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Iceland Can Be Considered Volcanologist “Heaven”
Iceland can be considered volcanologist “heaven” 1) Sub-aerial continuation of the Mid-Atlantic Ridge 2) Intersection of a mantle plume with a spreading ocean ridge 3) Volcanism associated with tectonic rifting 4) Sub-glacial volcanism 5) Tertiary flood (plateau) basalts 6) Bi-modal volcanism 7) Submarine volcanism 8) 18 historically active volcanoes 9) Eruptions roughly every 5 years 1. The North Atlantic opened about 54 Ma separating Greenland from Europe. 2. Spreading was initially along the now extinct Agir ridge (AER). 3. The Icelandic plume was under Greenland at that time. 4. The Greenland – Faeroe ridge represents the plume track during the history of the NE Atlantic. Kolbeinsey ridge (KR) 5. During the last 20 Ma the Reykjanes Ridge (RR) Icelandic rift zones have migrated eastward, stepwise, maintaining their position near the plume 6. The plume center is thought to be beneath Vatnajökull 1 North Rift Zone – currently active East Rift Zone – currently active West Rift Zone – last erupted about 1000-1300 AD [Also eastern (Oræfajökull) and western (Snæfellsnese) flank zones] Rift zones comprise en-echelon basaltic fissure swarms 5-15 km wide and up to 200 km long. Over time these fissures swarms develop a volcanic center, eventually maturing into a central volcano with a caldera and silicic Tertiary volcanics > 3.1 Ma volcanism Late Tertiary to Early Quaternary 3.1 – 0.7 Ma Neo-volcanic zone <0.7 - present Schematic representation of Iceland’s mantle plume. The crust is about 35 – 40 km thick Iceland’s mantle plume has been tomographically imaged down to 400 km. Some claim even deeper, through the transition zone, and down to the core – mantle boundary. -
Baula Esjan Hekla Katla Askja
GEFÐU STARFSFÓLKINU DAGAMUN Þótt árshátíðir og ýmis annar gleðskapur hafi fallið niður hjá fyrirtækjum og stofnunum er auðvelt að gefa starfsfólkinu glaðning og gera því glaðan dag. Við útbúum óskaskrín sérmerkt þínu fyrirtæki og með kveðju til starfsfólksins. Hafðu samband í síma 577 5600 eða [email protected]. Suðurlandsbraut 30 | 577 5600 | [email protected] | oskaskrin.is Askja VERÐ 5.900 KR. Handhafi Óskaskrínsins velur eina af eftirfarandi upplifunum DEKUR VEITINGAHÚS AFÞREYING SNYRTISTOFAN VERÐI ÞINN VILJI FJÖLSKYLDU- OG HÚSDÝRAGARÐURINN HEILSA OG ÚTLIT WHALES OF ICELAND HREYFING PODCASTSTÖÐIN BEAUTY LOUNGE BY SHE SÓLIR JÓGASTÚDÍÓ SNYRTISTOFA ÁGÚSTU - Vestmannaeyjar SKAUTAHÖLL AKUREYRAR HIÐ NÝJA LÍF - Akureyri BIKE CAVE BREWDOG REYKJAVÍK GRILLHÚSIÐ HAMBORGARAFABRIKKAN KEF RESTAURANT - Keflavík KRISP - Selfoss HVER RESTAURANT - Hveragerði HAMBORGARAFABRIKKAN - Akureyri Baula VERÐ 8.900 KR. Handhafi Óskaskrínsins velur eina af eftirfarandi upplifunum DEKUR VEITINGAHÚS ÚTIVIST OG AFÞREYING VON MATHÚS SÓLIR JÓGA HEIM Í STOFU KRYDD DIVE.IS NAUTHÓLL HELLA HORSE RENTAL - Hella THE COOCOO’S NEST LANGHÚS HORSE TOURS - Fljótum HREYFING BREWDOG 1238 BARÁTTAN UM ÍSLAND - Sauðárkróki HELENA FAGRA HVER - Hveragerði ICEBERG BOAT TOURS - Öræfi SNYRTISTOFAN DIMMALIMM KRISP - Selfoss SNYRTISTOFAN FEGURÐ STRIKIÐ - Akureyri GISTING FYRIR TVO TRIMFORM GEISLINN STRANDAGALDUR - Hólmavík GRÍMUR HÓTEL - Höfuðborgarsvæðið HEILSA OG ÚTLIT HÓTEL BLANDA - Blönduós BEAUTY LOUNGE BY SHE SNYRTIMIÐSTÖÐIN VERÐI ÞINN VILJI - SNYRTISTOFA SNYRTISTOFA ÁGÚSTU - VESTMANNAEYJAR -
Signature of Deep Mantle Melting in South Iceland Olivine
Contributions to Mineralogy and Petrology (2019) 174:43 https://doi.org/10.1007/s00410-019-1580-8 ORIGINAL PAPER Signature of deep mantle melting in South Iceland olivine Paavo Nikkola1,2 · Guðmundur H. Guðfnnsson2 · Enikő Bali2,3 · O. Tapani Rämö1 · Tobias Fusswinkel4 · Thorvaldur Thordarson2,3 Received: 1 December 2018 / Accepted: 26 April 2019 / Published online: 13 May 2019 © The Author(s) 2019 Abstract We present new high-precision major and trace element data on olivine macrocrysts from various volcano-tectonic settings in Iceland and use these data as a proxy for mantle mode and melting conditions. Within individual sampling sites examined (seven lavas and one tephra) olivine-dominated fractional crystallization, magma mixing and difusive re-equilibration control observed variability in olivine composition. High-pressure fractional crystallization of clinopyroxene may have lowered Ca and increased Fe/Mn in one olivine population and subsolidus difusion of Ni and Fe–Mg afected the mantle-derived Ni/Fo ratio in some compositionally zoned olivine macrocrysts. Interestingly, magmas erupted at the southern tip of the Eastern Volcanic Zone (SEVZ), South Iceland, have olivines with elevated Ni and low Mn and Ca contents compared to olivines from elsewhere in Iceland, and some of the SEVZ olivines have relatively low Sc and V and high Cr, Ti, Zn, Cu and Li in comparison to depleted Iceland rift tholeiite. In these olivines, the high Ni and low Mn indicate relatively deep melting (Pfnal > 1.4 GPa, ~ 45 km), Sc, Ti and V are compatible with low-degree melts of lherzolite mantle, and elevated Zn may suggest modal (low-olivine) or geochemical (high Zn) enrichment in the source. -
Table of Contents
Table of Contents Introduction 3 Index of Pictures 4 Places (cont.) Index of Battle Maps 4 Þjóðveldisbærinn Stöng 19 Places 5 Þingvellir 20 Region Maps of Iceland 5 Þórufoss 20 Akureyri 6 Vatnsfjörður 21 Askja 7 Vestmannaeyjar 21 Grjótagjá 7 Hekla 8 Helgafell 9 Höfn 9 Hofsjökull, Langjökull, and Vatnajökull 10 Húsavík 12 Kirkjufell 12 Reyðarfjall 13 Reykjavík 14 Reynisdrangar 14 Skálaholt 17 Skógafoss 17 Snæfellsjökull 18 Stokknes 19 Sample file 2 Introduction For those who are interested in other Viking-themed modules, I highly You may be asking yourself, “What recommend Iskloft and Journey to exactly am I supposed to do with this Ragnarök, both of which are available on Atlas?” DM Guild. They are very different from each other, but they are both clearly labors For starters, this Atlas is intended to be of love by their respective authors, and used in any D&D or Pathfinder game with a worth every cent to purchase. Finally, Norse/Viking theme, or any scenario taking Roll20.net and the Dungeon Painter Studio place in cold, northern regions. program (which is available on Steam) both have many resources for making maps in This Atlas seeks to breathe life into a game snowy areas. by providing photographs of real places in Iceland (known as “Garðarshólmi” during the Viking Age). Thus, for example, if the party is travelling across a great glacier, creeping through a frozen ice cave, or resting by a beautiful waterfall, don’t just tell them about it – show them! The Atlas also includes several versions of a map of Iceland that can be used to display the region overall, and each location’s place on the map. -
ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006
ICELAND 2006 Geodynamics Field Trip May 30 – June 8, 2006 Massachusetts Institute of Technology/ Woods Hole Oceanographic Institution Joint Program in Oceanography This field trip guide was compiled by Karen L. Bice using information from Bryndís Brandsdóttir, Richard S. Williams, Helgi Torfason, Helgi Bjornsson, Oddur Sigurðsson, the Iceland Tourist Board and World W. Web Maps from Thordarson and Hoskuldsson, 2002, Iceland (Classic Geology in Europe 3), Terra Publishing, UK. Logistical genius: Andrew T. Daly Field trip participants: Mark Behn, Karen Bice, Roger Buck, Andrew Daly, Henry Dick, Hans Schouten, Martha Buckley, James Elsenbeck, Pilar Estrada, Fern Gibbons, Trish Gregg, Sharon Hoffmann, Matt Jackson, Michael Krawczynski, Christopher Linder, Johan Lissenberg, Andrea Llenos, Rowena Lohman, Luc Mehl, Christian Miller, Ran Qin, Emily Roland, Casey Saenger, Rachel Stanley, Peter Sugimura, and Christopher Waters The Geodynamics Program is co-sponsored by Woods Hole Oceanographic Institution’s Academic Programs Office and Deep Ocean Exploration Institute. TUESDAY May 30 Estimated driving (km) Meet at Logan Airport, Icelandair ticket counter @ 7:00 PM (80 km ≈ 50 mi) Depart BOS 9:30 PM Icelandair flight Day 1 - WEDNESDAY May 31 Arrive Keflavík International Airport 6:30 AM (flight duration 5 hours) Pick up 2 vans, 2 trailers (Budget) Free day in Reykjavík Night @ Laugardalur campground, Reykjavík Dinner: on own in town Day 2 - THURSDAY June 1 270 Late start due to trailer problems (2 hrs @ AVIS) To Þingvellir N.P., then north to Hvalfjörður fjord, stop at Skorradalsvatn Night @ Sæberg Hostel (1 km. off Rte 1 in Hrútafjörður, west side of road) Tel. 354-4510015 Fax. 354-4510034 [email protected] Dinner: mexican-style chicken (Rachel, Trish, Chris) Day 3 - FRIDAY June 2 320 To Lake Myvatn Lunch stop in Akureyri, stop at Godafoss, stop at Skutustadir pseudocraters Night @ Ferdathjonustan Bjarg campsite, Reykjahlid, on shore of Lake Myvatn Tel. -
The Eruption on Heimaey, Vestmannaeyjar, Iceland
Man Against Volcano: The Eruption on Heimaey, Vestmannaeyjar, Iceland This booklet was originally published in 1976 under the title "Man Against Volcano: The Eruption on Heimaey, Vestmann Islands, Iceland." The revised second edition was published in 1983. This PDF file is a recreation of the 1983 booklet. Cover photograph: View looking southeast along streets covered by tephra (volcanic ash) in Vestmannaeyjar: Eldfell volcano (in background) is erupting and fountaining lava. View of Heimaey before the eruption: Town of Vestmannaeyjar with Helgafell in the right back- ground (photo courtesy of Sólarfilma). Man Against Volcano: The Eruption on Heimaey, Vestmannaeyjar, Iceland by Richard S. Williams, Jr., and James G. Moore Preface The U.S. Geological Survey carries out scientific studies in the geological, hydrological, and cartographic sciences generally within the 50 States and its territories or trusteeships, but also in cooperation with scientific organizations in many foreign countries for the investigation of unusual earth sciences phenome- na throughout the world. In 1983, the U.S. Geological Survey had 57 active sci- entific exchange agreements with 24 foreign countries, and 47 scientific exchange agreements were pending with 30 foreign countries. The following material discusses the impact of the 1973 volcanic eruption of Eldfell on the fishing port of Vestmannaeyjar on the island of Heimaey, Vestmannaeyjar, Iceland. Before the eruption was over, approximately one-third of the town of Vestmannaeyjar had been obliterated, but, more importantly, the potential damage probably was reduced by the spraying of seawater onto the advancing lava flows, causing them to be slowed, stopped, or diverted from the undamaged portion of the town. -
Pálsson, Grétar Már. 2015
Impact on households and critical infrastructures from electricity failure Two case studies and a survey on public preparedness Grétar Már Pálsson Faculty of Civil and Environmental Engineering University of Iceland 2015 Impact on households and critical infrastructures from electricity failure Two case studies and a survey on public preparedness Grétar Már Pálsson 30 ECTS thesis submitted in partial fulfillment of a Magister Scientiarum degree in Civil Engineering Advisors Dr. Björn Karlsson Böðvar Tómasson Faculty Representative Sveinn Júlíus Björnsson Faculty of Civil and Environmental Engineering School of Engineering and Natural Sciences University of Iceland Reykjavik, May 2015 Impact on households and critical infrastructures - Two case studies and a survey on public preparedness. 30 ECTS thesis submitted in partial fulfillment of a Magister Scientiarum degree in civil engineering Copyright © 2015 Grétar Már Pálsson All rights reserved Faculty of Civil and Environmental Engineering School of Engineering and Natural Sciences University of Iceland VR II, Hjarðarhaga 2-6 107, Reykjavik Iceland Telephone: 525 4600 Bibliographic information: Grétar Már Pálsson, 2015, Impact on households and critical infrastructures - Two case studies and a survey on public preparedness, Master’s thesis, Faculty of Civil and Environmental Engineering, University of Iceland, pp. 76. Printing: Háskólaprent, Fálkagata 2, 107 Reykjavík Reykjavik, Iceland, May 2015 Abstract This thesis studies the impact from electricity failure in Iceland on households and critical infrastructures. Households and critical infrastructures electricity dependence is discussed along with a theoretical identification of impacts towards these two subjects from electricity failure. Risk Assessment Plans for Iceland, Norway and Sweden are compared. The main focus of the comparison relates to how the countries focus on electricity, information and communication technologies and the role of the general public in these plans. -
Iceland Sample Pages
Day 2 Get the full itinerary on Simply Awesome Trip’s website or find it on Amazon. Overview- Today you’ll take the ferry to explore the volcanic history and stunning sights of Vestmannaeyjar, also known as the Westman Islands. One-third of Heimaey, the only inhabited island of Vestmannaeyjar, was buried under lava during a volcanic eruption in 1973. You can now walk along the lava field and climb to the top of the newly created volcanic cone, Eldfell, for amazing views. It’s not every day that you get to walk to the top of an active volcano! Approximate location of sites on Heimaey Island. Map courtesy of openstreetmaps.org. Heimaey is a compact village (only five square miles and four miles long) and most sites are within an easy 5-20 minute walking radius from the ferry with the exception of Stórhöfði (the Great Cape) which is located at the southern end of the island about 7km south of the ferry port. Copyright © 2019 Simply Awesome Trips. All Rights Reserved. You’ll find incredibly scenic hikes, a wonderful local museum, puffin watching, a tasty bakery, and an excellent brewery. This day will easily be one of the most memorable days of your trip. You could even consider staying overnight on this small charming island. There’s plenty more to do here. The small village on Heimaey Island The Ferry The ferry departs from the southern coast of Iceland at Landeyjahöfn, which is located approximately 25 minutes south of Hvolsvöllur. The ferry ride is a fun adventure for the kiddos and lasts about 35 minutes. -
Congress of Local and Regional Authorities of the Council of Europe Refers To: A
32nd SESSION CPL32(2017)06final 29 March 2017 Local democracy in Iceland Monitoring Committee Rapporteurs1: Zdenek BROZ, Czech Republic (L, ECR) Jakob WIENEN, Netherlands (L, EPP/CCE) Recommendation 402 (2017)..................................................................................................................2 Explanatory memorandum ......................................................................................................................4 Summary This report follows the second monitoring visit to Iceland since it ratified the European Charter of Local Self-Government in 1991. It shows that the country has a satisfactory level of local democracy. The report praises recent developments fostering local self-government, including the promotion of the involvement of local authorities in national decision-making and increased inter-municipal co-operation and citizen participation in local authorities. In particular, it underlines that the national and local authorities were able to deal with a major financial crisis and its economic and social consequences without undermining local self-government. Nevertheless, the rapporteurs draw the authorities’ attention to the absence of a clear division of responsibilities between central government and local authorities, the lack of direct applicability of the Charter in the domestic legal system and the fact that the capital, Reykjavik, has not been granted a special status in accordance with Recommendation 219 (2007). Lastly, local authorities still do not have adequate resources for performing all their functions. The Congress recommends that the Icelandic authorities clarify the division of responsibilities between central government and local authorities and pass legislation to give the Charter legal force in Iceland’s domestic legal system. It also urges them to provide local authorities with adequate and sufficient financial resources and grant the city of Reykjavik a special status to take account of its particular needs compared to other municipalities. -
The Best of Iceland
04_178416-ch01.qxp 5/29/08 8:59 AM Page 1 1 The Best of Iceland On each trip to Iceland, we are always struck by how often other travelers are—or intend to be—repeat visitors. Many come year after year, never exhausting Iceland’s endless variations of magnificent scenery and adventure. Returning travelers immedi- ately recognize the crisp, invigorating polar air, and what W. H. Auden called “the most magical light of anywhere on earth.” Iceland’s astonishing beauty often has an austere, primitive, or surreal cast that arouses reverence, wonderment, mystery, and awe. Lasting impressions could include a lone tuft of wildflowers amid a bleak desert moonscape or a fantastical promenade of icebergs calved into a lake from a magisterial glacier. The Icelandic people—freedom-loving, egalitarian, self-reliant, and worldly—are equally exceptional. They established a parliamentary democracy over a millennium ago, and today write, publish, purchase, and read more books per capita than any peo- ple on earth. Reykjavík, their capital, has become one of the world’s most fashionable urban hot spots. In November 2007, the U.N. named Iceland the world’s best coun- try to live in, based on life expectancy, education levels, medical care, income, and other criteria. 1 The Best Natural Wonders • Glymur: Iceland’s tallest waterfall is • Blue Lagoon: The central activity nimble and graceful: Streamlets at this spa—Iceland’s top tourist descend like ribbons of a maypole attraction—is bathing in a shallow, into a fathomless canyon mantled in opaque, blue-green lagoon amid a bird nests and lush mosses. -
Icelandic Seafood and Fishing Industry Innovation - Seafood Software Solutions - Smart Solutions
April // 2013 CoolCool Icelandic Seafood and Fishing Industry Innovation - seafood software solutions - smart solutions seafood solutions FIND US AT BOOTH 6127-2 EUROPEAN SEAFOODHALL 4 EXPOSITION, BRUSSEL APRIL 23RD - 25TH Wise Fishing Wise Processing Wise Trade Wise Quality Wise Peripherals Wise Aquaculture Wise Analyzer Wise Cubes Wise Reports Wise Dynamics Wise Contracts Wise Government Wise Jobs Wise Subscription 2 Wise is an Independent Software Vendor (ISV) for Wise solutions combine the best of standard Microsoft Microsoft Dynamics NAV and a Microsoft Gold Partner. Dynamics NAV with specialty add-on solutions. Founded in 1995, Wise has become one of the largest Under the Wise Dynamics umbrella is a wide range of resellers of Dynamics NAV in Iceland, oering a wide solutions that oer seafood industry-focused packages, range of business solutions for the international markets. business intelligence solutions and analytical tools. TM Borgartún 26, 105 Reykjavík » Hafnarstræti 102, 600 Akureyri Gold Enterprise Resource Planning tel: +354 545 3200 » [email protected] » www.wise.is Silver Independent Software Vendor (ISV) Codland – 100% utilisation New ideas for extracting additional value products. Haustak’s origins go back to 1999 from seafood of are constantly popping up and it is owned by two of Iceland’s best in Iceland’s fisheries sector. Many known seafood companies, Vísir hf and enterprising young companies have in the Thorbjörn hf. last few years and decades been able to build on smart thinking with solid Arnar Jónsson and Haukur Már Gestsson, marketing to give them a market foothold. project managers at the Iceland Ocean Now another green shoots company, Cluster, have both worked extensively on Codland, born of ambitious innovation and improving additional value from seafood. -
Iceland Living in a Plate Tectonic Boundary
Iceland Living in a plate tectonic boundary https://grapevine.is/n ews/2021/05/18/lava -knocking-at-your- back-door/ https://www.agu.org/meetings/chapman/2012/bcal l/pdf/Chapman_Outline_of_Geology_of_Iceland.pdf Accessed 1/4/2018 Iceland is oceanic crust; it is the subaerial part of the Iceland Basalt Plateau (IBP) • The IBP • Rises > 3000 m above the sea floor • Covers 350,000 km2 • 30% is above sea level • A 50 – 200 km-wide shelf slopes gently to depths of ~ 400m before dropping into the abyss • All of the rocks in Iceland are younger than 25 million years • The oldest rocks exposed at the surface in Iceland are 14 – 16 million years old. • Erosion removes ~ 1 million cubic meters/year • Volcanism and sedimentation more than counter-balance that erosion Postglacial_volcanism _in_Iceland.pdf Accessed 4/4/2021 • RR, Reykjanes Ridge; • RVB, Reykjanes Volcanic Belt; SISZ, South Iceland • Seismic Zone; • WVZ, West Volcanic Zone; • MIB, Mid-Iceland Belt; • EVZ, East Volcanic Zone; • NVZ, North Volcanic • Zone; • TFZ, Tjörnes Fracture Zone; KR, Kolbeinsey Ridge; Mantle Plume • • ÖVB, Öræfi Volcanic Belt; SVB, Snæfellsnes Volcanic Belt Distribution of active volcanic systems among volcanic zones/belts Thordarson, T and A. Hoskuldssom.2014. Classic Geology of Europe 3: Iceland. Dunedin Academic Press Ltd. Pahoehoe/helluhraun lavas form from very fluid magma. A’a/apalhraun lavas may form from more viscous magmas. Flows may change from aa to pahoehoe as they cool. Thordarson, T and A. Hoskuldssom.2014. Classic Geology of Effusive eruptions occur when lava pours out from a fissure or Europe 3: Iceland. cone and flows across the surface as coherent bodies of lava.