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Dieng Plateau (Javanese: ꦣꦶꦲꦾꦁ; Javanese pronunciation:) is a plateau in Central Java, Indonesia that forms the floor of the caldera complex on the Dieng Volcanic Complex. Administratively, this plateau is included in the territory of Banjarnegara Regency and Wonosobo Regency.
Minangkabau mosque circa 1892–1905 photographed by Christiaan Benjamin Nieuwenhuis. The Minangkabau Highlands (Indonesian: Dataran Tinggi Minangkabau, Minang: Minang Darek) is a mountainous area in the province of West Sumatra, located around three mountains—Mount Marapi, Mount Singgalang, and Mount Sago—in west-central Sumatra, Indonesia.
Gunung Padang is an archaeological site located in Karyamukti, West Java, Indonesia, 50 kilometres (31 mi) southwest of Cianjur.Located at 885 metres (2,904 ft) above sea level, the site covers a hill—an extinct volcano—in a series of five terraces bordered by retaining walls of stone that are accessed by 370 successive andesite steps rising about 95 metres (312 ft).
Mountains of Indonesia — many Indonesian mountains are known as Gunung, & most are active or dormant volcanoes. Subcategories. This category has the following 13 ...
A romantic view of a waterfall and country road in Preanger (Parahyangan) region near Sumedang, 1869. Parahyangan (Preanger) or Priangan (Sundanese script: ᮕᮛᮠᮡᮍᮔ᮪) is a cultural and mountainous region in West Java province on the Indonesian island of Java.
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.
The fertile Kedu plain around Borobudur.. Kedu Plain, also known as Progo River Valley, is the fertile volcanic plain that lies between the volcanoes Mount Sumbing and Mount Sundoro to the west, and Mount Merbabu and Mount Merapi to the east.
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.