Intertidal Mudflats Worldwide
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Coastal Flood Defences - Groynes
Coastal Flood Defences - Groynes Coastal flood defences are key to protecting our coasts against flooding, which is when normally dry, low lying flat land is inundated by sea water. Hard engineering methods are forms of coastal flood defences which mitigate the risk of flooding and coastal erosion and the consequential effects. Hard Engineering Hard engineering methods are often used as a temporary measure to protect against coastal flooding as they are costly and only last for a relatively short amount of time before they require maintenance. However, they are very effective at protecting the coastline in the short-term as they are immediately effective as opposed to some longer term soft engineering methods. But they are often intrusive and can cause issues elsewhere at other areas along the coastline. Groynes are low lying wood or concrete structures which are situated out to sea from the shore. They are designed to trap sediment, dissipate wave energy and restrict the transfer of sediment away from the beach through long shore drift. Longshore drift is caused when prevailing winds blow waves across the shore at an angle which carries sediment along the beach.Groynes prevent this process and therefore, slow the process of erosion at the shore. They can also be permeable or impermeable, permeable groynes allow some sediment to pass through and some longshore drift to take place. However, impermeable groynes are solid and prevent the transfer of any sediment. Advantages and Disadvantages +Groynes are easy to construct. +They have long term durability and are low maintenance. +They reduce the need for the beach to be maintained through beach nourishment and the recycling of sand. -
Norway and Its Marine Areas - a Brief Description of the Sea Floor
No.3 2003 IN FOCUS Norway and its marine areas - a brief description of the sea floor From the deep sea to the fjord floor Norwegian waters comprise widely differing environments - from the Bjørnøyrenna deep sea via the continental slope and continental shelf to the coastal zone with its strandflat, archipelagos and fjords.This constitutes a geologi- cal diversity that is unique in a European context. An exciting geological history lies Trænadjupet behind this diversity - a development that has taken place over more than 400 million years.The continents con- Vøringplatået sist of plates of solidified rock that float on partially molten rock, and these plates move relative to one another.Where they collide, the Earth's crust is folded and mountain chains are created.Where they drift apart, deep oceans form and new sea Storegga floor is created along rifts because molten rock (magma) streams up from below. A good example is the Mid-Atlantic Ridge, including Iceland, a which is a result of Greenland and n n e Europe drifting from each other at a r e rate of about 2 cm a year. k s r o The plates on which Norway and N Greenland rest collided more than 400 million years ago and formed mountain chains on either side of a Skagerrak shallow sea. Both Greenland and Norway are remnants of worn down mountain chains. Between these mountain chains, the shallow sea Figure 1.Norway and its neighbouring seas. gradually filled with sediments derived from the erosion of the chains.These sedi- ments became transformed into sandstones, shales and limestones and it is in these rocks we now find oil and gas on the Norwegian continental shelf. -
Ramsar Sites in Order of Addition to the Ramsar List of Wetlands of International Importance
Ramsar sites in order of addition to the Ramsar List of Wetlands of International Importance RS# Country Site Name Desig’n Date 1 Australia Cobourg Peninsula 8-May-74 2 Finland Aspskär 28-May-74 3 Finland Söderskär and Långören 28-May-74 4 Finland Björkör and Lågskär 28-May-74 5 Finland Signilskär 28-May-74 6 Finland Valassaaret and Björkögrunden 28-May-74 7 Finland Krunnit 28-May-74 8 Finland Ruskis 28-May-74 9 Finland Viikki 28-May-74 10 Finland Suomujärvi - Patvinsuo 28-May-74 11 Finland Martimoaapa - Lumiaapa 28-May-74 12 Finland Koitilaiskaira 28-May-74 13 Norway Åkersvika 9-Jul-74 14 Sweden Falsterbo - Foteviken 5-Dec-74 15 Sweden Klingavälsån - Krankesjön 5-Dec-74 16 Sweden Helgeån 5-Dec-74 17 Sweden Ottenby 5-Dec-74 18 Sweden Öland, eastern coastal areas 5-Dec-74 19 Sweden Getterön 5-Dec-74 20 Sweden Store Mosse and Kävsjön 5-Dec-74 21 Sweden Gotland, east coast 5-Dec-74 22 Sweden Hornborgasjön 5-Dec-74 23 Sweden Tåkern 5-Dec-74 24 Sweden Kvismaren 5-Dec-74 25 Sweden Hjälstaviken 5-Dec-74 26 Sweden Ånnsjön 5-Dec-74 27 Sweden Gammelstadsviken 5-Dec-74 28 Sweden Persöfjärden 5-Dec-74 29 Sweden Tärnasjön 5-Dec-74 30 Sweden Tjålmejaure - Laisdalen 5-Dec-74 31 Sweden Laidaure 5-Dec-74 32 Sweden Sjaunja 5-Dec-74 33 Sweden Tavvavuoma 5-Dec-74 34 South Africa De Hoop Vlei 12-Mar-75 35 South Africa Barberspan 12-Mar-75 36 Iran, I. R. -
Striped Bass Morone Saxatilis
COSEWIC Assessment and Status Report on the Striped Bass Morone saxatilis in Canada Southern Gulf of St. Lawrence Population St. Lawrence Estuary Population Bay of Fundy Population SOUTHERN GULF OF ST. LAWRENCE POPULATION - THREATENED ST. LAWRENCE ESTUARY POPULATION - EXTIRPATED BAY OF FUNDY POPULATION - THREATENED 2004 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2004. COSEWIC assessment and status report on the Striped Bass Morone saxatilis in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 43 pp. (www.sararegistry.gc.ca/status/status_e.cfm) Production note: COSEWIC would like to acknowledge Jean Robitaille for writing the status report on the Striped Bass Morone saxatilis prepared under contract with Environment Canada, overseen and edited by Claude Renaud the COSEWIC Freshwater Fish Species Specialist Subcommittee Co-chair. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Ếgalement disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur la situation de bar rayé (Morone saxatilis) au Canada. Cover illustration: Striped Bass — Drawing from Scott and Crossman, 1973. Her Majesty the Queen in Right of Canada 2004 Catalogue No. CW69-14/421-2005E-PDF ISBN 0-662-39840-8 HTML: CW69-14/421-2005E-HTML 0-662-39841-6 Recycled paper COSEWIC Assessment Summary Assessment Summary – November 2004 Common name Striped Bass (Southern Gulf of St. -
Firth of Lorn Management Plan
FIRTH OF LORN MARINE SAC OF LORN MARINE SAC FIRTH ARGYLL MARINE SPECIAL AREAS OF CONSERVATION FIRTH OF LORN MANA MARINE SPECIAL AREA OF CONSERVATION GEMENT PLAN MANAGEMENT PLAN CONTENTS Executive Summary 1. Introduction CONTENTS The Habitats Directive 1.1 Argyll Marine SAC Management Forum 1.2 Aims of the Management Plan 1.3 2. Site Overview Site Description 2.1 Reasons for Designation: Rocky Reef Habitat and Communities 2.2 3. Management Objectives Conservation Objectives 3.1 Sustainable Economic Development Objectives 3.2 4. Activities and Management Measures Management of Fishing Activities 4.1 Benthic Dredging 4.1.1 Benthic Trawling 4.1.2 Creel Fishing 4.1.3 Bottom Set Tangle Nets 4.1.4 Shellfish Diving 4.1.5 Management of Gathering and Harvesting 4.2 Shellfish and Bait Collection 4.2.1 Harvesting/Collection of Seaweed 4.2.2 Management of Aquaculture Activities 4.3 Finfish Farming 4.3.1 Shellfish Farming 4.3.2 FIRTH OF LORN Management of Recreation and Tourism Activities 4.4 Anchoring and Mooring 4.4.1 Scuba Diving 4.4.2 Charter Boat Operations 4.4.3 Management of Effluent Discharges/Dumping 4.5 Trade Effluent 4.5.1 CONTENTS Sewage Effluent 4.5.2 Marine Littering and Dumping 4.5.3 Management of Shipping and Boat Maintenance 4.6 Commercial Marine Traffic 4.6.1 Boat Hull Maintenance and Antifoulant Use 4.6.2 Management of Coastal Development/Land-Use 4.7 Coastal Development 4.7.1 Agriculture 4.7.2 Forestry 4.7.3 Management of Scientific Research 4.8 Scientific Research 4.8.1 5. -
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone. -
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, -
Safe Boating Through the St. Lucie Inlet
Information: Florida Fish & Wildlife Commission 850-488-4676 SAFE BOATING US Coast Guard - Ft. Pierce 772-461-7606 THROUGH THE ST. LUCIE INLET US Coast Guard Auxiliary 772-465-8128 US Army Corps of Engineers 772-221-3349 St. Lucie Inlet Coastal 772-225-2300 Weather Station HERE ARE SOME THINGS TO REMEMBER: • Listen to the most recent weather forecast for the times you plan to go out AND come back in the inlet. • Look in the Tide Tables or local newspapers for the times St. Lucie Inlet of predicted high and low tides for the day you plan to go out. Remember the outgoing (ebb) tital current at low Newcomers tide is the worst time to make a passage through the St. Lucie Inlet. If you are a boater new to this area, it is highly • Safe boating practices are even more important in inlets. recommended that you make your first passage of Check your boat before you head out. Life preservers the St. Lucie Inlet as an observer. An experienced should be worn when going through inlets. boater with local knowledge at the helm can point • Expect the unexpected. Watch the clouds to anticipate out various hazards and conditions to avoid. This is severe weather such as thunderstorms. Be on the lookout for shifting shoals and changing channels. especially important if you have no prior experience • Engine failure is common in small boats in rough seas. with any ocean inlets. The extra roughness agitates gasoline and settled dirt or water in the fuel system, which can cause engine failure Notes on Navigation at Night at a crtical time. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
The Case for a Marine Act for Scotland the Tangle of the Forth
The Case for a Marine Act for Scotland The Tangle of the Forth © WWF Scotland For more information contact: WWF Scotland Little Dunkeld Dunkeld Perthshire PH8 0AD t: 01350 728200 f: 01350 728201 The Case for a Marine Act for Scotland wwf.org.uk/scotland COTLAND’S incredibly Scotland’s territorial rich marine environment is waters cover 53 per cent of Designed by Ian Kirkwood Design S one of the most diverse in its total terrestrial and marine www.ik-design.co.uk Europe supporting an array of wildlife surface area Printed by Woods of Perth and habitats, many of international on recycled paper importance, some unique to Scottish Scotland’s marine and WWF-UK registered charity number 1081274 waters. Playing host to over twenty estuarine environment A company limited by guarantee species of whales and dolphins, contributes £4 billion to number 4016274 the world’s second largest fish - the Scotland’s £64 billion GDP Panda symbol © 1986 WWF – basking shark, the largest gannet World Wide Fund for Nature colony in the world and internationally 5.5 million passengers and (formerly World Wildlife Fund) ® WWF registered trademark important numbers of seabirds and seals 90 million tonnes of freight Scotland’s seas also contain amazing pass through Scottish ports deepwater coral reefs, anemones and starfish. The rugged coastline is 70 per cent of Scotland’s characterised by uniquely varied habitats population of 5 million live including steep shelving sea cliffs, sandy within 0km of the coast and beaches and majestic sea lochs. All of 20 per cent within km these combined represent one of Scotland’s greatest 25 per cent of Scottish Scotland has over economic and aesthetic business, accounting for 11,000km of coastline, assets. -
Social, Economic and Cultural Overview of Western Newfoundland and Southern Labrador
Social, Economic and Cultural Overview of Western Newfoundland and Southern Labrador ii Oceans, Habitat and Species at Risk Publication Series, Newfoundland and Labrador Region No. 0008 March 2009 Revised April 2010 Social, Economic and Cultural Overview of Western Newfoundland and Southern Labrador Prepared by 1 Intervale Associates Inc. Prepared for Oceans Division, Oceans, Habitat and Species at Risk Branch Fisheries and Oceans Canada Newfoundland and Labrador Region2 Published by Fisheries and Oceans Canada, Newfoundland and Labrador Region P.O. Box 5667 St. John’s, NL A1C 5X1 1 P.O. Box 172, Doyles, NL, A0N 1J0 2 1 Regent Square, Corner Brook, NL, A2H 7K6 i ©Her Majesty the Queen in Right of Canada, 2011 Cat. No. Fs22-6/8-2011E-PDF ISSN1919-2193 ISBN 978-1-100-18435-7 DFO/2011-1740 Correct citation for this publication: Fisheries and Oceans Canada. 2011. Social, Economic and Cultural Overview of Western Newfoundland and Southern Labrador. OHSAR Pub. Ser. Rep. NL Region, No.0008: xx + 173p. ii iii Acknowledgements Many people assisted with the development of this report by providing information, unpublished data, working documents, and publications covering the range of subjects addressed in this report. We thank the staff members of federal and provincial government departments, municipalities, Regional Economic Development Corporations, Rural Secretariat, nongovernmental organizations, band offices, professional associations, steering committees, businesses, and volunteer groups who helped in this way. We thank Conrad Mullins, Coordinator for Oceans and Coastal Management at Fisheries and Oceans Canada in Corner Brook, who coordinated this project, developed the format, reviewed all sections, and ensured content relevancy for meeting GOSLIM objectives. -
1 the Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration
1 The Influence of Groyne Fields and Other Hard Defences on the Shoreline Configuration 2 of Soft Cliff Coastlines 3 4 Sally Brown1*, Max Barton1, Robert J Nicholls1 5 6 1. Faculty of Engineering and the Environment, University of Southampton, 7 University Road, Highfield, Southampton, UK. S017 1BJ. 8 9 * Sally Brown ([email protected], Telephone: +44(0)2380 594796). 10 11 Abstract: Building defences, such as groynes, on eroding soft cliff coastlines alters the 12 sediment budget, changing the shoreline configuration adjacent to defences. On the 13 down-drift side, the coastline is set-back. This is often believed to be caused by increased 14 erosion via the ‘terminal groyne effect’, resulting in rapid land loss. This paper examines 15 whether the terminal groyne effect always occurs down-drift post defence construction 16 (i.e. whether or not the retreat rate increases down-drift) through case study analysis. 17 18 Nine cases were analysed at Holderness and Christchurch Bay, England. Seven out of 19 nine sites experienced an increase in down-drift retreat rates. For the two remaining sites, 20 retreat rates remained constant after construction, probably as a sediment deficit already 21 existed prior to construction or as sediment movement was restricted further down-drift. 22 For these two sites, a set-back still evolved, leading to the erroneous perception that a 23 terminal groyne effect had developed. Additionally, seven of the nine sites developed a 24 set back up-drift of the initial groyne, leading to the defended sections of coast acting as 1 25 a hard headland, inhabiting long-shore drift.