DOCSLIB.ORG

On the Trail of the Vikings

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
On the Trail of the Vikings ON THE TRAIL OF THE VIKINGS Follow the same Viking trail from Iceland to South Greenland made famous by Viking explorer Erik the Red 900 years ago. Discover Icelands exotic birdlife in Breidafjordur Bay, unspoiled nature and solitude in the Westfjords and fascinating volcanic archipelago of the Westman Islands. Our exploration of Greenland provides access to Viking Age sites, an inland ice cap, fertile coastal valleys with quaint sheep farms, deep blue fjords, and multi-coloured icebergs from calving glaciers. ITINERARY Day 1 Reykjavik Use your leisure time in Reykjavik to uncover the unique charm of the worlds northernmost capital or book one of our pre-programs for a unique Iceland experience. The Ocean Diamond docks in Old Reykjavik Harbor in the heart of the city, a five minute stroll to the main squares, shopping and dining. The ship departs Reykjavik harbor at 8 p.m. Day 2 Stykkisholmur We begin our exploration of Snaefellsnes Peninsula from the cheerful town of Stykkisholmur in West Iceland. The peninsula is dominated by Snaefellsnes National Park which represents nearly every type of nature seen in Iceland. With our on board Zodiacs you explore thousands of islets among Breidafjordur Bay (UNESCO) which are teeming with exotic birdlife, unique 01432 507 280 (within UK) [email protected] | small-cruise-ships.com basalt rock formations and marine wildlife. Adventurous spirits Day 6 Nanortalik and Qaqortoq may opt to join an expedition to Snaefellsjokull glacier which Early morning we reach Greenlands southernmost city of sits atop a 700,000 year old dormant volcano and served as Nanortalik which are framed by steep cliffs, deep blue fjords the mystical entrance to earths interior in Jules Vernes novel, and green coniferous forests. In the surrounding area you find Journey to the Centre of the Earth. various ruins from both Norse and Inuit settlers. While Norse settlers appreciated the fertile, green valleys, the Inuit preferred Day 3 Isafjordur seal hunting in the local waters. We continue our voyage to Todays destination is Isafjordur, honorary capital of the Qaqortoq, South Greenlands largest town. Located on an Westfjords. This secluded peninsula is connected to the iceberg filled bay surrounded by countless colourful houses, mainland by only a narrow strip of land and includes areas Qaqortoq is considered one of the most beautiful cities in where cars have never been. The landscape provides Greenland. Dont miss the outdoor art installation Stone and jaw-dropping views of dramatic fjords carved by ancient Man, which was conceptualized by local artist Aka Hegh and glaciers, sheer table mountains plunging into the sea and comprises granite sculptures and reliefs by 18 Nordic artists untouched vegetation. Enjoy the rarity of pure silence and the located throughout the city centre. tranquility of nature while sea-fishing or watching thousands of puffins on the tiny island of Vigur, or visiting the massive Day 7 Qassiarsuk/Narsarsuaq cascade of Dynjandi waterfall. Today we reach the small settlement of Qassiarsuk, founded by notorious Viking Erik the Red who named this area green land Day 4 Day at Sea/Denmark Strait because of the inviting green valleys around Qassiarsuk. During Today we sail across the Denmark Strait towards Greenland, our stop here you can learn about the lives of the islands early following the same maritime route used by Norse settlers more Norse settlers and visit a reconstructed Viking longhouse and than 900 years ago. Enroute you can attend fascinating small turf church. presentations by our Expedition Team members. Day 8 + Day 9 Day at Sea/ Denmark Strait Day 5 Day at Sea/Prins Christian Sound With Iceland set in our sights we cross the Denmark Strait again When conditions are favorable we travel along the 70 mile long heading east. Review the impressions of the last days or visit (112 km) Prins Christian Sound which connects the Labrador interesting lectures presented by our Expedition Team. Keep and Irminger Seas. In this narrow, often ice-choked channel, we your eyes open for whales, dolphins and seabirds! come so close to icebergs you can almost reach out and touch one. The force of Greenlands massive, inland ice cap pushes Day 10 Vestmannaeyjar (Westman Islands) glaciers towards the sea, where large hunks of ice break off and Located off the coast of South Iceland, the island group become floating icebergs. Vestmannaeyjar was formed by submarine volcanic eruptions 10,000 years ago. Surtsey Island emerged from the sea in 01432 507 280 (within UK) [email protected] | small-cruise-ships.com 1963 and is the youngest place on earth. We go ashore on Heimaey, the only inhabited island of the archipelago. Here the evidence of Icelands volcanic fury is on full display with half-buried houses in ash from a violent eruption in 1973 when the entire island had to be evacuated. Aboard Zodiacs we circumnavigate the island to take in the magical scenery and stop at places of interest to see the local bird life, visit caves and possibly spot whales. An epic experience here is to play a round of golf in a sunken volcanic crater. Day 11 Reykjavik In the morning we return to the port of Reykjavik. After breakfast its time to bid farewell to the Ocean Diamond. Extend your stay in Iceland and book one of our post-cruise programs or explore Reykjavik and the surrounding area on your own. This chic capital of friendly citizens is the perfect city for those who want to refresh the spirit and combine invigorating activity, good food, nature appreciation and worldclass cultural entertainment. Please Note: All routes and excursions are provisional and subject to change weather, sea and ice conditions may affect the itinerary. 01432 507 280 (within UK) [email protected] | small-cruise-ships.com YOUR SHIP: OCEAN DIAMOND PC YOUR SHIP: Ocean Diamond PC waste, the vessel is equipped with a Sewage Treatment system that processes the waste generated onboard. VESSEL TYPE: Expedition LENGTH: 124 metres PASSENGER CAPACITY: 224 BUILT/REFURBISHED: 1974 / 2012 Enjoy the breathtaking nature of Scotland, Iceland and Greenland aboard the Ocean Diamond. Thanks to two stabilizers that significantly reduce roll and an ice-strengthened hull (ice class 1D), the super yacht Ocean Diamond is the ideal ship for expeditions in the Arctic region. Due to the ship's compact size, The treated waste water is discharged at sea or shoreside. If we can take passengers to places off the traditional cruise discharged at sea it is done according to strict International routes to experience all the highlights of Scotland, Iceland and standards and Class required protocols that include distance Greenland. from shore, depth of the water, speed of the vessel and rate of With a maximum of 224 passengers, the Ocean Diamond discharge. features a range of modern onboard amenities and is staffed with outstanding officers and crew, as well as bilingual expedition leaders and guides. The 109 cabins and suites, all of them elegantly designed, offer modern amenities and exterior views. The ship's own Zodiacs are available for shore excursions. After a busy day of exploration, passengers can browse books or DVDs in the well-stocked Polar library or enjoy views of the spectacular Arctic scenery from the panorama salon. The vessel complies with all MARPOL (Marine Pollution Act)regulations. The vessel has a Garbage Management Plan to deal with garbage accumulated during a voyage. As for human 01432 507 280 (within UK) [email protected] | small-cruise-ships.com INSIDE YOUR SHIP 01432 507 280 (within UK) [email protected] | small-cruise-ships.com PRICING 01432 507 280 (within UK) [email protected] | small-cruise-ships.com.
Load more

Recommended publications
  • Archaeological Excavations at Qassiarsuk 2005 – 2006 Field Report (Data Structure Report)
    Archaeological Excavations at Qassiarsuk 2005 – 2006 Field report (Data Structure Report) Edited by Ragnar Edvardsson With contribution by Caroline Paulsen, Mike Church, Ian Simpson, Paul Adderly Albína Pálsdóttir and Thomas H. McGovern Náttúrustofa Vestfjarða NABO Grønlands Nationalmuseum & Arkiv Apríl 2007 NV.nr. 03-07 Náttúrustofa Vestfjarða Sími: 4567005 Kennitala: 610397-2209 Aðalstræti 21 Fax: 4567351 Netfang: [email protected] 415 Bolungarvík Heimasíða: http://nave.is 1. Introduction..................................................................................................................... 4 2. Aims and Methods .......................................................................................................... 4 3. Earlier Work at Ø29a...................................................................................................... 5 4. The Brattahlíð Excavations in 2005, KNK2629 (Ø29a)................................................. 6 4.1 Description of archaeological units .......................................................................... 7 4.2 Artifacts................................................................................................................... 11 4.3 C14 Analysis ............................................................................................................ 13 4.4 Conclusions of the 2005 excavation ....................................................................... 13 5. The Brattahlíð Excavation in 2006, KNK2629 (Ø29a) ...............................................
    [Show full text]
  • Kujalleq Nutaaq ERHVERVSUDVIKLINGS FORSLAG for Kommune Kujalleq
    Kujalleq Nutaaq ERHVERVSUDVIKLINGS FORSLAG for Kommune Kujalleq Version 1.0 - 2020 Innovation South Greenland A/S, Torvevej 34, Postboks 313, 3920 Qaqortoq, Greenland Oqarasuaat +299 537777, e-mail: [email protected] Forord Innovation South Greenland arbejder målrettet for at få udviklingen i gang i hele Sydgrønland. Dette dokument afspejler anbefalingerne til Kommunalbestyrelsen. 1. Ser man på infrastrukturen er det gennem en årrække blevet svært at rejse rundt i Kommunen. 2. Det er en udfordring at få vareforsyninger, dyrt og svært at sende varer fra sydgrønland og svært at holde møder osv. Af disse og flere andre årsager er udviklingen gået nærmest i stå. 3. Resultatet har været at der er sket en gradvis en fraflytning. Desuden har personer med højere kompetencer fået gode jobs andre steder. Det er ganske enkelt blevet svært at skabe et livsgrundlag på et personligt plan, for familier og for erhvervslivet. Derfor har man etableret Innovation South Greenland A/S for at skabe vækst, udvikling og rådgivning af iværksættere. En konkret opgave som er blevet givet Innovation South Greenland A/S er at finde en løsning for Narsarsuaq i et nyt scenarie. Det vigtige er imidlertid at se på hele Sydgrønland som en sammenhængende region. Den første forudsætning er at skabe håb og troværdighed. Dernæst at man får en tidssvarende infrastruktur på plads. Ydermere skal der opdyrkes en iværksætterkultur som understøttes af igangsætning af konkrete projekter. Sidst og ikke mindst skal der tiltrækkes investeringer udefra og indgås bilaterale aftaler som kan styrke regionen. Erhvervsudviklingen skal baseres på et tæt samarbejde med Erhvervslivet, Kommunen, Selvstyret og Uddannelsesinstitutionerne i kommunen.
    [Show full text]
  • Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
    - 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]].
    [Show full text]
  • Your Cruise Icelandic Nature and Traditions
    Icelandic nature and traditions From 8/11/2021 From Reykjavík Ship: LE DUMONT-D'URVILLE to 8/22/2021 to Reykjavík Discover the most beautiful landscapes on the Icelandic west coast during an 12-day PONANT cruise. On the edge of the Arctic, between vast glaciers, vertiginous fjords, volcanoes and boiling geysers, thiscircumnavigation will enable you to discover the wild and romantic landscapes of Iceland. Departing from Reykjavík, you will set off aboardLe Dumont-d’Urville, heading for Heimaey, the only inhabited island in the Westman archipelago. It is an exceptional place composed of volcanoes and almost- desert landscapes, where fishing is the main food source. You will then set sail for the bay ofGrundarfjörður , right near Kirkjufell. This stunning cone-shaped mountain possesses a unique charm and this will be an opportunity to take some beautiful photos. After visiting the villages ofÍsafjörður and Djúpavík, you will head for Siglurfjörður, to the north of Tröllaskagithe peninsula, whose mountainous silhouettes are reminiscent of French alpine reliefs. Founded in the 10th century, this small port reputed for herring fishing is also known for the beauty of its fjord. Le Dumont-d’Urville will sail for Grímsey, a small, hard-to-reach island where, in certain places, the volcanic rock forms magnificent basalt columns. Sea birds reign here. Akureyri, the capital of north Iceland, will welcome you on the shores of the Eyafjörður fjord, very close to the Arctic Circle. Your ship will then head south again toHornafjörður , in the Vatnajökull National Park, a UNESCO World Heritage Site. You will be dazzled by the beauty of the landscapes around the Jökulsarlon glacial lake.
    [Show full text]
  • Itinerary Route: Reykjavik, Iceland to Reykjavik, Iceland
    ICELAND AND GREENLAND: WILD COASTS AND ICY SHORES Itinerary route: Reykjavik, Iceland to Reykjavik, Iceland 13 Days Expeditions in: Aug Call us at 1.800.397.3348 or call your Travel Agent. In Australia, call 1300.361.012 • www.expeditions.com DAY 1: Reykjavik, Iceland / Embark padding Special Offers Arrive in Reykjavík, the world’s northernmost capital, which lies only a fraction below the Arctic Circle and receives just four hours of sunlight in FREE BAR TAB AND CREW winter and 22 in summer. Check in to our group TIPS INCLUDED hotel in the morning and take time to rest and We will cover your bar tab and all tips for refresh before lunch. In the afternoon, take a the crew on all National Geographic panoramic drive through the city’s Old Town Resolution, National Geographic before embarking National Explorer, National Geographic Geographic Endurance. (B,L,D) Endurance, and National Geographic Orion voyages. DAY 2: Flatey Island padding Explore Iceland’s western frontier by Zodiac cruise, visiting Flatey Island, a trading post for many centuries. In the afternoon, sail past the wild and scenic coast of Iceland’s Westfjords region. (B,L,D) DAY 3: Arnafjörður and Dynjandi Waterfall padding In the early morning our ship will glide into beautiful Arnafjörður along the northwest coast of Iceland. For a more active experience, disembark early and hike several miles along the base of the fjord to visit spectacular Dynjandi Waterfall. Alternatively, join our expedition staff on the bow of the ship as we venture ever deeper into the fjord and then go ashore by Zodiac to walk up to the base of the waterfall.
    [Show full text]
  • Marine Debris in the Coastal Environment of Iceland´S Nature Reserve, Hornstrandir - Sources, Consequences and Prevention Measures
    Master‘s thesis Marine Debris in the Coastal Environment of Iceland´s Nature Reserve, Hornstrandir - Sources, Consequences and Prevention Measures Anna-Theresa Kienitz Advisor: Hrönn Ólína Jörundsdóttir University of Akureyri Faculty of Business and Science University Centre of the Westfjords Master of Resource Management: Coastal and Marine Management Ísafjörður, May 2013 Supervisory Committee Advisor: Hrönn Ólína Jörundsdóttir Ph.D Matis Ltd. Food and Biotech Vinlandsteid 12, 143 Rekavík Reader: Dr. Helgi Jensson Ráðgjafi, Senior consultant Skrifstofa forstjóra, Human Resources Secretariat Program Director: Dagný Arnarsdóttir, MSc. Academic Director of Coastal and Marine Management Anna-Theresa Kienitz Marine Debris in the Coastal Environment of Iceland´s Nature Reserve, Hornstrandir - Sources, Consequences and Prevention Measures 45 ECTS thesis submitted in partial fulfilment of a Master of Resource Management degree in Coastal and Marine Management at the University Centre of the Westfjords, Suðurgata 12, 400 Ísafjörður, Iceland Degree accredited by the University of Akureyri, Faculty of Business and Science, Borgir, 600 Akureyri, Iceland Copyright © 2013 Anna-Theresa Kienitz All rights reserved Printing: Háskólaprent, May 2013 Declaration I hereby confirm that I am the sole author of this thesis and it is a product of my own academic research. ________________________ Theresa Kienitz Abstract Marine debris is a growing problem, which adversely affects ecosystems and economies world-wide. Studies based on a standardized approach to examine the quantity of marine debris are lacking at many locations, including Iceland. In the present study, 26 transects were established on six different bays in the north, west and south of the nature reserve Hornstrandir in Iceland, following the standardized approach developed by the OSPAR Commission.
    [Show full text]
  • The East Greenland Current North of Denmark Strait: Part I'
    The East Greenland Current North of Denmark Strait: Part I' K. AAGAARD AND L. K. COACHMAN2 ABSTRACT.Current measurements within the East Greenland Current during winter1965 showed that above thecontinental slope there were large on-shore components of flow, probably representing a westward Ekman transport. The speed did not decrease significantly with depth, indicatingthat the barotropic mode domi- nates the flow. Typical current speeds were10 to 15 cm. sec.-l. The transport of the current during winter exceeds 35 x 106 m.3 sec-1. This is an order of magnitude greater than previous estimates and, although there may be seasonal fluctuations in the transport, it suggests that the East Greenland Current primarily represents a circulation internal to the Greenland and Norwegian seas, rather than outflow from the central Polarbasin. RESUME. Lecourant du Groenland oriental au nord du dbtroit de Danemark. Aucours de l'hiver de 1965, des mesures effectukes danslecourant du Groenland oriental ont montr6 que sur le talus continental, la circulation comporte d'importantes composantes dirigkes vers le rivage, ce qui reprksente probablement un flux vers l'ouest selon le mouvement #Ekman. La vitesse ne diminue pas beau- coup avec laprofondeur, ce qui indique que le mode barotropique domine la circulation. Les vitesses typiques du courant sont de 10 B 15 cm/s-1. Au cows de l'hiver, le debit du courant dkpasse 35 x 106 m3/s-1. Cet ordre de grandeur dkpasse les anciennes estimations et, malgrC les fluctuations saisonnihres possibles, il semble que le courant du Groenland oriental correspond surtout B une circulation interne des mers du Groenland et de Norvhge, plut6t qu'8 un Bmissaire du bassin polaire central.
    [Show full text]
  • Representation of the Denmark Strait Overflow in a Z-Coordinate Eddying
    Geosci. Model Dev., 13, 3347–3371, 2020 https://doi.org/10.5194/gmd-13-3347-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Representation of the Denmark Strait overflow in a z-coordinate eddying configuration of the NEMO (v3.6) ocean model: resolution and parameter impacts Pedro Colombo1, Bernard Barnier1,4, Thierry Penduff1, Jérôme Chanut2, Julie Deshayes3, Jean-Marc Molines1, Julien Le Sommer1, Polina Verezemskaya4, Sergey Gulev4, and Anne-Marie Treguier5 1Institut des Géosciences de l’Environnement, CNRS-UGA, Grenoble, 38050, France 2Mercator Ocean International, Ramonville Saint-Agne, France 3Sorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, Paris, France 4P. P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia 5Laboratoire d’Océanographie Physique et Spatiale, Brest, France Correspondence: Pedro Colombo ([email protected]) Received: 23 September 2019 – Discussion started: 14 January 2020 Revised: 26 May 2020 – Accepted: 9 June 2020 – Published: 30 July 2020 Abstract. We investigate in this paper the sensitivity of the players contribute to the sinking of the overflow: the break- representation of the Denmark Strait overflow produced by a ing of the overflow into boluses of dense water which con- regional z-coordinate configuration of NEMO (version 3.6) tribute to spreading the overflow waters along the Greenland to the horizontal and vertical grid resolutions and to various shelf and within the Irminger Basin, and the resolved verti- numerical and physical parameters. Three different horizon- cal shear that results from the resolution of the bottom Ek- tal resolutions, 1=12, 1=36, and 1=60◦, are respectively used man boundary layer dynamics.
    [Show full text]
  • Lagrangian Perspective on the Origins of Denmark Strait Overflow
    AUGUST 2020 S A B E R I E T A L . 2393 Lagrangian Perspective on the Origins of Denmark Strait Overflow ATOUSA SABERI,THOMAS W. N. HAINE, AND RENSKE GELDERLOOS Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland M. FEMKE DE JONG Royal Netherlands Institute for Sea Research, and Utrecht University, Texel, Netherlands HEATHER FUREY AND AMY BOWER Woods Hole Oceanographic Institution, Woods Hole, Massachusetts (Manuscript received 1 September 2019, in final form 16 June 2020) ABSTRACT The Denmark Strait Overflow (DSO) is an important contributor to the lower limb of the Atlantic me- ridional overturning circulation (AMOC). Determining DSO formation and its pathways is not only im- portant for local oceanography but also critical to estimating the state and variability of the AMOC. Despite prior attempts to understand the DSO sources, its upstream pathways and circulation remain uncertain due to short-term (3–5 days) variability. This makes it challenging to study the DSO from observations. Given this complexity, this study maps the upstream pathways and along-pathway changes in its water properties, using Lagrangian backtracking of the DSO sources in a realistic numerical ocean simulation. The Lagrangian pathways confirm that several branches contribute to the DSO from the north such as the East Greenland Current (EGC), the separated EGC (sEGC), and the North Icelandic Jet (NIJ). Moreover, the model results reveal additional pathways from south of Iceland, which supplied over 16% of the DSO annually and over 25% of the DSO during winter of 2008, when the NAO index was positive. The southern contribution is about 34% by the end of March.
    [Show full text]
  • Boreal Marine Fauna from the Barents Sea Disperse to Arctic Northeast Greenland
    bioRxiv preprint doi: https://doi.org/10.1101/394346; this version posted December 16, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Boreal marine fauna from the Barents Sea disperse to Arctic Northeast Greenland Adam J. Andrews1,2*, Jørgen S. Christiansen2, Shripathi Bhat1, Arve Lynghammar1, Jon-Ivar Westgaard3, Christophe Pampoulie4, Kim Præbel1* 1The Norwegian College of Fishery Science, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Norway 2Department of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Norway 3Institute of Marine Research, Tromsø, Norway 4Marine and Freshwater Research Institute, Reykjavik, Iceland *Authors to whom correspondence should be addressed, e-mail: [email protected], kim.præ[email protected] Keywords: Atlantic cod, Barents Sea, population genetics, dispersal routes. As a result of ocean warming, the species composition of the Arctic seas has begun to shift in a boreal direction. One ecosystem prone to fauna shifts is the Northeast Greenland shelf. The dispersal route taken by boreal fauna to this area is, however, not known. This knowledge is essential to predict to what extent boreal biota will colonise Arctic habitats. Using population genetics, we show that Atlantic cod (Gadus morhua), beaked redfish (Sebastes mentella), and deep-sea shrimp (Pandalus borealis) specimens recently found on the Northeast Greenland shelf originate from the Barents Sea, and suggest that pelagic offspring were dispersed via advection across the Fram Strait. Our results indicate that boreal invasions of Arctic habitats can be driven by advection, and that the fauna of the Barents Sea can project into adjacent habitats with the potential to colonise putatively isolated Arctic ecosystems such as Northeast Greenland.
    [Show full text]
  • Marla J. Koberstein
    Master‘s thesis Expansion of the brown shrimp Crangon crangon L. onto juvenile plaice Pleuronectes platessa L. nursery habitat in the Westfjords of Iceland Marla J. Koberstein Advisor: Jόnas Páll Jόnasson University of Akureyri Faculty of Business and Science University Centre of the Westfjords Master of Resource Management: Coastal and Marine Management Ísafjörður, February 2013 Supervisory Committee Advisor: Name, title Reader: Name, title Program Director: Dagný Arnarsdóttir, MSc. Marla Koberstein Expansion of the brown shrimp Crangon crangon L. onto juvenile plaice Pleuronectes platessa L. nursery habitat in the Westfjords of Iceland 45 ECTS thesis submitted in partial fulfillment of a Master of Resource Management degree in Coastal and Marine Management at the University Centre of the Westfjords, Suðurgata 12, 400 Ísafjörður, Iceland Degree accredited by the University of Akureyri, Faculty of Business and Science, Borgir, 600 Akureyri, Iceland Copyright © 2013 Marla Koberstein All rights reserved Printing: Háskólaprent, Reykjavik, February 2013 Declaration I hereby confirm that I am the sole author of this thesis and it is a product of my own academic research. __________________________________________ Student‘s name Abstract Sandy-bottom coastal ecosystems provide integral nursery habitat for juvenile fishes, and threats to these regions compromise populations at this critical life stage. The threat of aquatic invasive species in particular can be difficult to detect, and climate change may facilitate the spread and establishment of new species. In 2003, the European brown shrimp Crangon crangon L. was discovered off the southwest coast of Iceland. This species is a concern for Iceland due to the combination of its dominance in coastal communities and level of predation on juvenile flatfish, namely plaice Pleuronectes platessa L., observed in its native range.
    [Show full text]
  • Report on the Availability of Whale Meat in Greenland
    1 Greenland survey: 77% of restaurants served whale meat in 2011/2012 Greenland claims that its current Aboriginal Subsistence Whaling (ASW) quota of 175 minke whales, 16 fin whales, nine humpback whales and two bowhead whales a year is insufficient to meet the nutritional needs of Greenlanders (people born in Greenland). It claims in its 2012 Needs Statement that West Greenland alone now requires 730 tonnes of whale meat annually. Greenland has around 50 registered restaurants used by tourists, including several in hotels, plus another 25 smaller "cafeterias, hot dog stands, grill bars, ice cream shops, etc.” which are licensed separately.1 WDCS, the Whale and Dolphin Conservation Society, visited Greenland in May 2011 to assess the availability of whale meat in registered restaurants. In September 2011, WDCS and the Animal Welfare Institute (AWI) visited again. In June 2012, AWI conducted (i) a telephone and email survey of all restaurants (31) for which contact information (phone/email) was available and (ii) extensive internet research in multiple languages of web entries referencing whale meat in Greenland’s restaurants in 2011/2012. Whale meat, including fin, bowhead and minke whale, was available to tourists at 24 out of 31 (77.4%) restaurants visited, contacted, and/or researched online in Greenland in 2011/2012. In addition, one other restaurant for which there was no online record of it serving whale meat indicated, when contacted, that though it did not currently have whale meat on the menu it could be provided if requested in advance for a large enough group. Others that did not have whale meat said that they could provide an introduction to a local family that would.
    [Show full text]