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The climate of Indonesia is almost entirely tropical. The uniformly warm waters that make up 81% of Indonesia's area ensure that temperatures on land remain fairly constant, with the coastal plains averaging 28 °C (82 °F), the inland and mountain areas averaging 26 °C (79 °F), and the higher mountain regions, 23 °C (73 °F).
This is a list of some of the regions of Indonesia. Many regions are defined in law or regulations by the central government. Many regions are defined in law or regulations by the central government. At different times of Indonesia 's history, the nation has been designated as having regions that do not necessarily correlate to the current ...
Kabaena and surrounding islands of the Buton Archipelago. Kabaena or Tokotua is an island in the Flores Sea, Indonesia, off the coast of Sulawesi.Most of it is a part of Bombana Regency within Southeast Sulawesi province, although the southernmost district (Talaga Raya) is administratively part of Central Buton Regency.
Laiwangi Wanggameti National Park is located on the island of Sumba in Indonesia.All forests types that exist on this island can be found in this national park. Some endemic plant species are protected in this national park, such as Syzygium species, Alstonia scholaris, Ficus species, Canarium oleosum, Cinnamomum zeylanicum, Myristica littoralis, Toona sureni, Sterculia foetida, Schleichera ...
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The region of Indonesia is not generally traversed by tropical cyclones although a lot of systems have historically formed there. [1] In an analysis of tropical cyclone data from the Bureau of Meteorology since 1907 to 2017 which was published after the dissipation of Cyclone Cempaka found that only around 0.62% of all cyclones in the Australian region during those years occurred north of the ...
Mount Arjuno-Welirang is a stratovolcano in the province of East Java in Java, Indonesia. Mount Arjuno-Welirang lies about 50 kilometers (31 mi) south of Surabaya, and 20 kilometers (12 mi) north of Malang. It is a twin volcano, with the 'twins' being Arjuno and Welirang.
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.