Tuhala Nõiakaev 4
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Tuhala Nõiakaev 4
Tuhala is a village in Kose Parish, Harju County in northern Estonia. As of the 2011 census, the settlement's population was 105. It is believed that settlement in Tuhala dates back around 3,000 years. The Tuhala Karst Area, named after the village, lies for the most part in neighbouring Kata village. It has Estonia's largest area of porous karst, with several underground rivers and sinkholes. The karst area is best known for its Witch's Well (also in Kata). Tuhala Manor Tuhala Manor was first mentioned in 1468 as ''Toall''. It belonged to several Baltic German families: Tödwen (1468–1517); Delwig (1517 – mid-16th century); Ulrich (?–1663); Wrangell (1663–1693); Mellin (1692–1863); Lilienfeld (1863–1919). The cartographer Ludwig August Mellin was born in the manor. The last main building had two storeys and was built 1800. Its early Classical appearance was changed to a more Neoclassical appearance in the 1880s. The manor was burned down during the Revolution o ...
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Populated Places In Estonia
Populated places in Estonia (officially: settlement units), are cities or settlement units of rural municipality, municipalities, but only cities have administrative functions. Settlement units are divided into settlements and urban regions (subdivisions of cities). Officially there are four types of settlement unit in Estonia: * village () - a sparsely populated settlement or a densely populated settlement with fewer than 300 permanent inhabitants * township () - a densely populated settlement with at least 300 permanent inhabitants * town () - a densely populated settlement with at least 1000 permanent inhabitants * city () As of 2024, there were 47 cities, 13 towns, 186 hamlets and 4457 villages in Estonia. See also *Municipalities of Estonia *List of cities and towns in Estonia *Counties of Estonia Notes References External links Place Names Board of Estonia
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Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ...
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