Relevant bibliographies by topics / Volcano Teide

Academic literature on the topic 'Volcano Teide'

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Published: 10 March 2023

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Journal articles on the topic "Volcano Teide"

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Alonso, Mar, Eleazar Padrón, Hirochika Sumino, Pedro A. Hernández, Gladys V. Melián, María Asensio-Ramos, Fátima Rodríguez, et al. "Heat and Helium-3 Fluxes from Teide Volcano, Canary Islands, Spain." Geofluids 2019 (June 23, 2019): 1–12. http://dx.doi.org/10.1155/2019/3983864.

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During July 2016, the first integrated heat flow, CO2, and 3He emission survey was conducted across 0.5 km2 of the summit cone and crater of Teide volcano, Tenerife, Canary Islands, Spain. The thermal energy released from Teide summit cone by diffuse degassing was 2.2 MW, and the heat flux calculated through Dawson’s method was 8.1 MW, difference due to the comparison of purely convective areas as the crater with diffusive areas as the flanks of the volcano. Diffuse CO2 output was 211±20 t d-1, and 3He emission was estimated to be within a range between 0.35 and 0.89 mol y-1. The obtained values of diffuse degassing and heat fluxes are close to others obtained for similar volcanic areas. The calculation of 3He/heat ratio for the first time in this volcanic system supports the presence of an important mantle source for the degassing of Teide volcano.
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Carracedo, Juan Carlos, Valentin R. Troll, Francisco J. Pérez, Eduardo Rodríguez Badiola, Alex Hansen Machín, Raphael Paris, Hervé Guillou, and Stéphane Scaillet. "Recent unrest at Canary Islands' Teide Volcano?" Eos, Transactions American Geophysical Union 87, no. 43 (October 24, 2006): 462–65. http://dx.doi.org/10.1029/2006eo430003.

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Vila, J., R. Ortiz, M. Tárraga, R. Macià, A. García, D. Kumar, and A. M. Correig. "Near-Real time analysis of seismic data of active volcanoes: Software implementations of time sequence data analysis." Natural Hazards and Earth System Sciences 8, no. 4 (July 31, 2008): 789–94. http://dx.doi.org/10.5194/nhess-8-789-2008.

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Abstract. This paper presents the development and applications of a software-based quality control system that monitors volcano activity in near-real time. On the premise that external seismic manifestations provide information directly related to the internal status of a volcano, here we analyzed variations in background seismic noise. By continuous analysis of variations in seismic waveforms, we detected clear indications of changes in the internal status. The application of this method to data recorded in Villarrica (Chile) and Tungurahua (Ecuador) volcanoes demonstrates that it is suitable to be used as a forecasting tool. A recent application of this developed software-based quality control to the real-time monitoring of Teide – Pico Viejo volcanic complex (Spain) anticipated external episodes of volcanic activity, thus corroborating the advantages and capacity of the methodology when implemented as an automatic real-time procedure.
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García, Alicia, Ramon Ortiz, Jose M. Marrero, Nieves S´nchez, Josep Vila, Antoni M. Correig, Ramon Marcià, Reinoud Sleeman, and Marta Tárraga. "Monitoring the reawakening of Canary Islands' Teide Volcano." Eos, Transactions American Geophysical Union 87, no. 6 (2006): 61. http://dx.doi.org/10.1029/2006eo060001.

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Pérez, Nemesio M., and Pedro A. Hernández. "Comment on “Recent unrest at Canary Islands' Teide Volcano?”." Eos, Transactions American Geophysical Union 88, no. 46 (November 13, 2007): 488. http://dx.doi.org/10.1029/2007eo460008.

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Zahorec, Pavol, Peter Vajda, Juraj Papčo, Sergio Sainz-Maza Aparicio, and Jorge Pereda De Pablo. "Prediction of vertical gradient of gravity and its significance for volcano monitoring – example from Teide volcano." Contributions to Geophysics and Geodesy 46, no. 3 (September 1, 2016): 203–20. http://dx.doi.org/10.1515/congeo-2016-0013.

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Abstract We present a detailed calculation of the topographic contribution to the vertical gradient of gravity (VGG) based on high-resolution digital elevation model (DEM) and new developed software (Toposk) for the purpose of predicting the actual VGGs in the field. The calculations presented here were performed for the Central Volcanic Complex (CVC) of Tenerife. We aimed at identifying the most extreme VGGs within the CVC, as well as predicting the VGGs at benchmarks of the former microgravity/deformation network set up to monitor the 2004/5 unrest. We have carried out an observational campaign in June 2016 to verify the predicted VGG values, both the extreme ones and those at the benchmarks. The comparison between the predicted and the in-situ verified VGGs is presented here. We demonstrate the sensitivity of the VGG prediction to the choice of the topo-rock density, which is inherent to the volcanic areas with high variability of rock densities. We illustrate the significance of the use of actual VGG in volcano monitoring microgravimetric surveys on a couple of benchmarks of the CVC network.
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Tárraga, M., R. Carniel, R. Ortiz, J. M. Marrero, and A. García. "On the predictability of volcano-tectonic events by low frequency seismic noise analysis at Teide-Pico Viejo volcanic complex, Canary Islands." Natural Hazards and Earth System Sciences 6, no. 3 (May 15, 2006): 365–76. http://dx.doi.org/10.5194/nhess-6-365-2006.

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Abstract. The island of Tenerife (Canary Islands, Spain), is showing possible signs of reawakening after its last basaltic strombolian eruption, dated 1909 at Chinyero. The main concern relates to the central active volcanic complex Teide - Pico Viejo, which poses serious hazards to the properties and population of the island of Tenerife (Canary Islands, Spain), and which has erupted several times during the last 5000 years, including a subplinian phonolitic eruption (Montaña Blanca) about 2000 years ago. In this paper we show the presence of low frequency seismic noise which possibly includes tremor of volcanic origin and we investigate the feasibility of using it to forecast, via the material failure forecast method, the time of occurrence of discrete events that could be called Volcano-Tectonic or simply Tectonic (i.e. non volcanic) on the basis of their relationship to volcanic activity. In order to avoid subjectivity in the forecast procedure, an automatic program has been developed to generate forecasts, validated by Bayes theorem. A parameter called "forecast gain" measures (and for the first time quantitatively) what is gained in probabilistic terms by applying the (automatic) failure forecast method. The clear correlation between the obtained forecasts and the occurrence of (Volcano-)Tectonic seismic events - a clear indication of a relationship between the continuous seismic noise and the discrete seismic events - is the explanation for the high value of this "forecast gain" in both 2004 and 2005 and an indication that the events are Volcano-Tectonic rather than purely Tectonic.
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Del Pezzo, E., M. La Rocca, and J. Ibanez. "Observations of high-frequency scattered waves using dense arrays at Teide Volcano." Bulletin of the Seismological Society of America 87, no. 6 (December 1, 1997): 1637–47. http://dx.doi.org/10.1785/bssa0870061637.

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Abstract A study of the seismic coda of seven small earthquakes recorded on the Teide Volcano-Canary Islands (Spain) was carried out using a temporary, small-aperture, 12-station, seismic array. The purpose was to measure backazimuth, apparent velocity and the type of waves that compose the coda in the frequency range 4 to 6 Hz. We used the zero-lag cross-correlation (ZLC) method to obtain the components of the wave vector and three-component analysis techniques based on the covariance matrix of the signal in the time domain to investigate the polarization properties of the signals. The results show that a great part of the coda signals in the analyzed frequency range are almost uncorrelated, while a low number of isolated correlated arrivals show an apparent slowness between 2 × 10−3 and 2.5 × 10−4 sec/m and an almost random distribution of backazimuths. The correlated arrivals have been interpreted as generated by strong scatterers, probably related to the presence, in the study area, of surface topography irregularities (the volcanic cone and the caldera rim). The wave type varies from pure S-type waves to mixed surface waves with some Rayleigh components.
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Battaglia, Maurizio, Joachim Gottsmann, Daniele Carbone, and José Fernández. "4D volcano gravimetry." GEOPHYSICS 73, no. 6 (November 2008): WA3—WA18. http://dx.doi.org/10.1190/1.2977792.

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Time-dependent gravimetric measurements can detect subsurface processes long before magma flow leads to earthquakes or other eruption precursors. The ability of gravity measurements to detect subsurface mass flow is greatly enhanced if gravity measurements are analyzed and modeled with ground-deformation data. Obtaining the maximum information from microgravity studies requires careful evaluation of the layout of network benchmarks, the gravity environmental signal, and the coupling between gravity changes and crustal deformation. When changes in the system under study are fast (hours to weeks), as in hydrothermal systems and restless volcanoes, continuous gravity observations at selected sites can help to capture many details of the dynamics of the intrusive sources. Despite the instrumental effects, mainly caused by atmospheric temperature, results from monitoring at Mt. Etna volcano show that continuous measurements are a powerful tool for monitoring and studying volcanoes.Several analytical and numerical mathematical models can beused to fit gravity and deformation data. Analytical models offer a closed-form description of the volcanic source. In principle, this allows one to readily infer the relative importance of the source parameters. In active volcanic sites such as Long Valley caldera (California, U.S.A.) and Campi Flegrei (Italy), careful use of analytical models and high-quality data sets has produced good results. However, the simplifications that make analytical models tractable might result in misleading volcanological inter-pretations, particularly when the real crust surrounding the source is far from the homogeneous/isotropic assumption. Using numerical models allows consideration of more realistic descriptions of the sources and of the crust where they are located (e.g., vertical and lateral mechanical discontinuities, complex source geometries, and topography). Applications at Teide volcano (Tenerife) and Campi Flegrei demonstrate the importance of this more realistic description in gravity calculations.
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Berlanga-Labari, Carlos, Leyre Catalán, José F. Palacio, Gurutze Pérez, and David Astrain. "Corrosion Behavior in Volcanic Soils: In Search of Candidate Materials for Thermoelectric Devices." Materials 14, no. 24 (December 12, 2021): 7657. http://dx.doi.org/10.3390/ma14247657.

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Thermoelectric generators have emerged as an excellent solution for the energy supply of volcanic monitoring stations due to their compactness and continuous power generation. Nevertheless, in order to become a completely viable solution, it is necessary to ensure that their materials are able to resist in the acidic environment characteristic of volcanoes. Hence, the main objective of this work is to study the resistance to corrosion of six different metallic materials that are candidates for use in the heat exchangers. For this purpose, the metal probes have been buried for one year in the soil of the Teide volcano (Spain) and their corrosion behavior has been evaluated by using different techniques (OM, SEM, and XRD). The results have shown excessive corrosion damage to the copper, brass, and galvanized steel tubes. After evaluating the corrosion behavior and thermoelectric performance, AISI 304 and AISI 316 stainless steels are proposed for use as heat exchangers in thermoelectric devices in volcanic environments.
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Dissertations / Theses on the topic "Volcano Teide"

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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 complex. One of the most representative eruptions is that of El Boqueron (5,660 yBP), a dome that generated an explosive event of VEI 3 with a minimum volume of 4-6x107 m3 and produced a plume with a height of up to 9km above sea level (MER 6.9-8.2x105 kg/s, during 9-15 h). The occurrence of these explosive events in the recent eruptive record of TPV is of major importance in evaluating the risk imposed by the volcanic complex on Tenerife. These eruptions have generated a wide range of direct hazards, such as fallout, emplacement of pyroclastic density currents, debris flows, lahars, and rock avalanches, which could occur again in case of a renewal of volcanic activity. The results obtained in our study are relevant to define realistic and precise eruptive scenarios for TPV and to assess its associated hazard, a necessary step in the evaluation and mitigations of volcanic risk in Tenerife
El complejo volcánico Teide Pico Viejo (TPV) es un stratovolcano situado en la isla de Tenerife, Islas Canarias, y ha sido considerado por la UNESCO el sistema volcánico activo más peligroso en Europa. Los eventos explosivos en el complejo TPV se han limitado tradicionalmente a la erupción subplinian de Montaña Blanca, que ocurrió hace unos 2000 años. Una reciente revisión de la estratigrafía muestra que la actividad explosiva fonolítica asociada a TPV ha sido significativa durante el Holoceno, presentado distintos episodios relacionados con erupciones que varían en tamaño de estromboliano a sub-pliniano. A través de las correlaciones estratigráficas obtenidas mediante observaciones de campo y datos de mineralógicos y geoquímicos, se han identificado 11 erupciones explosivas fonolítica relacionados con los domos satélite presentes en todo complejo TPV. Una de las erupciones más representativa es El Boquerón (5660 YBP), un domo que generó un evento explosivo de VEI 3 con un volumen mínimo de 4-6x107 m3 y produjo una columna con una altura de hasta 9 kilometros sobre el nivel del mar ( MER 6.9-8.2x105 kg / s, durante 9-15 h). La ocurrencia de estos eventos explosivos en el reciente registro eruptivo del complejo TPV es de gran importancia para evaluar el riesgo impuesto por el complejo volcánico en Tenerife. Estas erupciones han generado una amplia gama de amenazas directas, como los depósitos de caida, emplazamiento de las corrientes piroclásticas densidad, flujo de derrubios, lahares y avalanchas de roca, lo que podría ocurrir de nuevo en caso de renovación de la actividad volcánica. Los resultados obtenidos en nuestro estudio son relevantes para definir escenarios eruptivos realista y precisos para el complejo TPV y para evaluar su riesgo asociado, un paso necesario en la evaluación y mitigación del riesgo volcánico en Tenerife
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Ablay, Giray Jan. "Evolution of the Teide-Pico Viejo volcanic complex and magmatic system, Tenerife, Canary Islands." Thesis, University of Bristol, 1997. http://hdl.handle.net/1983/34b7cffc-09b2-4fc7-8f8b-f331abccd9ad.

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Ringmar, Ingrid Maria. "Entre vocablos y volcanes : Dificultades terminológicas y formas de dirigirse al lector en un texto especializado para turistas." Thesis, Linnéuniversitetet, Institutionen för språk (SPR), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-46203.

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This has paper has two main purposes: to analyze the translation of specialized terminology and ways of addressing the reader in a specialized tourist text in Spanish and its Swedish target text. The terminological difficulties on volcanism in the translation concerns the fact that the semantic field on this topic is diversified in the Canary Islands, contrary to the semantic field on volcanoes in Swedish. The theoretical background in this paper gives keys to describing the meaning of words in terms of connotation and denotation and describes how to use semantic components to solve the difficulties of terminology. The theory applied to the difficulties concerning ways of addressing the reader in the source text, explains the relation between the sender and the reader in terms of distance and closenes. The paper shows that the source text is inconsistent in this matter. To solve this task the translator has adopted a homogeneous way of addressing the reader, to achieve a target text loyal to the Swedish speaking reader and to consistency. The translation of tourist texts has been thought of as being an easy task, not demanding too much of its translators. This paper aims at showing that this is not the case.
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Books on the topic "Volcano Teide"

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Carracedo, Juan Carlos, and Valentin R. Troll, eds. Teide Volcano. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0.

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Carracedo, Juan Carlos, and Valentin R. Troll. Teide Volcano: Geology and Eruptions of a Highly Differentiated Oceanic Stratovolcano. Springer, 2013.

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Teide Volcano Geology And Eruptions Of A Highly Differentiated Oceanic Stratovolcano. Springer, 2012.

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Carracedo, Juan Carlos, and Valentin R. Troll. Teide Volcano: Geology and Eruptions of a Highly Differentiated Oceanic Stratovolcano. Springer, 2016.

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Book chapters on the topic "Volcano Teide"

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Carracedo, Juan Carlos, and Valentin R. Troll. "From Myth to Science: The Contribution of Mount Teide to the Advancement of Volcanology." In Teide Volcano, 1–21. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_1.

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Wiesmaier, Sebastian, Valentin R. Troll, Juan Carlos Carracedo, Robert M. Ellam, Ilya Bindeman, John A. Wolff, and Frances M. Deegan. "Magmatic Differentiation in the Teide–Pico Viejo Succession: Isotope Analysis as a Key to Deciphering the Origin of Phonolite Magma." In Teide Volcano, 173–90. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_10.

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Wiesmaier, Sebastian, Frances M. Deegan, Valentin R. Troll, Juan Carlos Carracedo, and Jane P. Chadwick. "Magma Mixing in the 1100 AD Montaña Reventada Composite Lava Flow: Interaction of Rift Zone and Central Complex Magmatism." In Teide Volcano, 191–211. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_11.

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Perez-Torrado, Francisco J., Juan Carlos Carracedo, Alejandro Rodriguez-Gonzalez, Eduardo Rodríguez-Badiola, Raphaël Paris, Valentin R. Troll, Hilary Clarke, and Sebastian Wiesmaier. "Eruptive Styles at the Teide Volcanic Complex." In Teide Volcano, 213–31. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_12.

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Soler-Javaloyes, Vicente, and Juan Carlos Carracedo. "Geophysical Investigations of the Teide Volcanic Complex." In Teide Volcano, 233–48. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_13.

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Carracedo, Juan Carlos, Alejandro Rodriguez-Gonzalez, Francisco J. Perez-Torrado, Jose-Luis Fernandez-Turiel, Raphaël Paris, Eduardo Rodríguez-Badiola, Gustavo Pestana-Pérez, Valentin R. Troll, and Sebastian Wiesmaier. "Geological Hazards in the Teide Volcanic Complex." In Teide Volcano, 249–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_14.

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Carracedo, Juan Carlos, and Francisco J. Perez-Torrado. "Geological and Geodynamic Context of the Teide Volcanic Complex." In Teide Volcano, 23–36. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_2.

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Rodriguez-Gonzalez, Alejandro, Raphaël Paris, Constantino Criado, and Jose-Luis Fernandez-Turiel. "The Teide Volcanic Complex: Physical Environment and Geomorphology." In Teide Volcano, 37–56. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_3.

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Carracedo, Juan Carlos, and Valentin R. Troll. "Structural and Geological Elements of Teide Volcanic Complex: Rift Zones and Gravitational Collapses." In Teide Volcano, 57–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_4.

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Troll, Valentin R., Frances M. Deegan, Audray Delcamp, Juan Carlos Carracedo, Chris Harris, Benjamin van Wyk de Vries, Michael S. Petronis, et al. "Pre-Teide Volcanic Activity on the Northeast Volcanic Rift Zone." In Teide Volcano, 75–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-25893-0_5.

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Conference papers on the topic "Volcano Teide"

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Amici, Stefania, Alessandro Piscini, and Maria Fabrizia Buongiorno. "Aster temperature and emissivity validation on Volcano Teide." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5649201.

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Piscini, Alessandro, Stefania Amici, and David Pieri. "Spectral analysis of aster and hyperion data for geological classification of volcano teide." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5652063.

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Weber, K., C. Fischer, G. Van Haren, K. Bothe, S. Pisirtsidis, M. Laue, Y. González Ramos, et al. "Ground-based remote sensing of gas emissions from Teide volcano (Tenerife, Canary Islands, Spain): first results." In Remote Sensing, edited by James R. Slusser, Klaus Schäfer, and Adolfo Comerón. SPIE, 2006. http://dx.doi.org/10.1117/12.714411.

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