A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand
Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Hackett, W. R. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1989 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag 1989 |
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| Übergeordnetes Werk: |
Enthalten in: Bulletin of volcanology - Springer-Verlag, 1986, 51(1989), 1 vom: Jan., Seite 51-68 |
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| Übergeordnetes Werk: |
volume:51 ; year:1989 ; number:1 ; month:01 ; pages:51-68 |
| Links: |
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| DOI / URN: |
10.1007/BF01086761 |
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| Katalog-ID: |
OLC2054790036 |
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| 245 | 1 | 0 | |a A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand |
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| 520 | |a Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. | ||
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| 650 | 4 | |a Aggradation | |
| 650 | 4 | |a Pyroclastic Deposit | |
| 650 | 4 | |a Intensity Rain | |
| 650 | 4 | |a Eruptive Style | |
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10.1007/BF01086761 doi (DE-627)OLC2054790036 (DE-He213)BF01086761-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Hackett, W. R. verfasserin aut A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1989 Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style Houghton, B. F. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 51(1989), 1 vom: Jan., Seite 51-68 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:51 year:1989 number:1 month:01 pages:51-68 https://doi.org/10.1007/BF01086761 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_267 GBV_ILN_2004 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4302 GBV_ILN_4323 AR 51 1989 1 01 51-68 |
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10.1007/BF01086761 doi (DE-627)OLC2054790036 (DE-He213)BF01086761-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Hackett, W. R. verfasserin aut A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1989 Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style Houghton, B. F. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 51(1989), 1 vom: Jan., Seite 51-68 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:51 year:1989 number:1 month:01 pages:51-68 https://doi.org/10.1007/BF01086761 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_267 GBV_ILN_2004 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4302 GBV_ILN_4323 AR 51 1989 1 01 51-68 |
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10.1007/BF01086761 doi (DE-627)OLC2054790036 (DE-He213)BF01086761-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Hackett, W. R. verfasserin aut A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1989 Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style Houghton, B. F. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 51(1989), 1 vom: Jan., Seite 51-68 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:51 year:1989 number:1 month:01 pages:51-68 https://doi.org/10.1007/BF01086761 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_267 GBV_ILN_2004 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4302 GBV_ILN_4323 AR 51 1989 1 01 51-68 |
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10.1007/BF01086761 doi (DE-627)OLC2054790036 (DE-He213)BF01086761-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Hackett, W. R. verfasserin aut A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1989 Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style Houghton, B. F. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 51(1989), 1 vom: Jan., Seite 51-68 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:51 year:1989 number:1 month:01 pages:51-68 https://doi.org/10.1007/BF01086761 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_267 GBV_ILN_2004 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4302 GBV_ILN_4323 AR 51 1989 1 01 51-68 |
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10.1007/BF01086761 doi (DE-627)OLC2054790036 (DE-He213)BF01086761-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ Hackett, W. R. verfasserin aut A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand 1989 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1989 Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style Houghton, B. F. aut Enthalten in Bulletin of volcanology Springer-Verlag, 1986 51(1989), 1 vom: Jan., Seite 51-68 (DE-627)130428833 (DE-600)635594-8 (DE-576)015927865 0258-8900 nnns volume:51 year:1989 number:1 month:01 pages:51-68 https://doi.org/10.1007/BF01086761 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_267 GBV_ILN_2004 GBV_ILN_2008 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4103 GBV_ILN_4302 GBV_ILN_4323 AR 51 1989 1 01 51-68 |
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550 VZ A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand Explosive Eruption Aggradation Pyroclastic Deposit Intensity Rain Eruptive Style |
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A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand |
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A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand |
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Hackett, W. R. |
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a facies model for a quaternary andesitic composite volcano: ruapehu, new zealand |
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A facies model for a quaternary andesitic composite volcano: Ruapehu, New Zealand |
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Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. © Springer-Verlag 1989 |
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Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. © Springer-Verlag 1989 |
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Abstract Ruapehu composite volcano is a dynamic volcanic-sedimentary system, characterised by high accumulation rates and by rapid lateral and vertical change in facies. Four major cone-building episodes have occurred over 250 Ka, from a variety of summit, flank and satellite vents. Eruptive styles include subplinian, strombolian, phreatomagmatic, vulcanian and dome-related explosive eruptions, and extrusion of lava flows and domes. The volcano can be divided into two parts: a composite cone of volume 110 $ km^{3} $, surrounded by an equally voluminous ring plain. Complementary portions of Ruapehu's history are preserved in cone-forming and ring plain environments. Cone-forming sequences are dominated by sheet- and autobrecciated-lava flows, which seldom reach the ring plain. The ring plain is built predominantly from the products of explosive volcanism, both the distal primary pyroclastic deposits and the reworked material eroded from the cone. Much of the material entering the ring plain is transported by lahars either generated directly by eruptions or triggered by the high intensity rain storms which characterise the region. Ring plain detritus is reworked rapidly by concentrated and hyperconcentrated streams in pulses of rapid aggradation immediately following eruptions and more gradually in the longer intervals between eruptions. © Springer-Verlag 1989 |
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