Part 1 Historical Shoreline Changes and Associated Coastal Land Loss Along the U.S

Total Page:16

File Type:pdf, Size:1020Kb

Part 1 Historical Shoreline Changes and Associated Coastal Land Loss Along the U.S National Assessment Of Shoreline Change: Part 1 Historical Shoreline Changes And Associated Coastal Land Loss Along The U.S. Gulf Of Mexico Robert A. Morton, Tara L. Miller, and Laura J. Moore Open-File Report 2004-1043 U.S. Department of the Interior U.S. Geological Survey National Assessment Of Shoreline Change: Part 1 Historical Shoreline Changes And Associated Coastal Land Loss Along The U.S. Gulf Of Mexico Robert A. Morton, Tara L. Miller, and Laura J. Moore Open File Report 2004-1043 U.S. Geological Survey Center for Coastal and Watershed Studies St. Petersburg, FL 33701 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S.Government. Morton, Robert A., Miller, Tara L., and Moore, Laura J., 2004, National assessment of shoreline change: Part 1: Historical shoreline changes and associated coastal land loss along the U.S. Gulf of Mexico: U.S. Geological Survey Open-file Report 2004-1043, 45p. U.S. Department of the Interior U.S. Geological Survey Open-File Report 2004-1043 i Contents EXECUTIVE SUMMARY..............................................................................................................................................................................4 INTRODUCTION ..........................................................................................................................................................................................4 U.S. Geological Survey National Assessment of Shoreline Change.........................................................................................4 Disclaimer ...........................................................................................................................................................................................5 Acknowledgments.............................................................................................................................................................................5 THE ROLE OF STATE AND FEDERAL GOVERNMENTS..........................................................................................................................5 PRIOR NATIONAL AND GULF COAST SHORELINE ASSESSMENTS..................................................................................................6 METHODS OF ANALYZING SHORELINE CHANGE.................................................................................................................................6 Compilation of Historical Shorelines ..............................................................................................................................................6 Delineation of a Modern (lidar-derived) Shoreline ......................................................................................................................7 Geographic Information System (GIS) Procedures .....................................................................................................................9 Calculation and Presentation of Rates of Change .....................................................................................................................10 Shoreline Definitions and Beach Alterations that Influence Rates of Change ..................................................................... 11 Shoreline Definitions.............................................................................................................................................................. 11 Human Activities.....................................................................................................................................................................12 Reliability of the Results .................................................................................................................................................................12 GEOMORPHOLOGY OF THE GULF COAST REGION .............................................................................................................................14 Gulf of Mexico Mainland Shores ..................................................................................................................................................16 Bays and Lagoons ...........................................................................................................................................................................16 Barrier Islands..................................................................................................................................................................................16 Origin and Evolution of Barriers ...........................................................................................................................................16 Morphologies of Gulf Coast Barrier Islands.......................................................................................................................18 Chenier Plain ....................................................................................................................................................................................20 Tidal Inlets.........................................................................................................................................................................................20 GEOLOGIC HISTORY AND SETTING ......................................................................................................................................................20 Climate ...............................................................................................................................................................................................21 Coastal Processes...........................................................................................................................................................................21 Sand Sources ...................................................................................................................................................................................24 GENERAL CHARACTERISTICS OF THE GULF SHORES BY STATE.....................................................................................................25 HISTORY OF INFRASTRUCTURE DEVELOPMENT ...............................................................................................................................26 SHORELINE CHANGE AND COASTAL LAND LOSS .............................................................................................................................27 West Florida......................................................................................................................................................................................27 Alabama ............................................................................................................................................................................................29 Mississippi ........................................................................................................................................................................................29 Louisiana ........................................................................................................................................................................................... 31 Texas ............................................................................................................................................................................................... 31 HUMAN RESPONSES TO COASTAL EROSION AND LAND LOSS.....................................................................................................32 DISCUSSION AND FURTHER CONSIDERATIONS ...............................................................................................................................38 Summary of Shoreline Changes....................................................................................................................................................38 Planned Updates and Related Research.....................................................................................................................................38 Influence of Human Activities .......................................................................................................................................................39 REFERENCES ............................................................................................................................................................................................39 Open-File Report 2004-1043 ii Open-File Report 2004-1043 iii Figures Figure 1. Example of a lidar profile from September 26, 1997 at Kitty Hawk, North Carolina for (a) the entire cross-shore region and (b) an expanded view of the foreshore region. .....................................................................9 Figure 2. Examples of common conditions where transects are eliminated in the absence of four shoreline intersections. .............................................................................................................................................. 11 Figure 3. Index map of the Gulf Coast region...................................................................................................................................15 Figure 4. Common coastal landforms of the Gulf Coast region. ...................................................................................................16
Recommended publications
  • Coastal Erosion - Orrin H
    COASTAL ZONES AND ESTUARIES – Coastal Erosion - Orrin H. Pilkey, William J. Neal, David M. Bush COASTAL EROSION Orrin H. Pilkey Program for the Study of Developed Shorelines, Division of Earth and Ocean Sciences, Duke University, Durham, NC, U.S.A. William J. Neal Department of Geology, Grand Valley State University, Allendale, MI, USA. David M. Bush Department of Geosciences, State University of West Georgia, Carrollton, GA, USA. Keywords: erosion, shoreline retreat, sea level rise, barrier islands, beach, coastal management, shoreline armoring, seawalls, sand supply Contents 1. Introduction 2. Causes of Erosion 2.1. Sea Level Rise 2.2. Sand Supply 2.3. Shoreline Engineering 2.4. Wave Energy and Storm Frequency 3. "Special" Cases 4. Solutions to Coastal Erosion 5. The Future Glossary Bibliography Biographical Sketches Summary Almost all of the world’s shorelines are retreating in a landward direction—a process called shoreline erosion. Sea level rise and the reduction of sand supply to the shoreline by damming of rivers, armoring of shorelines and the dredging of navigation channels are among the major causes of shoreline retreat. As sea levels continue to rise, sometimesUNESCO enhanced by subsidence caused – byEOLSS oil and water extraction, global erosion rates should increase in coming decades. Three response alternatives are available to "solve" the erosionSAMPLE problem. These are cons tructionCHAPTERS of seawalls and other engineering structures, beach nourishment and relocation or abandonment of buildings. No matter what path is chosen, response to the erosion problem is costly. 1. Introduction Coastal erosion is a major problem for developed shorelines everywhere in the world. Such erosion is regarded as a coastal hazard and is a common focus of local and national coastal management.
    [Show full text]
  • Alexander the Great's Tombolos at Tyre and Alexandria, Eastern Mediterranean ⁎ N
    Available online at www.sciencedirect.com Geomorphology 100 (2008) 377–400 www.elsevier.com/locate/geomorph Alexander the Great's tombolos at Tyre and Alexandria, eastern Mediterranean ⁎ N. Marriner a, , J.P. Goiran b, C. Morhange a a CNRS CEREGE UMR 6635, Université Aix-Marseille, Europôle de l'Arbois, BP 80, 13545 Aix-en-Provence cedex 04, France b CNRS MOM Archéorient UMR 5133, 5/7 rue Raulin, 69365 Lyon cedex 07, France Received 25 July 2007; received in revised form 10 January 2008; accepted 11 January 2008 Available online 2 February 2008 Abstract Tyre and Alexandria's coastlines are today characterised by wave-dominated tombolos, peculiar sand isthmuses that link former islands to the adjacent continent. Paradoxically, despite a long history of inquiry into spit and barrier formation, understanding of the dynamics and sedimentary history of tombolos over the Holocene timescale is poor. At Tyre and Alexandria we demonstrate that these rare coastal features are the heritage of a long history of natural morphodynamic forcing and human impacts. In 332 BC, following a protracted seven-month siege of the city, Alexander the Great's engineers cleverly exploited a shallow sublittoral sand bank to seize the island fortress; Tyre's causeway served as a prototype for Alexandria's Heptastadium built a few months later. We report stratigraphic and geomorphological data from the two sand spits, proposing a chronostratigraphic model of tombolo evolution. © 2008 Elsevier B.V. All rights reserved. Keywords: Tombolo; Spit; Tyre; Alexandria; Mediterranean; Holocene 1. Introduction Courtaud, 2000; Browder and McNinch, 2006); (2) establishing a typology of shoreline salients and tombolos (Zenkovich, 1967; The term tombolo is used to define a spit of sand or shingle Sanderson and Eliot, 1996); and (3) modelling the geometrical linking an island to the adjacent coast.
    [Show full text]
  • Cape Hatteras National Seashore
    05 542745 ch05.qxd 3/23/04 9:01 AM Page 105 CHAPTER 5 Cape Hatteras National Seashore Driving along Hatteras and Ocracoke islands national seashore and other nature preserves are on a narrow strip of sand with the ocean close wild and beautiful. Being here, it’s easy to on both sides, you may think that the Outer imagine what it was like when the first English Banks are a geographic miracle. Why should colonists landed more than 400 years ago, or this razor-thin rim of sand persist far out in the when the Wright brothers flew the first airplane sea? How wild it seems, a land of windy beach over a century ago. Both events are well inter- with no end, always in motion, always vulner- preted at their sites. The area is fascinating eco- able to the next, slightly larger wave. There’s so logically, too. Here, north and south meet, the much here to see and learn, and so much soli- mix of ocean currents, climate, fresh and salt tude to enjoy. You’re like a passenger on an water, and geography creating a fabulous diver- enormous ship, and unpredictable nature is the sity of bird and plant life at places like the Pea captain. Island National Wildlife Refuge (p. 124) and Oddly, many people don’t see Cape Hatteras Nags Head Woods Ecological Preserve (p. 124). this way. When they think of the Outer Banks, In this sense, the area is much like Point Reyes, they think of Nags Head or Kill Devil Hills, its counterpart on the West Coast, covered in towns where tourist development has pushed chapter 21, “Point Reyes National Seashore.” right up to the edge of the sea and, in many And for children, the national seashore is a places, gotten really ugly.
    [Show full text]
  • NATURAL ENGLAND Geomorphological Advice in Respect of Pagham Spit (West Sussex). April 2013
    Pagham Spit Advice 2013 NATURAL ENGLAND Geomorphological Advice in respect of Pagham spit (West Sussex). April 2013 Professor Julian Orford Queen’s University, Belfast Pagham Spit Advice 2013 Natural England Advice Request 1) Could the two recycling operations: i) 2010 and ii) 2012-13 have had a detrimental impact on the site’s functioning and its geomorphological interest? 2) What are the best sources for the current sediment recycling proposals? Note two joint operations to be considered: i) HW erosion at western Pagham and ii) re- armouring of the exposed armoured groyne 3) Is the channel likely to close? 4) What are the possible ways in which the spit might develop, both in the short and longer term? Of these, which is the most likely? 5) Is the rock armour the most effective way to protect the properties? 6) Our current view is that the on-going evolution of the Church Norton spit is a key component in the conservation of the geomorphological interest of the SSSI. Are there other elements we should also be concerned about? Glossary Berm: A constructive wave-built beach face feature generally occurring at the swash reach associated with any particular high tide position. Cumulatively over the neap to spring tidal half-cycle, one berm is realized, associated with highest tidal position. On the falling spring- neap cycle, a series of berms may be realized at each successive lower position achieved by the swash-reach of each successive falling tidal level. Cannibalisation: The tendency for a beach system where the longshore sediment supply has reduced or failed, to use the existing beach sediment as a further source for subsequent longshore sediment transport down-drift.
    [Show full text]
  • National Register of Historic Places Registration Form
    NPS Form 10-900 ^^ OMB No. 1024-0018 United States Department of the Interior, National Park Service \ NATIONAL REGISTER OF HISTORIC PLACES REGISTRATION FORM This form is for use in nominating or requesting determinations of eligibility for individual properties or districts. See instructions in "Guidelines for Completing National Register Forms" (National Register Bulletin 16). Complete each item by marking "x" in the appropriate box or by entering the requested information. If an item does not apply to the property being documented, enter "N/A" for "not applicable." For functions, styles, materials, and areas of significance, enter only the categories and subcategories listed in the instructions. For additional space use continuation sheets (Form 10-900a). Type all entries. 1. Name of Property_________________________{______________' historic name Lake Acworth Beach and Bathhouse other names/site number N/A NOV27T009 2. Location________________________________________________ street & number Lakeshore Drive city, town Acworth ( ) vicinity of county Cobb code 067 state Georgia code GA zip code 30101 ( ) not for publication 3. Classification____________________________________________ Ownership of Property: Category of Property: ( ) private ( ) building(s) (X) public-local (X) district ( ) public-state ( ) site (X) public-federal ( ) structure ( ) object Number of Resources within Property: Contributing Noncontributing buildings 1 1 sites 0 0 structures 1 4 objects 0 0 total 2 5 Contributing resources previously listed in the National Register: N/A Name of previous listing: N/A Name of related multiple property listing: N/A Lake Acworth Beach and Bathhouse, Cobb County, Georgia 4. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act of 1966, as amended, I hereby certify that this nomination meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60.
    [Show full text]
  • Sand 'N Sea Beach Homes Are Sleigh-Landing Approved
    Chron.com November 21, 2013 | Galveston Holiday Magic | Houston Chronicle Custom Publishing Group | 7 Sand ‘N Sea beach homes are sleigh-landing approved Imagine the panoramic beachfront view from the porches of Coastal Colors. Guests will be sitting pretty during the holidays on a Sand ‘N Sea beach house deck. With a selection of 150 properties, Sand ‘N Sea has the right place for groups of all sizes. Pet- friendly homes are available, too, so everyone can stay and play together. And if the youngsters ask, all homes have preapproved landing areas for Santa’s sleigh. Photos courtesy of Sand ‘N Sea Browse the vacation rental homes at sandnsea.com and see photos, floor plans, guest njoy a holiday home away from home at the beach this year. Celebrate with reviews and amenity lists for each house. Search by family and friends during the holidays or steal away for a relaxing retreat after preferred amenities, dates, or location and then book Ethe holidays — either way, a Sand ‘N Sea vacation home on Galveston Island is online or call the office. Join Sand ‘N Sea’s Guest Advan- the place to be. tage program and earn points toward a free weekend at a Make family memories this year preparing that special meal in a coastal kitchen, Sand ‘N Sea property. searching for sand dollars with family and friends, and toasting the view from a Rental agents are on standby, ready to help plan the ideal holiday vaca- beach or bay house porch. tion. Call 409-797-5500 or visit www.sandnsea.com..
    [Show full text]
  • Responses to Coastal Erosio in Alaska in a Changing Climate
    Responses to Coastal Erosio in Alaska in a Changing Climate A Guide for Coastal Residents, Business and Resource Managers, Engineers, and Builders Orson P. Smith Mikal K. Hendee Responses to Coastal Erosio in Alaska in a Changing Climate A Guide for Coastal Residents, Business and Resource Managers, Engineers, and Builders Orson P. Smith Mikal K. Hendee Alaska Sea Grant College Program University of Alaska Fairbanks SG-ED-75 Elmer E. Rasmuson Library Cataloging in Publication Data: Smith, Orson P. Responses to coastal erosion in Alaska in a changing climate : a guide for coastal residents, business and resource managers, engineers, and builders / Orson P. Smith ; Mikal K. Hendee. – Fairbanks, Alaska : Alaska Sea Grant College Program, University of Alaska Fairbanks, 2011. p.: ill., maps ; cm. - (Alaska Sea Grant College Program, University of Alaska Fairbanks ; SG-ED-75) Includes bibliographical references and index. 1. Coast changes—Alaska—Guidebooks. 2. Shore protection—Alaska—Guidebooks. 3. Beach erosion—Alaska—Guidebooks. 4. Coastal engineering—Alaska—Guidebooks. I. Title. II. Hendee, Mikal K. III. Series: Alaska Sea Grant College Program, University of Alaska Fairbanks; SG-ED-75. TC330.S65 2011 ISBN 978-1-56612-165-1 doi:10.4027/rceacc.2011 © Alaska Sea Grant College Program, University of Alaska Fairbanks. All rights reserved. Credits This book, SG-ED-75, is published by the Alaska Sea Grant College Program, supported by the U.S. Department of Commerce, NOAA National Sea Grant Office, grant NA10OAR4170097, projects A/75-02 and A/161-02; and by the University of Alaska Fairbanks with state funds. Sea Grant is a unique partnership with public and private sectors combining research, education, and technology transfer for the public.
    [Show full text]
  • Whale Shark Rhincodon Typus Populations Along the West Coast of the Gulf of California and Implications for Management
    Vol. 18: 115–128, 2012 ENDANGERED SPECIES RESEARCH Published online August 16 doi: 10.3354/esr00437 Endang Species Res Whale shark Rhincodon typus populations along the west coast of the Gulf of California and implications for management Dení Ramírez-Macías1,2,*, Abraham Vázquez-Haikin3, Ricardo Vázquez-Juárez1 1Centro de Investigaciones Biológicas del Noroeste, Mar Bermejo 195, Col. Playa Palo de Santa Rita, La Paz, Baja California Sur 23096, Mexico 2Tiburón Ballena México de Conciencia México, Manatí 4802, Col. Esperanza III, La Paz, Baja California Sur 23090, Mexico 3Asociación de Pesca Deportiva y Ecoturismo de Bahía de los Ángeles, Domicilio conocido Bahía de los Ángeles, Baja California 22980, Mexico ABSTRACT: We used photo-identification data collected from 2003 through 2009 to estimate pop- ulation structure, site fidelity, abundance, and movements of this species along the west coast of the Gulf of California to make recommendations for effective conservation and management. Of 251 whale sharks identified from 1784 photographs, 129 sharks were identified in Bahía de Los Ángeles and 125 in Bahía de La Paz. Only juveniles (mostly small) were found in these 2 bays. At Isla Espíritu Santo, we identified adult females; at Gorda Banks we identified 15 pregnant females. High re-sighting rates within and across years provided evidence of site fidelity among juvenile sharks in the 2 bays. Though the juveniles were not permanent residents, they used the areas regularly from year to year. A proportion of the juveniles spent days to a month or more in the coastal waters of the 2 bays before leaving, and periods of over a month outside the study areas before entering the bays again.
    [Show full text]
  • GEOG 101 PLACE NAME LIST for EXAM THREE
    GEOG 101 PLACE NAME LIST for EXAM THREE Each exam will have a place name location map section based on the list below, plus countries and political units. Consult the appropriate maps in the atlas and textbook to locate these places. The atlas has a detailed INDEX. Exam III will focus on place names from Asia and Oceania. This section of the exam will be in the form of a matching question. You will match the names to numbers on a map. ________________________________________________________________________________ I. CONTINENTS Australia Asia ________________________________________________________________________________ II. OCEANS Pacific Indian Arctic ________________________________________________________________________________ III. ASIA Seas/Gulfs/Bays/Lakes: Caspian Sea Sea of Japan Arabian Sea South China Sea Red Sea Aral Sea Lake Baikal East China Sea Bering Sea Persian Gulf Bay of Bengal Sea of Okhotsk ________________________________________________________________________________ Islands: New Guinea Taiwan Sri Lanka Singapore Maldives Sakhalin Sumatra Borneo Java Honshu Philippines Luzon Mindanao Cyprus Hokkaido ________________________________________________________________________________ Straits/Canals: Str. of Malacca Bosporas Dardanelles Suez Canal Str. of Hormuz ________________________________________________________________________________ Rivers: Huang Yangtze Tigris Euphrates Amur Ob Mekong Indus Ganges Brahmaputra Lena _______________________________________________________________________________ Mountains, Plateaus,
    [Show full text]
  • Mystique: the Pinnacle of the Ultra-Luxury Lifestyle in Naples
    + NAPLESNEWS.COM z FRIDAY, FEBRUARY 21, 2020 z 27T Mystique: The Pinnacle of the Ultra-Luxury Lifestyle in Naples ocated just steps from the beach and featuring a collection of elegantly-ap- amenities o er custom-designed interior spaces for socializing, including a club pointed and masterfully-designed residences, Mystique is redefi ning luxuri- room, parlor, salon, library and solarium/card room. Mystique also features a the- Lous beachfront living at one of Naples’ most prestigious addresses. ater, billiards room, board room, state-of-the-art health and fi tness club with the lat- The extraordinary lifestyle at this iconic 20-story tower surrounds residents in the est in exercise and wellness equipment, ladies’ and men’s steam rooms and showers, incomparable luxury – from expansive fl oorplans with walls of windows to spacious, and massage rooms with on-call masseurs and masseuses. private terraces showcasing breathtaking views, to world-class service and ameni- Residents may also enjoy the exclusive and renowned amenities of prestigious Peli- ties that cater to an exceptional lifestyle. can Bay, including private beachfront dining, extensive walking and biking trails, “Mystique is truly unique – even among the most luxurious o erings in Naples chau eured tram service, and private access to nearly three miles of unspoiled Gulf and beyond,” said Jennifer Urness, Director of Sales at Mystique. “It begins with the of Mexico beaches. prime location, the quality construction and the advanced technology. The extensive A limited number of estate residences at Mystique remain, ranging in size from resort-style amenities round out the incredible o ering.
    [Show full text]
  • LOUISIANA K. Meyer-Arendt Department of Geography
    65. USA--LOUISIANA K. Meyer-Arendt D.W. Davis Department of Geography Department of Earth Science Mississippi State University Nicholls State University Starkville, Mississippi 38759 Thibodaux, Louisiana 70301 United States of America United States of America INTRODUCTION Louisiana's 40,000 Inn 2 coastal zone developed over the last 7,000 years by the progradation, aggradation, and accretion of sediments introduced via various courses of the Mississippi River (Frazier 1967). The deltaic plain (32,000 km'), through which the modern river cuts diagon­ ally !Fig , 1), consists of vast wetlands and waterbodies. With eleva­ tions ranging from sea level up to 1.5 m, it is interrupted by natural levee ridges which decrease distally until they disappear beneath the marsh surface. The downdrift chenier plain of southwest Louisiana (8,000 km') consists of marshes, large round-to-oblong lakes, and stranded, oak covered beach ridges known as cheniers (Howe et al. 1935). This landscape is the result of alternating long-term phases of shoreline accretion and erosion that were dependent upon the proximit of an active sediment-laden river, and a low-energy marine environment (Byrne et al. 1959). Since the dyking of the Mississippi River, fluvial sedimentation in the deltaic plain has effectively been halted. Today, most Missis­ sippi River sediment is deposited on the outer continental shelf; only at the mouth of the Atchafalaya River distributary is deltaic sedimen­ tation subaerially significant (Adams and Baumann 1980). Over mos of the coastal zone, subsidence, saltwater intrusion, wave erosion, canalization, and other hydrologic modification have led to a rapid increase in the surface area of water (Davis 1986, Walker e al.
    [Show full text]
  • A Scientific Forum on the Gulf of Mexico: the Islands in the Stream Concept
    Proceedings: Gulf of Mexico Science Forum A Scientific Forum on the Gulf of Mexico: The Islands in the Stream Concept Proceedings of the Forum: 23 January 2008 Keating Education Center Mote Marine Laboratory Sarasota, Florida Proceedings: Gulf of Mexico Science Forum Table of Contents Forward (Ernest Estevez) .............................................................................................................4 Executive Summary.....................................................................................................................6 Acknowledgements ......................................................................................................................9 Organizing Committee ................................................................................................................9 Welcome and Introduction (Kumar Mahadevan and Daniel J. Basta) .....................................10 Introduction to the Forum (Billy D. Causey)...........................................................................12 Summary of Scientific Forum (John Ogden) ...........................................................................14 Panel 1: The Geological Setting...............................................................................................17 Geologic Underpinnings of the “Islands in the Stream”; West Florida Margin (Albert Hine and Stanley Locker)...............................................17 Shelf Edge of the Northwest Gulf of Mexico (Niall Slowey).............................................22
    [Show full text]