Surtsey Research Progress Report
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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. -
Paleoenvironmental Interpretation of Late Glacial and Post
PALEOENVIRONMENTAL INTERPRETATION OF LATE GLACIAL AND POST- GLACIAL FOSSIL MARINE MOLLUSCS, EUREKA SOUND, CANADIAN ARCTIC ARCHIPELAGO A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geography University of Saskatchewan Saskatoon By Shanshan Cai © Copyright Shanshan Cai, April 2006. All rights reserved. i PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geography University of Saskatchewan Saskatoon, Saskatchewan S7N 5A5 i ABSTRACT A total of 5065 specimens (5018 valves of bivalve and 47 gastropod shells) have been identified and classified into 27 species from 55 samples collected from raised glaciomarine and estuarine sediments, and glacial tills. -
Supplementary Material
Supplementary material S1 Eruptions considered Askja 1875 Askja, within Iceland’s Northern Volcanic Zone (NVZ), erupted in six phases of varying intensity, lasting 17 hours on 28–29 March 1875. The main eruption included a Subplinian phase (Unit B) followed by hydromagmatic fall and with some proximal pyroclastic flow (Unit C) and a magmatic Plinian phase (Unit D). Units C and D consisted of 4.5 x 108 m3 and 1.37 x 109 m3 of rhyolitic tephra, respectively [1–3]. Eyjafjallajökull 2010 Eyjafjallajökull is situated in the Eastern Volcanic Zone (EVZ) in southern Iceland. The Subplinian 2010 eruption lasted from 14 April to 21 May, resulting in significant disruption to European airspace. Plume heights ranged from 3 to 10 km and dispersing 2.7 x 105 m3 of trachytic tephra [4]. Hverfjall 2000 BP Hverfjall Fires occurred from a 50 km long fissure in the Krafla Volcanic System in Iceland’s NVZ. Magma interaction with an aquifer resulted in an initial basaltic hydromagmatic fall deposit from the Hverfjall vent with a total volume of 8 x 107 m3 [5]. Eldgja 10th century The flood lava eruption in the first half of the 10th century occurred from the Eldgja fissure within the Katla Volcanic System in Iceland’s EVZ. The mainly effusive basaltic eruption is estimated to have lasted between 6 months and 6 years, and included approximately 16 explosive episodes, both magmatic and hydromagmatic. A subaerial eruption produced magmatic Unit 7 (2.4 x 107 m3 of tephra) and a subglacial eruption produced hydromagmatic Unit 8 (2.8 x 107 m3 of tephra). -
Testing the Hypothesis of Tolerance Strategies in Hiatella Arctica L. (Mollusca: Bivalvia)
Helgol Mar Res (2005) 59: 187–195 DOI 10.1007/s10152-005-0218-6 ORIGINAL ARTICLE Vjacheslav V. Khalaman Testing the hypothesis of tolerance strategies in Hiatella arctica L. (Mollusca: Bivalvia) Received: 15 April 2004 / Revised: 14 February 2005 / Accepted: 14 February 2005 / Published online: 6 April 2005 Ó Springer-Verlag and AWI 2005 Abstract The physiological and biocenotic optima of Keywords Fluctuating asymmetry Æ Directional Hiatella arctica L. inhabiting shallow water fouling asymmetry Æ Hiatella arctica Æ Biofouling Æ communities of the White Sea were compared. The Tolerance strategy Æ The White Sea biomass and proportion of H. arctica in communities were used for the estimation of biocenotic optima or community success. The physiological state of popula- tions was assessed by means of the fluctuating asym- Introduction metry. The fluctuating asymmetry of H. arctica was calculated using the valve weights. It was determined Ramenskii (1935) described three main survival strat- that the shell of H. arctica possesses a slight directional egies in terrestrial plants: tolerance (S), ruderal (R) asymmetry, the right valve usually being larger (and and competitive (K) strategies. This classification was heavier) than the left one. The relationship between adopted in the Russian literature, but received little fluctuating and directional asymmetries is discussed. attention elsewhere. Almost 40 years later the classifi- High biomass and proportion of H. arctica in the cation of survival strategies was ‘‘rediscovered’’ by community generally correspond with high levels of Grime (1974), became widely adopted by plant ecol- fluctuating asymmetry. Thus, a discrepancy between ogists, and was then developed further. Tolerance physiological and ecological optima is observed, which strategies were divided into two categories, referring to is recognised as being characteristic of a tolerance plants that are tolerant to unfavourable abiotic envi- strategy. -
The Magmatic Plumbing System of the Askja Central Volcano, Iceland, As
PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE The magmatic plumbing system of the Askja central 10.1002/2016JB013163 volcano, Iceland, as imaged by seismic tomography Key Points: Tim Greenfield1, Robert S. White1, and Steven Roecker2 • Low velocities in the crust delineate the magmatic plumbing system 1Bullard Laboratories, University of Cambridge, Cambridge, UK, 2Rensselaer Polytechnic Institute, Troy, New York, USA beneath Askja volcano in Iceland • Primary magma storage region is at a depth of 5 km bsl but extends into the lower crust where melt movement Abstract The magmatic plumbing system beneath Askja, a volcano in the central Icelandic highlands, is generates microearthquakes imaged using local earthquake tomography. We use a catalog of more than 1300 earthquakes widely • Melt is distributed in discrete regions distributed in location and depth to invert for the P wave velocity (Vp) and the Vp/Vs ratio. Extensive synthetic throughout the crust to depths of over 20 km tests show that the minimum size of any velocity anomaly recovered by the model is ~4 km in the upper crust (depth < 8 km below sea level (bsl)), increasing to ~10 km in the lower crust at a depth of 20 km bsl. The plumbing system of Askja is revealed as a series of high-Vp/Vs ratio bodies situated at discrete depths Supporting Information: • Supporting Information S1 throughout the crust to depths of over 20 km. We interpret these to be regions of the crust which currently • Movie S1 store melt with melt fractions of ~10%. The lower crustal bodies are all seismically active, suggesting that • Movie S2 melt is being actively transported in these regions. -
Globally Widespread Bryophytes, but Rare in Europe
Portugaliae Acta Biol. 20: 11-24. Lisboa, 2002 GLOBALLY WIDESPREAD BRYOPHYTES, BUT RARE IN EUROPE Tomas Hallingbäck Swedish Threatened Species Unit, P.O. Box 7007, SE-75007 Uppsala, Sweden. [email protected] Hallingbäck, T. (2002). Globally widespread bryophytes, but rare in Europe. Portugaliae Acta Biol. 20: 11-24. The need to save not only globally threatened species, but also regionally rare and declining species in Europe is discussed. One rationale of red-listing species regionally is to be preventive and to counteract the local species extinction process. There is also a value in conserving populations at the edge of their geographical range and this is discussed in terms of genetic variation. Another reason is the political willingness of acting locally rather than globally. Among the rare and non-endemic species in Europe, some are rare and threatened both in Europe and elsewhere, others are more common outside Europe and a third group is locally common within Europe but rare in the major part. How much conservation effort should be put on these three European non-endemic species groups is briefly discussed, as well as why bryophytes are threatened. A discussion is given, for example, of how a smaller total distribution range, decreasing density of localities, smaller sites, less substrate and lower habitat quality affect the survival of sensitive species. This is also compared with species that have either high or low dispersal capacity or different longevity of either vegetative parts or spores. Examples from Sweden are given. Key words: Bryophytes, rarity, Europe, dispersal capacity, Sweden. Hallingbäck, T. (2002). -
The Surtsey 1963 Eruption Plume, Characteristics and Tephra Dispersal
Geophysical Research Abstracts Vol. 21, EGU2019-17144, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. The Surtsey 1963 eruption plume, characteristics and tephra dispersal Einar Sindri Ólafsson (1), Magnus T Guðmundsson (2), and Esther R. Guðmundsdóttir (3) (1) Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland ([email protected]), (2) Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland ([email protected]), (3) Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland ([email protected]) Surtsey is a basaltic island in the south-western end of Vestmannaeyjar archipelago off the south coast of Iceland and is a part of the Vestmannaeyjar volcanic system. It is built from the ocean floor at about 130 m depth in a series of eruptions during 1963-1967, one of the longest eruption in Iceland in historical times. The eruptions can be split into four phases. The first phase of the eruptions was explosive and phreatomagmatic in character. The aim of this study is to put constraints on the mass of tephra transported with the plume. This is done in two ways: (1) Study soil profiles on Heimaey and on the mainland to look for tephra deposits from Surtsey as well as note contemporary descriptions of tephra fallout; and (2) by compiling existing contemporary records of plume height and use plume height – mass transport systematics to estimate the transport. Finally, we compare the outcomes of (1) and (2). Eruption started on 14 November 1963. It was explosive and fed an eruption plume rising typically to 5-9 km in November and December 1963. -
1783-84 Laki Eruption, Iceland
1783-84 Laki eruption, Iceland Eruption History and Atmospheric Effects Thor Thordarson Faculty of Earth sciences, University of Iceland 12/8/2017 1 Atmospheric Effects of the 1783-84 Laki Eruption in Iceland Outline . Volcano-Climate interactions - background Laki eruption . Eruption history . Sulfur release and aerosol loading . Plume transport and aerosol dispersal . Environmental and climatic effects 12/8/2017. Concluding Remarks 2 Santorini, 1628 BC Tambora, 1815 Etna, 44 BC Lakagígar, 1783 Toba, 71,000 BP Famous Volcanic Eruptions Krakatau, 1883 Pinatubo, 1991 El Chichón, 1982 Agung, 1963 St. Helens, 1980 Major volcanic eruptions of the past 250 years Volcano Year VEI d.v.i/Emax IVI Lakagígar [Laki craters], Iceland 1783 4 2300 0.19 Unknown (El Chichón?) 1809 0.20 Tambora, Sumbawa, Indonesia 1815 7 3000 0.50 Cosiguina, Nicaragua 1835 5 4000 0.11 Askja, Iceland 1875 5 1000 0.01* Krakatau, Indonesia 1883 6 1000 0.12 Okataina [Tarawera], North Island, NZ 1886 5 800 0.04 Santa Maria, Guatemala 1902 6 600 0.05 Ksudach, Kamchatka, Russia 1907 5 500 0.02 Novarupta [Katmai], Alaska, US 1912 6 500 0.15 Agung, Bali, Indonesia 1963 4 800 0.06 Mt. St. Helens, Washington, US 1980 5 500 0.00 El Chichón, Chiapas, Mexico 1982 5 800 0.06 Mt. Pinatubo, Luzon, Philippines 1991 6 1000 — Volcano – Climate Interactions Key to Volcanic Forcing is: SO2 mass loading, eruption duration plume height replenishment aerosol production, residence time 12/8/2017 5 Volcanic Forcing: sulfur dioxide sulfate aerosols SO2 75%H2SO4+ 25%H2O clear sky 1991 Pinatubo aerosols -
About the Book the Format Acknowledgments
About the Book For more than ten years I have been working on a book on bryophyte ecology and was joined by Heinjo During, who has been very helpful in critiquing multiple versions of the chapters. But as the book progressed, the field of bryophyte ecology progressed faster. No chapter ever seemed to stay finished, hence the decision to publish online. Furthermore, rather than being a textbook, it is evolving into an encyclopedia that would be at least three volumes. Having reached the age when I could retire whenever I wanted to, I no longer needed be so concerned with the publish or perish paradigm. In keeping with the sharing nature of bryologists, and the need to educate the non-bryologists about the nature and role of bryophytes in the ecosystem, it seemed my personal goals could best be accomplished by publishing online. This has several advantages for me. I can choose the format I want, I can include lots of color images, and I can post chapters or parts of chapters as I complete them and update later if I find it important. Throughout the book I have posed questions. I have even attempt to offer hypotheses for many of these. It is my hope that these questions and hypotheses will inspire students of all ages to attempt to answer these. Some are simple and could even be done by elementary school children. Others are suitable for undergraduate projects. And some will take lifelong work or a large team of researchers around the world. Have fun with them! The Format The decision to publish Bryophyte Ecology as an ebook occurred after I had a publisher, and I am sure I have not thought of all the complexities of publishing as I complete things, rather than in the order of the planned organization. -
Antimicrobial Activity of Tooth Powder Containing Hekla Lava and Calendula
Swathi.A et al /J. Pharm. Sci. & Res. Vol. 7(10), 2015, 882-884 Antimicrobial Activity of Tooth Powder Containing Hekla Lava and Calendula Swathi.A, Muralidharan.N.P Bachelor of Dental Surgery,Saveetha Dental College and Hospital,Chennai Aim And Objective To study anti microbial activity of tooth powder containing Hekla lava and calendula. Background Homeopathy medicine is always a cheaper alternate and called as poor mans medicine. Hekla lava with calendula is available as a tooth powder in the market. It is a homeopathy remedy used in treating gingivitis and loose sockets which are the major problems in old age patients. It's properties can be explored as a intracanal medicament in root canal treatment as well. Materials And Methods Hekla lava with calendula powder, chlorhexidine gel and calcium hydroxide are obtained. The antibacterial activity of Hekla lava with calendula was tested against the odontogenic bacteria such as Streptococcus mutans and Enterococcus. They were subjected for the anti microbial activity by agar well diffusion method. Results In our study, we have found that the tooth powder containing hekla lava and calendula have considerable antimicobial effects ,which are compared with chlorhexidine and calcium hydroxide ,which are already in practice. Conclusion The study reveals that the tooth powder hekla lava with calendula has a good anti microbial effect against mutans and enterococcus ,which can be used in treating various dental problems. INTRODUCTION sesquiterpenes, flavonoid glycosides, triterpene saponins, The most common forms of human periodontal disease are triterpene alcohols, flavonoids, carotenoids, xanthophylls, gingivitis and periodontitis. Gingivitis is defined as an phenolic acids, steroids, mucilage, tocopherol, and inflammation of the gingiva. -
Part 2 – Fruticose Species
Appendix 5.2-1 Vegetation Technical Appendix APPENDIX 5.2‐1 Vegetation Technical Appendix Contents Section Page Ecological Land Classification ............................................................................................................ A5.2‐1‐1 Geodatabase Development .............................................................................................. A5.2‐1‐1 Vegetation Community Mapping ..................................................................................... A5.2‐1‐1 Quality Assurance and Quality Control ............................................................................ A5.2‐1‐3 Limitations of Ecological Land Classification .................................................................... A5.2‐1‐3 Field Data Collection ......................................................................................................... A5.2‐1‐3 Supplementary Results ..................................................................................................... A5.2‐1‐4 Rare Vegetation Species and Rare Ecological Communities ........................................................... A5.2‐1‐10 Supplementary Desktop Results ..................................................................................... A5.2‐1‐10 Field Methods ................................................................................................................. A5.2‐1‐16 Supplementary Results ................................................................................................... A5.2‐1‐17 Weed Species -
Using GIS to Study Potential Lahar Hazards from Hekla and Grímsvötn, Southern Iceland
Using GIS to Study Potential Lahar Hazards from Hekla and Grímsvötn, Southern Iceland The University of Texas at Austin Jackson School of Geosciences Ian Yeats 12/04/2014 Introduction Iceland is an island nation far in the northern hemisphere, with a portion of the country included in the Arctic Circle. Its position over a magmatic hotspot and the Atlantic mid-ocean ridge cause it to have a very active volcanic setting. Some of these eruptions, like that of Eyjafjallajökull in 2010, make worldwide news due to large ash clouds disrupting global air traffic, but many of them go unnoticed to the world. Hence, Icelandic people are very accustomed to responding to volcanic hazards, and it is essential to understand the possible risks involved with living near these active volcanoes. One major hazard associated with volcanism is lahars, or jökulhlaups in Icelandic. In Iceland, these form from the rapid melting of glaciers and snow and the addition of large quantities of volcanic material. These are very large, and sometimes hot, mudslides that even occur without a present eruption. This project used ArcMap to predict potential flow paths of lahars from two major volcanoes in southern Iceland: Hekla and Grímsvötn. Both of these have very active histories, with their last eruptions occurring in 2000 and 2011, respectively. The end goal is to produce maps that highlight these hazards, as well as towns and roads that may stand in their way. Data and Analysis This project required detailed national elevation data, a country boundary, roads, towns, rivers, and the locations of Icelandic volcanoes.