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Indonesia's climate is almost entirely tropical, dominated by the tropical rainforest climate found in every major island of Indonesia, followed by the tropical monsoon climate that predominantly lies along Java's coastal north, Sulawesi's coastal south and east, and Bali, and finally the tropical savanna climate, found in isolated locations of ...
Indonesia, [c] officially the Republic of Indonesia, [d] is a country in Southeast Asia and Oceania, between the Indian and Pacific oceans. Comprising over 17,000 islands, including Sumatra, Java, Sulawesi, and parts of Borneo and New Guinea, Indonesia is the world's largest archipelagic state and the 14th-largest country by area, at 1,904,569 square kilometres (735,358 square miles).
The location of Indonesia An enlargeable map of the Republic of Indonesia (excluding North Kalimantan, Riau Islands, West Papua, and West Sulawesi). The following outline is provided as an overview of and topical guide to Indonesia:
Indonesia provinces blank map.svg Module:Location map/data/Indonesia provinces is a location map definition used to overlay markers and labels on an equirectangular projection map of Indonesia . The markers are placed by latitude and longitude coordinates on the default map or a similar map image.
The following is a list of ecoregions in Indonesia. An ecoregion is defined by the WWF as a "large area of land or water that contains a geographically distinct assemblage of natural communities". There are terrestrial, freshwater, and marine ecoregions. Ecoregions classified into biomes or major habitat types.
Gunung Sewu Geopark or Sewu Mountains (Indonesian: Pegunungan Sewu) is a series of mountains stretching along the southern coast of Gunung Kidul Regency and Wonogiri Regency of Central Java, to Pacitan Regency of East Java in the island of Java, Indonesia.
Lombok, [a] is an island in West Nusa Tenggara province, Indonesia.It forms part of the chain of the Lesser Sunda Islands, with the Lombok Strait separating it from Bali to the west and the Alas Strait between it and Sumbawa 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.