Interpretation of Nisyros volcanic terrain using land surface parameters generated from the ASTER Global Digital Elevation Model
Identifieur interne : 000008 ( PascalFrancis/Checkpoint ); précédent : 000007; suivant : 000009Interpretation of Nisyros volcanic terrain using land surface parameters generated from the ASTER Global Digital Elevation Model
Auteurs : Dimitrios Zouzias [Grèce] ; George Ch. Miliaresis [Grèce] ; Karen St. Seymour [Grèce, Canada]Source :
- Journal of volcanology and geothermal research [ 0377-0273 ] ; 2011.
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Abstract
To model the morphotectonic evolution of Nisyros stratovolcano in the Aegean Volcanic Arc (36° 35' N, 27° 10' E), a 30 m resolution ASTER GDEM was used. Nisyros is characterized by a relative pristine volcanic terrain. Elevation, slope and aspect images, the corresponding frequency distributions and rose diagrams enabled the geomorphometric analysis of Nisyros revealing the major geomorphological structures that are associated to both endogenetic and exogenetic processes acting on the island either new or previously reported in the literature. New elements include the number, loci of issue, relative age, ogive structures of the voluminous precalderan Nikia flows and their contact relationships with the Avlaki flows. The tectonic control, fine feature morphology and flow paths of lavas and smaller domes associated with the main postcalderan domes become visually apparent. Particularities of the hydrographic network accentuate and bring forward non-mapped radial faults. Intense landslide scarring and the volcanic stratigraphy of the intact units were revealed in the northeastern quadrant of Nisyros. Major, new volcano-tectonic features include the division of the island into three northwesterly trending sectors and the dipping of Nisyros towards the southeast as a result of segmentation by two major ring faults the Kos Ring Fault (KRF) and Perigussa Ring trapdoor Fault (PRF) which represent ring faults of the Kos sagging-caldera. The ASTER GDEM has provided suitable thematic information content in the geomorphometric analysis of Nisyros and therefore it offers a reconnaissance tool in the geomorphological analysis of a volcanic landscape.
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Miliaresis</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>Rion 26504, Hellas</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Rion 26504, Hellas</wicri:noRegion></affiliation></author><author><name sortKey="Seymour, Karen St" sort="Seymour, Karen St" uniqKey="Seymour K" first="Karen St." last="Seymour">Karen St. Seymour</name><affiliation wicri:level="1"><inist:fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>Rion 26504, Hellas</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Rion 26504, Hellas</wicri:noRegion></affiliation><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Department of Geography, Urban Planning and Environment, Concordia University</s1><s2>Montreal, H3G1M8</s2><s3>CAN</s3><sZ>3 aut.</sZ></inist:fA14><country>Canada</country><wicri:noRegion>Montreal, H3G1M8</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno><imprint><date when="2011">2011</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Kos</term><term>calderas</term><term>domes</term><term>fine-grained materials</term><term>flow</term><term>frequency</term><term>global</term><term>interpretation</term><term>landscapes</term><term>landslides</term><term>lava</term><term>models</term><term>morphology</term><term>networks</term><term>radial faults</term><term>relative age</term><term>segmentation</term><term>slopes</term><term>stratigraphy</term><term>stratovolcanoes</term><term>tectonic controls</term><term>tectonics</term><term>terrains</term><term>volcanic arcs</term><term>volcanoes</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Interprétation</term><term>Terrain</term><term>Monde</term><term>Modèle</term><term>Stratovolcan</term><term>Arc volcanique</term><term>Versant</term><term>Fréquence</term><term>Age relatif</term><term>Ecoulement</term><term>Contrôle tectonique</term><term>Fraction fine</term><term>Morphologie</term><term>Lave</term><term>Dôme</term><term>Réseau</term><term>Faille radiale</term><term>Glissement terrain</term><term>Stratigraphie</term><term>Volcan</term><term>Tectonique</term><term>Segmentation</term><term>Caldeira</term><term>Paysage</term><term>Ile Cos</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Interprétation</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">To model the morphotectonic evolution of Nisyros stratovolcano in the Aegean Volcanic Arc (36° 35' N, 27° 10' E), a 30 m resolution ASTER GDEM was used. Nisyros is characterized by a relative pristine volcanic terrain. Elevation, slope and aspect images, the corresponding frequency distributions and rose diagrams enabled the geomorphometric analysis of Nisyros revealing the major geomorphological structures that are associated to both endogenetic and exogenetic processes acting on the island either new or previously reported in the literature. New elements include the number, loci of issue, relative age, ogive structures of the voluminous precalderan Nikia flows and their contact relationships with the Avlaki flows. The tectonic control, fine feature morphology and flow paths of lavas and smaller domes associated with the main postcalderan domes become visually apparent. Particularities of the hydrographic network accentuate and bring forward non-mapped radial faults. Intense landslide scarring and the volcanic stratigraphy of the intact units were revealed in the northeastern quadrant of Nisyros. Major, new volcano-tectonic features include the division of the island into three northwesterly trending sectors and the dipping of Nisyros towards the southeast as a result of segmentation by two major ring faults the Kos Ring Fault (KRF) and Perigussa Ring trapdoor Fault (PRF) which represent ring faults of the Kos sagging-caldera. The ASTER GDEM has provided suitable thematic information content in the geomorphometric analysis of Nisyros and therefore it offers a reconnaissance tool in the geomorphological analysis of a volcanic landscape.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0377-0273</s0></fA01><fA02 i1="01"><s0>JVGRDQ</s0></fA02><fA03 i2="1"><s0>J. volcanol. geotherm. res.</s0></fA03><fA05><s2>200</s2></fA05><fA06><s2>3-4</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Interpretation of Nisyros volcanic terrain using land surface parameters generated from the ASTER Global Digital Elevation Model</s1></fA08><fA11 i1="01" i2="1"><s1>ZOUZIAS (Dimitrios)</s1></fA11><fA11 i1="02" i2="1"><s1>MILIARESIS (George Ch.)</s1></fA11><fA11 i1="03" i2="1"><s1>SEYMOUR (Karen St.)</s1></fA11><fA14 i1="01"><s1>Department of Geology, University of Patras</s1><s2>Rion 26504, Hellas</s2><s3>GRC</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Department of Geography, Urban Planning and Environment, Concordia University</s1><s2>Montreal, H3G1M8</s2><s3>CAN</s3><sZ>3 aut.</sZ></fA14><fA20><s1>159-170</s1></fA20><fA21><s1>2011</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>17236</s2><s5>354000194630180050</s5></fA43><fA44><s0>0000</s0><s1>© 2011 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>1 p.1/4</s0></fA45><fA47 i1="01" i2="1"><s0>11-0218061</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Journal of volcanology and geothermal research</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fC01 i1="01" l="ENG"><s0>To model the morphotectonic evolution of Nisyros stratovolcano in the Aegean Volcanic Arc (36° 35' N, 27° 10' E), a 30 m resolution ASTER GDEM was used. Nisyros is characterized by a relative pristine volcanic terrain. Elevation, slope and aspect images, the corresponding frequency distributions and rose diagrams enabled the geomorphometric analysis of Nisyros revealing the major geomorphological structures that are associated to both endogenetic and exogenetic processes acting on the island either new or previously reported in the literature. New elements include the number, loci of issue, relative age, ogive structures of the voluminous precalderan Nikia flows and their contact relationships with the Avlaki flows. The tectonic control, fine feature morphology and flow paths of lavas and smaller domes associated with the main postcalderan domes become visually apparent. Particularities of the hydrographic network accentuate and bring forward non-mapped radial faults. Intense landslide scarring and the volcanic stratigraphy of the intact units were revealed in the northeastern quadrant of Nisyros. Major, new volcano-tectonic features include the division of the island into three northwesterly trending sectors and the dipping of Nisyros towards the southeast as a result of segmentation by two major ring faults the Kos Ring Fault (KRF) and Perigussa Ring trapdoor Fault (PRF) which represent ring faults of the Kos sagging-caldera. The ASTER GDEM has provided suitable thematic information content in the geomorphometric analysis of Nisyros and therefore it offers a reconnaissance tool in the geomorphological analysis of a volcanic landscape.</s0></fC01><fC02 i1="01" i2="2"><s0>001E01F01</s0></fC02><fC02 i1="02" i2="2"><s0>222A01</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Interprétation</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>interpretation</s0><s5>01</s5></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Interpretación</s0><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Terrain</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>terrains</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Monde</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>global</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Mundo</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Modèle</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>models</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" 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l="SPA"><s0>Europa</s0><s2>564</s2></fC07><fN21><s1>143</s1></fN21><fN44 i1="01"><s1>OTO</s1></fN44><fN82><s1>OTO</s1></fN82></pA></standard></inist><affiliations><list><country><li>Canada</li><li>Grèce</li></country></list><tree><country name="Grèce"><noRegion><name sortKey="Zouzias, Dimitrios" sort="Zouzias, Dimitrios" uniqKey="Zouzias D" first="Dimitrios" last="Zouzias">Dimitrios Zouzias</name></noRegion><name sortKey="Miliaresis, George Ch" sort="Miliaresis, George Ch" uniqKey="Miliaresis G" first="George Ch." last="Miliaresis">George Ch. Miliaresis</name><name sortKey="Seymour, Karen St" sort="Seymour, Karen St" uniqKey="Seymour K" first="Karen St." last="Seymour">Karen St. Seymour</name></country><country name="Canada"><noRegion><name sortKey="Seymour, Karen St" sort="Seymour, Karen St" uniqKey="Seymour K" first="Karen St." last="Seymour">Karen St. Seymour</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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|wiki= Wicri/Terre
|area= NissirosV1
|flux= PascalFrancis
|étape= Checkpoint
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|clé= Pascal:11-0218061
|texte= Interpretation of Nisyros volcanic terrain using land surface parameters generated from the ASTER Global Digital Elevation Model
}}
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