Geomythology: Geological Origins of Myths and Legends
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The Paroxysmal Activity at Stromboli Volcano in 2019–2021
geosciences Article The Monitoring of CO2 Soil Degassing as Indicator of Increasing Volcanic Activity: The Paroxysmal Activity at Stromboli Volcano in 2019–2021 Salvatore Inguaggiato 1,* , Fabio Vita 1 , Marianna Cangemi 2 , Claudio Inguaggiato 3,4 and Lorenzo Calderone 1 1 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, Via Ugo La Malfa, 90146 Palermo, Italy; [email protected] (F.V.); [email protected] (L.C.) 2 Dipartimento di Scienze della Terra e del Mare, Via Archirafi 36, 90123 Palermo, Italy; [email protected] 3 Departamento de Geología, Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California (CICESE), Carretera Ensenada-Tijuana 3918, 22860 Ensenada, Mexico; [email protected] 4 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Via Donato Creti 12, 40128 Bologna, Italy * Correspondence: [email protected]; Tel.: +39-091-6809435 Abstract: Since 2016, Stromboli volcano has shown an increase of both frequency and energy of the volcanic activity; two strong paroxysms occurred on 3 July and 28 August 2019. The paroxysms were followed by a series of major explosions, which culminated on January 2021 with magma overflows and lava flows along the Sciara del Fuoco. This activity was monitored by the soil CO2 flux network of Istituto Nazionale di Geofisica e Vulcanologia (INGV), which highlighted significant changes Citation: Inguaggiato, S.; Vita, F.; before the paroxysmal activity. The CO2 flux started to increase in 2006, following a long-lasting Cangemi, M.; Inguaggiato, C.; positive trend, interrupted by short-lived high amplitude transients in 2016–2018 and 2018–2019. Calderone, L. The Monitoring of CO2 Soil Degassing as Indicator of This increasing trend was recorded both in the summit and peripheral degassing areas of Stromboli, Increasing Volcanic Activity: The indicating that the magmatic gas release affected the whole volcanic edifice. -
A Pictorial Summary of the Life and Work of George Patrick Leonard Walker
A pictorial summary of the life and work of George Patrick Leonard Walker SCOTT K. ROWLAND1* & R. S. J. SPARKS2 1Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East–West Road, Honolulu, Hawaii, USA 2Department of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK *Corresponding author (e-mail: [email protected]) Abstract: George Patrick Leonard Walker was one of the fathers of modern volcanology. He worked in many parts of the world and contributed to the understanding of a huge range of volca- nological processes. He was a field geologist at heart, and one of his greatest skills was the ability to quantify volcanological ideas – not with obscure statistical treatments or complex numerical models, but with clear graphical relationships supported by tremendous amounts of carefully col- lected field data. Here we present some glimpses of his life and work in photographs and diagrams. George Walker was born on 2 March 1926 in Iceland, as well as to India, Italy, the Azores and London. In 1939, when he was 13, the family Africa, among other locations. In 1978 George moved to Northern Ireland. In 1948 and 1949, moved to the University of Auckland and in 1982 respectively, George received his Bachelors and he moved to the University of Hawaii. Over the Masters degrees from Queen’s University, Belfast. span of his career he visited almost every volcanic In 1956 he completed his PhD at the University of region in the world, including Australia, the Azores, Leeds with a dissertation on secondary minerals in the Canary Islands, Chile, China, Costa Rica, igneous rocks of Northern Iceland. -
Sicily, Malta & Aeolian Islands
SICILY, MALTA & THE AEOLIAN ISLANDS 15 CAPTIVATING DAYS | P ALERMO TO VALLETTA Stay on 4 incredible Mediterranean islands - Lipari, in the gorgeous Aeolian islands, pretty Ortigia Island by Syracuse, Sicily and sensational Malta. Cruise to whitewashed Panarea, Vulcano island with its hot sulphur mud baths, and Stromboli to witness the volcano’s fiery eruptions against the night sky. Stroll through the baroque heart of delightful Noto, Ragusa Ibla and Scicli, and enjoy a special ‘Modica Experience’ evening. In Malta, stay four nights in beautiful Valletta, visit Gozo, the Blue Grotto and 5,000-year-old stone temples. Enjoy lazy lunches and dinners on seaside terraces, in classic restaurants and unusual locations in the Sicilian countryside. Utterly amazing! TOUR INCLUSIONS ALL excursions, scenic drives, sightseeing and entrances as described Fully escorted by our experienced Tour Manager Travel in first-class air-conditioned coaches for touring, transfers and sightseeing 14 nights specially selected hotel accommodation Hotel porterage (1 bag per person) 23 Meals – including breakfast daily, 3 lunches and 6 dinners Tea, coffee and a complimentary beverage with all included dinners Hand Selected Albatross Experiences - Aeolian Islands cruise to Panarea and Stromboli, visit to Vulcano island, Malta Two Harbour boat cruise, visits St John’s Co-Cathedral and the Malta Experience, day trip to Gozo, the Ħaġar Qim and Mnajdra stone temples, Blue Grotto boat ride. Local guides as described in the itinerary ALL tips to your Tour Manager, Driver and Local Guides Personal audio system whilst on tour Free WiFi on most coaches and at hotels Add a subheading THE ALBATROSS DIFFERENCE Leisurely 2, 3 and 4 night stays Small group sizes - from just 10 to 28 Genuinely inclusive, NO extra 'on tour' costs Stay in traditional style hotels in superb locations Easier days with 'My Time' guaranteed! MESSAGE FROM THE MO: WANDERLUST… “To have seen Italy without having seen Sicily is not to have seen Italy at all,” said German writer Goethe in 1787. -
Mars Field Geology, Biology, and Paleontology Workshop, Summary
MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston, Houston, Texas LPI Contribution No. 968 MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston Edited by Nancy Ann Budden Lunar and Planetary Institute Sponsored by Lunar and Planetary Institute National Aeronautics and Space Administration Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 968 Compiled in 1999 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautcis and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This volume may be cited as Budden N. A., ed. (1999) Mars Field Geology, Biology, and Paleontology Workshop: Summary and Recommendations. LPI Contribution No. 968, Lunar and Planetary Institute, Houston. 80 pp. This volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling. _________________ Cover: Mars test suit subject and field geologist Dean Eppler overlooking Meteor Crater, Arizona, in Mark III Mars EVA suit. PREFACE In November 1998 the Lunar and Planetary Institute, under the sponsorship of the NASA/HEDS (Human Exploration and Development of Space) Enterprise, held a workshop to explore the objectives, desired capabilities, and operational requirements for the first human exploration of Mars. -
Journal of Geodynamics Structural Features Of
Journal of Geodynamics 47 (2009) 288–292 Contents lists available at ScienceDirect Journal of Geodynamics journal homepage: http://www.elsevier.com/locate/jog Technical note Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): Implications for the 2002–2003 unrest Valerio Acocella a,∗, Marco Neri b, Thomas R. Walter c a Dip. Sc. Geologiche Roma Tre. L.S.L. Murialdo 1, 00146 Rome, Italy b Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Piazza Roma 2, 95123 Catania, Italy c Deutsches GeoForschungsZentrum (GFZ) Potsdam, Dept. Physics of the Earth, Telegrafenberg, 14473 Potsdam, Germany article info abstract Article history: Panarea, characterized by gas unrest in 2002–2003, is the volcanic island with the least constrained Received 8 October 2008 structure in the eastern-central Aeolian Arc (Italy). Based on structural measurements, we define here its Received in revised form 13 January 2009 deformation pattern relative to the Arc. The main deformations are subvertical extension fractures (63% Accepted 13 January 2009 of data), normal faults (25%) and dikes (12%). The mean orientation of the extension fractures and faults is ∼N38◦E, with a mean opening direction of N135◦ ± 8◦, implying extension with a moderate component Keywords: of dextral shear. These data, matched with those available for Stromboli volcano (pure opening) and Arc volcanoes Vulcano, Lipari and Salina volcanoes (predominant dextral motions) along the eastern-central Arc, suggest Extension Unrest a progressive westward rotation of the extension direction and an increase in the dextral shear. The dextral shear turns into compression in the western arc. The recent unrest at Panarea, coeval to that of nearby Stromboli, may also be explained by the structural context, as both volcanoes lie along the portion of the Arc subject to extension. -
Educators Guide
EDUCATORS GUIDE 02 | Supervolcanoes Volcanism is one of the most creative and destructive processes on our planet. It can build huge mountain ranges, create islands rising from the ocean, and produce some of the most fertile soil on the planet. It can also destroy forests, obliterate buildings, and cause mass extinctions on a global scale. To understand volcanoes one must first understand the theory of plate tectonics. Plate tectonics, while generally accepted by the geologic community, is a relatively new theory devised in the late 1960’s. Plate tectonics and seafloor spreading are what geologists use to interpret the features and movements of Earth’s surface. According to plate tectonics, Earth’s surface, or crust, is made up of a patchwork of about a dozen large plates and many smaller plates that move relative to one another at speeds ranging from less than one to ten centimeters per year. These plates can move away from each other, collide into each other, slide past each other, or even be forced beneath each other. These “subduction zones” are generally where the most earthquakes and volcanoes occur. Yellowstone Magma Plume (left) and Toba Eruption (cover page) from Supervolcanoes. 01 | Supervolcanoes National Next Generation Science Standards Content Standards - Middle School Content Standards - High School MS-ESS2-a. Use plate tectonic models to support the HS-ESS2-a explanation that, due to convection, matter Use Earth system models to support cycles between Earth’s surface and deep explanations of how Earth’s internal and mantle. surface processes operate concurrently at different spatial and temporal scales to MS-ESS2-e form landscapes and seafloor features. -
Structural Features of Panarea Volcano in the Frame of the Aeolian Arc (Italy): Implications for the 2002–2003 Unrest V
Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): implications for the 2002–2003 unrest V. Acocella, M. Neri, T. Walter To cite this version: V. Acocella, M. Neri, T. Walter. Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): implications for the 2002–2003 unrest. Journal of Geodynamics, Elsevier, 2009, 47 (5), pp.288. 10.1016/j.jog.2009.01.004. hal-00518307 HAL Id: hal-00518307 https://hal.archives-ouvertes.fr/hal-00518307 Submitted on 17 Sep 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Title: Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): implications for the 2002–2003 unrest Authors: V. Acocella, M. Neri, T. Walter PII: S0264-3707(09)00017-9 DOI: doi:10.1016/j.jog.2009.01.004 Reference: GEOD 876 To appear in: Journal of Geodynamics Received date: 8-10-2008 Revised date: 13-1-2009 Accepted date: 13-1-2009 Please cite this article as: Acocella, V., Neri, M., Walter, T., Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): implications for the 2002–2003 unrest, Journal of Geodynamics (2008), doi:10.1016/j.jog.2009.01.004 This is a PDF file of an unedited manuscript that has been accepted for publication. -
HTS Aeolian Islands
SOUTHERN ITALY - MEDITERRANEAN SEA DISCOVER THE ARCHIPELAGO OF THE AEOLIAN ISLANDS - A unique UNESCO World Heritage Site BRIGANTINE FLORETTE Historical Tallship Sailing LTD Mediterranean Sea Southern Italy - Aeolian Archipelago Set Sail with the wooden Tallship Florette the last of her kind and sail in her home waters to explore the unique archipelago of the Unesco-protected Aeolian Islands. The seven islands, including Lipari, Vulcano, Salina, Panarea, Stromboli, are a little piece of paradise, a magical outdoor playground. Our guests from all walks of life looking for adventure and that something different. Take a Vespa island tour on Lipari, experience the charm of Panarea and hike the nature reserve of Salina. Enjoy the creative "Cucina Eoliana" and explore the 6000-year-old culture of these islands. Swim and snorkel in secluded bays with crystal clear water and dark beaches made of fine, black lava sand. Marvel at the most active volcano in Europe. Explore Stromboli on an adventurous night hike. Climb Vulcano slumbering in the sulfur steam and then enjoy a healing bath in the sulfur mud. DISCOVER THE MEDITERRANEAN SEA: SOUTHERN ITALY - CALABRIA-AEOLIAN ISLANDS ARCHIPELAGO A unique UNESCO World Heritage Site You can expect sailing fun, hiking on active volcanoes, breathtaking nature, culture & adventure and all that with the right breeze from Italy's Dolce Vita. Travel dates are weekly from May 8th, 2021 - October 23rd, 2021 from 849.- Euro Included in the voyage price: • 7 days sailing trip on the historical windjammer as an active sailor • Half board with breakfast and six delicious meals • Diesel costs & tender services land - ship • Snorkelling gear, kayaks and SUPs are available onboard • Safety briefing with a basic knot & sailing school • Professional crew with the Haynes family guarantee an unforgettable experience Not included in the voyage price: • Arrival and departure transfers, shore excursions, drinks, visas and personal insurance. -
GSA TODAY December Vol
Vol. 5, No. 12 December 1995 INSIDE • New Members, Fellows, Student Associates, p. 247 GSA TODAY South-Central Section Meeting, p. 250 • A Publication of the Geological Society of America • Northeastern Section Meeting, p. 253 Seismic Images of the A B Core-Mantle Boundary Michael E. Wysession, Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130 C D ABSTRACT INTRODUCTION Seismology presents several ways While most geologists, including of providing images of the geologic specialists in the field of seismology, structures that exist in the lowermost study rocks at Earth’s surface, more mantle just above the core-mantle attention also is being paid to the boundary (CMB). An understanding planet’s other major boundary, that of the possibly complex geophysical between the core and mantle. With a E F processes occurring at this major density jump of 4.3 kg/m3 between discontinuity requires the combined the silicate lower mantle and the liquid efforts of many fields, but it is the iron outer core, as well as a tempera- role of seismology to geographically ture increase of possibly 1500 °C map out this largely uncharted terri- between the lower mantle adiabat and tory. Seismic phases that reflect, outer core, the core-mantle boundary diffract, and refract across the CMB (CMB) may well be Earth’s most signifi- can all be used to provide different cant and dramatic discontinuity. Our Figure 1. Images from a motion picture showing the propagation of seismic shear energy information in different ways. increasing knowledge of this highly through the mantle (Wysession and Shore, 1994). -
Sharon R. Allen Is a Physical Volcanologist Who Has Worked On
Sharon R. Allen is a physical volcanologist who Timothy H. Druitt is a volcanologist who works has worked on the processes and products of felsic on the processes and products of explosive volca effusive and explosive volcanism in both subaerial nism. His approaches include the field study of and submarine environments from a range of tec volcanic products, laboratory analogue experi tonic settings. She has been researching the South ments, and the petrology and chemistry of magmas. Aegean volcanic arc since 1993, first as a PhD He has used Santorini Volcano (Greece) as a natural student at Monash University (Australia), later as a laboratory for identifying fundamental questions postdoc at the University of Tasmania (UTAS) (Australia), and currently related to volcanism and for testing hypotheses. He obtained his PhD as a university associate at UTAS. Her scientific interests include subae at the University of Cambridge (UK) and is currently Professor of rial caldera forming eruptions, the dynamics of pyroclastic currents Volcanology at ClermontAuvergne University (France). He was Editor on land and when interacting with water, submarine pyroclastic erup inChief of the Bulletin of Volcanology for four years and received the tions and mechanisms for the formation of pumice in submarine set 2018 Norman L. Bowen Award of the American Geophysical Union. tings. Her approach includes field studies of volcanic products and laboratory analogue experimentation. Lorella Francalanci is a geochemist and volcano logist who investigates active volcanoes to reveal Olivier Bachmann is a professor of volcanology the preeruptive processes that are relevant to the and magmatic petrology at the Eidgenössische dynamics of volcanic eruptions. -
CORE of SICILY 8 Days to Discover a Gem of History and Nature
CORE OF SICILY 8 days to discover a gem of history and nature D01: ARRIVAL TO CATANIA Catania is Sicily’s second main city for its population and cultural richness. The population survived through the Greeks deportation, the Carthaginians and the stream of lava from Mount Etna. Nowadays Piazza del Duomo, Via Etnea and many of the historical buildings has heightened Catania’s charme. Many structures are built from three-centuries old lava (the black buildings) which, combined with baroque architecture, treats the city a singular darken twisted beauty. Overnight in Catania. D02: ETNA VOLCAN (SOFT TREKKING UP TO CRATER GUIDED ENVIRONMENTAL VISIT) - SIRACUSA Mount Etna is the major and highest vulcano in Europe. Only the cone of the crater rises to 11000 feet above sea level. Plato sailed to Sicily just to catch a glimpse of it in 387 BC. Etna is still an active vulcano and has erupted a dozen times in the past 30 years and more, most spectacularly in 1971, 1982, 2001, 2002 and 2005. Fumes from the top of the vulcano are always a constant companion of Catanese’s days. A trip nearby of the crater depends on Mount Etna’s temperament, but generally it's possible to walk and enjoy this most unique sublime force of nature. Overnight in Siracusa D03: SIRACUSA Syracuse is a jewel of Sicily. Astonishing and wonderful, the great ancient capital of Western civilization at the Greek times was founded in 734 BC. Soon it was the major city of Sicily to compete against Athens in beauty, splendor and power. -
Earthsciencesnews Issue No 05 2014
Department of earth Sciences Magazine EarthScienceSNEWS iSSue no 05 2014 P4 Fundamental Fieldtrips P8 From Himalayas to Marcellus P10 Mineralogy in Myanmar P12 earthquake Risk in Turkey P16 London Volcano 1 modern process, underpins climate science. In diverse and subtle ways, earth sciences weLcoMe influence the discussion of windmills and carbon taxes at the present Lima climate conference or next year’s major Paris by Professor Gideon Henderson meeting. Head of Department Climate science is also important, along with many other branches of the earth sciences, in the help and guidance it provides to developing nations. Oxford earth scientists work all over the world; climate events help to initiate a burst Does the study of climate literally from Abu Dhabi to Zambia. Many of evolution? Geological understanding nations have significant natural resources, belong in an earth-sciences of climate is also important for more fascinating geology, and are threatened applied questions. Past warm periods of department? by geological hazards and environmental ocean anoxia led to the preservation of change, but lack modern geological tools Sometimes, amongst the swirl of debate hydrocarbons, still critical to global energy and the understanding to benefit from their about wind-farms, carbon taxes, and the production. And it is the winds, sun, tides resources or assess their risks. Universities policy response to warming, it is possible and waves of the earth system that offer such as Oxford have a huge amount to offer to wonder what climate has to do with the alternatives we must rapidly adopt for such nations, as evident in the department’s geology.