Dr. Juan Prieto
Universidad Politécnica de Madrid
'%3e%3cpath%20d='M22.1642%2019.0924C21.7317%2018.068%2021.1041%2017.1375%2020.3163%2016.3527C19.5309%2015.5656%2018.6006%2014.9381%2017.5766%2014.5048C17.5674%2014.5002%2017.5582%2014.4979%2017.5491%2014.4933C18.9774%2013.4616%2019.9059%2011.7811%2019.9059%209.88504C19.9059%206.74408%2017.3611%204.19922%2014.2201%204.19922C11.0792%204.19922%208.53429%206.74408%208.53429%209.88504C8.53429%2011.7811%209.46282%2013.4616%2010.8912%2014.4956C10.882%2014.5002%2010.8728%2014.5025%2010.8636%2014.5071C9.83652%2014.9404%208.91487%2015.5617%208.1239%2016.355C7.33685%2017.1404%206.70933%2018.0707%206.276%2019.0947C5.85031%2020.0972%205.62072%2021.172%205.59967%2022.2609C5.59905%2022.2853%205.60335%2022.3097%205.61229%2022.3325C5.62123%2022.3553%205.63465%2022.376%205.65174%2022.3935C5.66883%2022.4111%205.68926%2022.425%205.71182%2022.4345C5.73437%2022.444%205.7586%2022.4489%205.78308%2022.4489H7.15868C7.25956%2022.4489%207.3398%2022.3686%207.3421%2022.2701C7.38795%2020.5001%208.09868%2018.8425%209.35506%2017.5861C10.655%2016.2862%2012.3814%2015.5709%2014.2201%2015.5709C16.0588%2015.5709%2017.7852%2016.2862%2019.0852%2017.5861C20.3415%2018.8425%2021.0523%2020.5001%2021.0981%2022.2701C21.1004%2022.3709%2021.1807%2022.4489%2021.2815%2022.4489H22.6571C22.6816%2022.4489%2022.7058%2022.444%2022.7284%2022.4345C22.751%2022.425%2022.7714%2022.4111%2022.7885%2022.3935C22.8056%2022.376%2022.819%2022.3553%2022.8279%2022.3325C22.8369%2022.3097%2022.8412%2022.2853%2022.8406%2022.2609C22.8176%2021.165%2022.5907%2020.0989%2022.1642%2019.0924ZM14.2201%2013.8284C13.1678%2013.8284%2012.1773%2013.418%2011.4322%2012.6729C10.6871%2011.9278%2010.2767%2010.9374%2010.2767%209.88504C10.2767%208.83271%2010.6871%207.84227%2011.4322%207.09715C12.1773%206.35204%2013.1678%205.94165%2014.2201%205.94165C15.2724%205.94165%2016.2629%206.35204%2017.008%207.09715C17.7531%207.84227%2018.1635%208.83271%2018.1635%209.88504C18.1635%2010.9374%2017.7531%2011.9278%2017.008%2012.6729C16.2629%2013.418%2015.2724%2013.8284%2014.2201%2013.8284Z'%20fill='%238590A2'/%3e%3c/g%3e%3c/svg%3e)
Co-authors
Following
Followers
Research Focus & Metrics
Explore full metrics on Scilit
Academic Career Length
23Years (2004-Present)
(Calculated once Scilit publication data is synced: current year − year of first publication + 1)
Representative Publications
View All Publications28 January 2021 in Scientific Reports
Journal Article
Jose Fernandez
Joaquin Escayo MenendezZHZhongbo Hu
Zhongbo Hu
ACAntonio G. Camacho
Antonio G. Camacho
SSSergey V. Samsonov
Sergey V. Samsonov
EAEumenio Ancochea
Eumenio Ancochea
+4
La Palma island is one of the highest potential risks in the volcanic archipelago of the Canaries and therefore it is important to carry out an in-depth study to define its state of unrest. This has been accomplished through the use of satellite radar observations and an original state-of-the-art interpretation technique. Here we show the detection of the onset of volcanic unrest on La Palma island, most likely decades before a potential eruption. We study its current evolution seeing the spatial and temporal changing nature of activity at this potentially dangerous volcano at unprecedented spatial resolutions and long time scales, providing insights into the dynamic nature of the associated volcanic hazard. The geodetic techniques employed here allow tracking of the fluid migration induced by magma injection at depth and identifying the existence of dislocation sources below Cumbre Vieja volcano which could be associated with a future flank failure. Therefore they should continue being monitored using these and other techniques. The results have implications for the monitoring of steep-sided volcanoes at oceanic islands.
3 October 2018 in Scientific Reports
Journal Article
Jose FernandezJuan PrietoJoaquin Escayo MenendezACAntonio G. Camacho
Antonio G. Camacho
FLFrancisco Luzón
Francisco Luzón
JMJordi J. Mallorqui
Jordi J. Mallorqui +11
Land subsidence associated with overexploitation of aquifers is a hazard that commonly affects large areas worldwide. The Lorca area, located in southeast Spain, has undergone one of the highest subsidence rates in Europe as a direct consequence of long-term aquifer exploitation. Previous studies carried out on the region assumed that the ground deformation retrieved from satellite radar interferometry corresponds only to vertical displacement. Here we report, for the first time, the two- and three-dimensional displacement field over the study area using synthetic aperture radar (SAR) data from Sentinel-1A images and Global Navigation Satellite System (GNSS) observations. By modeling this displacement, we provide new insights on the spatial and temporal evolution of the subsidence processes and on the main governing mechanisms. Additionally, we also demonstrate the importance of knowing both the vertical and horizontal components of the displacement to properly characterize similar hazards. Based on these results, we propose some general guidelines for the sustainable management and monitoring of land subsidence related to anthropogenic activities.
25 February 2009 in Geophysical Research Letters
Journal Article
Jose FernandezPTPietro Tizzani
Pietro TizzaniMMMariarosaria Manzo
Mariarosaria ManzoABA. Borgia
A. Borgia
PGPablo Gonzales
Pablo GonzalesRLRiccardo Lanari
Riccardo Lanari +6
We study the state of deformation of Tenerife (Canary Islands) using Differential Synthetic Aperture Radar Interferometry (DInSAR). We apply the Small BAseline Subset (SBAS) DInSAR algorithm to radar images acquired from 1992 to 2005 by the ERS sensors to determine the deformation rate distribution and the time series for the coherent pixels identified in the island. Our analysis reveals that the summit area of the volcanic edifice is characterized by a rather continuous subsidence extending well beyond Las Cañadas caldera rim and corresponding to the dense core of the island. These results, coupled with GPS ones, structural and geological information and deformation modeling, suggest an interpretation based on the gravitational sinking of the dense core of the island into a weak lithosphere and that the volcanic edifice is in a state of compression. We also detect more localized deformation patterns correlated with water table changes and variations in the deformation time series associated with the seismic crisis in 2004.
23 May 2009 in Journal of Geophysical Research
Journal Article
ACA. G. Camacho
A. G. CamachoJose FernandezPGPablo Gonzales
Pablo GonzalesJRJ. B. Rundle
J. B. Rundle
Juan PrietoAAA. Arjona
A. ArjonaA recent gravity survey composed of 317 bench marks all over the island of La Palma (Canary Islands) is used, in combination with satellite data for regional aspects, to obtain results about structural properties of the island connected with the tectonic environment and local volcanism. To that end, a nonlinear three‐dimensional gravity inversion approach is considered. The inversion scheme provides, in a nonsubjective form, the geometry of the anomalous bodies constructed in a random growth process. Results from the inversion can be interpreted in the framework of the geologic evolution of this ocean island volcano as a complex composite volcano with a large central body with high‐density corresponding to the older intrusive part of the basalt complex. New unexpected features are enlightened, such as large thermal anomalies in the upper mantle southward of La Palma, as well as fracture en echelon zones associable to a slow active process of dislocation related to the recent volcanism in the southern half of the island. The results obtained for La Palma as a test site testify to the usefulness of the developed gravity inversion methodology for structural studies on islands in general.
12 December 2013 in Bulletin of Volcanology
Journal Article
BSBenoît Smets
Benoît SmetsNDNicolas D'Oreye
Nicolas D'OreyeFKFrançois Kervyn
François Kervyn
MKMatthieu Kervyn
Matthieu KervynFAFabien Albino
Fabien AlbinoMYMathieu M. Yalire
Mathieu M. Yalire
+23
12 December 2022 in Scientific Reports
Journal Article
Jose FernandezJEJoaquin Escayo
Joaquin Escayo
ACAntonio G. Camacho
Antonio G. Camacho
MPMimmo Palano
Mimmo Palano
Juan PrietoEAEumenio Ancochea
Eumenio Ancochea
+3
La Palma, Canary Islands, underwent volcanic unrest which culminated in its largest historical eruption. We study this unrest along 2021 using Interferometric Synthetic Aperture Radar (InSAR) and a new improved interpretation methodology, comparing achieved results with the crustal structure. We reproduce the final phase of La Palma volcanic unrest, highligthing a shallow magma accumulation which begins about 3.5 months before the eruption in a crustal volume charactherized by low density and fractured rocks. Our modeling, together with our improved pictures of the crustal structure, allows us to explain the location and characteristics of the eruption and to detect failed eruption paths. These can be used to explain post-eruptive phenomena and hazards to the local population, such as detected gases anomalies in La Bombilla and Puerto Naos. Our results have implications for understanding volcanic activity in the Canaries and volcano monitoring elsewhere, helping to support decision-making and providing significant insights into urban and infrastructure planning in volcanic areas.
About Me
Juan F. Prieto holds a PhD in geodesy and geomatics (Universidad Politécnica de Madrid, Spain). Since 2000, he has been teaching in the technical engineering programs in the School of Surveying, Geodesy, and Cartography Engineering (UPM). His research is developed within the framework of geodesy and geomatics, and its application to the shape and dimensions of the Earth, to natural risks (earthquakes, volcanoes, terrain instabilities), and anthropogenics, using terrestrial and space techniques, and data processing. His research also involves the development of national GNSS geodetic networks in general (Europe, Asia, and Africa), as well as of crustal displacements and gravity variations fields in volcanic and seismic areas (Spain). All these works are fundamental tools for studying the situations of volcanic crisis, or the crustal properties of the Earth and the mantle in general. Concerning geodetic monitoring, he has jointly applied new observational and data processing methodologies in Radar Synthetic Aperture Interferometry (InSAR), gravimetry and GNSS, in collaboration with other Spanish national and international research groups. He has participated in more than 50 research projects (Spanish national, EU, ESA, NASA, and other space agencies, the World Bank, and international organizations), serving as the coordinator or responsible investigator in seven of them . He has directed, or co-directed, more than 50 B.S. and M.S theses.