commerce of North Carolina 1763-1789. New Haven: Yale University Press, 1936, p. 8. NPS Form 10-900-a OMB No. -
Hatteras Island FAM Itinerary April 15 – 19, 2013
Hatteras Island FAM Itinerary April 15 – 19, 2013 The Outer Banks Visitors Bureau PR Team Aaron Tuell, PR Manager, OBVB office 252.473.2138 or [email protected] Martin Armes, OBVB PR Rep Dana Grimstead, Events and MarKeting Assistant, OBVB Media Guests WELCOME! Monday, April 15, 2013 12:30 PM Arrive NorfolK International Airport (Drive time is about 1 hour, 30 minutes) 1:00 PM Dana Grimstead gets the Key for “Southern Belle” rental home and drops off food for media cottage. 2:00 PM Lunch at Awful Arthur’s Oyster Bar in Kill Devil Hills 2106 N Virginia Dare Trail, Kill Devil Hills, NC 27948 252-441-5955 2:30 PM Call Josh Boles, National ParK Service, prior for tour of Wright Brothers. 3:00 PM Wright Brothers National Memorial - tour and flight room-talK with Josh. See where on a cold day in December, 1903 Wilbur and Orville Wright changed the world forever as their powered airplane, the “Wright Flyer”, sKimmed over the sands of the Outer BanKs for 12 seconds before returning to the ground. See the flight museum which still has exhibits from the First Flight Centennial Celebration. 5:00 PM Jomi, owner, Ketch 55 restaurant and catering gets into the home to begin prep for cooKing dinner. 6:00 PM ChecK into Rental Home, www.2OBR.com/450 “Southern Belle” in Avon, NC – 7 bedroom / 7 bath, 41375 Oceanview Dr, Avon, NC Home provided by Outer Beaches Realty 800.627.3150 www.OuterBeaches.com Alex J. Risser, President 800.627.3150 x3280 [email protected] Linda Walton, Guest Services Manager 252.995.7372 [email protected] 7:00 PM Dinner catered at Southern Belle rental home by Ketch 55, Avon Tuesday, April 16, 2013 Sunrise beach walK and Breakfast at your leisure.