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Hydrothermal hexahydrite spherules erupted during the 2008–2010 summit eruption of Kīlauea Volcano, Hawai`i
Small (1–3 mm), hollow spherules of hexahydrite have been collected falling out of the magmatic gas plume downwind of Kīlauea’s summit vent. The spherules were observed on eight separate occasions during 2009–2010 when a lake of actively spattering lava was present ~150–200 m below the rim of the ve...
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Published in: | Bulletin of volcanology 2011-11, Vol.73 (9), p.1369-1375 |
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container_title | Bulletin of volcanology |
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creator | Hon, Ken Orr, Tim |
description | Small (1–3 mm), hollow spherules of hexahydrite have been collected falling out of the magmatic gas plume downwind of Kīlauea’s summit vent. The spherules were observed on eight separate occasions during 2009–2010 when a lake of actively spattering lava was present ~150–200 m below the rim of the vent. The shells of the spherules have a fine bubbly foam structure less than 0.1 mm thick, composed almost entirely of hexahydrite [MgSO
4
·6H
2
O] Small microspherules of lava ( |
doi_str_mv | 10.1007/s00445-011-0484-x |
format | article |
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4
·6H
2
O] Small microspherules of lava (<5 μm across) along with mineral and rock fragments from the magmatic plume adhered to the outside of the hexahydrite spherules. Phase relationships and the particulate matter in the magmatic plume indicate that the spherules originated as a bubbly solution injected into and mixed with the magmatic plume. The most likely mechanism for production of hexahydrite spherules is boiling of MgSO
4
-saturated meteoric water in the walls of the conduit above the surface of the lava lake. Solfataric sulfates may thus be recycled and reinjected into the plume, creating particulates of sulfate minerals that can be distributed far from their original source.</description><identifier>ISSN: 0258-8900</identifier><identifier>EISSN: 1432-0819</identifier><identifier>DOI: 10.1007/s00445-011-0484-x</identifier><identifier>CODEN: BUVOEW</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer-Verlag</publisher><subject>Crystalline rocks ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Exact sciences and technology ; Geology ; Geophysics/Geodesy ; Igneous and metamorphic rocks petrology, volcanic processes, magmas ; Lakes ; Lava ; Magma ; Meteoric water ; Mineralogy ; Minerals ; Natural hazards: prediction, damages, etc ; Particulate matter ; Research Article ; Sedimentology ; Sulfates ; Volcanoes ; Volcanology</subject><ispartof>Bulletin of volcanology, 2011-11, Vol.73 (9), p.1369-1375</ispartof><rights>Springer-Verlag 2011</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a400t-fdf286e67d428cfbdc40e1142d0586e553ff91a985e20898b3067a2922347fcb3</citedby><cites>FETCH-LOGICAL-a400t-fdf286e67d428cfbdc40e1142d0586e553ff91a985e20898b3067a2922347fcb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24747175$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Hon, Ken</creatorcontrib><creatorcontrib>Orr, Tim</creatorcontrib><title>Hydrothermal hexahydrite spherules erupted during the 2008–2010 summit eruption of Kīlauea Volcano, Hawai`i</title><title>Bulletin of volcanology</title><addtitle>Bull Volcanol</addtitle><description>Small (1–3 mm), hollow spherules of hexahydrite have been collected falling out of the magmatic gas plume downwind of Kīlauea’s summit vent. The spherules were observed on eight separate occasions during 2009–2010 when a lake of actively spattering lava was present ~150–200 m below the rim of the vent. The shells of the spherules have a fine bubbly foam structure less than 0.1 mm thick, composed almost entirely of hexahydrite [MgSO
4
·6H
2
O] Small microspherules of lava (<5 μm across) along with mineral and rock fragments from the magmatic plume adhered to the outside of the hexahydrite spherules. Phase relationships and the particulate matter in the magmatic plume indicate that the spherules originated as a bubbly solution injected into and mixed with the magmatic plume. The most likely mechanism for production of hexahydrite spherules is boiling of MgSO
4
-saturated meteoric water in the walls of the conduit above the surface of the lava lake. Solfataric sulfates may thus be recycled and reinjected into the plume, creating particulates of sulfate minerals that can be distributed far from their original source.</description><subject>Crystalline rocks</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Igneous and metamorphic rocks petrology, volcanic processes, magmas</subject><subject>Lakes</subject><subject>Lava</subject><subject>Magma</subject><subject>Meteoric water</subject><subject>Mineralogy</subject><subject>Minerals</subject><subject>Natural hazards: prediction, damages, etc</subject><subject>Particulate matter</subject><subject>Research Article</subject><subject>Sedimentology</subject><subject>Sulfates</subject><subject>Volcanoes</subject><subject>Volcanology</subject><issn>0258-8900</issn><issn>1432-0819</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNp1kEFKxDAUhoMoOI4ewF0QxI3VlzRt06WIOqLgRt3GTJs4GdqmJi2OO-_gMbyGJ_EkZuygILh68L_v_Tw-hHYJHBGA7NgDMJZEQEgEjLNosYZGhMU0Ak7ydTQCmvCI5wCbaMv7OUBYptkINZOX0tluplwtKzxTCzkLgekU9m0I-0p5HEbbqRKXvTPNIw4wpgD88_WNAgHs-7o23UAZ22Cr8dXHeyV7JfG9rQrZ2EM8kc_SPJhttKFl5dXOao7R3fnZ7ekkur65uDw9uY4kA-giXWrKU5VmJaO80NOyYKAIYbSEJORJEmudE5nzRFHgOZ_GkGaS5pTGLNPFNB6jg6G3dfapV74TtfGFqirZKNt7kdOUc8JSEsi9P-Tc9q4Jz4kcKCcpz5IAkQEqnPXeKS1aZ2rpXgQBsfQvBv8i-BdL_2IRbvZXxdIXstJONoXxP4eUZSwj39104Hy71Kvc7wP_l38BgtuWeg</recordid><startdate>20111101</startdate><enddate>20111101</enddate><creator>Hon, Ken</creator><creator>Orr, Tim</creator><general>Springer-Verlag</general><general>Springer</general><general>Springer Nature B.V</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20111101</creationdate><title>Hydrothermal hexahydrite spherules erupted during the 2008–2010 summit eruption of Kīlauea Volcano, Hawai`i</title><author>Hon, Ken ; Orr, Tim</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a400t-fdf286e67d428cfbdc40e1142d0586e553ff91a985e20898b3067a2922347fcb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Crystalline rocks</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Engineering and environment geology. Geothermics</topic><topic>Exact sciences and technology</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Igneous and metamorphic rocks petrology, volcanic processes, magmas</topic><topic>Lakes</topic><topic>Lava</topic><topic>Magma</topic><topic>Meteoric water</topic><topic>Mineralogy</topic><topic>Minerals</topic><topic>Natural hazards: prediction, damages, etc</topic><topic>Particulate matter</topic><topic>Research Article</topic><topic>Sedimentology</topic><topic>Sulfates</topic><topic>Volcanoes</topic><topic>Volcanology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hon, Ken</creatorcontrib><creatorcontrib>Orr, Tim</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Science Journals</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Bulletin of volcanology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hon, Ken</au><au>Orr, Tim</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrothermal hexahydrite spherules erupted during the 2008–2010 summit eruption of Kīlauea Volcano, Hawai`i</atitle><jtitle>Bulletin of volcanology</jtitle><stitle>Bull Volcanol</stitle><date>2011-11-01</date><risdate>2011</risdate><volume>73</volume><issue>9</issue><spage>1369</spage><epage>1375</epage><pages>1369-1375</pages><issn>0258-8900</issn><eissn>1432-0819</eissn><coden>BUVOEW</coden><abstract>Small (1–3 mm), hollow spherules of hexahydrite have been collected falling out of the magmatic gas plume downwind of Kīlauea’s summit vent. The spherules were observed on eight separate occasions during 2009–2010 when a lake of actively spattering lava was present ~150–200 m below the rim of the vent. The shells of the spherules have a fine bubbly foam structure less than 0.1 mm thick, composed almost entirely of hexahydrite [MgSO
4
·6H
2
O] Small microspherules of lava (<5 μm across) along with mineral and rock fragments from the magmatic plume adhered to the outside of the hexahydrite spherules. Phase relationships and the particulate matter in the magmatic plume indicate that the spherules originated as a bubbly solution injected into and mixed with the magmatic plume. The most likely mechanism for production of hexahydrite spherules is boiling of MgSO
4
-saturated meteoric water in the walls of the conduit above the surface of the lava lake. Solfataric sulfates may thus be recycled and reinjected into the plume, creating particulates of sulfate minerals that can be distributed far from their original source.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer-Verlag</pub><doi>10.1007/s00445-011-0484-x</doi><tpages>7</tpages></addata></record> |
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subjects | Crystalline rocks Earth and Environmental Science Earth Sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Geology Geophysics/Geodesy Igneous and metamorphic rocks petrology, volcanic processes, magmas Lakes Lava Magma Meteoric water Mineralogy Minerals Natural hazards: prediction, damages, etc Particulate matter Research Article Sedimentology Sulfates Volcanoes Volcanology |
title | Hydrothermal hexahydrite spherules erupted during the 2008–2010 summit eruption of Kīlauea Volcano, Hawai`i |
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