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The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996–2008 observations
This paper considers the geoecological impacts of eruptions on Karymskii Volcano and the Tokareva crater for the 1996–2008 period, which resulted in changes in (a) the relief around these edifices, (b) the discharge and composition of water in the Karymskii River and other streams in the area, and (...
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Published in: | Journal of volcanology and seismology 2012-11, Vol.6 (6), p.329-340 |
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container_end_page | 340 |
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container_title | Journal of volcanology and seismology |
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creator | Andreev, V. I. Nikolaeva, A. G. |
description | This paper considers the geoecological impacts of eruptions on Karymskii Volcano and the Tokareva crater for the 1996–2008 period, which resulted in changes in (a) the relief around these edifices, (b) the discharge and composition of water in the Karymskii River and other streams in the area, and (c) the discharge and composition of gases in thermal springs. It was found that the concentration of CH
4
previously had been abnormally high in free gases that emanate from the new Piipovskii Springs and an explanation is provided of the decrease in their concentration over time. We detected variations in the radon activity, OARn (Bq/m
3
), in free gases that are released in the Karymskii caldera hydrothermal occurrences; the variations are consistent with those in the eruptive activity of Karymskii Volcano in 2005–2006. We describe permafrost rocks in the Karymskii caldera that favor the generation of a cryolithic zone. |
doi_str_mv | 10.1134/S0742046312060024 |
format | article |
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4
previously had been abnormally high in free gases that emanate from the new Piipovskii Springs and an explanation is provided of the decrease in their concentration over time. We detected variations in the radon activity, OARn (Bq/m
3
), in free gases that are released in the Karymskii caldera hydrothermal occurrences; the variations are consistent with those in the eruptive activity of Karymskii Volcano in 2005–2006. We describe permafrost rocks in the Karymskii caldera that favor the generation of a cryolithic zone.</description><identifier>ISSN: 0742-0463</identifier><identifier>EISSN: 1819-7108</identifier><identifier>DOI: 10.1134/S0742046312060024</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Calderas ; Earth and Environmental Science ; Earth Sciences ; Environmental impact ; Freshwater ; Gases ; Geochemistry ; Geology ; Geophysics/Geodesy ; Hot springs ; Lithosphere ; Permafrost ; Radon ; Streams ; Volcanoes</subject><ispartof>Journal of volcanology and seismology, 2012-11, Vol.6 (6), p.329-340</ispartof><rights>Pleiades Publishing, Ltd. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c349t-760bf17b474a0a9fcf3a6552b3559c2d0143b640061245d4ee7bc61148782fb43</citedby><cites>FETCH-LOGICAL-c349t-760bf17b474a0a9fcf3a6552b3559c2d0143b640061245d4ee7bc61148782fb43</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></links><search><creatorcontrib>Andreev, V. I.</creatorcontrib><creatorcontrib>Nikolaeva, A. G.</creatorcontrib><title>The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996–2008 observations</title><title>Journal of volcanology and seismology</title><addtitle>J. Volcanolog. Seismol</addtitle><description>This paper considers the geoecological impacts of eruptions on Karymskii Volcano and the Tokareva crater for the 1996–2008 period, which resulted in changes in (a) the relief around these edifices, (b) the discharge and composition of water in the Karymskii River and other streams in the area, and (c) the discharge and composition of gases in thermal springs. It was found that the concentration of CH
4
previously had been abnormally high in free gases that emanate from the new Piipovskii Springs and an explanation is provided of the decrease in their concentration over time. We detected variations in the radon activity, OARn (Bq/m
3
), in free gases that are released in the Karymskii caldera hydrothermal occurrences; the variations are consistent with those in the eruptive activity of Karymskii Volcano in 2005–2006. We describe permafrost rocks in the Karymskii caldera that favor the generation of a cryolithic zone.</description><subject>Calderas</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Environmental impact</subject><subject>Freshwater</subject><subject>Gases</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Hot springs</subject><subject>Lithosphere</subject><subject>Permafrost</subject><subject>Radon</subject><subject>Streams</subject><subject>Volcanoes</subject><issn>0742-0463</issn><issn>1819-7108</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp1kT1u20AQhReBA0RwdIB0C6RxYdozy_0h3RmG_xADKaykJYarpUyJ5Mq7pABX9h18w5wkpJUiiJHqFfO9N4M3jH1BOEFM5ek9GClA6hQFaAAhP7AZZpgnBiE7YLNpnEzzT2we4xoAMFMiFWrGnhcPjq-cd9Y3flVbanjdbsn23FfchWHb176L3Hf8G4WnNm7qmv_0jaXOc-qWfOE3FNyOuA3Uu3DMLymOOuGtfaB-Q2d8WoF5rn-9vAqAjPsyurCjt-TP7GNFTXTzP3rIflxdLi5ukrvv17cX53eJTWXeJ0ZDWaEppZEElFe2SkkrJcpUqdyKJaBMSy0BNAqpltI5U1qNKDOTiaqU6SE72udug38cXOyLto7WNQ11zg-xQKNVrjVKHNGv_6BrP4RuvK5AobUZ61NmpHBP2eBjDK4qtqFux44KhGL6SvHuK6NH7D1xZLuVC38l_9f0G7HujQY</recordid><startdate>20121101</startdate><enddate>20121101</enddate><creator>Andreev, V. I.</creator><creator>Nikolaeva, A. G.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</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>C1K</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>20121101</creationdate><title>The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996–2008 observations</title><author>Andreev, V. I. ; Nikolaeva, A. 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I.</au><au>Nikolaeva, A. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996–2008 observations</atitle><jtitle>Journal of volcanology and seismology</jtitle><stitle>J. Volcanolog. Seismol</stitle><date>2012-11-01</date><risdate>2012</risdate><volume>6</volume><issue>6</issue><spage>329</spage><epage>340</epage><pages>329-340</pages><issn>0742-0463</issn><eissn>1819-7108</eissn><abstract>This paper considers the geoecological impacts of eruptions on Karymskii Volcano and the Tokareva crater for the 1996–2008 period, which resulted in changes in (a) the relief around these edifices, (b) the discharge and composition of water in the Karymskii River and other streams in the area, and (c) the discharge and composition of gases in thermal springs. It was found that the concentration of CH
4
previously had been abnormally high in free gases that emanate from the new Piipovskii Springs and an explanation is provided of the decrease in their concentration over time. We detected variations in the radon activity, OARn (Bq/m
3
), in free gases that are released in the Karymskii caldera hydrothermal occurrences; the variations are consistent with those in the eruptive activity of Karymskii Volcano in 2005–2006. We describe permafrost rocks in the Karymskii caldera that favor the generation of a cryolithic zone.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0742046312060024</doi><tpages>12</tpages></addata></record> |
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source | Springer Nature |
subjects | Calderas Earth and Environmental Science Earth Sciences Environmental impact Freshwater Gases Geochemistry Geology Geophysics/Geodesy Hot springs Lithosphere Permafrost Radon Streams Volcanoes |
title | The geoecological impact of eruptions on Karymskii Volcano and Tokareva crater, Eastern Kamchatka: The 1996–2008 observations |
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