Understanding Sediment Bypassing Processes Through Analysis of High- Frequency Observations of Ameland Inlet, the Netherlands T ⁎ Edwin P.L
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Annual Report Fishing for Litter 2011
Annual Report Fishing for Litter 2011 Fishing For Litter Annual Report Fishing for Litter project 2011 Edited by KIMO Nederland en België March 2012 Bert Veerman Visual design: Baasimmedia Annual Report Fishing for Litter project 2011 Index: Pag: Message from the Chairman ................................................................................................. 5 1.0 Introduction .............................................................................................................. 7 2.0 Project description ................................................................................................... 8 3.0 Goals of the project .................................................................................................. 9 4.0 Monitors ................................................................................................................ 10 4.1 Waste from the beaches of Ameland ......................................................... 10 4.2 Waste through the ports ............................................................................ 10 5.0 Consultation structure ............................................................................... 11 6.0 Administration ........................................................................................... 11 7.0 Publicity .................................................................................................... 11 7.1 Documentary “Fishing for Litter” ................................................................ 11 8.0 A summary of activities -
PLASTIC MANAGEMENT and DEVELOPMENT on ISLANDS Research Project
\ Source: Frerck, n.d. PLASTIC MANAGEMENT AND DEVELOPMENT ON ISLANDS Research Project Nelle Kloosterboer IVM Supervisors: dr. P.J.H. van Beukering & H. Dijkstra Abstract The plastic soup is caused by large consumption and improper waste management of plastics worldwide. A global change in plastic management is needed to counter further growth of this problem. Many studies have been done on improving plastic management in large countries and regions, but islands have often been overlooked. Additionally, plastic pollution often ends up on the shorelines of islands, making sustainable plastic management a necessity on islands. This study investigates plastic management measures that contribute most effectively to sustainable plastic management and development on Texel and Sint Maarten. Firstly, the West Frisian Islands and the Dutch Caribbean Islands are analysed according to the island characteristics that influence the local plastic management system. Secondly, Material Flow Analyses of plastics are conducted for the West Frisian Islands and the Dutch Caribbean Islands to get an overview of the plastic product, waste, and pollution flows and discover specific trends surrounding plastics on the islands. Thirdly, Scenario Analyses are presented for the two case studies Texel and Sint Maarten, which show potential pathways towards sustainable plastic management on these islands. The results show that reducing plastic consumption is a slightly more effective strategy to improve sustainable plastic management and development than managing plastic waste and pollution. Furthermore, the methods utilized in this study have shown to be innovative and effective in improving plastic management systems on islands. Still, additional research is needed on macro- and microplastic flows, measures, and their impacts on islands worldwide to significantly contribute in reducing the plastic soup. -
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 °... -
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 . -
Wadden Sea Quality Status Report Geomorphology
Photo: Rijkswaterstaat, NL (https://beeldbank.rws.nl). Zuiderduin 2011. Wadden Sea Quality Status Report Geomorphology A. P. Oost, C. Winter, P. Vos, F. Bungenstock, R. Schrijvershof, B. Röbke, J. Bartholdy, J. Hofstede, A. Wurpts, A. Wehrmann This report downloaded: 2018-11-23. This report last updated: 2017-12-21. This report should be cited as: Oost A. P., Winter C., Vos P., Bungenstock F., Schrijvershof R., Röbke B., Bartholdy J., Hofstede J., Wurpts A. & Wehrmann A. (2017) Geomorphology. In: Wadden Sea Quality Status Report 2017. Eds.: Kloepper S. et al., Common Wadden Sea Secretariat, Wilhelmshaven, Germany. Last updated 21.12.2017. Downloaded DD.MM.YYYY. qsr.waddensea-worldheritage.org/reports/geomorphology 1. Introduction The hydro- and morphodynamic processes of the Wadden Sea form the foundation for the ecological, cultural and economic development of the area. Its extraordinary ecosystems, its physical and geographical values and being an outstanding example of representing major stages of the earth’s history are factors why the Wadden Sea received a World Heritage area qualification (UNESCO, 2016). During its existence, the Wadden Sea has been a dynamic tidal system in which the geomorphology of the landscape continuously changed. Driving factors of the morphological changes have been: Holocene sea-level rise, geometry of the Pleistocene surface, development of accommodation space for sedimentation, sediment transport mechanisms (tides and wind) and, the relatively recent, strong human interference in the landscape. In this report new insights into the morphology of the trilateral Wadden Sea gained since the Quality Status Report (QSR) in 2009 (Wiersma et al., 2009) are discussed. After a summary of the Holocene development (sub-section 2.1), the sand-sharing inlet system approach as a building block for understanding the morhodynamic functioning of the system with a special emphasis on the backbarrier (sub-section 2.2) is discussed, followed by other parts of the inlet-system. -
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. -
Putting Frisian Names on the Map
GEGN.2/2021/68/CRP.68 15 March 2021 English United Nations Group of Experts on Geographical Names Second session New York, 3 – 7 May 2021 Item 12 of the provisional agenda * Geographical names as culture, heritage and identity, including indigenous, minority and regional languages and multilingual issues Putting Frisian names on the map Submitted by the Netherlands** * GEGN.2/2021/1 ** Prepared by Jasper Hogerwerf, Kadaster GEGN.2/2021/68/CRP.68 Introduction Dutch is the national language of the Netherlands. It has official status throughout the Kingdom of the Netherlands. In addition, there are several other recognized languages. Papiamentu (or Papiamento) and English are formally used in the Caribbean parts of the Kingdom, while Low-Saxon and Limburgish are recognized as non-standardized regional languages, and Yiddish and Sinte Romani as non-territorial minority languages in the European part of the Kingdom. The Dutch Sign Language is formally recognized as well. The largest minority language is (West) Frisian or Frysk, an official language in the province of Friesland (Fryslân). Frisian is a West Germanic language closely related to the Saterland Frisian and North Frisian languages spoken in Germany. The Frisian languages as a group are closer related to English than to Dutch or German. Frisian is spoken as a mother tongue by about 55% of the population in the province of Friesland, which translates to some 350,000 native speakers. In many rural areas a large majority speaks Frisian, while most cities have a Dutch-speaking majority. A standardized Frisian orthography was established in 1879 and reformed in 1945, 1980 and 2015. -
Tourism Development in the Dutch Wadden Area: Spatial-Temporal Characteristics and Monitoring Needs
Environmental Management and Sustainable Development ISSN 2164-7682 2015, Vol. 4, No. 2 Tourism Development in the Dutch Wadden Area: Spatial-Temporal Characteristics and Monitoring Needs Frans J. Sijtsma (Corresponding author) University of Groningen, P.O. Box 800, 9700 AV, Groningen, The Netherlands E-mail: [email protected] Lourens Broersma University of Groningen, P.O. Box 800, 9700 AV, Groningen, The Netherlands E-mail: [email protected] Michiel N. Daams University of Groningen, P.O. Box 800, 9700 AV, Groningen, The Netherlands E-mail: [email protected] Hendrik Hoekstra University of Groningen, P.O. Box 800, 9700 AV, Groningen, The Netherlands Gelijn Werner Raad voor de Wadden, Leeuwarden, The Netherlands Received: March 11, 2015 Accepted: March 25, 2015 doi:10.5296/emsd.v4i2.8561 URL: http://dx.doi.org/10.5296/emsd.v4i2.8561 Abstract The paper presents a spatial and temporal analysis of tourism in the Dutch Wadden area and identifies policy dilemmas and monitoring needs. The analysis is temporal because historical, current and future aspects of tourism development are addressed; it is spatial because the spatial differentiaton of tourism within the Wadden area is examined. For the assessment of the historical and current situation focus is on visitor and employment data and especially the 217 www.macrothink.org/emsd Environmental Management and Sustainable Development ISSN 2164-7682 2015, Vol. 4, No. 2 relative degree of specialization of the local economy on tourism. For the future direction of tourism and possible investment options, the paper draws on surveyed views of 91 tourism entrepreneurs in the Wadden area. -
Routes Over De Waddenzee
5a 2020 Routes over de Waddenzee 7 5 6 8 DELFZIJL 4 G RONINGEN 3 LEEUWARDEN WINSCHOTEN 2 DRACHTEN SNEEK A SSEN 1 DEN HELDER E MMEN Inhoud Inleiding 3 Aanvullende informatie 4 5 1 Den Oever – Oudeschild – Den Helder 9 5 2 Kornwerderzand – Harlingen 13 5 3 Harlingen – Noordzee 15 5 4 Vlieland – Terschelling 17 5 5 Ameland 19 5 6 Lauwersoog – Noordzee 21 5 7 Lauwersoog – Schiermonnikoog – Eems 23 5 8 Delfzijl 25 Colofon 26 Het auteursrecht op het materiaal van ‘Varen doe je Samen!’ ligt bij de Convenantpartners die bij dit project betrokken zijn. Overname van illustraties en/of teksten is uitsluitend toegestaan na schriftelijke toestemming van de Stichting Waterrecreatie Nederland, www waterrecreatienederland nl 2 Voorwoord Het bevorderen van de veiligheid voor beroeps- en recreatievaart op dezelfde vaarweg. Dat is kortweg het doel van het project ‘Varen doe je Samen!’. In het kader van dit project zijn ‘knooppunten’ op vaarwegen beschreven. Plaatsen waar beroepsvaart en recreatievaart elkaar ontmoeten en waar een gevaarlijke situatie kan ontstaan. Per regio krijgt u aanbevelingen hoe u deze drukke punten op het vaarwater vlot en veilig kunt passeren. De weergegeven kaarten zijn niet geschikt voor navigatiedoeleinden. Dat klinkt wat tegenstrijdig voor aanbevolen routes, maar hiermee is bedoeld dat de kaarten een aanvulling zijn op de officiële waterkaarten. Gebruik aan boord altijd de meest recente kaarten uit de 1800-serie en de ANWB-Wateralmanak. Neem in dit vaargebied ook de getijtafels en stroomatlassen (HP 33 Waterstanden en stromen) van de Dienst der Hydrografie mee. Op getijdenwater is de meest actuele informatie onmisbaar voor veilige navigatie. -
“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 -
On the Beach Nature Explained
BOOK REVIEWS land disappeared under water, including viewing it as an indifferently designed work On the beach the legendary Rungholt, east of the of other purpose. The author's skills lie in present island of Pellworm. A second Donald J.P. Swift the collecting and ordering of information. Mandrdnke occurred on 11 October, Chapters that attempt to take an overview, 1694. But the main and partially enduring such as those on natural preconditions and The Morphodynamlcs of the Wadden land losses, resulting in the formation of barrier-island development, are not Sea. By Jurgen Ehlers. A.A. Balkema: Jade Bay, the Dollart and the Zuider Zee, altogether successful, although they are 1988. Pp.397. DM 185, £52. 75. did not occur as the result of single events, always interesting. On the other hand, the but gradually, through many smaller relentless procession of maps, aerial THE Wadden Sea is the intertidal zone of stages. These land losses were due to a photographs and, above all, photograph the German Bight of the North Sea. lack of technical infrastructure capable of after photograph at ground level, has a Varying in width from 10 to 50 km, it is an protecting the vast forelands from the hypnotic effect. Somewhere through the expanse of tidal channels, flats, inlets, destructive effects of later surges in later 393 figures, these vistas of misty dunes, flood and ebb deltas, barrier islands and decades. Land reclamation occurred, but beaches and marshes, and of tidal flats estuaries that extends from Den Helder only through projects that lasted for extending to the horizon, seep into the in the Netherlands to Blavandshuk in centuries. -
Het Recreatielandschap Van Ameland
Het recreatielandschap van Ameland Een interdisciplinair onderzoek naar de historische ontwikkeling van de relatie tussen de recreatie en het landschap op Ameland tussen 1855 en 1980 Robin Weiland Voorblad: Duinoord 1929. Familie Postma:Jacob Postma en Hiske Westhof met hun kinderen Metty, Klaas, Jelly, Jan en Grietje (en nog meer families). Foto is van Jaap Postma, zoon van Jan. Het Postmapad is naar hen vernoemd. 1e overgang vanaf de Strandweg. (Amelander historie) Opgeweld uit wier en zand gans omspoeld door zilte baren Moge God het steeds bewaren ons plekje, rijk aan duin en strand het ons zo lieve Ameland! 2 Kollum, april 2019. Auteur: Robin Weiland Masterscriptie Landschapsgeschiedenis Rijksuniversiteit Groningen Scriptiebegeleider: prof. dr. ir. Th. (Theo) Spek (Rijksuniversiteit Groningen) Tweede lezer: drs. Anne Wolff (Rijksuniversiteit Groningen) Het recreatielandschap van Ameland Een interdisciplinair onderzoek naar de historische ontwikkeling van de relatie tussen de recreatie en het landschap op Ameland tussen 1852 en 1980 3 Samenvatting Recreatie is een betrekkelijk nieuw verschijnsel, dat echter zijn stempel stevig op het landschap heeft gedrukt. Dit onderzoek richt zich op de recreatie aan zee, specifiek op het eiland Ameland. Hoe is de recreatie hier ontstaan, hoe reguleerde de lokale, regionale en nationale overheden de toeristenstroom en hoe pasten de Amelanders de recreatie in in de beperkte ruimte die het eiland verschaft? In het eerste deel staat het landschap van Ameland centraal. Hoe is Ameland ontstaan en met welke omstandigheden hebben de eilanders te doen gehad? Ook wordt er uiteengezet welke bodemtypen Ameland bevat en hoe een standaardeiland is opgebouwd. Dit verklaart de ligging van de dorpen en schijnt een licht op waar de ruimtelijke kansen voor recreatie lagen.