A Paradigm Shift in Volcanological Remote Sensing

Total Page:16

File Type:pdf, Size:1020Kb

A Paradigm Shift in Volcanological Remote Sensing remote sensing Review The Spatial and Spectral Resolution of ASTER Infrared Image Data: A Paradigm Shift in Volcanological Remote Sensing Michael S. Ramsey * and Ian T.W. Flynn Department of Geology and Environmental Science, University of Pittsburgh, 4107 O’Hara Street, Pittsburgh, PA 15260-3332, USA; [email protected] * Correspondence: [email protected] Received: 26 December 2019; Accepted: 12 February 2020; Published: 23 February 2020 Abstract: During the past two decades, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument on the Terra satellite has acquired nearly 320,000 scenes of the world’s volcanoes. This is ~10% of the data in the global ASTER archive. Many of these scenes captured volcanic activity at never before seen spatial and spectral scales, particularly in the thermal infrared (TIR) region. Despite this large archive of data, the temporal resolution of ASTER is simply not adequate to understand ongoing eruptions and assess the hazards to local populations in near real time. However, programs designed to integrate ASTER into a volcanic data sensor web have greatly improved the cadence of the data (in some cases, to as many as 3 scenes in 48 h). This frequency can inform our understanding of what is possible with future systems collecting similar data on the daily or hourly time scales. Here, we present the history of ASTER’s contributions to volcanology, highlighting unique aspects of the instrument and its data. The ASTER archive was mined to provide statistics including the number of observations with volcanic activity, its type, and the average cloud cover. These were noted for more than 2000 scenes over periods of 1, 5 and 20 years. Keywords: ASTER; thermal infrared data; volcanic processes; image archive; future concepts 1. Introduction 1.1. ASTER Instrument and History The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) instrument was launched on the NASA Terra satellite on 18 December 1999. Prior to the instrument beginning its operational phase on 4 March 2000, ASTER acquired several images including the first thermal infrared (TIR) image on 6 February (Figure1). That image was of Erta Ale volcano (Ethiopia), and initiated a long association of ASTER data with volcanological observations. ASTER was developed and built in Japan under the Japanese Ministry of Economy, Trade and Industry (METI), and is one of five Earth observing instruments on Terra. The combined science team of Japanese and United States investigators has changed over the years, however always maintaining a strong volcanological component [1,2]. During the past two decades, the data from ASTER have been applied to numerous questions and scales of surface processes, most notably for volcanic activity, e.g., [3–6]. ASTER was designed to observe the surface at multiple spatial and spectral resolutions as well as from different viewing geometries. It is actually a suite of three instruments with independent bore-sighted telescopes, originally having 14 spectral channels in the visible/near-infrared (VNIR), the shortwave infrared (SWIR), and the thermal infrared (TIR) regions [7]. The VNIR instrument (0.52–0.86 µm) has three spectral channels at a spatial resolution of 15 m/pixel paired with one channel Remote Sens. 2020, 12, 738; doi:10.3390/rs12040738 www.mdpi.com/journal/remotesensing Remote Sens. 2020, 12, 738 2 of 40 Remote Sens. 2020, 12, x FOR PEER REVIEW 2 of 39 oriented in a backward look direction for the creation of digital elevation models (DEMs). The SWIR channel oriented in a backward look direction for the creation of digital elevation models (DEMs). µ instrumentThe SWIR (1.6–2.43instrumentm) (1.6–2.43 unfortunately μm) unfortunately failed in 2008,failed butin 2008, originally but originally had six had channels six channels at a spatialat a resolutionspatial resolution of 30 m/pixel. of 30 Finally, m/pixel. and Finally, perhaps and most perhaps important most forimportant many aspects for many of volcanological aspects of remotevolcanological sensing, remote the TIR sensing, instrument the TIR (8.13–11.65 instrumentµm) (8.13–11.65 has five μ channelsm) has five at achannels spatial at resolution a spatial of 90resolution m/pixel. of During 90 m/pixel. the lifetime During ofthe the lifetime mission, of the ASTER mission, has ASTER acquired has overacquired 3.5 millionover 3.5 individual million scenes—approximatelyindividual scenes—approximately 22% of which 22% were of which collected were collected at night. at Here, night. weHere, describe we describe the two-decade the two- historydecade of history ASTER, of specific ASTER, programs specific programs to improve to the improve observational the observational frequency frequency of volcanoes, of volcanoes, and present examplesand present of those examples data. of those data. FigureFigure 1. 1.The The first first Advanced Advanced SpaceborneSpaceborne Thermal Emis Emissionsion and and Reflection Reflection Radiometer Radiometer (ASTER) (ASTER) multispectralmultispectral thermal thermal infraredinfrared (TIR)(TIR) imageimage acquired on on 6 6 February February 2000, 2000, before before the the start start of ofthe the instrument’sinstrument’s science science operational operational phase. phase. Erta Erta Ale volcano,Ale volcano, Ethiopia Ethiopia (summit (summit location: location: 13.60◦ N,13.60°N, 40.67◦ E), is40.67°E), shown using is shown a decorrelation using a decorrelation stretch (DCS) stretch of (DCS the) TIRof the bands TIR bands 14, 12, 14, 10 12, in 10 red, in red, green, green, and and blue, respectively.blue, respectively. Color variationsColor variations are mainly are mainly caused caused by rock by rock and and soil compositionalsoil compositional diff differences,erences, and and only possibleonly possible with the with ASTER the AS multispectralTER multispectral TIR TIR data. data. The The blues blues andand purple colors colors are are indicative indicative of of dominantlydominantly basaltic basaltic lava lava flows. flows. The The smallsmall cluster of white white pixels pixels in in the the lower lower central central part part of ofthe the image image is theis the summit summit lava lava lake lake thermal thermal anomaly. anomaly. TheThe ASTER DCS DCS data data are are overlain overlain on on a visible a visible Google Google Earth Earth imageimage for for context. context. Image Image credit:credit: NASANASA/METI/AIST/Japan/METI/AIST/Japan Space Space Sy Systems,stems, and and U.S./Japan U.S./Japan ASTER ASTER ScienceScience Team. Team. Remote Sens. 2020, 12, 738 3 of 40 Remote Sens. 2020, 12, x FOR PEER REVIEW 3 of 39 1.2. Twenty Years ofof VolcanicVolcanic StudiesStudies UsingUsing ASTERASTER DataData The ASTER Science Team created useful derived sciencescience products that have benefitedbenefited numerous scientificscientific fieldsfields such such as volcanology.as volcanology. These These include include a robust a temperaturerobust temperature emissivity emissivity separation separation algorithm foralgorithm the first for orbital the first high orbital spatial high resolution spatial resolution multispectral multispectral TIR data TIR [8], programsdata [8], programs such as thesuch Science as the TeamScience Acquisition Team Acquisition Request (STAR)Request to (STAR) acquire to data acquir focusede data on focused important on important science questions science ofquestions individual of usersindividual/teams, users/teams, as well as the as abilitywell as to the generate ability DEMsto generate [9]. These DEMs individual-scene [9]. These individual-scene DEMs of 60 byDEMs 60 km of were60 by later60 km composited were later globallycomposited into globally the ASTER into Globalthe ASTER DEM Global or GDEM—version DEM or GDEM—version 3 of which was3 of releasedwhich was in Augustreleased 2019 in August [10,11]. 2019 [10,11]. Arguably, volcanologyvolcanology is one ofof thethe scientificscientific disciplinesdisciplines on whichwhich ASTER data have had the greatest impact.impact. InIn orderorder to to quantify quantify this this impact impact and and gather gather all volcanologyall volcanology related related studies studies together together into oneinto referenceone reference document, document, we have we performed have performed an extensive an extensive literature literature review (Appendix review (SupplementaryA). This found 271materials). peer-reviewed This found publications 271 peer-reviewed from 1 January publications 1995 to from 1 December 1 January 2019, 1995 anto average1 December of nearly 2019, an 11 peraverage year of (Figure nearly2). 11 Papers per year published (Figure 2). prior Papers to the published Terra launch prior were to the considered Terra launch precursory were considered studies, commonlyprecursory describingstudies, commonly how the future describing ASTER how data th woulde future be usedASTER for certaindata would volcanic be used studies. for Thiscertain list ofvolcanic271 publications studies. Thiswas list subdividedof 271 publications into 12 was categories subdivided based into on 12 the categories volcanic based focus on of the the volcanic papers. Thefocus category of the namespapers. and The number category of papersnames inand those numb categorieser of papers (shown in inthose parentheses) categories are: (shown Analogs in (3),parentheses) Calibration are: (4), Analogs Lava Flows (3), Calibration (4), Gas/Plumes (4), Lava (30), GeothermalFlows (4), Gas/Plumes (9), Mapping (30), (54), Geothermal Modeling (16),(9), MonitoringMapping (54), (96), Modeling
Recommended publications
  • And Gas-Based Geochemical Prospecting Of
    Water- and gas-based geochemical prospecting of geothermal reservoirs in the Tarapacà and Antofagasta regions of northern Chile Tassi, F.1, Aguilera, F.2, Vaselli, O.1,3, Medina, E.2, Tedesco, D.4,5, Delgado Huertas, A.6, Poreda, R.7 1) Department of Earth Sciences, University of Florence, Via G. La Pira 4, 50121, Florence, Italy 2) Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, 1280, Antofagasta, Chile 3) CNR-IGG Institute of Geosciences and Earth Resources, Via G. La Pira 4, 50121, Florence, Italy 4)Department of Environmental Sciences, 2nd University of Naples, Via Vivaldi 43, 81100 Caserta, Italy 5) CNR-IGAG National Research Council, Institute of Environmental Geology and Geo-Engineering, Pzz.e A. Moro, 00100 Roma, Italy. 6) CSIS Estacion Experimental de Zaidin, Prof. Albareda 1, 18008, Granada, Spain. 7) Department of Earth and Environmental Sciences, 227 Hutchinson Hall, Rochester, NY 14627, U.S.A.. Studied area The Andean Central Volcanic Zone, which runs parallel the Central Andean Cordillera crossing from North to This study is mainly focused on the geochemical characteristics of water and gas South the Tarapacà and Antofagasta regions of northern Chile, consists of several volcanoes that have shown phases of thermal fluids discharging in several geothermal areas of northern Chile historical and present activity (e.g. Tacora, Guallatiri, Isluga, Ollague, Putana, Lascar, Lastarria). Such an intense (Fig. 1); volcanism is produced by the subduction process thrusting the oceanic Nazca Plate beneath the South America Plate. The anomalous geothermal gradient related to the geodynamic assessment of this extended area gives El Tatio, Apacheta, Surire, Puchuldiza-Tuya also rise to intense geothermal activity not necessarily associated with the volcanic structures.
    [Show full text]
  • Community Risk Assessment
    COMMUNITY RISK ASSESSMENT Squamish-Lillooet Regional District Abstract This Community Risk Assessment is a component of the SLRD Comprehensive Emergency Management Plan. A Community Risk Assessment is the foundation for any local authority emergency management program. It informs risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflects their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property. SLRD Emergency Program [email protected] Version: 1.0 Published: January, 2021 SLRD Community Risk Assessment SLRD Emergency Management Program Executive Summary This Community Risk Assessment (CRA) is a component of the Squamish-Lillooet Regional District (SLRD) Comprehensive Emergency Management Plan and presents a survey and analysis of known hazards, risks and related community vulnerabilities in the SLRD. The purpose of a CRA is to: • Consider all known hazards that may trigger a risk event and impact communities of the SLRD; • Identify what would trigger a risk event to occur; and • Determine what the potential impact would be if the risk event did occur. The results of the CRA inform risk reduction strategies, emergency response and recovery plans, and other elements of the SLRD emergency program. Evaluating risks is a requirement mandated by the Local Authority Emergency Management Regulation. Section 2(1) of this regulation requires local authorities to prepare emergency plans that reflect their assessment of the relative risk of occurrence, and the potential impact, of emergencies or disasters on people and property.
    [Show full text]
  • Eruptive Activity of Planchón-Peteroa Volcano for Period 2010-2011, Southern Andean Volcanic Zone, Chile
    Andean Geology 43 (1): 20-46. January, 2016 Andean Geology doi: 10.5027/andgeoV43n1-a02 www.andeangeology.cl Eruptive activity of Planchón-Peteroa volcano for period 2010-2011, Southern Andean Volcanic Zone, Chile *Felipe Aguilera1, 2, Óscar Benavente3, Francisco Gutiérrez3, Jorge Romero4, Ornella Saltori5, Rodrigo González6, Mariano Agusto7, Alberto Caselli8, Marcela Pizarro5 1 Servicio Nacional de Geología y Minería, Avda. Santa María 0104, Santiago, Chile. 2 Present address: Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avda. Angamos 0610, Antofagasta, Chile. [email protected] 3 Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile. [email protected]; [email protected] 4 Centro de Investigación y Difusión de Volcanes de Chile, Proyecto Archivo Nacional de Volcanes, Santiago, Chile. [email protected] 5 Programa de Doctorado en Ciencias mención Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile. [email protected]; [email protected] 6 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Avda. Angamos 0610, Antofagasta, Chile. [email protected] 7 Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Ciudad Universitaria, Pabellón 2, 1428EHA, Buenos Aires, Argentina. [email protected] 8 Laboratorio de Estudio y Seguimiento de Volcanes Activos (LESVA), Universidad Nacional de Río Negro, Roca 1242, (8332) Roca, Argentina. [email protected] * Corresponding author: [email protected] ABSTRACT. Planchón-Peteroa volcano started a renewed eruptive period between January 2010 and July 2011. This eruptive period was characterized by the occurrence of 4 explosive eruptive phases, dominated by low-intensity phreatic activity, which produced almost permanent gas/steam columns (200-800 m height over the active crater).
    [Show full text]
  • Full-Text PDF (Final Published Version)
    Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H.
    [Show full text]
  • Geología De La Cadena Volcánica Paniri-Toconce, Zona Volcánica Central, Altiplano De La Región De Antofagasta, Chile
    Geología de la cadena volcánica Paniri-Toconce, Zona Volcánica Central, Altiplano de la Región de Antofagasta, Chile Edmundo Polanco 1*, Jorge Clavero 1 y Aldo Giavelli 1 1 Energía Andina S.A. Darío Urzúa 2165, Providencia, Santiago, Chile *E-mail: [email protected] conformado por los volcanes del León (5.753 m s.n.m.) y Resumen. La cadena volcánica del Paniri-Toconce (NW- Lagunita (5.404 m s.n.m.) que se ubican al W del volcán SE) localizada en el Altiplano de la Región de Antofagasta Toconce. El Volcán Lagunita corresponde a un se caracteriza por un fuerte control estructural a través de estratovolcán más antiguo fuertemente erosionado, de más su evolución durante el Pleistoceno. Esta cadena volcánica de 7 km de diámetro en dirección E-W que presenta de más de 30 km de longitud es dominada por dacitas de anfíbola y biotita y subordinadamente por andesita de importantes zonas afectadas por procesos de alteración piroxeno±anfíbola±biotita e incluye al domo torta más hidrotermal y está constituido por coladas de lava voluminoso del planeta, el Domo Chao, donde nuevas andesíticas y dacíticas (59 y 65-66% en peso de SiO2) y dataciones Ar/Ar señalan su actividad culminaría en el depósitos piroclásticos de bloques y ceniza. El Volcán del Pleistoceno Superior. Evidencias de terreno, petrográficas León es un estratovolcán de más de 6 km de diámetro y geoquímicas indican la cristalización fraccionada como conformado principalmente por coladas de lava andesíticas proceso dominante durante la evolución de los magmas y dacíticas de piroxeno y anfíbola aunque también tiene que dieron origen a las rocas a los distintos centros depósitos piroclásticos de bloques y ceniza asociados.
    [Show full text]
  • Effects of Volcanism, Crustal Thickness, and Large Scale Faulting on the He Isotope Signatures of Geothermal Systems in Chile
    PROCEEDINGS, Thirty-Eighth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 11-13, 2013 SGP-TR-198 EFFECTS OF VOLCANISM, CRUSTAL THICKNESS, AND LARGE SCALE FAULTING ON THE HE ISOTOPE SIGNATURES OF GEOTHERMAL SYSTEMS IN CHILE Patrick F. DOBSON1, B. Mack KENNEDY1, Martin REICH2, Pablo SANCHEZ2, and Diego MORATA2 1Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720 USA 2Departamento de Geología y Centro de Excelencia en Geotermia de los Andes, Universidad de Chile, Santiago, CHILE [email protected] agree with previously published results for the ABSTRACT Chilean Andes. The Chilean cordillera provides a unique geologic INTRODUCTION setting to evaluate the influence of volcanism, crustal thickness, and large scale faulting on fluid Measurement of 3He/4He in geothermal water and gas geochemistry in geothermal systems. In the Central samples has been used to guide geothermal Volcanic Zone (CVZ) of the Andes in the northern exploration efforts (e.g., Torgersen and Jenkins, part of Chile, the continental crust is quite thick (50- 1982; Welhan et al., 1988) Elevated 3He/4He ratios 70 km) and old (Mesozoic to Paleozoic), whereas the (R/Ra values greater than ~0.1) have been interpreted Southern Volcanic Zone (SVZ) in central Chile has to indicate a mantle influence on the He isotopic thinner (60-40 km) and younger (Cenozoic to composition, and may indicate that igneous intrusions Mesozoic) crust. In the SVZ, the Liquiñe-Ofqui Fault provide the primary heat source for the associated System, a major intra-arc transpressional dextral geothermal fluids. Studies of helium isotope strike-slip fault system which controls the magmatic compositions of geothermal fluids collected from activity from 38°S to 47°S, provides the opportunity wells, hot springs and fumaroles within the Basin and to evaluate the effects of regional faulting on Range province of the western US (Kennedy and van geothermal fluid chemistry.
    [Show full text]
  • A Structural and Geochronological Study of Tromen Volcano
    Volcanism in a compressional Andean setting: A structural and geochronological study of Tromen volcano (Neuqu`enprovince, Argentina) Olivier Galland, Erwan Hallot, Peter Cobbold, Gilles Ruffet, Jean De Bremond d'Ars To cite this version: Olivier Galland, Erwan Hallot, Peter Cobbold, Gilles Ruffet, Jean De Bremond d'Ars. Vol- canism in a compressional Andean setting: A structural and geochronological study of Tromen volcano (Neuqu`enprovince, Argentina). Tectonics, American Geophysical Union (AGU), 2007, 26 (4), pp.TC4010. <10.1029/2006TC002011>. <insu-00180007> HAL Id: insu-00180007 https://hal-insu.archives-ouvertes.fr/insu-00180007 Submitted on 29 Jun 2016 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. TECTONICS, VOL. 26, TC4010, doi:10.1029/2006TC002011, 2007 Volcanism in a compressional Andean setting: A structural and geochronological study of Tromen volcano (Neuque´n province, Argentina) Olivier Galland,1,2 Erwan Hallot,1 Peter R. Cobbold,1 Gilles Ruffet,1 and Jean de Bremond d’Ars1 Received 28 June 2006; revised 6 February 2007; accepted 16 March 2007; published 2 August 2007. [1] We document evidence for growth of an active [3] In contrast, a context of crustal thickening, where the volcano in a compressional Andean setting.
    [Show full text]
  • Lawrence Berkeley National Laboratory Recent Work
    Lawrence Berkeley National Laboratory Recent Work Title Assessment of high enthalpy geothermal resources and promising areas of Chile Permalink https://escholarship.org/uc/item/9s55q609 Authors Aravena, D Muñoz, M Morata, D et al. Publication Date 2016 DOI 10.1016/j.geothermics.2015.09.001 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Assessment of high enthalpy geothermal resources and promising areas of Chile Author links open overlay panel DiegoAravena ab MauricioMuñoz ab DiegoMorata ab AlfredoLahsen ab Miguel ÁngelParada ab PatrickDobson c Show more https://doi.org/10.1016/j.geothermics.2015.09.001 Get rights and content Highlights • We ranked geothermal prospects into measured, Indicated and Inferred resources. • We assess a comparative power potential in high-enthalpy geothermal areas. • Total Indicated and Inferred resource reaches 659 ± 439 MWe divided among 9 areas. • Data from eight additional prospects suggest they are highly favorable targets. • 57 geothermal areas are proposed as likely future development targets. Abstract This work aims to assess geothermal power potential in identified high enthalpy geothermal areas in the Chilean Andes, based on reservoir temperature and volume. In addition, we present a set of highly favorable geothermal areas, but without enough data in order to quantify the resource. Information regarding geothermal systems was gathered and ranked to assess Indicated or Inferred resources, depending on the degree of confidence that a resource may exist as indicated by the geoscientific information available to review. Resources were estimated through the USGS Heat in Place method. A Monte Carlo approach is used to quantify variability in boundary conditions.
    [Show full text]
  • Mud Volcano Eruptions and Earthquakes in the Northern Apennines and Sicily, Italy
    Tectonophysics 474 (2009) 723–735 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Mud volcano eruptions and earthquakes in the Northern Apennines and Sicily, Italy Marco Bonini Consiglio Nazionale delle Ricerche, Istituto di Geoscienze e Georisorse, Via G. La Pira 4, I-50121 Florence, Italy article info abstract Article history: The relations between earthquakes and the eruption of mud volcanoes have been investigated at the Pede–Apennine Received 28 November 2008 margin of the Northern Apennines and in Sicily. Some of these volcanoes experiencederuptionsorincreased Received in revised form 1 April 2009 activity in connection with historical seismic events, showing a good correlation with established thresholds of Accepted 20 May 2009 hydrological response (liquefaction) to earthquakes. However, the majority of eruptions have been documented to Available online 25 May 2009 be independent of seismic activity, being mud volcanoes often not activated even when the earthquakes were of suitable magnitude and the epicentre at the proper distance for the triggering. This behaviour suggests that Keywords: fi fl Mud volcanoes paroxysmal activity of mud volcanoes depends upon the reaching of a speci c critical state dictated by internal uid Vents pressure, and implies that the strain caused by the passage of seismic waves can activate only mud volcanoes in near- Earthquakes critical conditions (i.e., close to the eruption). Seismogenic faults, such as the Pede–Apennine thrust, often Eruptions structurally control the fluid reservoirs of mud volcanoes, which are frequently located at the core of thrust-related Northern Apennines folds. Such an intimate link enables mud volcanoes to represent features potentially suitable for recording Sicily perturbations associated with the past and ongoing tectonic activity of the controlling fault system.
    [Show full text]
  • Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H
    St. Louis Area Earthquake Hazards Mapping Project: Seismic and Liquefaction Hazard Maps by Chris H. Cramer, Robert A. Bauer, Jae-won Chung, J. David Rogers, Larry Pierce, Vicki Voigt, Brad Mitchell, David Gaunt, Robert A. Wil- liams, David Hoffman, Gregory L. Hempen, Phyllis J. Steckel, Oliver S. Boyd, Connor M. Watkins, Kathleen Tucker, and Natasha S. McCallister ABSTRACT We present probabilistic and deterministic seismic and liquefac- (NMSZ) earthquake sequence. This sequence produced modi- tion hazard maps for the densely populated St. Louis metropolitan fied Mercalli intensity (MMI) for locations in the St. Louis area area that account for the expected effects of surficial geology on that ranged from VI to VIII (Nuttli, 1973; Bakun et al.,2002; earthquake ground shaking. Hazard calculations were based on a Hough and Page, 2011). The region has experienced strong map grid of 0.005°, or about every 500 m, and are thus higher in ground shaking (∼0:1g peak ground acceleration [PGA]) as a resolution than any earlier studies. To estimate ground motions at result of prehistoric and contemporary seismicity associated with the surface of the model (e.g., site amplification), we used a new the major neighboring seismic source areas, including the Wa- detailed near-surface shear-wave velocity model in a 1D equiva- bashValley seismic zone (WVSZ) and NMSZ (Fig. 1), as well as lent-linear response analysis. When compared with the 2014 U.S. a possible paleoseismic earthquake near Shoal Creek, Illinois, Geological Survey (USGS) National Seismic Hazard Model, about 30 km east of St. Louis (McNulty and Obermeier, 1997). which uses a uniform firm-rock-site condition, the new probabi- Another contributing factor to seismic hazard in the St.
    [Show full text]
  • Patagonia Luxury Hiking Excursion
    Patagonia Luxury Hiking Excursion Please note that all of the itineraries listed in our web site are actual private tour itineraries we have prepared for clients over the past 12-18 months. By the very nature of what we do, each private tour itinerary is custom, exclusive and unique unto itself. Our over-riding goal is to create lifelong memories that you and your family will forever carry deep within your hearts. Overview Though our past hikes on the Milford Track (New Zealand), Inca Trail (Machu Picchu), Glacier (U.S.), and various areas of Switzerland and Austria were particularly memorable, we must confess that the hiking, horseback riding, and spectacular setting of, relatively inaccessible, Patagonia is unparalleled. The critical contrast is Patagonia’s pristine remoteness: no mass tourism or crowded hiking trails here! When hiking the wide range of areas in Patagonia, it is easy to see how this vast landscape still has hundreds of unnamed mountains, with many points inaccessible and unexplored. Located at the tip of the South American continent, the outstanding national parks (Torres del Paine!) and private reserves stretch across Chile and Argentina, divided by the Andes Mountains. The features of Patagonia are remarkable: wild rivers, muddy rainforests, glaciated peaks, granted monoliths, and vast steppes. This is a place for reflection, deep solitude, and unforgettable outdoor activities. Best Travel Time: Fall Winter Spring CHILE ARGENTINA Day 1 Temperature Range Temperature Range Fly to Santiago Highs: Mid 80’s Highs: Low 80’s Through our sister company, premium air provider Lows: Mid 50’s Lows: High 60’s TRAVNET, we may assist with your international airfare, as Area Area well as with mileage points conversion.
    [Show full text]
  • Response of Mud Volcanoes to Earthquakes: Role of Static Strains and Frequency-Dependence of Ground Motion
    IAVCEI 2013 Scientific Assembly - July 20 - 24, Kagoshima, Japan Forecasting Volcanic Activity - Reading and translating the messages of nature for society 1P2_2B-O1 Room A3 Date/Time: July 21 17:00-17:15 Response of mud volcanoes to earthquakes: role of static strains and frequency-dependence of ground motion Michael Manga1, Maxwell Rudolph2, Marco Bonini3 1University of California, Berkeley, USA, 2University of Colorado, Boulder, USA, 3Consiglio Nazionale delle Ricerche, Florence, Italy E-mail: [email protected] Distant earthquakes can trigger the eruption of mud volcanoes. We report observations of the response of the Davis-Schrimpf, California, mud volcanoes to 2 earthquakes and non-response to 4 other earthquakes. We find that eruptions are triggered by dynamic stresses and that the mud volcanoes are more sensitive to long period seismic waves than short period waves with the same amplitude. These observations are consistent with models in which fluid mobility is enhanced by dislodging bubbles by the time-varying flows produced by seismic waves. In the Northern Apennines, Italy, we document responses and non-responses to the May-June 2012 Emilia seismic sequence. Here we find that discharge only increases where dikes under the vents are unclamped by the static stresses produced by the earthquakes. Mud volcanoes can thus respond to static stress changes (if feeder dikes are unclamped) and dynamic stresses produced by seismic waves (possibly by mobilizing bubbles). ©IAVCEI 2013 Scientific Assembly. All rights reserved. 290 IAVCEI
    [Show full text]