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  2. Great Sumatran fault - Wikipedia

    en.wikipedia.org/wiki/Great_Sumatran_fault

    The Great Sumatran fault, also known as Semangko fault, is a large strike-slip fault running the entire length of the island of Sumatra.This Indonesian island is located in a highly seismic area of the world, including a subduction zone off the west coast of the island.

  3. Geology of Indonesia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Indonesia

    The tectonics processes in Indonesia formed major structures in Indonesia. The most prominent fault in the west of Indonesia is the Semangko Fault or the Great Sumatran Fault, a dextral strike-slip fault along Sumatra Island (about 1,900 km). The formation of this fault zone is related to the subduction zone in the west of Sumatra.

  4. List of faults in Indonesia - Wikipedia

    en.wikipedia.org/wiki/List_of_faults_in_Indonesia

    Print/export Download as PDF ... Indonesia is a country located close to tectonic plate boundaries which causes it to have many active ... Citarik Fault [3] Cimandiri ...

  5. 20 years later: A look at the deadliest disaster to strike ...

    www.aol.com/20-years-later-look-deadliest...

    On Dec. 26, 2004, a 9.2-magnitude earthquake shook Southeast Asia, triggering the worst tsunami in recorded history. According to United Nations estimates, more than 220,000 people were killed ...

  6. Mount Besar - Wikipedia

    en.wikipedia.org/wiki/Mount_Besar

    Mount Besar (Indonesian: Gunung Besar, means: Big Mountain) is a stratovolcano in the southeast of Sumatra, Indonesia.A minor sulfur deposit can be found in the crater.A big solfatara field called Marga Bayur is located along its north–south-west flanks or the Semangko fault system.

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  9. Earthquake rupture - Wikipedia

    en.wikipedia.org/wiki/Earthquake_Rupture

    A tectonic earthquake begins by an initial rupture at a point on the fault surface, a process known as nucleation. The scale of the nucleation zone is uncertain, with some evidence, such as the rupture dimensions of the smallest earthquakes, suggesting that it is smaller than 100 m while other evidence, such as a slow component revealed by low-frequency spectra of some earthquakes, suggest ...

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