Erosion in Europe
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Towards a New Relationship of Man and Nature in Temperate Lands Vers Un Nouveau Type De Relations Entre L'homme Et La Nature En Région Tempérée
IUCN Publications new series No 8 Tenth Technical Meeting / Dixième Réunion technique LUCERNE (SWITZERLAND - SUISSE) June / juin 1966 Proceedings and Papers / Procès-verbaux et rapports Towards a new Relationship of Man and Nature in Temperate Lands Vers un nouveau type de relations entre l'homme et la nature en région tempérée PART II Town and Country Planning Problems Problèmes d'aménagement du territoire Published with the assistance of UNESCO International Union Union Internationale for the Conservation of Nature pour la Conservation de la Nature and Natural Resources et de ses Ressources Morges, Switzerland 1967 The International Union for Conservation of Nature and Natural Resources (IUCN) was founded in 1948 and has its headquarters in Morges, Switzerland; it is an independent international body whose membership comprises states, irrespective of their political and social systems, government departments and private institutions as well as international organisations. It represents those who are concerned at man's modification of the natural environment through the rapidity of urban and industrial development and the excessive exploitation of the earth's natural resources, upon which rest the foundations of his survival. IUCN's main purpose is to promote or support action which will ensure the perpetuation of wild nature and natural resources on a world-wide basis, not only for their intrinsic cultural or scientific values but also for the long-term economical and social welfare of mankind. This objective can be achieved through active conservation pro- grammes for the wise use of natural resources in areas where the flora and fauna are of particular importance and where the landscape is especially beautiful or striking or of historical or cultural or scientific significance. -
Morsum 1.4.Pub
Vielen Dank für Ihr Interesse an der Ferienwohnung Sylter Rabe! ANREISE NACH SYLT Die Ferienwohnung Sylter Rabe liegt im Ort Morsum auf der Insel Sylt. Sylt ist die wohl bekannteste deutsche Ferieninsel und in der Nordsee gelegen. Für die Anreise stehen die Bahn (Personen– und Autozug), die Fähren, oder das Flugzeug zur Verfügung. Das dabei am häufigsten genutzte Verkehrsmittel, ist zweifelsfrei die Bahn (Autozug für PKW Hin- und Rückfahrt ab Niebüll derzeit 92,00€ / stand Frühjahr 2016). Der größte Andrang am Autozug (Verladung erfolgt im Ort Niebüll) ist samstags, da der Samstag der klassische Wechseltag auf der Insel im Bereich der Ferienunterkünfte ist. Das bedeutet, dass die meisten Mieter bis 10.00 Uhr Ihre Unterkünfte räumen müssen und sich je Autozug nach Westerland nach Wetterlage aufmachen, die Insel zu verlas- sen. Bei schlechtem Wetter wollen alle gleich weg, bei gutem Wetter verbringt man den Tag noch auf der Insel. Diese Umstände gilt es zu berücksichti- gen, wenn man Wartezeiten am Zug vermeiden möchte. Auch wenn sich die Bahn auf Spitzenzei- ten in Verbindung mit Ferien- und Feiertagen einstellt, kann es durchaus vorkommen, dass man nicht mehr auf den geplanten Zug kommt, da be- reits einige andere Fahrzeuge in den vielen War- tespuren stehen. Dann kommt es zu Wartezeiten von 30 Min. oder länger — die Abfahrt- zeiten können online unter www.sylt-shuttle.de ebenso abgefragt werden, wie die aktuelle Lage an der Autoverladung. Seit 2016 fährt auch die RDC Deutschland einige Zeiten. Bei der Anreise können Sie an einem der vielen DRIVE-IN Schaltern in Niebüll u.a. be- quem mit EC Karte zahlen und das Rückfahrtticket gleich mitbuchen. -
Erosion Is the Process Where Soft Shorelines (Sand, Gravel Or Cobble) Disappear and Land Is Lost
COASTAL EROSION Action Guide What is Coastal Erosion? Erosion is the process where soft shorelines (sand, gravel or cobble) disappear and land is lost. Erosion generally comes in two forms: 1. A Natural part of the coastal environment where a soft shore moves and changes in response to cyclic climate conditions and 2. Erosion can be induced by human interference of natural sand movement and budget patterns. Erosion can be slow and ongoing over many years or fast and dramatic following large storm events. Many erosion problems in the Pacific today, occur because of poor planning, inappropriate shoreline development, overcrowding, beach mining for building material and due to reef degradation. Erosion is a natural process It is important to understand that erosion is a natural process and in many cases is accompanied by its equal and opposite process “accretion”. Put simply, sandy shorelines are dynamic and should be expected to shift and change over time, sometimes by 100’s of meters. This process becomes an “erosion problem” if development is not carefully planned to avoid unstable shorelines. Why is it that erosion seems more of a problem these days? In past times, people lived in harmony with their moving coasts. Their houses could be easily moved to and shoreline homes were built in way which did not disturb shoreline processes (eg. On stilts or pylons). People knew and avoided dangerous or unstable locations. Today, building styles have changed and homes cannot be easily moved or replaced and lack of space often results in people building in locations which are known to be inappropriate. -
PDF Brunel Et Al., 2014
Geomorphology 204 (2014) 625–637 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph 20th century sediment budget trends on the Western Gulf of Lions shoreface (France): An application of an integrated method for the study of sediment coastal reservoirs C. Brunel a,⁎,R.Certaina, F. Sabatier b,N.Robina, J.P. Barusseau a,N.Alemana, O. Raynal a a Université de Perpignan, Laboratoire d'Etudes des Géo-Environnements Marins, 52 av. P Alduy, 66860 Perpignan, France b Aix Marseille Université, CEREGE, UMR 7330 CNRS, Europôle Méditerranéen de l'Arbois, 13545 Aix en Provence Cedex 4, France article info abstract Article history: This paper presents a shoreface sediment budget established for the 20th century (1895–1984–2009) along the Received 17 April 2013 microtidal wave-dominated coast of the western Gulf of Lions (Languedoc-Roussillon, Mediterranean Sea, SE Received in revised form 6 September 2013 France). The implementation of a diachronic bathymetric approach, coupled with the definition of sand reser- Accepted 12 September 2013 voirs (upper sand unit — USU) by very high-resolution seismic surveys and the results of LiDAR investigations, Available online 2 October 2013 offers a new means of defining precisely the magnitude and change trends of the sediment budget. The aim of this study is to link the Large Scale Coastal Behaviour (LSCB) of the littoral prism (expressed in terms of shoreface Keywords: Shoreface sediment budget sediment budget, shoreface sediment volume and spatial distribution pattern of cells) to climatic change, river Large Scale Coastal Behaviour sediment input to the coast, longshore sediment transport distribution, impact of hard coastal defence structures Seismic surveys and artificial beach nourishment. -
ADVENTURE GUIDE Getting Away from It All on Sylt
ADVENTURE GUIDE Getting away from it all on Sylt. Sylt Shuttle: the fast and relaxed way to travel. You can rely on our decades of experience. We offer the highest capacity and guarantee to get you on the move with our double-decker car trains. Running 14,000 trains a year, we are there for you from early morning to late evening: your fast, safe and reliable shuttle service. We look forward to welcoming you aboard. More information at bahn.de/syltshuttle 14,000 trains a year. The Sylt Shuttle. www.sylt.de Last update November 2019 Anz_Sylt_Buerostuhl_engl_105x210_mm_apu.indd 1 01.02.18 08:57 ADVENTURE GUIDE 3 SYLT Welcome to Sylt Boredom on Sylt? Wrong! Whether as a researcher in Denghoog or as a dis- coverer in the mudflats, whether relaxed on the massage bench or rapt on a surfboard, whether as a daydreamer sitting in a roofed wicker beach chair or as a night owl in a beach club – Sylt offers an exciting and simultaneously laid-back mixture of laissez-faire and savoir-vivre. Get started and explore Sylt. Enjoy the oases of silence and discover how many sensual pleasures the island has in store for you. No matter how you would like to spend your free time on Sylt – you will find suitable suggestions and contact data in this adventure guide. Content NATURE . 04 CULTURE AND HISTORY . 08 GUIDED TOURS AND SIGHTSEEING TOURS . 12 EXCURSIONS . 14 WELLNESS FOR YOUR SOUL . 15 WELLNESS AND HEALTH . 16 LEISURE . 18 EVENT HIGHLIGHTS . .26 SERVICE . 28 SYLT ETIQUETTE GUIDE . 32 MORE ABOUT SYLT . -
Predicting Shoreline Evolution on a Centennial Scale Using the Example of the Vistula (Baltic) Spit I
ISSN 00014370, Oceanology, 2012, Vol. 52, No. 5, pp. 700–709. © Pleiades Publishing, Inc., 2012. Original Russian Text © I.O. Leont’yev, 2012, published in Okeanologiya, 2012, Vol. 52, No. 5, pp. 757–767. MARINE GEOLOGY Predicting Shoreline Evolution on a Centennial Scale Using the Example of the Vistula (Baltic) Spit I. O. Leont’yev Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia Email: [email protected] Received March 31, 2011; in final form, November 22, 2011 Abstract—The proposed algorithm comprises three main steps. The first step is the evaluation of the sedi ment transport and budget. It was shown that the root segment of the Vistula Spit is dominated by eastward longshore sediment transport (up to 50 thousand m3/year). Over the rest of the spit, the shoreline’s orienta tion causes westward sediment transport (more than 100 thousand m3/year). The gradients of the longshore and cross shore sediment transport become the major contributors to the overall sediment balance. The only exception is the northeastern tip of the spit due to the appreciable imbalance of the sediment budget (13 m3 m–1 yr–1). The second step in the prediction modeling is the estimation of the potential sealevel changes during the 21st century. The third step involves modeling of the shoreline’s behavior using the SPELT model [6, 7, 8]. In the most likely scenario, the rate of the recession is predicted to be about 0.3 m/year in 2010–2050 and will increase to 0.4 m/year in 2050–2100. The sand deficit, other than the sealevel rise, will be a key factor in the control of the shoreline’s evolution at the northeastern tip of the spit, and the amount of recession will range from 160 to 200 m in 2010–2100. -
Sea Level Rise and Coastal Morphological Changes on Tropical Islands New Caledonia and French Polynesia (South Pacific) the Project
Manuel Garcin, Marissa Yates, Goneri Le Cozannet, Patrice Walker, Vincent Donato Sea level rise and coastal morphological changes on tropical islands New Caledonia and French Polynesia (South Pacific) The Project • Work completed within the CECILE project (Coastal Environmental Changes: Impact of sea LEvel rise )=> See Poster Le Cozannet et al. same session • Project objectives: to contribute to assessing the physical impact of sea level rise on shorelines during the recent past (last 50 years) and near future (next 100 years). • Focus on tropical islands : New Caledonia, French Polynesia, La Réunion (Indian Ocean), French Caribbean • What is the importance of recent sea level rise with respect to other causes of change ? • What will be the consequences of sea level rise for coastal change in the future ? GARCIN M., YATES M., LE COZANNET G., WALKER P., DONATO V. (EGU 2011) ‐ Sea level rise and coastal morphological changes on tropical islands Generic driving factors influencing coastline mobility, dynamics and morphology Coastline mobility is an indicator integrating numerous parameters • 5 families of driving factors affecting coastline mobility Erosion, accretion, transport... – Climate change External geodynamics – External geodynamic processes Pluviometry processes linked to climate change Biological Sea Level – Internal geodynamic Change, processes winds, storms, processes pluviometry... – Biological processes Coastline Anthropogenic Climate change actions and – Anthropogenic actions and mobility impacts impacts Tectonic, vertical Sea defences, • To note : interactions & movements, gravels isostasy... extraction, mining, retroactions daming.... Internal geodynamics processes GARCIN M., YATES M., LE COZANNET G., WALKER P., DONATO V. (EGU 2011) ‐ Sea level rise and coastal morphological changes on tropical islands Driving factors Or The data problem GARCIN M., YATES M., LE COZANNET G., WALKER P., DONATO V. -
Beach Erosion in the Gulf of Castellammare Di Stabia in Response to the Trapping of Longshore Drifting Sediments of the Gulf of Napoli (Southern Italy)
geosciences Article Beach Erosion in the Gulf of Castellammare di Stabia in Response to the Trapping of Longshore Drifting Sediments of the Gulf of Napoli (Southern Italy) Micla Pennetta ID Dipartimento di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università degli Studi di Napoli “Federico II”, 80138 Naples, Italy; [email protected] Received: 10 May 2018; Accepted: 25 June 2018; Published: 27 June 2018 Abstract: The results of this study have allowed verification that longshore sediment transport along the coast of Napoli Gulf (southern Italy) takes place from Northwest to Southeast. The current analysis describes the results of an integrated sedimentological and geomorphological study of the Neapolitan coastal area. A sedimentological and morphosedimentary study was carried out by bathymetric survey and sampling of bottom sediments. The analysis of modal isodensity curves shows that all the sediments are moved from NW to SE by longshore currents parallel to the coastline. The morphological evolution of the Castellammare di Stabia Gulf coastal area, based on historical coastline changes, starts from 1865, when the sandy littoral was wide and in its natural state. Since the construction of the Torre Annunziata harbor in 1871, sediments transported by a NW-SE longshore drift have become trapped, inducing the genesis of a new wide triangular-shaped beach on the updrift side (NW) of the harbor breakwall. This process induced a significant shoreline retreat of the south-east sector of the littoral. Widespread beach erosion of the coastal physiographic unit of Castellammare di Stabia Gulf (delimited by two ports) is more developed in the southern portion. -
Beach Nourishment Effects Hald Beach - Denmark 1984
Beach nourishment effects Hald beach - Denmark 1984 July 2020 Project Building with Nature (EU-InterReg) Start date 01.11.2016 End date 01.04.2020 Project manager (PM) Ane Høiberg Nielsen Project leader (PL) Per Sørensen Project staff (PS) Henrik Vinge Karlsson Time registering 402412 Approved date 27.01.2020 Signature Report Analysis of the effect of a beach nourishment, Hald beach, Denmark Author Henrik Vinge Karlsson, Per Sørensen Keyword Beach nourishment, Coastal protection, Building with nature, Hald beach Distribution www.kyst.dk, www.buildingwithnature.com Referred to as Kystdirektoratet (2020), Beach nourishment effects – Hald Beach, Kystdirek- toratet, Lemvig. 2 Beach Nourishment Effects Contents 1 Introduction .............................................................................................................. 5 1.1 Objective ............................................................................................................................................................................... 6 1.2 Criteria’s for the nourishment stretch .....................................................................................................................7 1.3 Decision on nourishment stretch ..............................................................................................................................7 1.4 Financing of the beach nourishment ...................................................................................................................... 8 1.5 Definitions and term diagram ................................................................................................................................... -
CORONA Teststationen Im Überblick Entwurf.Indd
präsentiert die Standorte der SCHNELLTEST-STATIONEN LIST AM FÄHRANLEGER DER SYLTFÄHRE 1 Am Fähranleger, List HAFEN PARKPLATZ 2 Hafenstrasse, List KAMPEN KURHAUSSTRASSE 3 2 Ecke Hauptstraße, Kampen LIST 1 STURMHAUBE PARKPLATZ 4 Riperstieg 1, Kampen KAAMPHÜS 5 Hauptstr. 12, Kampen Zugang nur über den Innenhof, keine Parkplätze BUHNE 16 PARKPLATZ (ab KW17) 6 6 Listlandstr. 133b, Kampen WENNINGSTEDT PASTORAT WENNINGSTEDT WESTERLAND KAMPEN 7 Bi Kiar 3, Wenningstedt 11 BAHNWEG 31 DRIVE-IN 4 PARKPLATZ BEIM MINIGOLF 8 NORDSEEKLINIK 3 5 Dünenstraße 1000, Wenningstedt 12 Norderstraße 81, Westerland NÄHE STRANDPROMENADE Mo-Fr: 7-9:00/14-16:00/19-21:00 Uhr & 9-13:00 Uhr WENNINGSTEDT 9 BRADERUP 710 SYLTNESS CENTER INSELZIRKUS FAHRRAD DRIVEIN 13 10 Dr. Nicolas-Str. 3, Westerland 9 8 Kampener Weg, Wenningstedt SCHULZENTRUM WALK-IN/ohne Anmeldung 12 KEITUM 14 Tonderner Straße 10-12, Westerland WESTERLAND PARKPLATZ WEST Montags, Mittwochs, Freitags 8-14:00 Uhr 14 23 13 11 Gurtstig 21, am Kreisverkehr ZOB WESTERLAND WALK-IN/ ohne Anmeldung 17 15 20 TOURISTINFORMATION KEITUM ab 22. April 2021 - täglich 7-14:00 Uhr 19 21 24 16 Gurtstig 23, Keitum BAHNHOF WESTERLAND 15 16 Trift 1, Westerland 23 24 Eingang zu Fuß direkt rechts, neben der ESSO Tankstelle 22 23 HOTEL STADT HAMBURG KEITUM 17 Strandstr. 2, Westerland 18 neben Wellnessbereich auf der Wiese (ab KW17) CAMPINGPLATZ WESTERLAND 18 Süderstr. 66, Westerland RANTUM 27 VILLA KUNTERBUNT 19 Obere Promenade, Westerland 26 TINNUM FLUGHAFEN WESTERLAND DRIVE-IN 20 Flughafen Sylt, Halle 74, Tinnum - max. Durchfahrtshöhe 2m 28 RANTUM TURNHALLE AM EHEM. FLIEGERHORST SANSIBAR PARKPLATZ 21 Flughafen 1, Tinnum 25 Hörnumer Str. -
Short Course on Principles and Applications of Beach Nourishment
Sediment storage at tidal inlets Item Type book_section Authors Mehta, Ashish J. Publisher University of Florida Coastal and Oceanographic Engineering Department Download date 02/10/2021 02:44:06 Link to Item http://hdl.handle.net/1834/18142 UFL/COEL - 89/002 SHORT COURSE ON PRINCIPLES AND APPLICATIONS OF BEACH NOURISHMENT February 21, 1989 * * Instructors * * Thomas Campbell Robert G. Dean Ashish J. Mehta Hsiang Wang S* Organized by * FLORIDA SHORE AND BEACH PRESERVATION ASSOCIATION DEPARTMENT OF COASTAL AND OCEANOGRAPHIC ENGINEERING. UNIVERSITY OF FLORIDA Short Course on Principles and Applications of Beach Nourishment February 21, 1989 Organized by Florida Shore and Beach Preservation Association Department of Coastal and Oceanographic Engineering, University of Forida Instructors Thomas Campbell Robert G.Dean Ashish J. Mehta Hsiang Wang Chapter 4 SEDIMENT STORAGE AT TIDAL INLETS Ashish J. Mehta Coastal and Oceanographic Engineering Department University of Florida, Gainesville INTRODUCTION Accumulation of sediment around tidal inlets has become a matter of renewed interest mainly for three reasons. The first of these is the need to estimate the shoal volumes, particularly in the ebb shoal, as a potential source of sediment for beach nourishment. Portions of the ebb shoal can be transferred to the beach provided there are no measurable adverse effects on navigation, or on the stability of the shoreline near the inlet. Such an operation, for example, has been carried out successfully at Redfish Pass, on the Gulf of Mexico coast of Florida (Olsen, 1979). A schematic example of a potential site for ebb shoal excavation and sand transfer to the downdrift beach is shown in Fig. -
Aeolian Sediment Transport and Natural Dune Development, Skodbjerge, Denmark
Aeolian Sediment Transport and Natural Dune Development, Skodbjerge, Denmark January 2020 Project Building with Nature (EU-InterReg) Start date 01.11.2016 End date 01.07.2020 Project manager (PM) Ane Høiberg Nielsen Project leader (PL) Per Sørensen Project staff (PS) Henrik Vinge Karlsson and Britt Gadsbølle Larsen Time registering 402412 Approved date 27.01.2020 Signature Report Aeolian sediment transport and natural dune development, Skodbjerge, Denmark. Author Henrik Vinge Karlsson and Britt Gadsbølle Larsen Keyword Aeolian sediment transport, Aeolian sedimentary budget, Skodbjerge, Dune development, Building with nature, Distribution www.kyst.dk, www.northsearegion.eu/building-with-nature/ Kystdirektoratet, BWN Krogen, 2018 Referred to as Kystdirektoratet (2020), Aeolian sediment transport and natural dune de- velopment, Skodbjerge, Denmark. Lemvig. 2 Aeolian Sediment Transport and Natural Dune Development, Skodbjerge, Denmark Abstract This study is part of the EU-InterReg project Building with Nature. The focus of this report is the natural development of a 3.7 km dune stretch at Skodbjerge located on the North Sea coast of Denmark. Since 2005, the designated study area has been subject to high-resolution digital elevation mappings (DEMs). The DEMs derive from LIDAR scans and serve as primary data resource throughout this report. Previous analyses of the coast assume that sediment accumulation inland of the dune top could be dis- regarded when analyzing the sedimentary budget of the coast, as the volumes in question were consi- dered insignificant. The analysis of this report suggests otherwise, as considerable amounts of sediment accumulated in the area leeward of the dune crest during the study period. Findings are based on the changes in elevation over time, obtained by analyzing the DEMs and thereby determining the sedimen- tary budget between dune face and dune leeside.