ANALISIS DEFORMASI GUNUNGAPI MERAPI DENGAN METODE GEODETIK-GPS
Understanding of magmatic phenomena and monitoring of <br /> Merapi Volcano will require a deformation study. Deformation study is a <br /> multidiscipline study. Geodesy is one of a discipline that deals with <br /> deformation from geometric point of view, in terms of de...
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Format: | Theses |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/1707 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Understanding of magmatic phenomena and monitoring of <br />
Merapi Volcano will require a deformation study. Deformation study is a <br />
multidiscipline study. Geodesy is one of a discipline that deals with <br />
deformation from geometric point of view, in terms of determining the <br />
magnitude, pattern, and parameters of the deformation. The well known <br />
geodetic method which is used in monitoring the deformation of Merapi <br />
Volcano is Global Positioning System (GPS). <br />
This research emphasizes on the analysis of deformation of <br />
Merapi Volcano with the geodetic method using GPS surveys. GPS <br />
monitoring network is established covering the body of Merapi Volcano <br />
and its surrounding. The coordinates of the points of the monitoring <br />
network obtained from GPS surveys, are used to determine the magnitude <br />
and direction of the vector displacements of the points. These vector <br />
displacements are useful information for developing the model of <br />
deformation analysis which then is used to determine deformation <br />
parameters of Merapi Volcano. <br />
This research concludes that, 1) the single frequency GPS <br />
receiver can be used to monitor the deformation of Merapi Volcano, 2) <br />
during the period of November 1996-March 1998, Merapi Volcano had <br />
exploded twice and deformed. This can be proved from geodetic and <br />
physics points of view. From the geometric point of view the magnitude <br />
of vector displacement, deformation parameters, as well as the principal <br />
strain show significance values; while from physics point of view Merapi <br />
shows the growing dome and it has exploded twice in January 17, 1997 <br />
and July, 1998, 3) the characteristics of deformation can be geometrically <br />
useful to predict the physical activities of Merapi Volcano, 4) the study of <br />
deformation model of Merapi Volcano can be approached by two models. <br />
The first is a model that includes translation, strain and rotation, while the <br />
second one is a model that includes just strain and rotation (no <br />
translation). Based on geological and geophysical information, the second <br />
model seems to be more realistic for describing the deformation of <br />
Merapi Volcano. |
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