Search results
Results from the WOW.Com Content Network
The full official Indonesian name is the Pusat Vulkanologi dan Mitigasi Bencana Geologi (English: Volcanology and Geological Hazard Mitigation Center), often abbreviated to PVMBG. [1] It is based in Bandung in West Java. [2] It was preceded by the Netherlands East Indies Volcanological Survey. [3]
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.
Particularly for Indonesia, Simkin and Siebert used a catalogue of active volcanoes from the International Association of Volcanology and Chemistry of the Earth's Interior publication series. [ b ] The Simkin and Siebert list is the most complete list of volcanoes in Indonesia, but the accuracy of the record varies from one region to another in ...
A study conducted in 2001 determined that Tangkuban Perahu had erupted at least 30 times in the previous 40,750 years. Studies of the tephra layers within three kilometres of the crater revealed that 21 were minor eruptions and the remaining were significant eruptions.
The Bandung Geological Museum opened in Bandung, Indonesia in 1928. On December 10, 1871, six meteorites fell in Sindanglaut, West Java, Indonesia. This rare fall of a LL6 chondrite included an 11.5 kg TKW that is held by the Bandung Geological Museum and the Paris Museum of History.
Mount Sumbing (Indonesian: Gunung Sumbing) is an active stratovolcano in Central Java, Indonesia. This volcano is symmetrical like its neighbor, Mount Sindoro which lies to its northwest. Administratively, The volcano is divided between 3 regencies: Temanggung, Wonosobo, and Magelang. The only report of historical eruptions is from 1730.
Simplified geologic map of Kalimantan (Borneo) Island Map of Borneo and surrounding features. Made using GeoMapApp. The basement rock of Borneo is a complex mosaic of geologic terrains, commonly interpreted as the product of primarily Mesozoic accretion of micro-continental fragments, island arc material, oceanic crustal material and marginal basin fill onto the Paleozoic core of the Schwaner ...
A halo at Ngobaran beach. The Geopark has many caves, some of which have underground rivers. [5] where tubing activities can be carried on.[6]Nglanggeran primeval volcano in the Patuk area is only 600 meters high but there are excellent views from the peak to the north towards Mount Merapi and to the south across to the coast of Java.