Studies of volcanic ash from two recent Central American eruptions
Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and simi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rose, W. I. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1973 |
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| Schlagwörter: |
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| Anmerkung: |
© Stabilimento Tipografico Francesco Gianni & Figli 1973 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Bulletin of volcanology - Springer-Verlag, 1986, 37(1973), 3 vom: Sept., Seite 338-364 |
|---|---|
| Übergeordnetes Werk: |
volume:37 ; year:1973 ; number:3 ; month:09 ; pages:338-364 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02597633 |
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| 520 | |a Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. | ||
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10.1007/BF02597633 doi (DE-627)OLC2054784036 (DE-He213)BF02597633-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Rose, W. I. verfasserin aut Studies of volcanic ash from two recent Central American eruptions 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Stabilimento Tipografico Francesco Gianni & Figli 1973 Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. Tephra Soluble Material Vulcanian Explosion Hekla Eruption Fuego Volcano Bonis, S. aut Stoiber, R. E. aut Keller, M. aut Bickford, T. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 37(1973), 3 vom: Sept., Seite 338-364 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:37 year:1973 number:3 month:09 pages:338-364 https://doi.org/10.1007/BF02597633 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO AR 37 1973 3 09 338-364 |
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10.1007/BF02597633 doi (DE-627)OLC2054784036 (DE-He213)BF02597633-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Rose, W. I. verfasserin aut Studies of volcanic ash from two recent Central American eruptions 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Stabilimento Tipografico Francesco Gianni & Figli 1973 Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. Tephra Soluble Material Vulcanian Explosion Hekla Eruption Fuego Volcano Bonis, S. aut Stoiber, R. E. aut Keller, M. aut Bickford, T. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 37(1973), 3 vom: Sept., Seite 338-364 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:37 year:1973 number:3 month:09 pages:338-364 https://doi.org/10.1007/BF02597633 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO AR 37 1973 3 09 338-364 |
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10.1007/BF02597633 doi (DE-627)OLC2054784036 (DE-He213)BF02597633-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Rose, W. I. verfasserin aut Studies of volcanic ash from two recent Central American eruptions 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Stabilimento Tipografico Francesco Gianni & Figli 1973 Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. Tephra Soluble Material Vulcanian Explosion Hekla Eruption Fuego Volcano Bonis, S. aut Stoiber, R. E. aut Keller, M. aut Bickford, T. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 37(1973), 3 vom: Sept., Seite 338-364 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:37 year:1973 number:3 month:09 pages:338-364 https://doi.org/10.1007/BF02597633 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO AR 37 1973 3 09 338-364 |
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10.1007/BF02597633 doi (DE-627)OLC2054784036 (DE-He213)BF02597633-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Rose, W. I. verfasserin aut Studies of volcanic ash from two recent Central American eruptions 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Stabilimento Tipografico Francesco Gianni & Figli 1973 Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. Tephra Soluble Material Vulcanian Explosion Hekla Eruption Fuego Volcano Bonis, S. aut Stoiber, R. E. aut Keller, M. aut Bickford, T. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 37(1973), 3 vom: Sept., Seite 338-364 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:37 year:1973 number:3 month:09 pages:338-364 https://doi.org/10.1007/BF02597633 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO AR 37 1973 3 09 338-364 |
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Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. © Stabilimento Tipografico Francesco Gianni & Figli 1973 |
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Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. © Stabilimento Tipografico Francesco Gianni & Figli 1973 |
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Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. These changes are believed to reflect changes in the composition of eruptive gases. © Stabilimento Tipografico Francesco Gianni & Figli 1973 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2054784036</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230403072645.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s1973 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02597633</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2054784036</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02597633-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Rose, W. I.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Studies of volcanic ash from two recent Central American eruptions</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1973</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Stabilimento Tipografico Francesco Gianni & Figli 1973</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The 1971 eruptions of Cerro Negro volcano in Nicaragua and Fuego volcano in Guatemala produced ash blankets with minimum volumes of 7 × $ 10^{7} $ $ m^{3} $ and 6 × $ 10^{7} $ $ m^{3} $, respectively. Seven new chemical analyses show that ash produced by both eruptions was basaltic and similar to previously — erupted lavas of both volcanoes. Both ash blankets were sampled areally and stratigraphically before they were affected by rain. Chemical analyses of soluble materials leached from these ashes show that near the end of both eruptions the concentrations of soluble materials increased by about an order of magnitude. 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E.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Keller, M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bickford, T.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Bulletin of volcanology</subfield><subfield code="d">Springer-Verlag, 1986</subfield><subfield code="g">37(1973), 3 vom: Sept., Seite 338-364</subfield><subfield code="w">(DE-627)130428833</subfield><subfield code="w">(DE-600)635594-8</subfield><subfield code="w">(DE-576)015927865</subfield><subfield code="x">0258-8900</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:37</subfield><subfield code="g">year:1973</subfield><subfield code="g">number:3</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:338-364</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02597633</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">37</subfield><subfield code="j">1973</subfield><subfield code="e">3</subfield><subfield code="c">09</subfield><subfield code="h">338-364</subfield></datafield></record></collection>
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