DETERMINATION OF MOUNT IJEN VOLCANO-TECTONIC (VT) EARTHQUAKE HYPOCENTERS DISTRIBUTION USING GEIGER METHOD BASED ON EARTHQUAKE DATA FOR AUGUST - SEPTEMBER 2022 PERIOD
Indonesia has 127 active volcanoes spread across Sumatra, Java, Nusa Tenggara, Maluku and Sulawesi. One of the 127 active volcanoes is Mount Ijen, East Java. On January 7, 2023 at 14.00 WIB, the status of Mount Ijen was raised one level from level I (Normal) to level II (Alert). The increase in t...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/77978 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Indonesia has 127 active volcanoes spread across Sumatra, Java, Nusa Tenggara,
Maluku and Sulawesi. One of the 127 active volcanoes is Mount Ijen, East Java.
On January 7, 2023 at 14.00 WIB, the status of Mount Ijen was raised one level
from level I (Normal) to level II (Alert). The increase in the status of volcanoes is
certainly carried out based on the results of observations of several geophysical
methods. One of the geophysical methods that can be applied is the seismic
method which can detect volcanic-tectonic earthquakes (VT) on volcanoes. This
study determined the distribution of VT earthquakes on Mount Ijen and estimated
VTA and VTB earthquake clusters. The data used is seismogram data recorded by
seven seismic stations belonging to the Center for Volcanology and Geological
Hazard Mitigation (CVGHM) around Mount Ijen between August 2022 to
September 2022. Data processing began by picking the arrival time of P and S
waves for each event using “Seisgram2k” software, producing 400 VT earthquake
event data consisting of 20 VTA earthquake events and 300 VTB earthquake
events. Next, the positioning of VT earthquake hypocenters using the Geiger
method with “Geiger's with Adaptive Damping (GAD)” software. The results of
determining the hypocenter of the VT earthquake on Mount Ijen show that the
position of the earthquake hypocenter tends to be centralized south to east of the
crater, with the depth of the VTA earthquake hypocenter being at 1.5 – 7.5 km
below the crater and VTB earthquakes at a depth of 0-2 km below the crater. The
hypocenter of VTB earthquakes tends to be centralized, while the hypocenter
position of VTA earthquakes spreads further from the crater. The existence of VTB
earthquake clusters close to the crater indicates a fracture arising from the
movement of magma that is getting closer to the crater. |
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