DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION

Eruption of Kelud Volcano within 2007 started with increasing in seismic activity on November 2007 and ended with Lava Dome Formation inside Crater Lake on 3 November 2007. This phenomena was the changes of eruption behavior, previous last eruption on February 1990 was explosive one. Research on def...

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Main Author: Haerani, Nia
Format: Theses
Language:Indonesia
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Online Access:https://digilib.itb.ac.id/gdl/view/64912
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:64912
spelling id-itb.:649122022-06-16T10:58:53ZDEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION Haerani, Nia Teknik (Rekayasa, enjinering dan kegiatan berkaitan) Indonesia Theses volcano, deformation, GPS method, pressure source location, magma supply, injected magma INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/64912 Eruption of Kelud Volcano within 2007 started with increasing in seismic activity on November 2007 and ended with Lava Dome Formation inside Crater Lake on 3 November 2007. This phenomena was the changes of eruption behavior, previous last eruption on February 1990 was explosive one. Research on deformation of Kelud Volcano after November 2007 Lava Dome formation carried out to determine characteristic and mechanism of deformation that has been occurred. Prediction of pressure source location and its geometry was analyzed using two different methods, which are: Mogi Model and Closed Pipe Model. Mogi Model is used based on its common application on volcano area, while Closed Pipe Model based on recent condition of Kelud volcano that plugged by lava dome. Pressure source location determined by both models then validated with seismic, EDM, tilt and geology data. Result from GPS observation method during three period, which are: April, August, and October 2008 showed that vector displacement on each measured point affected dominantly by structural geology forces. Mostly crustal stability after last phase of November 2007 eruption. There also minor displacement as result of magma migration around the points that close to the Lava Dome. Magma migration occurred in a very shallow depth and associated with aseismic zone. Deformation that occurred as result of magma migration toward the surface calculated to determine magma supply and magma injected. The result then compare to illustrate mechanism of deformation during April – October 2008. Comparison of magma supply and magma injected within these periods showed that inflation is still occurred, but it does not supported by surface manifestation. This inflation could be false because of data discontinuity, it is actually a part of deflation trend. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
topic Teknik (Rekayasa, enjinering dan kegiatan berkaitan)
spellingShingle Teknik (Rekayasa, enjinering dan kegiatan berkaitan)
Haerani, Nia
DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
description Eruption of Kelud Volcano within 2007 started with increasing in seismic activity on November 2007 and ended with Lava Dome Formation inside Crater Lake on 3 November 2007. This phenomena was the changes of eruption behavior, previous last eruption on February 1990 was explosive one. Research on deformation of Kelud Volcano after November 2007 Lava Dome formation carried out to determine characteristic and mechanism of deformation that has been occurred. Prediction of pressure source location and its geometry was analyzed using two different methods, which are: Mogi Model and Closed Pipe Model. Mogi Model is used based on its common application on volcano area, while Closed Pipe Model based on recent condition of Kelud volcano that plugged by lava dome. Pressure source location determined by both models then validated with seismic, EDM, tilt and geology data. Result from GPS observation method during three period, which are: April, August, and October 2008 showed that vector displacement on each measured point affected dominantly by structural geology forces. Mostly crustal stability after last phase of November 2007 eruption. There also minor displacement as result of magma migration around the points that close to the Lava Dome. Magma migration occurred in a very shallow depth and associated with aseismic zone. Deformation that occurred as result of magma migration toward the surface calculated to determine magma supply and magma injected. The result then compare to illustrate mechanism of deformation during April – October 2008. Comparison of magma supply and magma injected within these periods showed that inflation is still occurred, but it does not supported by surface manifestation. This inflation could be false because of data discontinuity, it is actually a part of deflation trend.
format Theses
author Haerani, Nia
author_facet Haerani, Nia
author_sort Haerani, Nia
title DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
title_short DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
title_full DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
title_fullStr DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
title_full_unstemmed DEFORMATION OF KELUD VOLCANO POST NOVEMBER 2007 LAVA DOME FORMATION
title_sort deformation of kelud volcano post november 2007 lava dome formation
url https://digilib.itb.ac.id/gdl/view/64912
_version_ 1822004702151180288