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Karst topography is a geological formation shaped by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite, but also in gypsum. [1] It has also been documented for weathering -resistant rocks, such as quartzite , given the right conditions. [ 2 ]
Karst (/ k ɑːr s t /) is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like ...
Lake Tamblingan (Balinese: Danu Tamblingan ᬤᬦᬸᬢᬫ᭄ᬩᭂᬮᬶᬗᬦ᭄, Indonesian: Danau Tamblingan) is a caldera lake located in Buleleng Regency, Bali. The lake is located at the foot of Mount Lesung in Munduk administrative village, Banjar district, Buleleng Regency, Bali, Indonesia. The lake is one of the three lakes that ...
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Lake Matano (Indonesian: Danau Matano), also known as Matana, is a tropical lake in East Luwu Regency, South Sulawesi province, Indonesia, that is noteworthy for the unique environment in its deeper layers.
The Sangkulirang-Mangkalihat Karst is a karstique area in Sub Kelay, Biatan, Talisayan, Batu Putih, and Biduk-biduk Berau districts of East Kalimantan province on the island of Borneo in Indonesia. It covers an area of 105,000 hectares, including the Mangkalihat Peninsula .
The Lake Sentarum National Park (Indonesian: Taman Nasional Danau Sentarum) is a national park protecting one of the world's most biodiverse lake systems, [2] located in the heart of Borneo Island, Kapuas Hulu Regency, West Kalimantan Province, Indonesia. It lies in the upper Kapuas River tectonic basin some 700 kilometres upstream from the delta.
Karst caves caves that have formed by dissolution of rock. They can be further sub− categorized into 4 specific types of karst they were formed within, Gypsum, Limestone, Quartzite, or Marble. Subcategories