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  • 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous  (24)
  • 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
  • 631.4
  • INGV  (29)
  • Blackwell Publishing Ltd  (5)
  • Blackwell publishing
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  • 1
    Publication Date: 2020-10-27
    Description: In this paper we show results from the combinantion of GPS and CGPS data to estimate the velocity and strain fields across the Messina Straits. Data from CGPS networks of ASI, RING and ITALPOS together with GPS data collected since 1980 during repeated campaigns and recently in the frame of the "Progetto Messina" funded by DPC, are discussed and interpreted to improve the current kinematics of this seismic area.
    Description: Published
    Description: Reggio Calabria
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: GPS, Stretto di Messina ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 2
    Publication Date: 2017-04-04
    Description: We have developed a Bayesian method for the inversion of static ground deformations at volcanic areas.
    Description: Published
    Description: 935-946
    Description: partially_open
    Keywords: Bayesian inversion ; deformation ; Geodesy ; magma ; Mt Etna ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 473 bytes
    Format: 827257 bytes
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  • 3
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    INGV
    Publication Date: 2017-04-03
    Description: Emeritus Professor Samuel Warren Carey passed away on 20 March 2002 at age 90. He was born at Campbelltown, New South Wales on 1st November 1911, and attended school at the Canterbury Boys High School. Carey’s father was a printer, who became a public lecturer when he arrived in Australia. His mother’s people were early Australian settlers. The Carey home was a farm near Campbelltown and as a boy, little Samuel walked nearly seven miles to School and back each day, an activity that prepared him for work in harsh climatic and environmental conditions. Sam Carey’s large family included two sisters and four brothers, one of whom died in World War II. At the University of Sydney, in 1929, Carey enrolled in chemistry, physics, and mathematics and only as a fourth subject – geology. However, he was soon reoriented towards geology as his main subject by Sir Edgeworth David, an Antarctic explorer. This preference developed from his liking for fieldwork in geology, combined with lab work. He was strongly inclined towards sports (hockey, sailing, rugby, marksmanship, canoeing) and physical activities (cave exploration, rock climbing, hiking, jungle expeditions, parachuting). He graduated in Geology from the University of Sydney earning a Bachelor of Science with First Class Honours in 1933, Master of Science in 1934, and Doctor of Science in 1939. At university he founded the Student’s Geological Society in 1931 and was its first president. He has been a pioneer in geology all his life. He was fortunate to participate as a protagonist for two and possibly three revolutions in the Earth sciences. He challenged the concept of continents in fixed positions from the outset and from 1946 to 1956 he taught a version of intercontinental movement with subduction in deep ocean trenches. This came to be called ‘plate tectonics’ some twenty years later but at the time when no one believed in any form of intercontinental movement, Carey’s version was also called ‘continental drift’ by default. Carey developed a new way to interpret orogens. He did not ascribe the building of mountain chains to compression – as is commonly accepted by the geological community involved in contraction or pulsation tectonics. Carey ascribed it to isostatic instability where rising mantle beneath deep sediment filled trenches causes diapiric uplift. The observed folding was explained as the consequent downward gravitational sliding of uplifted strata. This mountain building concept is still considered valid today and it constitutes part of a more diversified classification of mountain evolution that has been developed by Cliff Ollier. Carey proposed abandonment of the subduction concept, and put forward step by step the concept of Earth expansion. Carey – using the orocline concept – generalised his views on movement between continents, demonstrating that the continents could fit together better if the Earth was smaller in size.
    Description: Published
    Description: 85-95
    Description: open
    Keywords: History of global tectonic theories ; Expanding Earth ; S.W. Carey ; Hobart ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
    Format: 1089204 bytes
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  • 4
    Publication Date: 2017-04-04
    Description: Il Vesuvio è noto nel mondo soprattutto per la grande eruzione del 79 d.C., che distrusse in soli due giorni Pompei, Ercolano, Oplonti e Stabia. Dopo il 79 d.C., il Vesuvio ha alternato periodi di attività, caratterizzati da frequenti eruzioni di media energia, a periodi di riposo, lunghi anche molti secoli e interrotti da violente eruzioni esplosive come quelle del 472 d.C. e del 1631. L’attività del vulcano negli ultimi tre secoli è stata caratterizzata da eruzioni di moderata energia ma di grande effetto spettacolare, che hanno reso il Vesuvio meta di viaggiatori, scienziati, letterati e artisti da tutto il mondo. Dopo l’eruzione del 1944, il vulcano è entrato in una fase di quiescenza, la cui durata è impossibile da prevedere. Negli ultimi decenni il vulcano è stato caratterizzato da una debole attività fumarolica, prevalentemente nell’area craterica, e da attività sismica con scosse di energia medio-bassa. La storia eruttiva del Vesuvio indica che il vulcano non può essere considerato estinto ed è molto probabile che l’attuale quiescenza venga interrotta da una nuova, violenta eruzione. L’Osservatorio Vesuviano, inaugurato nel 1845 da Ferdinando II re delle Due Sicilie, è il primo osservatorio vulcanologico al mondo. Ha permesso per oltre centocinquanta anni l’osservazione minuziosa delle eruzioni vesuviane e dei loro precursori. Oggi vigila sullo stato di attività dei vulcani campani, pronto a cogliere i primi segni di riattivazione. La mostra Vesuvio: 2000 anni di osservazioni conduce il visitatore attraverso un affascinante percorso nel mondo dei vulcani, e del Vesuvio in particolare: descrive i vari tipi di eruzioni e i pericoli relativi, spiega come si ricostruisce la storia di un vulcano, presenta ricche collezioni di campioni di rocce e minerali vesuviani e di strumenti storici, libri e dipinti. È possibile anche osservare la registrazione in tempo reale di dati sismici della rete dell’INGV - Osservatorio Vesuviano. L’obiettivo principale del Museo è fornire soprattutto agli abitanti dell’area vesuviana, ma anche al vasto pubblico che visita il Vesuvio, informazioni sui principali pericoli vulcanici attesi e sulle metodologie di monitoraggio.
    Description: Published
    Description: 5.8. TTC - Formazione e informazione
    Description: open
    Keywords: museo ; vesuvio ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book
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  • 5
    Publication Date: 2017-04-04
    Description: Giovanni Capellini (1833-1922) was one of the leading representatives of the Italian and international scientific community from the mid-19th century until 1922, the year of his death. Professor of Geology at the University of Bologna from 1860, geologist, palaeontologist and archaeologist, in 1871 he organised, straight after the unification of Italy, the 5th International Congress in Archaeology and Prehistoric Anthropology, first in Italy, and in 1881 brought to Bologna, for the first time ever in Italy, the 2nd International Geological Congress. His studies and publications strongly influenced the geological thinking of his times. At the Archiginnasio Library in Bologna there are as many as 30,000 documents from his scientific letters (The Capellini Archive), the result of an intense correspondence he had with geologists, seismologists, astronomers and meteorologists, but also with people from the world of culture and politics. The letters relating to the earth sciences, from scientific but also political point of view, are the majority. The archive includes letters from more then 4,300 senders, of which at least 25% foreign ones incuding Charles Lyell (geologist), Emmanuel Friedlaender (volcanologist), Philip Eduard De Verneuil (naturalist), Henry James Johnston Lavis (volcanologist).
    Description: Published
    Description: 667-677
    Description: 5.2. TTC - Banche dati di sismologia strumentale
    Description: JCR Journal
    Description: open
    Keywords: Giovanni Capellini ; history of earth sciences ; scientific letters ; 2nd International Geological Congress ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2017-04-04
    Description: The main points of the life and scientific production of Ott Christoph Hilgenberg (1896-1976) have been reconstructed. The events took place between America and Berlin: in America from 1925 to 1928 the young Hilgenberg, with a diploma in Mechanical Engineering, worked as a Geophysicist in an oil prospecting company. It was there that he probably developed his interdisciplinary ideas, which, influenced in various ways by the European cultural climate, brought him into the field of global tectonics. He conceived a theory about the expansion of the Earth based on the nature of the gravity field. In 1933, the theory was published in his classic work 'Vom wachsenden Erdball'. Upon his return in Germany he performed various types of research at the School of Engineering, then that of Geology and Paleontology at the Technical University of Berlin. He was also briefly involved as editor of the scientific publications at the Technical University of Berlin, where he made a contribution towards saving the book collection as the war ended. During the years spent in Berlin, he continued to refine his elegant version of the theory of Earth’s expansion publishing articles and books on this subject up to the last years in his life. The importance of Hilgenberg lies in the fact that he marks the beginning of the integration of various scientific disciplines from Physics to Paleontology and Paleomagnetism, in support of a universal tectonic theory, and that he made paleogeographic reconstructions on globes with smaller radii than the present one. All those who have worked or are working with one of the versions of expansion tectonics owe him enormous gratitude for his inspiration and for the scientific and moral lesson of fifty years spent in unflagging defence of his ideas. The material gathered and kindly made available by his daughter Helge has been indispensable for this recalling.
    Description: Published
    Description: 25-41
    Description: open
    Keywords: Tectonic theories ; expanding Earth ; O.C. Hilgenberg ; Berlin ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 7
    Publication Date: 2017-04-04
    Description: Roberto Mantovani, violinist and scientist,born in Parma on March 25, 1854. He was part of an orches-tral team reaching the volcanic Réunion Island in 1878. During his stay on the island, Mantovani had the occasion of observing the huge volcanic fractures on the Indian ocean shore near the town of Saint Denis. He argued that, on a global scale, all the continents might have undergone the same disjunction processes as the volcanic flanks. The global fractures are today the oceans. After several years from his observations, Mantovani published his idea in 1889 in the Bulletin of the Societé des Sciences et des Arts of Saint Denis, where the Italian established his family and became Consul of Italy. After an economic crisis and an epidemic plague in the Réunion Island, Roberto Mantovani left his post as Consul to go and live in San Servan, near the port of Saint Malo, in northern France, where he continued his activity as violinist, managing a school of music. As a scientist, he gave public conferences on the idea of planetary expansion. Mantovani was not a mere precursor of the continental drift idea: instead, Mantovani’s ideas on Earth expansion were more general compared to those of Wegener who was not taking into account the possibility of variation of the Earth’s radius. Roberto Mantovani, violinist and scientist, was part of an orches-tral team reaching the volcanic Réunion Island in 1878. During his stay on the island, Mantovani had the occasion of observing the huge volcanic fractures on the Indian ocean shore near the town of Saint Denis. He argued that, on a global scale, all the continents might have undergone the same disjunction processes as the volcanic flanks. The global fractures are today the oceans. After several years from his observations, Mantovani published his idea in 1889 in the Bulletin of the Societé des Sciences et des Arts of Saint Denis, where the Italian established his family and became Consul of Italy. After an economic crisis and an epidemic plague in the Réunion Island, Roberto Mantovani left his post as Consul to go and live in San Servan, near the port of Saint Malo, in northern France, where he continued his activity as violinist, managing a school of music. As a scientist, he gave public conferences on the idea of planetary expansion. His more famous paper, quoted later by Wegener, was published in 1909, in a popular magazine 'Je m’instruis'. The paper contains the first suggestive mapping of the breakup of the Pangea continent based on geological arguments. The great novelty in the 1909 paper was the mapping of the Pacific view: dotted lines were drown between pairs of geographical points which once were in contact while today are separated by the huge extension of the Pacific basin. The idea was that the corresponding points were in contact before the expansion of the Earth. The enlarging of the huge fractures formed all oceans. We had to wait the sixties to find the same kind of lines in the Indian and Atlantic oceans in plate tectonics. According to plate tectonics this is not true for the Pacific Ocean, because in this case the plate movement is inverse and the ocean tends towards closing. The 1909 Pacific map was forgotten, and only Mantovani’s Pangea representation is reproduced today in some books dealing with the history of science.
    Description: Published
    Description: 71-74
    Description: open
    Keywords: Hystory of global tectonic theories ; Expanding Earth ; R. Mantovani ; Parma ; Réunion ; San Malò, Paris ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
    Format: 720454 bytes
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  • 8
    Publication Date: 2017-04-04
    Description: The tectonic deformation of the Lipari-Vulcano complex, one of the most important active volcanic areas of Mediterranean region, is studied here through the analysis of ten years (1996-2006) of GPS data from both 3 permanent and 13 non-permanent stations. This area can be considered crucial for the understanding of the Eurasia-Africa plates interaction in the Mediterranean area, and, in general, this work emphasize a methodological approach, already applied in other areas worldwide (e.g. Shen et al., 1996, El-Fiki and Kato, 1999) where geodetic data and strain parameters maps of critical areas can help to improve our understanding of their geodynamical aspects. In this framework, this study is aimed at providing a kinematic deformation model on the basis of the dense geodetically estimated velocities of the Lipari-Vulcano complex. In particular, the observed deformation pattern can be described by a mix between 1) the main N-S regional compression and 2) a NNE-SSW compression with a small right-lateral strike slip component acting along a tectonic structure N°40W trending located between the two islands. This pattern was inspected through a simplified synthetic model.
    Description: This research has benefited from funding provided by the Italian Presidenza del Consiglio dei Ministri – Dipartimento della Protezione Civile (DPC).
    Description: Published
    Description: 370–377
    Description: 1.9. TTC - Rete GPS nazionale
    Description: JCR Journal
    Description: reserved
    Keywords: GPS ; Aeolian Islands ; strain ; modelling ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2012-02-03
    Description: Since 2002, between Catanzaro and Vibo Valentia (Calabria), has been set up a new high resolution GPS network. The aim of this network is to record the interseismic and co-seismic deformations of this active region which experienced destructive earthquakes but it is not yet occupied by a GPS geodetic network.
    Description: Published
    Description: Reggio Calabria
    Description: 3.2. Tettonica attiva
    Description: open
    Keywords: GPS, Calabria, Stretto di Messina ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 10
    Publication Date: 2017-04-04
    Description: Il terremoto del 1908 che ha distrutto le città di Reggio Calabria e Messina costituisce il primo esempio in cui, attraverso l’utilizzo di dati geodetici, è stato possibile ricostruire il campo di deformazione verticale collegato al catastrofico evento. In questo lavoro vengono riassunti i principali risultati della ricerca incentrata sulla caratterizzazione cinematica dell’area dello Stretto di Messina e vengono presentati i primi risultati della rete misurata con modalità GPS nel corso del 2001 e del 2003 nella stessa area. Questi risultati confermano l’importanza dell’approfondimento delle attività di monitoraggio geodetico tra il complesso peloritano calabro e quello siciliano, anche allo scopo di chiarire le numerose ambiguità riscontrate, in questi anni, nella definizione delle strutture che hanno originato il terremoto del 1908.
    Description: Published
    Description: 1-18
    Description: open
    Keywords: GPS ; 04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations ; 04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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