Color and Morphology of Lava Flows on Io

Analyses of color and morphologic changes in Voyager images of lava flows on Io were conducted to extend previous flow studies to additional volcanoes in preparation for comparison to Galileo data. Blue and orange filter images of Atar, Daedalus, and Ra Paterae were examined to identify systematic d...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Icarus (New York, N.Y. 1962) N.Y. 1962), 2000-12, Vol.148 (2), p.407-418
Hauptverfasser: Piatek, Jennifer L., McElfresh, Sarah B.Z., Byrnes, Jeffrey M., Hale, Amy Snyder, Crown, David A.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 418
container_issue 2
container_start_page 407
container_title Icarus (New York, N.Y. 1962)
container_volume 148
creator Piatek, Jennifer L.
McElfresh, Sarah B.Z.
Byrnes, Jeffrey M.
Hale, Amy Snyder
Crown, David A.
description Analyses of color and morphologic changes in Voyager images of lava flows on Io were conducted to extend previous flow studies to additional volcanoes in preparation for comparison to Galileo data. Blue and orange filter images of Atar, Daedalus, and Ra Paterae were examined to identify systematic downflow decreases in blue/orange reflectivity suggested in earlier studies as diagnostic of color changes in cooled sulfur flows. Analyses of the color and morphology of 21 lava flows were conducted at these volcanoes, with additional morphologic analysis of lava flows at Agni, Masaaw, Mbali, Shoshu, and Talos Paterae. A total of 66 lava flows of up to 245 km in length were mapped to identify morphologic changes consistent with the rheologic changes expected to occur in sulfur flows. Although downflow color changes are observed, the trends are not consistent, even at the same edifice. Individual flows exhibit a statistically significant increase in blue/orange ratio, decrease in blue/orange ratio, or a lack of progressive downflow color variation. Color changes have similar magnitudes downflow and across flow, and the color ranges observed are similar from volcano to volcano, suggesting that similar processes are controlling color ratios at these edifices. In addition, using flow widening and branching as an indicator of the low viscosity exhibited by sulfur cooling from high temperatures, these flows do not exhibit morphologic changes consistent with the systematic behavior expected from the simple progressive cooling of sulfur.
doi_str_mv 10.1006/icar.2000.6501
format Article
fullrecord <record><control><sourceid>elsevier_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1006_icar_2000_6501</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0019103500965011</els_id><sourcerecordid>S0019103500965011</sourcerecordid><originalsourceid>FETCH-LOGICAL-a264t-f7c160efccd9fa27db07a3e27444b309bfb23e3bbf396a5afac9e36ea75b98c53</originalsourceid><addsrcrecordid>eNp1jzFPwzAQRi0EEqWwMntkSTjHsROPKKJQKYgFZuvs2GAU4squivrvSVRWptNJ9-77HiG3DEoGIO-DxVRWAFBKAeyMrBgoKCpZ83OyAmCqYMDFJbnK-Wu-Eq3iK3LXxTEmitNAX2Lafc7bx5FGT3s8IN2M8SfTONFtvCYXHsfsbv7mmrxvHt-656J_fdp2D32Bc9K-8I1lEpy3dlAeq2Yw0CB3VVPXteGgjDcVd9wYz5VEgR6tclw6bIRRrRV8TcrTX5tizsl5vUvhG9NRM9CLp1489eKpF88ZaE-Am1sdgks62-Am64aQnN3rIYb_0F9HKFjh</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Color and Morphology of Lava Flows on Io</title><source>ScienceDirect Journals (5 years ago - present)</source><creator>Piatek, Jennifer L. ; McElfresh, Sarah B.Z. ; Byrnes, Jeffrey M. ; Hale, Amy Snyder ; Crown, David A.</creator><creatorcontrib>Piatek, Jennifer L. ; McElfresh, Sarah B.Z. ; Byrnes, Jeffrey M. ; Hale, Amy Snyder ; Crown, David A.</creatorcontrib><description>Analyses of color and morphologic changes in Voyager images of lava flows on Io were conducted to extend previous flow studies to additional volcanoes in preparation for comparison to Galileo data. Blue and orange filter images of Atar, Daedalus, and Ra Paterae were examined to identify systematic downflow decreases in blue/orange reflectivity suggested in earlier studies as diagnostic of color changes in cooled sulfur flows. Analyses of the color and morphology of 21 lava flows were conducted at these volcanoes, with additional morphologic analysis of lava flows at Agni, Masaaw, Mbali, Shoshu, and Talos Paterae. A total of 66 lava flows of up to 245 km in length were mapped to identify morphologic changes consistent with the rheologic changes expected to occur in sulfur flows. Although downflow color changes are observed, the trends are not consistent, even at the same edifice. Individual flows exhibit a statistically significant increase in blue/orange ratio, decrease in blue/orange ratio, or a lack of progressive downflow color variation. Color changes have similar magnitudes downflow and across flow, and the color ranges observed are similar from volcano to volcano, suggesting that similar processes are controlling color ratios at these edifices. In addition, using flow widening and branching as an indicator of the low viscosity exhibited by sulfur cooling from high temperatures, these flows do not exhibit morphologic changes consistent with the systematic behavior expected from the simple progressive cooling of sulfur.</description><identifier>ISSN: 0019-1035</identifier><identifier>EISSN: 1090-2643</identifier><identifier>DOI: 10.1006/icar.2000.6501</identifier><language>eng</language><publisher>Elsevier Inc</publisher><ispartof>Icarus (New York, N.Y. 1962), 2000-12, Vol.148 (2), p.407-418</ispartof><rights>2000 Academic Press</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a264t-f7c160efccd9fa27db07a3e27444b309bfb23e3bbf396a5afac9e36ea75b98c53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1006/icar.2000.6501$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids></links><search><creatorcontrib>Piatek, Jennifer L.</creatorcontrib><creatorcontrib>McElfresh, Sarah B.Z.</creatorcontrib><creatorcontrib>Byrnes, Jeffrey M.</creatorcontrib><creatorcontrib>Hale, Amy Snyder</creatorcontrib><creatorcontrib>Crown, David A.</creatorcontrib><title>Color and Morphology of Lava Flows on Io</title><title>Icarus (New York, N.Y. 1962)</title><description>Analyses of color and morphologic changes in Voyager images of lava flows on Io were conducted to extend previous flow studies to additional volcanoes in preparation for comparison to Galileo data. Blue and orange filter images of Atar, Daedalus, and Ra Paterae were examined to identify systematic downflow decreases in blue/orange reflectivity suggested in earlier studies as diagnostic of color changes in cooled sulfur flows. Analyses of the color and morphology of 21 lava flows were conducted at these volcanoes, with additional morphologic analysis of lava flows at Agni, Masaaw, Mbali, Shoshu, and Talos Paterae. A total of 66 lava flows of up to 245 km in length were mapped to identify morphologic changes consistent with the rheologic changes expected to occur in sulfur flows. Although downflow color changes are observed, the trends are not consistent, even at the same edifice. Individual flows exhibit a statistically significant increase in blue/orange ratio, decrease in blue/orange ratio, or a lack of progressive downflow color variation. Color changes have similar magnitudes downflow and across flow, and the color ranges observed are similar from volcano to volcano, suggesting that similar processes are controlling color ratios at these edifices. In addition, using flow widening and branching as an indicator of the low viscosity exhibited by sulfur cooling from high temperatures, these flows do not exhibit morphologic changes consistent with the systematic behavior expected from the simple progressive cooling of sulfur.</description><issn>0019-1035</issn><issn>1090-2643</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNp1jzFPwzAQRi0EEqWwMntkSTjHsROPKKJQKYgFZuvs2GAU4squivrvSVRWptNJ9-77HiG3DEoGIO-DxVRWAFBKAeyMrBgoKCpZ83OyAmCqYMDFJbnK-Wu-Eq3iK3LXxTEmitNAX2Lafc7bx5FGT3s8IN2M8SfTONFtvCYXHsfsbv7mmrxvHt-656J_fdp2D32Bc9K-8I1lEpy3dlAeq2Yw0CB3VVPXteGgjDcVd9wYz5VEgR6tclw6bIRRrRV8TcrTX5tizsl5vUvhG9NRM9CLp1489eKpF88ZaE-Am1sdgks62-Am64aQnN3rIYb_0F9HKFjh</recordid><startdate>20001201</startdate><enddate>20001201</enddate><creator>Piatek, Jennifer L.</creator><creator>McElfresh, Sarah B.Z.</creator><creator>Byrnes, Jeffrey M.</creator><creator>Hale, Amy Snyder</creator><creator>Crown, David A.</creator><general>Elsevier Inc</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20001201</creationdate><title>Color and Morphology of Lava Flows on Io</title><author>Piatek, Jennifer L. ; McElfresh, Sarah B.Z. ; Byrnes, Jeffrey M. ; Hale, Amy Snyder ; Crown, David A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a264t-f7c160efccd9fa27db07a3e27444b309bfb23e3bbf396a5afac9e36ea75b98c53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2000</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Piatek, Jennifer L.</creatorcontrib><creatorcontrib>McElfresh, Sarah B.Z.</creatorcontrib><creatorcontrib>Byrnes, Jeffrey M.</creatorcontrib><creatorcontrib>Hale, Amy Snyder</creatorcontrib><creatorcontrib>Crown, David A.</creatorcontrib><collection>CrossRef</collection><jtitle>Icarus (New York, N.Y. 1962)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Piatek, Jennifer L.</au><au>McElfresh, Sarah B.Z.</au><au>Byrnes, Jeffrey M.</au><au>Hale, Amy Snyder</au><au>Crown, David A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Color and Morphology of Lava Flows on Io</atitle><jtitle>Icarus (New York, N.Y. 1962)</jtitle><date>2000-12-01</date><risdate>2000</risdate><volume>148</volume><issue>2</issue><spage>407</spage><epage>418</epage><pages>407-418</pages><issn>0019-1035</issn><eissn>1090-2643</eissn><abstract>Analyses of color and morphologic changes in Voyager images of lava flows on Io were conducted to extend previous flow studies to additional volcanoes in preparation for comparison to Galileo data. Blue and orange filter images of Atar, Daedalus, and Ra Paterae were examined to identify systematic downflow decreases in blue/orange reflectivity suggested in earlier studies as diagnostic of color changes in cooled sulfur flows. Analyses of the color and morphology of 21 lava flows were conducted at these volcanoes, with additional morphologic analysis of lava flows at Agni, Masaaw, Mbali, Shoshu, and Talos Paterae. A total of 66 lava flows of up to 245 km in length were mapped to identify morphologic changes consistent with the rheologic changes expected to occur in sulfur flows. Although downflow color changes are observed, the trends are not consistent, even at the same edifice. Individual flows exhibit a statistically significant increase in blue/orange ratio, decrease in blue/orange ratio, or a lack of progressive downflow color variation. Color changes have similar magnitudes downflow and across flow, and the color ranges observed are similar from volcano to volcano, suggesting that similar processes are controlling color ratios at these edifices. In addition, using flow widening and branching as an indicator of the low viscosity exhibited by sulfur cooling from high temperatures, these flows do not exhibit morphologic changes consistent with the systematic behavior expected from the simple progressive cooling of sulfur.</abstract><pub>Elsevier Inc</pub><doi>10.1006/icar.2000.6501</doi><tpages>12</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0019-1035
ispartof Icarus (New York, N.Y. 1962), 2000-12, Vol.148 (2), p.407-418
issn 0019-1035
1090-2643
language eng
recordid cdi_crossref_primary_10_1006_icar_2000_6501
source ScienceDirect Journals (5 years ago - present)
title Color and Morphology of Lava Flows on Io
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T09%3A05%3A37IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-elsevier_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Color%20and%20Morphology%20of%20Lava%20Flows%20on%20Io&rft.jtitle=Icarus%20(New%20York,%20N.Y.%201962)&rft.au=Piatek,%20Jennifer%20L.&rft.date=2000-12-01&rft.volume=148&rft.issue=2&rft.spage=407&rft.epage=418&rft.pages=407-418&rft.issn=0019-1035&rft.eissn=1090-2643&rft_id=info:doi/10.1006/icar.2000.6501&rft_dat=%3Celsevier_cross%3ES0019103500965011%3C/elsevier_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_els_id=S0019103500965011&rfr_iscdi=true