Relevant bibliographies by topics / Volcanis islands

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Volcanis islands'

Author: Grafiati
Published: 7 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Volcanis islands"

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Smellie, John L. "Chapter 3.2a Bransfield Strait and James Ross Island: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 227–84. http://dx.doi.org/10.1144/m55-2018-58.

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AbstractFollowing more than 25 years of exploration and research since the last regional appraisal, the number of known subaerially exposed volcanoes in the northern Antarctic Peninsula region has more than trebled, from less than 15 to more than 50, and that total must be increased at least three-fold if seamounts in Bransfield Strait are included. Several volcanoes remain unvisited and there are relatively few detailed studies. The region includes Deception Island, the most prolific active volcano in Antarctica, and Mount Haddington, the largest volcano in Antarctica. The tectonic environmen
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McDOUGALL, IAN. "Age of volcanism and its migration in the Samoa Islands." Geological Magazine 147, no. 5 (2010): 705–17. http://dx.doi.org/10.1017/s0016756810000038.

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AbstractPotassium–argon (K–Ar) ages on whole rock samples have been measured on lavas from the subaerial Samoa Islands, which form a broadly linear volcanic chain that extends from the ESE to the WNW for about 360 km. The Manu'a Islands near the southeast limit of the chain exhibit youthful ages, with most <0.4 Ma, in keeping with the geological observations. Tutuila consists of several volcanoes, and previous work yielded a mean K–Ar age of 1.26 ± 0.15 Ma for the shield-building volcanism. Upolu, to the WNW of Tutuila, gives a mean age of 2.15 ± 0.35 Ma for the shield-building phase, repre
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Haldar, D., T. Laskar, P. C. Bandyopadhyay, N. K. Sarkar, and J. K. Biswas. "Volcanic eruption of the Barren Island Volcano, Andaman Sea." Journal Geological Society of India 39, no. 5 (1992): 411–19. http://dx.doi.org/10.17491/jgsi/1992/390506.

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Abstract Geotectonically the Barren and Narcondum islands lie on the Neogene Inner volcanic are, which proceeds from the recent volcanoes of Central Burma in the North to the Miocene to Recent volcanoes of Indonesia in the SE and are believed to have evolved as a result of eastward subduction of the Indian Ocean lithosphere below the SE Asian plate. The Barren island volcano is characterised by resurgent volcanism; so far, three distinct volcanic episodes have been recorded. An initially submarine volcanism, possibly taking place in late to Post-Pleistocene time formed a giant volcanic cone re
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Simurda, Christine, Lori A. Magruder, Jonathan Markel, James B. Garvin, and Daniel A. Slayback. "ICESat-2 Applications for Investigating Emerging Volcanoes." Geosciences 12, no. 1 (2022): 40. http://dx.doi.org/10.3390/geosciences12010040.

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Submarine volcanism in shallow waters (<100 m), particularly in remote settings, is difficult to monitor quantitatively and, in the rare formation of islands, it is challenging to understand the rapid-paced erosion. However, these newly erupted volcanic islands become observable to airborne and/or satellite remote sensing instruments. NASA’s ICESat-2 satellite laser altimeter, combined with visible imagery (optical and microwave), provide a novel method of evaluating the elevation characteristics of newly emerged volcanoes and their subaerial eruption products. Niijima Fukutoku-Okanoba (NFO
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Leat, Philip T., and Teal R. Riley. "Chapter 3.1a Antarctic Peninsula and South Shetland Islands: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 185–212. http://dx.doi.org/10.1144/m55-2018-52.

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AbstractThe voluminous continental margin volcanic arc of the Antarctic Peninsula is one of the major tectonic features of West Antarctica. It extends from the Trinity Peninsula and the South Shetland Islands in the north to Alexander Island and Palmer Land in the south, a distance ofc.1300 km, and was related to east-directed subduction beneath the continental margin. Thicknesses of exposed volcanic rocks are up toc.1.5 km, and the terrain is highly dissected by erosion and heavily glacierized. The arc was active from Late Jurassic or Early Cretaceous times until the Early Miocene, a period o
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Griffiths, Chris J., and Richard D. J. Oglethorpe. "The stratigraphy and geochronology of Adelaide Island." Antarctic Science 10, no. 4 (1998): 462–75. http://dx.doi.org/10.1017/s095410209800056x.

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The Mesozoic-Cenozoic volcanic arc of the Antarctic Peninsula is represented on Adelaide Island by a sedimentary and volcanic succession intruded by plutons. 40Ar-39 Ar step-heating age spectra have been obtained from volcanic rocks and hornblende separates from sedimentary clasts of plutonic origin. These spectra show evidence for some argon loss, but, in general, have plateau ages which are consistent with the mapped stratigraphy and with other geochronological controls, suggesting that they approximate to original ages. As a result the following events in the evolution of Adelaide Island ca
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Geyer, A., D. Pedrazzi, J. Almendros, et al. "Chapter 7.1 Deception Island." Geological Society, London, Memoirs 55, no. 1 (2021): 667–93. http://dx.doi.org/10.1144/m55-2018-56.

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AbstractDeception Island (South Shetland Islands) is one of the most active volcanoes in Antarctica, with more than 15 explosive eruptive events registered over the past two centuries. Recent eruptions (1967, 1969 and 1970) and volcanic unrest episodes in 1992, 1999 and 2014–15 demonstrate that the occurrence of future volcanic activity is a valid and pressing concern for scientists, logistic personnel and tourists that are visiting or are working on or near the island. Over the last few decades, intense research activity has been carried out on Deception Island to decipher the origin and evol
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Dimitrov, Dimitar, and Banush Banushev. "Geological-geomorphological characteristics and petrographical composition of the St. Anastasia Island." Acta Scientifica Naturalis 8, no. 1 (2021): 118–25. http://dx.doi.org/10.2478/asn-2021-0010.

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Abstract St. Anastasia Island is one of the symbols of the cultural and historical heritage of the Republic of Bulgaria. This raises the need for the study of risky oceanographic factors, climatic phenomena, risky geological processes as well as detailed petrographical characteristics of the Upper Cretaceous volcanic rocks forming the islands. The results of the petrographical study show that the island was built by Alkali feldspar trachytes. The volcanics from St. Anastasia Island shows a close petrochemical similarity to the volcanics from Alatepenski paleovolcano belonging to the “Periphera
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Mutaqin, Bachtiar W., Muh Aris Marfai, Danang Sri Hadmoko, et al. "Geomorphology of the small island of Tidore and Hiri (North Maluku, Indonesia)." E3S Web of Conferences 325 (2021): 03012. http://dx.doi.org/10.1051/e3sconf/202132503012.

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Tidore and Hiri Islands in North Maluku Province is the result of a complex tectonic setting. In contrast with Ternate Island and its well-known volcano, Gamalama volcano, there is still a lack of research about volcanic information or volcanic landform in Tidore and Hiri Islands. Even though the two islands also have volcanoes, i.e., Hiri and Tidore/Kiematubu volcano. This study aims to provide geomorphological information, especially in Tidore and Hiri Islands, since this information is hard to find whereas it is very important to disaster mitigation and landuse planning. We used remote sens
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Patrick, Matthew R., and John L. Smellie. "Synthesis A spaceborne inventory of volcanic activity in Antarctica and southern oceans, 2000–10." Antarctic Science 25, no. 4 (2013): 475–500. http://dx.doi.org/10.1017/s0954102013000436.

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AbstractOf the more than twenty historically active volcanoes in Antarctica and the sub-Antarctic region only two, to our knowledge, host any ground-based monitoring instruments. Moreover, because of their remoteness, most of the volcanoes are seldom visited, thus relegating the monitoring of volcanism in this region almost entirely to satellites. In this study, high temporal resolution satellite data from the Hawaii Institute of Geophysics and Planetology's MODVOLC system using MODIS (Moderate Resolution Imaging Spectroradiometer) are complemented with high spatial resolution data (ASTER, or
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Dissertations / Theses on the topic "Volcanis islands"

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García, Pérez Olaya. "The explosive volcanism of Teide-Pico Viejo volcanic complex, Canary Island." Doctoral thesis, Universitat de Barcelona, 2013. http://hdl.handle.net/10803/130923.

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The explosive events in Teide Pico Viejo (TPV) complex in Tenerife Island (Spain) have traditionally been restricted to the subplinian eruption of Montaña Blanca, which occurred about 2000 years ago. A recent revision of the stratigraphy of TPV shows that phonolitic explosive activity has been significant during the Holocene, with several distinct episodes related to eruptions ranging from Strombolian to sub-plinian. Using field, mineralogical and geochemical stratigraphic correlations, we have identified 11 phonolitic explosive eruptions related to the satellite domes present all around TPV
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Maund, J. G. "The volcanic geology, petrology and geochemistry of Caldeira volcano, Graciosa, Azores, and its bearing on contemporaneous felsic-mafic oceanic island volcanism." Thesis, University of Reading, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.370121.

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Letham-Brake, Mark. "Geological constraints on fluid flow at Whakaari volcano (White Island)." Thesis, University of Canterbury. Department of Geological Sciences, 2013. http://hdl.handle.net/10092/8728.

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This study assesses the geological constraints on fluid flow within the main crater of Whakaari volcano (White Island) which is located in the Bay of Plenty, New Zealand. A review of the volcanological and morphological history, field mapping, and permeability experiments were used to propose a model for single-state (gas or liquid water) fluid flow in the volcano. Three structural scales were of most importance: (a) the elongate main crater (1.2 km by 0.5 km); which contains (b) three subcraters (~300-500 m in diameter); and (c) >14 historic eruption craters and crater complexes (30-300 m in
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Sigmarsson, Olgeir. "Geochimie isotopique du thorium des iles oceaniques (islande, canaries) et des zones de subduction (indonesie et chili)." Clermont-Ferrand 2, 1990. http://www.theses.fr/1990CLF21284.

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La geochimie isotopique du thorium, associee a celle de l'o, du sr et du nd et a des mesures precises des teneurs en u et th dans les roches volcaniques actuelles, permet d'etudier la genese et l'evolution des magmas dans plusieurs contextes geodynamiques. Les resultats essentiels de ce travail sont les suivants: 1) la mise en evidence, en islande, de l'importance des phenomenes de contamination crustale: l'assimilation de croute profonde se produit aussi bien dans les zones de rift (produisant des tholeiites a quartz normatif a partir de tholeiites a olivine), que dans la zone laterale sud de
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Belien, Isolde L. M. B. (Leo Maria Beatrijs) 1985. "Gas Migration Through Crystal-Rich Mafic Volcanic Systems and Application to Stromboli Volcano, Aeolian Islands, Italy." Thesis, University of Oregon, 2011. http://hdl.handle.net/1794/12107.

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xvii, 171 p. : ill. (some col.)<br>Crystals influence the migration of gas through magma. At low concentrations, they increase the bulk fluid properties, especially viscosity. At concentrations close to maximum packing, crystals form a rigid framework and magma cannot erupt. However, erupted pyroclasts with crystal contents close to the packing concentration are common at mafic volcanoes that exhibit Strombolian behavior. In this dissertation, I study the influence of solid particles on gas migration. I apply my results to Stromboli volcano, Italy, type locality of the normal Strombolian erupt
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Hevia, Cruz Francisco. "Climatic and landscape evolution of the Azores over the past million years." Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ035.

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L'évolution des îles volcaniques résulte d'interactions complexes entre croissance des volcans et processus de destruction (éruptions explosives, glissements de terrain, érosion fluviale, altération). Les changements climatiques peuvent influencer ces processus sur des échelles variées. A l’échelle événementielle, des précipitations intenses peuvent engendrer des épisodes érosifs extrêmes. Sur le long-terme, des variations des taux d'altération, sensibles aux précipitations et à la température, peuvent impacter la fertilité des sols et le cycle global du carbone.Les îles volcaniques des Açores
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Dávila, Harris Pablo. "Explosive ocean-island volcanism : the 1.8–0.7 Ma explosive eruption history of Cañadas volcano recorded by the pyroclastic successions around Adeje and Abona, southern Tenerife, Canary Islands." Thesis, University of Leicester, 2009. http://hdl.handle.net/2381/9931.

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The 1.8 to 0.7 Ma explosive eruption history of Las Cañadas volcano is recorded by the pyroclastic stratigraphy of southern Tenerife. A large pyroclastic apron is well exposed in the Bandas del Sur. It is divided into two regions, Adeje (southwest) and Abona (southeast). The lower stratigraphy of both successions is described here for the first time, and is divided into soil-bound eruption-units. The lithofacies record repeated phonolite explosive eruptions involving Plinian eruption columns and ignimbrite emplacement, with sedimentary reworking and soilification during repose intervals. The
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Grunewald, Uwe. "Measuring and modelling of volcanic pollutants from White Island and Ruapehu volcanoes assessment of related hazard in the North Island /." Thesis, University of Canterbury. Geological Sciences, 2007. http://hdl.handle.net/10092/1428.

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White Island and Ruapehu are currently the most active volcanoes in New Zealand. During non-eruptive periods, intense quiescent degassing through fumaroles can occur. The current project studies the quiescent degassing plumes, including aerosol sampling on White Island and dispersion modelling of SO₂ and PM₁₀ from White Island and Ruapehu volcanoes. Aerosol sampling from fumaroles at the crater floor on White Island volcano was carried out on 9 February and 6 April 2005. The exposed filters were analysed for various anions and cations and the particle mass concentration and molar concentration
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Meletlidis, Tsiogalos Stavros. "Eruptive dynamics and petrological evolution of recent volcanism on the El Hierro Island : Implications for volcanic hazard assessment." Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/461582.

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The Canarian archipelago, extends over approximately 500 km in total along the passive continental margin off NW Africa, comprises seven major and four minor islands, and it is part of the so called Macaronesia region, together with the archipelagos of Azores, Madeira, Salvajes and Cape Verde. Within the oceanic geodynamic context, the Canary archipelago is located on oceanic crust of the big African plate, specifically upon the passive continental margin, with thickness exceeding 20 km. It is a good example of oceanic intraplate alkaline volcanism. According the radioisotopic data available
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Palmiotto, Camilla <1985&gt. "Transform Tectonics and Non-Volcanic Oceanic Islands." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2014. http://amsdottorato.unibo.it/6472/1/Palmiotto_Camilla_Tesi.pdf.

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Oceanic islands can be divided, according to their origin, in volcanic and tectonic. Volcanic islands are due to excess volcanism. Tectonic islands are mainly formed due to vertical tectonic motions of blocks of oceanic lithosphere along transverse ridges flanking transform faults at slow and ultraslow mid-ocean ridges. Vertical tectonic motions are due to a reorganization of the geometry of the transform plate boundary, with the transition from a transcurrent tectonics to a transtensive and/or transpressive tectonics, with the formation of the transverse ridges. Tectonic islands can be locate
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Books on the topic "Volcanis islands"

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Greensmith, J. T. Lanzarote, Canary Islands. Geologists' Association, 2000.

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Luigina, Vezzoli, ed. Island of Ischia. Consiglio nazionale delle ricerche, 1988.

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Tagliaferro, Linda. How does a volcano become an island? Raintree, 2010.

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K, Sako Maurice, Geological Survey (U.S.), and Northern Mariana Islands. Disaster Control Office, eds. Volcanic investigations in the Commonwealth of the Northern Mariana Islands, April to May 1994. U.S. Geological Survey, 1995.

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Sigurður, Steinþórsson, ed. Volcano island. Forlagið, 2010.

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D, Ayres L., and Geological Association of Canada, eds. Pyroclastic volcanism and deposits of cenozoic intermediate to felsicvolcanic islands: With implications for precambrian greenstone-belt volcanoes. U.M.I., 1987.

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Gill, Robin. Tenerife Canary Islands. 2nd ed. The Geologists' Association, 2003.

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Miyakemura(tōkyōto). Volcanic eruptions on Miyakejima Island in 2000: The year 2000 record of disastrous eruptions on Miyakejima Island/overview : living with volcanoes. Miyake Village, 2008.

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Geological Survey (U.S.), ed. EDM station descriptions for Mauna Kea, Mauna Loa, and Hualalai Island of Hawaii. U.S. Dept. of the Interior, Geological Survey, 1987.

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Geological Survey (U.S.), ed. EDM station descriptions for Mauna Kea, Mauna Loa, and Hualalai Island of Hawaii. U.S. Dept. of the Interior, Geological Survey, 1987.

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Book chapters on the topic "Volcanis islands"

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Hernández Ramos, William, Victor Ortega, Monika Przeor, Nemesio M. Pérez, and Pedro A. Hernández. "Submarine Eruption of El Hierro, Geotourism and Geoparks." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_11.

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AbstractThe year 2011 remained in the memory of the residents of the island of El Hierro (Canary Island, Spain) because of the volcanic episode that originated in its vicinity. From the beginning of the first precursory signs in July 2011, the island’s inhabitants reminded that the islands’ geological origin is volcanic and, what are the consequent threats of living on them. The eruption, however, has occurred in the marine realm leaving the only threats to the population, strong earthquakes, and diffuse emission of volcanic gases. The Tagoro eruption has not caused any loss of human life, how
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Dóniz-Páez, Javier, and Rafael Becerra-Ramírez. "Geomorphosites of El Hierro UNESCO Global Geopark (Canary Islands, Spain): Promotion of Georoutes for Volcanic Tourism." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_8.

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AbstractGeotourism is a relatively recent concept and a novel kind of tourism, which has acquired a significant boom in the last decades, associated with the creation and consolidation of the UNESCO global geoparks network. There are two approaches to geotourism, one geological and the other geographical, much more global and inclusive of the elements of the natural and cultural heritage. In this chapter, we have chosen to use the geographical approach of geotourism, to apply it to the El Hierro global geopark and diversify the island's tourism, traditionally focused on diving and hiking, thro
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Guillén-Martín, Cayetano, and Carmen Romero. "Volcanic Geomorphology in El Hierro Global Geopark." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_3.

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AbstractFew oceanic islands express their geomorphological history in such a marked way as the island of El Hierro. Indeed, on El Hierro, its geomorphology goes hand in hand with the evolution of its insular geology. In fact, seventy percent of places of geological interest in El Hierro’s Geopark have geomorphological features as their main or secondary interest, which is indicative of the importance of geomorphology in the configuration of the island’s relief. However, there are few studies that have addressed the processes or features of the island’s geomorphology. In this study, the first g
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Gill, Jim. "Island Arc Volcanism, Volcanic Arcs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_20-2.

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Gill, Jim. "Island Arc Volcanism, Volcanic Arcs." In Encyclopedia of Marine Geosciences. Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-94-007-6238-1_20.

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Schmincke, Hans-Ulrich. "Seamounts and Volcanic Islands." In Volcanism. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-642-18952-4_6.

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De la Cruz-Modino, Raquel, Cristina Piñeiro-Corbeira, Shankar Aswani, et al. "Cultural Seascapes in the ‘Sea of Calms’ and La Restinga Coast." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_10.

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AbstractEl Hierro has been characterized by the balance between human development and environmental sustainability. The island was historically far from the mass tourism developments dominant on the other Canary Islands. Tourism accommodations in El Hierro are few compared to more developed coastal areas in the Archipelago, and recreational activities are mainly linked to cultural and natural sites and resources. This chapter focuses on La Restinga fishing village and its coasts, where the ‘Sea of Calms’ and one multiple-use Marine Reserve (MR) are located, both of which became popular over th
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Schmieder, Robert William. "Volcanic features." In Heard Island. Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-20343-5_12.

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Casillas Ruiz, Ramón, Yurena Pérez Candelario, and Cristina Ferro Fernández. "Geoheritage Inventory of the El Hierro UNESCO Global Geopark." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_4.

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AbstractIn 2014 the Island of El Hierro (Canary Islands) was declared a Geopark of the Unesco network, thus becoming the first UNESCO geopark of the Canary Islands. The geological history of the Island of El Hierro can be understood through the visit of 61 geosites, which are representative of the growth and destruction of an oceanic Island in an intraplate environment. The geological heritage represented by these geosites has as foremost exponents those related to the formation of mega-landslides and the formation of extensive fields of pahoehoe lava-flows related to the historical or prehist
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Beltrán-Yanes, Esther, and Isabel Esquivel-Sigut. "The Vegetation Landscapes of a Oceanic Recent Volcanic Island." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_5.

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AbstractThe aim of this chapter is to characterise the vegetation landscapes of El Hierro’s Geopark, highlighting the important role played by the island’s volcanic morphology in the richness and diversity of its landscapes. To this end, some of its most representative vegetation landscapes have been selected at various spatial scales, recognising their main discontinuities and internal organisation, and identifying the integrated combinations of the geographical factors that determine them have been identified, with special interest in the volcanic morphostructural conditioning factors. This
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Conference papers on the topic "Volcanis islands"

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Moody, Kenneth J. "Corrosion Protection of H-3 Highway Facilities Oahu, Hawaii." In CORROSION 1991. NACE International, 1991. https://doi.org/10.5006/c1991-91538.

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Abstract One final portion of the Federal Highway System involves a 10.7-mile (17.22 kilometer) section on the Island of Oahu in Hawaii. The H-3 Highway connects Honolulu and the Haiku side of the island and involves approximately 5,200 feet (1,585 meters) of double tunnel through the volcanic soils of the Koolau Mountain Range. Portions of one elevated section traverses the Omega VLF Transmitter Station at Haiku. The project presented a unique design challenge due to the combination of marine, combustion exhaust, volcanic soil, and interference environments. This paper discusses the investiga
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DUEÑAS-TOVAR, JAIRO, FERNANDO MORANTE-CARBALLO, EMELY LOOR-MEDRANDA, MARÍA JAYA-MONTALVO, and PAÚL CARRIÓN-MERO. "ENVIRONMENTAL ASSESSMENT OF QUARRYING IN VOLCANIC ISLANDS: THE CASE OF ‘CERRO QUEMADO’, GALAPAGOS, ECUADOR." In SDP 2024. WIT Press, 2024. http://dx.doi.org/10.2495/sdp240611.

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Mohamed, E. Syed, and M. Yasmin Regina. "Modelling of Tsunami Wave Generated by Volcanic EruptionUsing Impulsive Disturbance for 2022, Tonga Island Tsunami." In 2025 8th International Conference on Data Science and Machine Learning Applications (CDMA). IEEE, 2025. https://doi.org/10.1109/cdma61895.2025.00007.

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Esposito, Paolo, Giuseppe Ferri, and Vincenzo Stornelli. "Monitoring Systems for a Volcanic Area Subjected to Rockfall: Case Study in the Island of Ischia." In 2024 11th International Conference on Electrical, Electronic and Computing Engineering (IcETRAN). IEEE, 2024. http://dx.doi.org/10.1109/icetran62308.2024.10645126.

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Waibel, Al, and Adam Jones. "Near-Offshore Oceanic Geothermal Resources Developed from On-Shore Directional Drilling." In Offshore Technology Conference. OTC, 2024. http://dx.doi.org/10.4043/35417-ms.

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New opportunities have emerged for the application of oilfield technologies transfer, such as directional drilling, to utilize base-load renewable energy. Development of geothermal resources have largely been restricted to on-shore sites, yet a major category of untapped geothermal development prospects are near-shore resources. Development of near-shore geothermal resources can provide renewable base-load electrical power options to areas that are now served by non-renewable power generation which can supply domestic, commercial, or industrial land-based and marine use. It may also support em
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Septama, E. "Java Volcanic Arc, what lies beneath?" In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-257.

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Java Island is an active volcanic arc that resides in the southwestern - southern boundary of Sundaland edges. The volcanic arc consists of several volcanism episodes, with a relatively younging trend northward (Late Oligocene to Pleistocene), following the Indo-Australian plates inward migration. In contrast to the prolific neighboring Northwest and Northeast Java Basins in the Northern edges of Java Island; the basin reconstruction and development in the East-West trending depression in median ranges of Java (from Bogor to Kendeng Troughs) are overlooked and lays bare the challenge to the se
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Feng, Jianyun, Xiaorui Yun, Jun Luo, et al. "Structural Deformation Characteristics and Geological Significance of the Mesoproterozoic Augen Granite Gneiss in Hainan Island, China." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0303.

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ABSTRACT: The oldest basement rock discovered so far in Hainan Island is the augen granite gneiss of the Gezhencun Formation in the Middle Proterozoic era. By studying its petrology and geometry, the stress and temperature pressure conditions during rock formation can be restored and reconstructed, which is of great significance for reconstructing the early tectonic framework and geological environment of Hainan Island. Field geological, geochemical, and tectonic geological studies have shown that the upper part of the Gezhencun Formation is mainly composed of biotite plagioclase gneiss or mix
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Иванов, А. Н. "TO THE QUESTION OF POLYSTRUCTURAL ORGANISATION OF LANDSCAPE SPACE." In Геосистемы Северо-Восточной Азии. Crossref, 2021. http://dx.doi.org/10.35735/tig.2021.61.88.005.

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Обсуждается понятие полиструктурности ландшафтного пространства. Объект исследований – остров Матуа с активным вулканом, отсутствием поверхностного стока и широким развитием селевых и лавинных комплексов. Разработана ландшафтная карта, основанная на структурно-генетических принципах, внутри островного ландшафта выделены три географические местности. Предложена модель нуклеарной системы с ядром в виде кратера вулкана, по степени влияния вулкана на природные комплексы выделены три зоны. В составе парадинамических геосистем, связанных однонаправленными потоками вещества и энергии, выделены и проа
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Asgary, Ali. "Holovulcano: Augmented Reality simulation of volcanic eruptions." In The 8th International Defence and Homeland Security Simulation Workshop. CAL-TEK srl, 2018. http://dx.doi.org/10.46354/i3m.2018.dhss.007.

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"This paper describes an interactive holographic simulation of volcanic eruption. The aim of the project is to use Augmented Reality (AR) technology to visualize different volcanic eruptions for public education, emergency training, and preparedness planning purposes. To achieve this goal, a 3D model of the entire Vulcano Island in Italy has been created using real elevation data. Unity game engine and Microsoft Visual Studio have been used to develop HoloVulcano augmented/virtual reality simulation application. The current version of HoloVulcano simulates normal and unrest situations, single
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Yanis, Muhammad, Zaini Nasrullah, Muhammad Isa, Ananda Riski, Muzakir Zainal, and Andri Yadi Paembonan. "Optimizing the Gravity Data and Geological Observation for Mapping the Local Fault around the Jaboi Volcano." In The 5th International Conference on Science and Technology Applications. Trans Tech Publications Ltd, 2024. http://dx.doi.org/10.4028/p-mezta6.

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Geothermal is a very expensive investment industry. Therefore, it is necessary to map a geological structure in the sub-surface, i.e., faults, and rock formations that control volcanic hydrothermal systems to reduce investment risk in the exploitation of geothermal. On the other hand, the hydrothermal system aims for flow paths connecting reservoir wells for fluid production. The Jaboi Volcano, with an estimated 80 MWe located on Weh Island, Indonesia, has been planned by the government to develop electrical energy, where the excess energy will be exported to Banda Aceh via undersea cables. We
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Reports on the topic "Volcanis islands"

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Tweet, Justin S., Vincent L. Santucci, Kenneth Convery, Jonathan Hoffman, and Laura Kirn. Channel Islands National Park: Paleontological resource inventory (public version). National Park Service, 2020. http://dx.doi.org/10.36967/nrr-2278664.

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Channel Island National Park (CHIS), incorporating five islands off the coast of southern California (Anacapa Island, San Miguel Island, Santa Barbara Island, Santa Cruz Island, and Santa Rosa Island), has an outstanding paleontological record. The park has significant fossils dating from the Late Cretaceous to the Holocene, representing organisms of the sea, the land, and the air. Highlights include: the famous pygmy mammoths that inhabited the conjoined northern islands during the late Pleistocene; the best fossil avifauna of any National Park Service (NPS) unit; intertwined paleontological
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Haggart, J. W., L. T. Dafoe, K. M. Bell, et al. Historical development of a litho- and biostratigraphic framework for onshore Cretaceous-Paleocene deposits along western Baffin Bay. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321828.

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Cretaceous-Paleogene strata along the eastern coast of Baffin Island, on Bylot Island, and on associated islands north of Cape Dyer, have been known since the early days of exploration of Baffin Bay in the mid-nineteenth century. Studies of these strata in the 1970s-1990s established their clastic nature and revealed details of their stratigraphy, ages, and depositional settings. Onshore strata in the Cape Dyer area accumulated in close association with volcanic deposits related to late-stage rifting in the Late Cretaceous to Early Paleocene that eventually formed Baffin Bay. In contrast, depo
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Taylor, Oliver-Denzil, and Joseph Dunbar. Seismic analysis for Pohnpei Island, Federated States of Micronesia. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/49432.

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The purpose of this study was to determine the seismic hazards that can affect Pohnpei Island and provide estimates of the ground motion parameters. The primary parameters are peak ground acceleration (PGA), pseudo-spectral acceleration (PSA), and velocity. These values were determined both probabilistically and deterministically to illustrate the overall seismic hazard to Pohnpei Island. A review was conducted of the technical literature to determine geologic studies that have been performed for characterization of the island’s volcanism, stratigraphy, and tectonism. This report is a desktop
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Peterson, T. D., N. Wodicka, S J Pehrsson, et al. The Rae Province at 2.6 Ga: a sanukitoid storm on the Canadian Shield, Nunavut. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332505.

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Between 2.62 and 2.58 Ga, Rae Province was intruded from Lake Athabasca to Melville Peninsula (more than 1700 km) by mafic to felsic plutons (Snow Island Suite), and overlain by volcanic rocks that are now mostly preserved beneath Paleoproterozoic basins. The Snow Island Suite was preceded by offshore arc volcanism and possible back-arc basin activity, with a U-Pb age peak at 2.635 Ga (Marjorie peak). About 50% of the Snow Island Suite is an infracrustal granitoid with K-enriched and tonalitic subtypes; the remainder lies on a sanukitoid spectrum. The sanukitoidal rocks are dominantly orthopyr
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Narvaez, Liliana, Joerg Szarzynski, and Zita Sebesvari. Technical Report: Tonga volcano eruption. United Nations University - Institute for Environment and Human Security (UNU-EHS), 2022. http://dx.doi.org/10.53324/ysxa5862.

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On 15 January 2022, the Hunga-Tonga-Hunga-Ha'apai volcano eruption was felt across the Pacific Ocean and beyond, releasing energy equivalent to hundreds of Hiroshima nuclear explosions and creating supersonic air pressure waves that were observed from space. In the archipelago Kingdom of Tonga, the ashfall, tsunami and shock waves caused widespread devastation on several islands. The only fibre-optic cable that connects the islands with the rest of the world was severely damaged, leaving the entire country offline for more than three weeks. The case the Hunga Tonga-Hunga Ha’apai volcano erupti
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Berndt, Christian. RV SONNE Fahrtbericht / Cruise Report SO277 OMAX: Offshore Malta Aquifer Exploration, Emden (Germany) – Emden (Germany), 14.08. – 03.10.2020. GEOMAR Helmholtz Centre for Ocean Research Kiel, 2021. http://dx.doi.org/10.3289/geomar_rep_ns_57_20.

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SO277 OMAX served two scientific projects. The objectives of the first project, SMART, were to develop multi-disciplinary methodologies to detect, quantify, and model offshore groundwater reservoirs in regions dominated by carbonate geology such as the Mediterranean Sea. To this end we acquired controlled-source electromagnetic, seismic, hydroacoustic, geochemical, seafloor imagery data off Malta. Preliminary evaluation of the geophysical data show that there are resisitivity anomalies that may represent offshore freshwater aquifers. The absence of evidence for offshore springs means that thes
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Nye, C. J., W. E. Scott, O. K. Neill, C. F. Waythomas, C. E. Cameron, and A. T. Calvert. Geology of Kasatochi volcano, Aleutian Islands, Alaska. Alaska Division of Geological & Geophysical Surveys, 2017. http://dx.doi.org/10.14509/29718.

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Saumur, B. M., M. C. Williamson, and C. A. Evenchick. Volcanic-intrusive complexes of western Axel Heiberg Island. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/297374.

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Williamson, M. C., B. M. Saumur, and C. A. Evenchick. HALIP volcanic-intrusive complexes, Axel Heiberg Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297491.

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Williamson, M. C., B. M. Saumur, and C. A. Evenchick. HALIP volcanic-intrusive complexes, Axel Heiberg Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297784.

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