Loading…

Steady-state magma discharge at Etna 1971-81

Throughout the past decade Mount Etna has been in almost continuous activity and even during periods of repose incandescent lava has often been visible in at least one of the summit vents. Using observations by Italian, British and French volcanological teams we have estimated the volumes of lava pr...

Full description

Saved in:
Bibliographic Details
Published in:Nature (London) 1981-12, Vol.294 (5841), p.548-550
Main Authors: Wadge, G, Guest, J. E
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3
cites cdi_FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3
container_end_page 550
container_issue 5841
container_start_page 548
container_title Nature (London)
container_volume 294
creator Wadge, G
Guest, J. E
description Throughout the past decade Mount Etna has been in almost continuous activity and even during periods of repose incandescent lava has often been visible in at least one of the summit vents. Using observations by Italian, British and French volcanological teams we have estimated the volumes of lava produced by each eruption from 1971 to July 1981. The computed output of magma for this period approximates to a rate of 0.7 m 3 s −1 . We now compare this with our output rate estimates for Etna's historic past. The steady-state nature of the output during the past decade has implications for the interpretation of the volcano's internal plumbing and the petrology of its lavas, and the assumption that this state will be maintained allows us to discuss the timing and magnitude of future eruptions.
doi_str_mv 10.1038/294548a0
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_23865697</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>23865697</sourcerecordid><originalsourceid>FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3</originalsourceid><addsrcrecordid>eNpt0DtPwzAQB3ALgUQpSHwClAmBRMCvxPaIqvKQKjEAs3V1LqFVkxTbGfrtcRXoxHTL7_73IOSS0XtGhX7gRhZSAz0iEyZVmctSq2MyoZTrnGpRnpKzENaU0oIpOSF37xGh2uUhQsSshaaFrFoF9wW-wQxiNo8dZMwolmt2Tk5q2AS8-K1T8vk0_5i95Iu359fZ4yJ3gomYKy5NuW9xtEYp0hznaml4rXFZ1ZQL4xQtQAFDLCUzBWJlKq5ZBW6ZkJiS6zF36_vvAUO0bVoJNxvosB-C5UKXRWlUgjcjdL4PwWNtt37Vgt9ZRu3-HfbvHYnejjQk0jXo7boffJfO-M9ejbaDOHg8hB7ADzLfZqc</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>23865697</pqid></control><display><type>article</type><title>Steady-state magma discharge at Etna 1971-81</title><source>Springer Nature - Connect here FIRST to enable access</source><creator>Wadge, G ; Guest, J. E</creator><creatorcontrib>Wadge, G ; Guest, J. E</creatorcontrib><description>Throughout the past decade Mount Etna has been in almost continuous activity and even during periods of repose incandescent lava has often been visible in at least one of the summit vents. Using observations by Italian, British and French volcanological teams we have estimated the volumes of lava produced by each eruption from 1971 to July 1981. The computed output of magma for this period approximates to a rate of 0.7 m 3 s −1 . We now compare this with our output rate estimates for Etna's historic past. The steady-state nature of the output during the past decade has implications for the interpretation of the volcano's internal plumbing and the petrology of its lavas, and the assumption that this state will be maintained allows us to discuss the timing and magnitude of future eruptions.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/294548a0</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>Humanities and Social Sciences ; letter ; multidisciplinary ; Science ; Science (multidisciplinary)</subject><ispartof>Nature (London), 1981-12, Vol.294 (5841), p.548-550</ispartof><rights>Springer Nature Limited 1981</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3</citedby><cites>FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,2725,27922,27923</link.rule.ids></links><search><creatorcontrib>Wadge, G</creatorcontrib><creatorcontrib>Guest, J. E</creatorcontrib><title>Steady-state magma discharge at Etna 1971-81</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>Throughout the past decade Mount Etna has been in almost continuous activity and even during periods of repose incandescent lava has often been visible in at least one of the summit vents. Using observations by Italian, British and French volcanological teams we have estimated the volumes of lava produced by each eruption from 1971 to July 1981. The computed output of magma for this period approximates to a rate of 0.7 m 3 s −1 . We now compare this with our output rate estimates for Etna's historic past. The steady-state nature of the output during the past decade has implications for the interpretation of the volcano's internal plumbing and the petrology of its lavas, and the assumption that this state will be maintained allows us to discuss the timing and magnitude of future eruptions.</description><subject>Humanities and Social Sciences</subject><subject>letter</subject><subject>multidisciplinary</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1981</creationdate><recordtype>article</recordtype><recordid>eNpt0DtPwzAQB3ALgUQpSHwClAmBRMCvxPaIqvKQKjEAs3V1LqFVkxTbGfrtcRXoxHTL7_73IOSS0XtGhX7gRhZSAz0iEyZVmctSq2MyoZTrnGpRnpKzENaU0oIpOSF37xGh2uUhQsSshaaFrFoF9wW-wQxiNo8dZMwolmt2Tk5q2AS8-K1T8vk0_5i95Iu359fZ4yJ3gomYKy5NuW9xtEYp0hznaml4rXFZ1ZQL4xQtQAFDLCUzBWJlKq5ZBW6ZkJiS6zF36_vvAUO0bVoJNxvosB-C5UKXRWlUgjcjdL4PwWNtt37Vgt9ZRu3-HfbvHYnejjQk0jXo7boffJfO-M9ejbaDOHg8hB7ADzLfZqc</recordid><startdate>19811210</startdate><enddate>19811210</enddate><creator>Wadge, G</creator><creator>Guest, J. E</creator><general>Nature Publishing Group UK</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>19811210</creationdate><title>Steady-state magma discharge at Etna 1971-81</title><author>Wadge, G ; Guest, J. E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1981</creationdate><topic>Humanities and Social Sciences</topic><topic>letter</topic><topic>multidisciplinary</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wadge, G</creatorcontrib><creatorcontrib>Guest, J. E</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wadge, G</au><au>Guest, J. E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Steady-state magma discharge at Etna 1971-81</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>1981-12-10</date><risdate>1981</risdate><volume>294</volume><issue>5841</issue><spage>548</spage><epage>550</epage><pages>548-550</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>Throughout the past decade Mount Etna has been in almost continuous activity and even during periods of repose incandescent lava has often been visible in at least one of the summit vents. Using observations by Italian, British and French volcanological teams we have estimated the volumes of lava produced by each eruption from 1971 to July 1981. The computed output of magma for this period approximates to a rate of 0.7 m 3 s −1 . We now compare this with our output rate estimates for Etna's historic past. The steady-state nature of the output during the past decade has implications for the interpretation of the volcano's internal plumbing and the petrology of its lavas, and the assumption that this state will be maintained allows us to discuss the timing and magnitude of future eruptions.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/294548a0</doi><tpages>3</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0028-0836
ispartof Nature (London), 1981-12, Vol.294 (5841), p.548-550
issn 0028-0836
1476-4687
language eng
recordid cdi_proquest_miscellaneous_23865697
source Springer Nature - Connect here FIRST to enable access
subjects Humanities and Social Sciences
letter
multidisciplinary
Science
Science (multidisciplinary)
title Steady-state magma discharge at Etna 1971-81
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-09T10%3A22%3A06IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Steady-state%20magma%20discharge%20at%20Etna%201971-81&rft.jtitle=Nature%20(London)&rft.au=Wadge,%20G&rft.date=1981-12-10&rft.volume=294&rft.issue=5841&rft.spage=548&rft.epage=550&rft.pages=548-550&rft.issn=0028-0836&rft.eissn=1476-4687&rft_id=info:doi/10.1038/294548a0&rft_dat=%3Cproquest_cross%3E23865697%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c313t-724961971c0fe43174ccf492f8ebdf0239c705a7a1ee64195eed9d281dacbf8e3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=23865697&rft_id=info:pmid/&rfr_iscdi=true