Relevant bibliographies by topics / Volcanoes

Contents

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

Academic literature on the topic 'Volcanoes'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Volcanoes"

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Espinasa-Pereña, Ramón. "Monitoring volcanoes in Mexico." Volcanica 4, S1 (2021): 223–46. http://dx.doi.org/10.30909/vol.04.s1.223246.

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Mexico has at least 46 volcanic centers (including monogenetic volcanic fields) that are considered active or potentially active. Due to the federal governance of the country, the Centro Nacional de Prevención de Desastres (CENAPRED) is the entity responsible for monitoring natural hazards. Individual Mexican states also monitor active volcanoes within their territoryand through local universities. Specific observatories exist for Colima, Citlaltépetl (Pico de Orizaba), San Martín Tuxtla, El Chichón, and Tacaná volcanoes, which are considered among the volcanoes with the highest hazard potenti
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Koloskov, A. V., M. Yu Davydova, D. V. Kovalenko та V. V. Ananyev. "New data on age, material composition and geological structure of the Central Kamchatka depression (CKD). Part 1. Rocks types. Age, petrological and isotopo-geochemical characteristicsн". Вулканология и сейсмология, № 3 (14 травня 2019): 3–24. http://dx.doi.org/10.31857/s0203-0306201933-24.

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The paper presents new age and isotope geochemical characteristics for plateau effusive rocks from the Central Kamchatka Depression (CKD) and Nikolka Volcano. We compared these data with the data on rocks from the Klyuchevskoy group of volcanoes and also Sheveluch, Kharchinsky, Zarechny, Nachikinsky, Bakening volcanoes and NEB-adakites from Pliocene shield volcano between the Ozernaya Kamchatka and Pravaya Kamchatka rivers. It is shown that the evolutionally advanced (often more alkaline) rock from Nachikinsky, Bakening, Nikolka volcanoes and the Pliocene shield volcanoe significantly differ i
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Koloskov, A. V., M. Yu Davydova та D. V. Kovalenko. "New data on age, material composition and geological structure of the Central Kamchatka depression (CKD). Part 1. Rocks types. Age, petrological and isotopo-geochemical characteristicsн". Вулканология и сейсмология, № 3 (14 травня 2019): 3–24. http://dx.doi.org/10.31857/s0205-9614201933-24.

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The paper presents new age and isotope geochemical characteristics for plateau effusive rocks from the Central Kamchatka Depression (CKD) and Nikolka Volcano. We compared these data with the data on rocks from the Klyuchevskoy group of volcanoes and also Sheveluch, Kharchinsky, Zarechny, Nachikinsky, Bakening volcanoes and NEB-adakites from Pliocene shield volcano between the Ozernaya Kamchatka and Pravaya Kamchatka rivers. It is shown that the evolutionally advanced (often more alkaline) rock from Nachikinsky, Bakening, Nikolka volcanoes and the Pliocene shield volcanoe significantly differ i
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Wan, Zhifeng, Jinfeng Zhang, Guoqing Lin, et al. "Formation Mechanism of Mud Volcanoes/Mud Diapirs Based on Physical Simulation." Geofluids 2021 (July 22, 2021): 1–16. http://dx.doi.org/10.1155/2021/5531957.

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The formation of mud volcanoes/mud diapirs is directly related to oil and gas accumulation and gas-hydrate mineralization. Their eruptive activities easily cause engineering accidents and may increase the greenhouse effect by the eruption of methane gas. Many scholars have performed much research on the developmental characteristics, geochemistry, and carbon emissions of mud diapirs/mud volcanoes, but the formation mechanism of mud diapirs/mud volcanoes is still controversial. Mud diapirs and mud volcanoes are especially developed in the northern South China Sea and are accompanied by abundant
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Aguilar Contreras, Rigoberto, Edu Taipe Maquerhua, Yanet Antayhua Vera, Mayra Ortega Gonzales, Fredy Apaza Choquehuayta, and Luis Cruz Mamani. "Hazard assessment studies and multiparametric volcano monitoring developed by the Instituto Geológico, Minero y Metalúrgico in Peru." Volcanica 4, S1 (2021): 73–92. http://dx.doi.org/10.30909/vol.04.s1.7392.

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Urban development in the areas surrounding active volcanoes has led to increasing risks in southern Peru. In order to evaluate the hazard, the Instituto Geológico, Minero y Metalúrgico (INGEMMET) created a Volcano Observatory (OVI) to carry out detailed geological investigations to understand eruption histories and provide volcanic hazard maps. The generation of geological information on volcanoes has allowed the identification of scenarios and zoning of potentially impacted areas. This information has also allowed OVI to implement surveillance networks giving priority to the volcanoes that po
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Layana, Susana, Felipe Aguilera, Germán Rojo, et al. "Volcanic Anomalies Monitoring System (VOLCANOMS), a Low-Cost Volcanic Monitoring System Based on Landsat Images." Remote Sensing 12, no. 10 (2020): 1589. http://dx.doi.org/10.3390/rs12101589.

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The practice of monitoring active volcanoes, includes several techniques using either direct or remote measurements, the latter being more important for volcanoes with limited accessibility. We present the Volcanic Anomalies Monitoring System (VOLCANOMS), a new, online, low-cost and semiautomatic system based on Landsat imagery. This system can detect permanent and/or temporal thermal anomalies in near-infrared (NIR), short-wave infrared (SWIR), and thermal infrared (TIR) bands. VOLCANOMS allows researchers to calculate several thermal parameters, such as thermal radiance, effective temperatur
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Hansen, Kristian, Simon Barker, Finnigan Illsley-Kemp, Craig Anslow, Christof Mueller, and Graham Leonard. "VolcanoVR: A virtual reality environment for volcanic data visualisation and communication." Volcanica 8, no. 1 (2025): 175–87. https://doi.org/10.30909/vol/vccy3095.

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With the increasing size and complexity of geological datasets relating to volcano monitoring and research, effective visualisation can be challenging. Here, we demonstrate the possibilities of volcanic data visualisation utilising virtual reality (VR) and 3D game engine technology to create a robust and adaptable program called VolcanoVR. VolcanoVR can display multiple complex datasets and has been developed to investigate volcanoes in the Taupō Volcanic Zone, New Zealand. To assess the usability and effectiveness of VolcanoVR a survey was conducted, involving 33 participants, ranging in educ
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Garcia, Sebastian, and Gabriela Badi. "Towards the development of the first permanent volcano observatory in Argentina." Volcanica 4, S1 (2021): 21–48. http://dx.doi.org/10.30909/vol.04.s1.2148.

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Argentina is a country that presents a complex situation regarding volcanic risk, where a total of 38 volcanoes are considered active. Although Argentina has no major cities close to these volcanoes, the continuous increase in economic activity and infrastructure near the Andean Codillera will increase exposure to volcano hazards in the future. Further, volcanic activity on the border between Argentina and Chile poses a unique challenge in relation to volcano monitoring and the management of volcanic emergencies. Additionally, due to atmospheric circulation patterns in the region (from West to
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Richter, Nicole, and Jean-Luc Froger. "The role of Interferometric Synthetic Aperture Radar in Detecting, Mapping, Monitoring, and Modelling the Volcanic Activity of Piton de la Fournaise, La Réunion: A Review." Remote Sensing 12, no. 6 (2020): 1019. http://dx.doi.org/10.3390/rs12061019.

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Synthetic Aperture Radar (SAR) remote sensing plays a significant role in volcano monitoring despite the measurements’ non real-time nature. The technique’s capability of imaging the spatial extent of ground motion has especially helped to shed light on the location, shape, and dynamics of subsurface magmatic storage and transport as well as the overall state of activity of volcanoes worldwide. A variety of different deformation phenomena are observed at exceptionally active and frequently erupting volcanoes, like Piton de la Fournaise on La Réunion Island. Those offer a powerful means of inve
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Loginov, V. A., L. I. Gontovaya, and S. L. Senyukov. "Avachinsky and Koryaksky Group of Volcanoes: Geophysical Inhomogeneity of the Lithosphere and Deep Processes (Kamchatka)." Вулканология и сейсмология 17, no. 1 (2023): 32–43. http://dx.doi.org/10.31857/s0203030622700031.

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The article presents the results of our gravimetric, seismic and electromagnetic research, as well as the data on deep seismicity of the lithosphere in the area of the active Avachinsky and Koryaksky group of volcanoes, which is the part of the East Kamchatka volcanic belt. We managed to develop the comprehensive geophysical model of the Earth’s crust and lithospheric mantle of this area. Based on the distribution scheme of the Earth’s crust geophysical inhomogeneities in general, and particularly beneath Avachinsky Volcano, we revealed specific features for both intracrustal fluid saturation
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Dissertations / Theses on the topic "Volcanoes"

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Bell, Andrew Forbes. "Patterns of volcano-tectonic seismicity at basaltic volcanoes." Thesis, University College London (University of London), 2008. http://discovery.ucl.ac.uk/1444163/.

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Accelerating rates of volcano-tectonic (VT) earthquakes are a common precursor to volcanic eruptions and reflect fracture growth within the edifice. Theoretical models interpret the patterns in terms of failure of the volcanic edifice under the magmatic load and promise improved eruption forecasting. However, many eruptions at frequently active basaltic volcanoes are reported to begin with little change in the rate of VT earthquakes, apparently in conflict with edifice failure models. This thesis investigates the spatial and temporal patterns of VT earthquakes associated with eruptive and intr
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Gulmammadov, Rashad. "Seismic geomechanics of mud volcanoes." Thesis, University of Manchester, 2017. https://www.research.manchester.ac.uk/portal/en/theses/seismic-geomechanics-of-mud-volcanoes(e579a3af-0881-4f52-b14a-dd360304f337).html.

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Mud volcanoes constitute an important component of petroliferous basins and their understanding is essential for successful exploration and development of hydrocarbon fields. They occur in both extensional and compressive tectonic settings, along with passive and active continental margins. Although extensive research exists on the geochemistry, geomorphology and stratigraphic evolution of these localized fluid flow structures, little is known about their geomechanical characteristics. This research investigates the geomechanics of mud volcanoes from the South Caspian Basin and West Nile Delta
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Auer, Sara Lynn. "Diverse oxygen isotope values and high magmatic water contents within the volcanic record of Klyuschevskoy Volcano, Kamchatka, Russia /." Connect to title online (Scholars' Bank), 2007. http://handle.net/1794/6054.

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Burrell, Rhian. "Volcanic instability and associated uncertainties at Soufrière Hills Volcano, Montserrat and other volcanoes." Thesis, Lancaster University, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.435873.

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Lane, Lucille Richards. "Hazard Vulnerability in Socio-Economic Context: An Example from Ecuador." [Tampa, Fla. : s.n.], 2003. http://purl.fcla.edu/fcla/etd/SFE0000076.

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Beachly, Matthew William 1986. "The Upper Crustal P-wave Velocity Structure of Newberry Volcano, Central Oregon." Thesis, University of Oregon, 2011. http://hdl.handle.net/1794/11475.

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xii, 98 p. : ill. (some col.)<br>The upper-crustal seismic-velocity structure of Newberry volcano, central Oregon, is imaged using P-wave travel time tomography. The inversion combines a densely-spaced seismic line collected in 2008 with two USGS seismic experiments from the 1980s. A high-velocity ring (7 km EW by 5 km NS) beneath the inner caldera faults suggests an intrusive ring complex 200 to 500 m thick. Within this ring shallow low velocities (<2 km depth) are interpreted as caldera fill and a subsided block. High velocities below 2 km depth could be intrusive complexes. There appears to
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Jolis, Ester M. "Magma-Crust Interaction at Subduction Zone Volcanoes." Doctoral thesis, Uppsala universitet, Berggrundsgeologi, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-198085.

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The focus of this work is magma-crust interaction processes and associated crustal volatile release in subduction zone volcanoes, drawing on rock, mineral, and gas geochemistry as well as experimental petrology. Understanding the multitude of differentiation processes that modify an original magma during ascent to the surface is vital to unravel the contributions of the various sources that contribute to the final magmas erupted at volcanoes. In particular, magma-crust interaction (MCI) processes have been investigated at a variety of scales, from a local scale in the Vesuvius, Merapi, and Kel
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Palma, Lizana José Luis. "Degassing of open-vent low-silica volcanoes." Thesis, Open University, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.499458.

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Open-vent activity at volcanoes of low-silica composition, such as Stromboli (Italy), Villarrica (Chile), Mt. Erebus (Antarctica), Masaya (Nicaragua), is characterised by persistent passive gas emission and recurrent mild explosive outgassing. Four styles of bubble bursting activity have been recognised in such volcanoes: seething magma, small short-lived lava fountains, strombolian explosions and gas puffing. Whilst strombolian explosions are perhaps the most common among these volcanoes, seething magma and small lava fountains have been observed only at the surface of active lava lakes. At V
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Allen, Daniel R. "Temperature and Variability of Three Ionian Volcanoes." BYU ScholarsArchive, 2010. https://scholarsarchive.byu.edu/etd/2591.

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Cassini spacecraft images of Io obtained during its flyby of Jupiter in late 2000 and early 2001 were used to determine the lava composition and eruption style of three faint hotspots, Pillan, Wayland, and Loki. We found a maximum color temperature of 1130+/-289 K for Pillan and maximum color temperatures of 1297+/-289 K and 1387+/-287 K for Wayland and Loki, respectively. These temperatures are suggestive of basaltic lava. The temperatures with the best signal-to-noise ratios also suggested basaltic lava and were found to be 780+/-189 K, 1116+/-250 K, and 1017+/-177 K for Pillan, Wayland, and
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Woog, Friederike. "Ecology and behavior of reintroduced Hawaiian geese." [S.l. : s.n.], 1999. http://deposit.ddb.de/cgi-bin/dokserv?idn=959320423.

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Books on the topic "Volcanoes"

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Schuh, Mari C. Volcanes =: Volcanoes. Pebble Plus Books, 2011.

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Rau, Dana Meachen. Volcanoes =: Los volcanes. Marshall Cavendish Benchmark, 2008.

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Woods, Eric. Encyclopedia of volcanos [i.e. volcanoes]. Global Media, 2007.

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Schreiber, Anne. Volcanoes! National Geographic, 2008.

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Rose, Susanna Van. Volcanoes. 2nd ed. Harvard, 1991.

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Pyle, David. Volcanoes. Eagle Editions, 2003.

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Schreiber, Anne. Volcanoes! National Geographic, 2008.

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Wood, J. Volcanoes. PUFFIN BOOKS, 1990.

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Wallace, Patrick. Volcanoes. Gallery Books, 1991.

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Park, Louise. Volcanoes. Smart Apple Media, 2007.

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Book chapters on the topic "Volcanoes"

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Jain, Sreepat. "Volcanoes." In Fundamentals of Physical Geology. Springer India, 2014. http://dx.doi.org/10.1007/978-81-322-1539-4_16.

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Stahr, Alexander, and Ewald Langenscheidt. "Volcanoes." In Landforms of High Mountains. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-53715-8_3.

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Siegel, Frederic R. "Volcanoes." In Mitigation of Dangers from Natural and Anthropogenic Hazards. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-38875-5_8.

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Karol, Paul J. "Volcanoes." In The Legacy of Carbon Dioxide. CRC Press, 2019. http://dx.doi.org/10.1201/9780429200649-13.

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Keller, Edward A., and Duane E. DeVecchio. "Volcanoes." In Natural Hazards. Routledge, 2019. http://dx.doi.org/10.4324/9781315164298-5.

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Reilly, Benjamin. "Volcanoes." In Disasters in World History. Routledge, 2024. http://dx.doi.org/10.4324/9781003436805-5.

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Goudie, Andrew. "Volcanoes." In Rocky Landscapes of the World with Google Earth. Springer Nature Switzerland, 2024. https://doi.org/10.1007/978-3-031-77418-8_4.

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Gao, Jay. "Volcanoes." In Remote Sensing of Natural Hazards. CRC Press, 2023. http://dx.doi.org/10.1201/9781003354321-12.

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Bennett, Matthew R. "Volcanoes." In Our Dynamic Earth: A Primer. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-90351-0_3.

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Punongbayan, Raymundo S. "Volcanoes." In International Perspectives on Natural Disasters: Occurrence, Mitigation, and Consequences. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-2851-9_2.

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Conference papers on the topic "Volcanoes"

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Jatu, C. "The Grobogan Mud Volcano Complex: An Identification to Reveal the Opportunity of Hydrocarbon Exploration." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-sg-362.

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Mud volcanoes in Grobogan are referred as the Grobogan Mud Volcanoes Complex in Central Java where there is evidence of oil seepages. This comprehensive research is to determine the characteristics and hydrocarbon potential of the mud volcanoes in the Central Java region as a new opportunity for hydrocarbon exploration. The Grobogan Mud Volcano Complex consists of eight mud volcanoes that have its characteristics based on the study used the geological surface data and seismic literature as supporting data on eight mud volcanoes. The determination of geological surface characteristics is based
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Apel, Ted, and Jeffrey B. Johnson. "Portable Realtime Volcano Infrasound Auditory Display Devices." In ICAD 2021: The 26th International Conference on Auditory Display. International Community for Auditory Display, 2021. http://dx.doi.org/10.21785/icad2021.012.

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Active open-vent volcanoes produce intense infrasound airwaves, and volcanoes with prominent craters can create strongly resonant signals, which are inaudible to humans, and often peak around 1 Hz. Study of volcano infrasound is used to model eruption dynamics, the structure of volcanic craters, and can be used as a component of volcano monitoring infrastructure. We have developed a portable on-site real-time sonification device that emits an audible sound in response to an infrasonic airwave. This device can be used near an active volcano both as a real-time educational aid and as an accessib
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Tenberga, Ieva. "Enhancing Geography Education through Virtual Reality: Exploring Pedagogical and Technological Principles Ieva Tenberga." In 82nd International Scientific Conference of the University of Latvia. University of Latvia Press, 2024. http://dx.doi.org/10.22364/htqe.2024.22.

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The new educational content framework Skola2030, which was implemented from 2020 to 2023 in Latvia, made it possible to improve the teaching of geography at the secondary level in order to deepen students’ understanding of the intricate relationships between natural environments and human activities. All traditional educational tools, such as textbooks, infographics, movies, maps, and simulations focusing on the movement of plate tectonics, are available to students. Still, they address only a small portion of the complex internal operations. Textbooks may provide simplified diagrams of volcan
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Amici, Stefania, and Barbara Castello. "PAPER VOLCANOES LABORATORY." In 11th annual International Conference of Education, Research and Innovation. IATED, 2018. http://dx.doi.org/10.21125/iceri.2018.2491.

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Weibring, P., T. Lindström, H. Edner, et al. "Assessment of the total emission of sulphur dioxide from Italian volcanoes in simultaneous shipborne measurements using lidar, doas and correlation spectroscopy." In The European Conference on Lasers and Electro-Optics. Optica Publishing Group, 1998. http://dx.doi.org/10.1364/cleo_europe.1998.cmi4.

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Volcanoes contribute substantial amounts of sulphur dioxide to the global atmosphere, and thus reliable measurements are needed for an accurate assessment of the relative roles of natural and antropogenic emissions. Normally, gas correlation measurements based on COSPEC instruments are performed, observing in ground-based traverses the spectral imprint of the gas in the spectrum of the down-welling ambient radiation. However, because of complicated scattering conditions above, within and below the volcanic plume, data are complex. The differential optical absorption spectroscopy (doas) techniq
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Urai, Minoru. "Volcano observations with aster and ASTER Image Database for Volcanoes." In IGARSS 2011 - 2011 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2011. http://dx.doi.org/10.1109/igarss.2011.6050018.

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Kent, Adam J. R., Christy Till, and Kari Cooper. "What Makes Volcanoes Erupt?" In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1282.

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Gulmammadov, Rashad. "Seismic geomechanics of mud volcanoes." In International Conference and Exhibition, Barcelona, Spain, 3-6 April 2016. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2016. http://dx.doi.org/10.1190/ice2016-6328337.1.

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Nunez, Luis A., Ricardo de Leon-Barrios, Jesús Peña-Rodríguez, et al. "Muography for the Colombian Volcanoes." In 37th International Cosmic Ray Conference. Sissa Medialab, 2021. http://dx.doi.org/10.22323/1.395.0280.

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Georgen, Jen. "MARINE VOLCANOES AND SEAFLOOR ERUPTIONS." In Joint 56th Annual North-Central/ 71st Annual Southeastern Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022nc-375798.

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Reports on the topic "Volcanoes"

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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

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This report presents an analysis of the threat posed by active volcanoes in Canada and outlines directives to bring Canadian volcano monitoring and research into alignment with global best practices. We analyse 28 Canadian volcanoes in terms of their relative threat to people, aviation and infrastructure. The methodology we apply to assess volcanic threat was developed by the United States Geological Survey (USGS) as part of the 2005 National Volcano Early Warning System (NVEWS). Each volcano is scored on a number of hazard and exposure factors, producing an overall threat score. The overall t
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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

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This report presents an analysis of the threat posed by active volcanoes in Canada and outlines directives to bring Canadian volcano monitoring and research into alignment with global best practices. We analyse 28 Canadian volcanoes in terms of their relative threat to people, aviation and infrastructure. The methodology we apply to assess volcanic threat was developed by the United States Geological Survey (USGS) as part of the 2005 National Volcano Early Warning System (NVEWS). Each volcano is scored on a number of hazard and exposure factors, producing an overall threat score. The overall t
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Kelman, M., G. Williams-Jones, and Warwick. Volcanoes. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330529.

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Nye, C. J. Volcanoes of Alaska. Alaska Division of Geological & Geophysical Surveys, 1995. http://dx.doi.org/10.14509/484.

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Nye, C. J. Volcanoes of Alaska. Alaska Division of Geological & Geophysical Surveys, 1998. http://dx.doi.org/10.14509/7043.

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Nye, C. J. Aleutian Arc Volcanoes. Alaska Division of Geological & Geophysical Surveys, 1995. http://dx.doi.org/10.14509/1678.

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Hickson, C. J., and B. R. Edwards. Volcanoes and volcanic hazards. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212217.

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Cameron, C. E., J. R. Schaefer, and K. M. Mulliken. Historically active volcanoes of Alaska. Alaska Division of Geological & Geophysical Surveys, 2018. http://dx.doi.org/10.14509/30142.

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Cameron, C. E., J. R. Schaefer, and P. G. Ekberg. Historically active volcanoes of Alaska. Alaska Division of Geological & Geophysical Surveys, 2020. http://dx.doi.org/10.14509/30426.

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Woods, Ken. Historically Active Volcanoes of Alaska. DGGS, 2012. http://dx.doi.org/10.14509/historically_active_volcanoes.

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