EIS 1080 ABO1 9714 Coastline Management Manual
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Potentially Useful Beach Nourishment and Associated Studies/Projects – References
Sand Nourishment Forum – Sand Nourishment Reference list October 2013 Updated from Coasts & Ports Conference, Sydney 2013 Potentially Useful Beach Nourishment and Associated Studies/Projects – References Foreword: The Coasts & Ports 2013 Organising Committee introduced a half- day Sand Nourishment Forum comprising a Questions and Answers format directed to an experienced Panel with audience participation to explore and promote the use of sand nourishment as a viable method for managing short term erosion and long term coastal recession. The Forum emanated from great interest in beach nourishment around Australia, with a long history of successful projects from Adelaide to Noosa and major projects on the Gold Coast. The 2013 Conference was launched with a keynote address from Dr Stefan Aarninkhof who was intricately involved in the Delfland Sand Engine project in the Netherlands, which has introduced 21.5M m3 of offshore sands to the Dutch coast to provide coastal protection and prevent coastal inundation. As a precursor to the Beach Nourishment Forum at the Coast & Ports Conference 2013 in Sydney, A. D. Gordon (Forum Moderator) compiled the following list of reference material with contributions from J.T. Carley, E.D. Couriel, A. L. Jackson, A.R Jones, D.B. Lord, A.F. Nielsen, T.D. Shand, R.B. Tomlinson, T. Stul, R. Tucker. The list is intended to be a start on a “live “ document that can be added to, as further reference material becomes available/unearthed. The list has been compiled to assist those carrying out or contemplating beach nourishment, beach scraping and entrance by-passing or back-passing projects. It is hoped that other special interest topics to the coastal and port engineering profession may be run in similar forums as part of the future Coasts & Ports Conference series. -
The Strait of Anian and British Northwest America: Cook's Third Voyage in Perspective*
The Strait of Anian and British Northwest America: Cook's Third Voyage in Perspective* JOHNNORRIS For local patriots of British Columbia, Captain Cook's third voyage is unsatisfactory. His stay at Nootka was so brief, his exploration of the coast so perfunctory, and his preoccupation with Alaska so much to be deplored. We are driven, in asking the reasons for these solecisms, to examine his instructions from the Admiralty for the third voyage. Alas, they hardly mention the coast of Northwest America between 45 ° and 65 ° North. Did their Lordships of the Admiralty slip up? Was Cook, that supreme professional who had had a hand in drawing up his own instructions, at less than his expert best? Did Palinurus nod at the helm? Cook's landing at Nootka was the result of his instructions "to put into the first convenient Port to recruit your Wood and Water and procure Refreshments . .Jîl But the prolongation of his stay to four weeks (29 March to 26 April 1778) was traceable to the bad fitting-out of his ships by the Navy Board, which resulted in the rotten foretop and mizzen masts of the Resolution having to be replaced after the strain of the spring gales of the North Pacific. Further, the avoidance of virtually all the rest of the British Columbia coast was in accordance with those instructions, since Cook was ordered to: ... proceed Northward along the Coast as far as the Latitude of 65 °, or farther, if you are not obstructed by Lands or Ice; taking care not to lose any time in exploring Rivers or Inlets, or upon any other account, until you get into the before-mentioned latitude of 65 °... -
U N C O R R Ec Ted Pr O
SED 773 Dispatch: 1.2.06 Journal: SED CE: Hari Journal Name Manuscript No. B Author Received: No. of pages: 18 PE: Revathi Sedimentology (2006) 1–18 doi: 10.1111/j.1365-3091.2006.00773.x Sedimentology and stratigraphy of a transgressive, muddy gravel beach: waterside beach, Bay of Fundy, Canada F SHAHIN E. DASHTGARD*, MURRAY K. GINGRAS* and KARL E. BUTLER *Department of Earth and Atmospheric Sciences, 1-26 Earth Sciences Building, University of Alberta, Edmonton, AB, Canada T6E 2G3 (E-mail: [email protected]) O Department of Geology, University of New Brunswick, PO Box 4400, Fredericton, NB, Canada E3B 5A3 ABSTRACT O Sediments exposed at low tide on the transgressive, hypertidal (>6 m tidal range) Waterside Beach, New Brunswick, Canada permit the scrutinyR of sedimentary structures and textures that develop at water depths equivalent to the upper and lower shoreface. Waterside Beach sediments are grouped into eleven sedimentologically distinct deposits that represent threeP depositional environments: (1) sandy foreshore and shoreface; (2) tidal-creek braid-plain and delta; and, (3) wave-formed gravel and sand bars, and associated deposits. The sandy foreshore and shoreface depositional environment encompasses the backshore; moderately dipping beachface; and, a shallowlyD seaward-dipping terrace of sandy middle and lower intertidal, and muddy sub-tidal sediments. Intertidal sediments reworked and deposited by tidal creeks comprise the tidal-creek braid plain and delta. Wave-formedE sand and gravel bars and associated deposits include: sediment sourced from low-amplitude, unstable sand bars; gravel deposited from large (up to 5Æ5 m high, 800 m long), landward-migrating gravel bars; and, zones ofT mud deposition developed on the landward side of the gravel bars. -
Map of the Division of Cook
COOK C C L H M k E W AR S L S T T P H A A A E ST A R T K e Tonbridge T R E S S ST L H I W PA T C Y E H O A VE Gannons ST Y A A C R Beverley F V S e W WE E E R F C PL R L S E S V E A A O T S R E M r E R A I A T D S O R E E E H N MULGA RD E R T O F O E O A C D Street D B R T B O W 1 T K R A L S D Ê C K Ë 151°3'EPark E151°4'E 151°5'E 151°6'E AN 151°7'ES R Y E 151°8'E 151°9'E 151°10'E 151°11'E 151°12'E 151°13'E 151°14'E T T N E E T U I V T T Park Golf S R A O S S P C S S L D N P RES D I N E D R O P T N T HE AV Y Y M S E Poulton O L N S H U T H R T D R Reserve M R Y n H A R O S T I T C LO A I R L E A N O S F T C A G E T T Course L C H N D T O AR D w U PAYTEN ST E E R A R k KES N L E L E T Park R S W I S E A S L T A G L C e E L G H T T R PL R D L A U I T D T S D A O T S S L D VIE K A R IN R ND R no e GS A E S A D R R A r C E R O O W P U K ME FL SA A e E T OR P W F D O Y N UR E N P UN S o R N WA R CRE C ER U D A C R E H T N E I L O DE T LDING T g N TS P Y R Q R O L L I A E T W A RD CK S C a P E E S B G R I S D T M G Oatley E S S S R L S D r R LA ST NG N HAI V a R S S D T D A M B S C A P Lime Kiln AS T A RES D T R h L D 33°59'S G D E A E A E OU A U R V E L DO L HE T O L A A O R E KOGARAH S I T B Bowling P Moore R D V I F B W E A D C R K T ST I H I G A C R T P B U T A D GO COOK A A R R T H N A R Bay I F A E A D E OATLEY R R A U T A R RAMSGATE HURSTVILLE I MS M Club Reserve N Y P E I R IT AV R T R R P S T T T T E A T L RD R C G O R E E P C K n R K AT T M A A I I E W B S D R K E A O E S H E K E D ST o N S N EN Y D E C N H A R t D S E S L a D T D -
“Major World Deltas: a Perspective from Space
“MAJOR WORLD DELTAS: A PERSPECTIVE FROM SPACE” James M. Coleman Oscar K. Huh Coastal Studies Institute Louisiana State University Baton Rouge, LA TABLE OF CONTENTS Page INTRODUCTION……………………………………………………………………4 Major River Systems and their Subsystem Components……………………..4 Drainage Basin………………………………………………………..7 Alluvial Valley………………………………………………………15 Receiving Basin……………………………………………………..15 Delta Plain…………………………………………………………...22 Deltaic Process-Form Variability: A Brief Summary……………………….29 The Drainage Basin and The Discharge Regime…………………....29 Nearshore Marine Energy Climate And Discharge Effectiveness…..29 River-Mouth Process-Form Variability……………………………..36 DELTA DESCRIPTIONS…………………………………………………………..37 Amu Darya River System………………………………………………...…45 Baram River System………………………………………………………...49 Burdekin River System……………………………………………………...53 Chao Phraya River System……………………………………….…………57 Colville River System………………………………………………….……62 Danube River System…………………………………………………….…66 Dneiper River System………………………………………………….……74 Ebro River System……………………………………………………..……77 Fly River System………………………………………………………...…..79 Ganges-Brahmaputra River System…………………………………………83 Girjalva River System…………………………………………………….…91 Krishna-Godavari River System…………………………………………… 94 Huang He River System………………………………………………..……99 Indus River System…………………………………………………………105 Irrawaddy River System……………………………………………………113 Klang River System……………………………………………………...…117 Lena River System……………………………………………………….…121 MacKenzie River System………………………………………………..…126 Magdelena River System……………………………………………..….…130 -
BUS TIMETABLE So We Can Adjust Services If Necessary
Opal, the only way to travel to and from school Although some might have a free pass, all students must tap on and tap off, every time SCHOOL BUS TIMETABLE so we can adjust services if necessary. Report lost, stolen, or damaged card immediately. www.transdevnsw.com.au While waiting for the replacement Opal card, students must T: (02) 8700 0555 use a Child/Youth Opal card or purchase a Single Trip ticket. Visit transportnsw.info/school-students or call 131 500 Woolooware High School (Woolooware) T: (02) 9523 6752 Effective Monday 20 July 2020 Route Departure MORNING Route Description Number Time From Port Hacking shops and Dolans Bay via Port Hacking Rd (L) Telopea (R)Saunders Bay (R) Parthenia (L) Port Hacking Rd (R) Turriell Point (R) Lilli Pilli Point, Port Hacking Rd (L) Crescent (R) 978 06:46 Willarong (06:59) (R) President (L) Kingsway (Caringbah Station, Kingsway 07:08) via (R) Banksia (L) Denman (L) Woolooware (R) Restormel to school (07:18) Note: DOES NOT OPERATE ON THURSDAY From Burraneer Point via (L) Rutherford, Eurabalong (R) Woolooware (L) Burraneer Bay Rd (R) S386 07:00 Gannons (R) Denman (L) Woolooware (R) Restormel to school (07:18) Note: DOES NOT OPERATE ON THURSDAY From Burraneer Point via Rutherford, Eurabalong (R) Woolooware (L) Burraneer Bay Rd (R) Gannons 988 (L) Kingsway (R) Banksia, Hay to Caringbah Shops (08:04) Becomes Route 969 via Hay (R) Kingsway 07:47 969 (R) Willarong (R) Dianella (R) Carwarra (L) Taronga (R) Irrubel (R) Burrawalla (L) Nullaburra (L) Denman (L) Woolooware (R) Sturt (08:15) From Miranda Interchange -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals -
The Colorado River Damming Impact on the Shrimp Fishery in the Upper
FRONTERA NORTE VOL. 33, ART. 9, 2021 https://doi.org/10.33679/rfn.v1i1.2137 The Colorado River Damming Impact on the Shrimp Fishery in the Upper Gulf of California, Mexico El impacto del represamiento del Río Colorado en la pesquería del camarón en el Alto Golfo de California, México Manuel Salvador Galindo Bect,1 Carlos Israel Vázquez León,2 & David Aguilar Montero3 ABSTRACT The objective oF this work is to demonstrate the relationship among the Colorado River Flows and volumes of shrimp caught in the Upper GulF of CaliFornia (AGC). A correlation analysis was applied to historical series of data about landed shrimp catch, fishing effort and flow from the Colorado River towards the gulf. Dependence, proportionality, and linear relationship indicators were obtained. The main results showed that the interannual captures were lower in periods without water input From the river and higher with the water inputs to the estuary. In addition, the results showed that the contributions of nutrients carried in the river water to the estuary could increase the Carbon Fixation. This study is important because it contributes to the discussion and strengthens the Fact that this river is important in the environmental and fishing dynamics in the AGC. Keywords: 1. Colorado River, 2. Fisheries, 3. shrimp, 4. damming, 5. Upper GulF oF CaliFornia. RESUMEN El objetivo de este trabajo es demostrar la relación entre los Flujos del Río Colorado y los volúmenes de camarón capturados en el Alto GolFo de CaliFornia (AGC). Se aplicó un análisis de correlación a series históricas de datos de captura del desembarque de camarón, el esfuerzo pesquero y el flujo del Río Colorado hacia el Delta. -
The Second Twenty Years, 1971-1991
Northwestern Michigan College The Second IVvenfy Years 1971 -1991 Al Shumsky Assisted by Carole Marlatt NORTHWESTERN MICHIGAN COLLEGE The Second Twenty Years 1971-1991 A1 Shumsky Assisted by Carole Marlatt February 1994 ACKNOWLEDGMENTS Thanks are due many people who helped with this project. First to the two people without whom it could not have been done: Tim Quinn and Carole Marlatt. Tim initiated the project and supported it with released time, and with no directions whatsoever beyond "Have a good time!" Carole not only prepared the manuscript, assembled the rosters in the appendix, chose the pictures, and both provided her own and edited my memories; she also is the one who recorded the Board minutes for these twenty years and then indexed them and preserved the hard copy so it was available to this amateur historian. (She, in fact, is the one to go to if you want to know what really went on during these years.) Thanks are also due these many others who graciously provided information or corroborated memories: Bob Buttleman, Doug Campbell, Becky Chartier, Jan Gasnik, Kathleen Guy, Chet Janik, Bill King, George Kuhn, Keith MacPhee, Nancy McArthur, Shelley Merrill, Dick Minor, Shirley Okerstrom, Barbara Raehl, Joe Rogers, PatSalathiel, Bill Shaw, Don Shikoski, Chuck Shreve, Robbie Teahen, Bob Warner, and Steve Westphal. Recognition is also due the hundreds of people—Board members, faculty and staff—whose names do not appear in this account, but who in fact constituted the College. Without them, there would be no history to write. I apologize to all whose contributions have not been specifically mentioned. -
Impacts of Sand Mining on Beaches in Suriname
Impacts of sand mining on beaches in Suriname Braamspunt beach, February 2016 Edward J. Anthony Consultant in Geomorphology and Shoreline Management June, 2016. Background p. 3 Abstract p. 4 Summary of recommendations p. 5 Part 1. The environment, context and formation of sandy beaches in Suriname p. 6 1.1. Introduction p. 7 1.2. The Guianas mud-bank system p. 11 1.3. Cheniers and chenier beaches: natural wave-energy buffers and ecosystems p. 15 1.4. Bank and inter-bank phases, and inter-bank chenier development p. 17 1.5. River mouths and chenier development p. 19 1.6. The Suriname Coastal Plain and long-term chenier development p. 22 Part 2. Recent shoreline changes in Suriname: general morphodynamics, methodology and results for Braamspunt beach p. 27 2.1. Chenier morphodynamics – cross-shore and longshore processes p. 28 2.1. The Maroni and Surniname river-mouth contexts and Braamspunt beach p. 33 2.2. Methodology: recent shoreline changes and evolution of Braamspunt beach p. 35 2.2.1. Mesoscale (multi-decadal changes) p. 35 2.2.2. Field surveys of the morphology and dynamics of Braamspunt beach p. 38 2.3. Recent bank and inter-bank phases on the Suriname coast p. 43 2.3.1. The Maroni-Suriname sector p. 44 2.3.2. The Suriname-Coppename sector p. 44 2.3.3. The Coppename-Corantijn sector p. 45 2.4. Morphodynamics of Braamspunt beach p. 45 2.4.1. Offshore and nearshore hydrodynamic conditions p. 45 2.4.2. Grain-size and sedimentology of Braamspunt beach p. -
Physiography
.1· , Atlantic Continental Shelf and Slope ~. of the United States ·- •t.,........_,C',...,.~~~""' 11:'·~~. '"''"' ~.~..-.. ......-.,· ....... ~ ·-,}........ ·. '~':7'n:.~~-... "" • '•ilfl::.t,l.>.o;r,~... ,, ~· ·-·· ·-. - '··~~ ..~-~'·· ··_ -·· ·~~--~----1 .., Physiography GEOLOGICAL SURVEY PROFESSIONAL PAPER 529-C Atlantic Continental · Shelf and Slope of The United States- Physiography By ELAZAR UCHUPI GEOLOGICAL SURVEY PROFESSIONAL PAPER 529-C Description of the submarine physiography of the continental margin between Nova Scotia and the Florida Keys UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director ~ : . For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract __________________________________________ _ C1 Continental margin-Continued Introduction ______________________________________ _ 1 Intermediate provinces _________________________ _ C17 General statement _____________________________ _ 1 Blake Plateau_·____________________________ _ 17 Acknowledgments ______ -.- ______________________ _ 3 Straits of Florida __________________________ _ 19 Continental margin ________________________________ _ 3 Continental slope ______________________________ _ 21 General setting________________________________ _ 3 Provinces seaward of the continental slope ________ _ 27 Continental shelf ______________________________ _ 3 Continental rise ___________________________ -
River Channel Bars and Dunes- Theory of Kinematic Waves
River Channel Bars and Dunes- Theory of Kinematic Waves GEOLOGICAL SURVEY PROFESSIONAL PAPER 422-L River Channel Bars and Dunes- Theory of Kinematic Waves By WALTER B. LANGBEIN and LUNA B. LEOPOLD PHYSIOGRAPHIC AND HYDRAULIC STUDIES OF RIVERS GEOLOGICAL SURVEY PROFESSIONAL PAPER 422-L UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 20 cents (paper cover) CONTENTS Page Page Abstract_________________________________________ LI Effect of rock spacing on rock movement in an ephemeral Introduction.______________________________________ 1 stream._________________________________________ L9 Flux-concentration relations________________________ 2 Waves in bed form________________________________ 12 Relation of particle speed to spacing a flume experi- General features________________________________ 12 ment______-_____-____-____-_-____________--____. 4 Kinematic properties_._______-._________________ 15 Transport of sand in pipes and flumes_________________ 5 Gravel bars____________________________________ 17 Flux-concentration curve for pipes________________ 6 Summary__________________________________________ 19 Flume transport of sand_________________________ 7 References________________.______________________ 19 ILLUSTRATIONS Page FIGURE 1. Flux-concentration curve for traffic___________________________________________________-_-_-__-___-