Taevaskoja
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Taevaskoja
Taevaskoja ( vro, Taivaskua) is a village in Põlva Parish, Põlva County in southeastern Estonia, (retrieved 28 July 2021) known for its outcrops of Devonian sandstone on the banks of Ahja river The Ahja ( et, Ahja jõgi) is a river in Estonia. The river is long. The river begins at Lake Erastvere and empties into the River Emajõgi Emajõgi (; meaning ''"Mother River"'') is a river in Estonia which flows from Lake Võrtsjärv thro .... References Villages in Põlva County Tourist attractions in Põlva County {{Põlva-geo-stub ...
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Ahja River
The Ahja ( et, Ahja jõgi) is a river in Estonia. The river is long. The river begins at Lake Erastvere and empties into the River Emajõgi Emajõgi (; meaning ''"Mother River"'') is a river in Estonia which flows from Lake Võrtsjärv through Tartu County into Lake Peipsi, crossing the city of Tartu for 10 km. It has a length of 100 km. The Emajõgi is sometimes called .... Gallery Ahja jõgi, Läänistel, 2008.jpg, The Ahja in Lääniste in 2008 Ahja river, Valgemetsa.JPG, The Ahja near Valgemetsa Kiidjärve_vesiveski.jpg, Kiidjärve watermill, built in 1914 Väike Taevaskoda 2011.jpg, Taevaskoja Talv Väike-Taevaskojas.jpg, Winter in 2016 External links Rivers of Estonia {{Estonia-river-stub ...
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Põlva Parish
Põlva Parish ( et, Põlva vald) is a rural municipality in Põlva County, southeastern Estonia. On 1 January 2009, it had a population of 3,882 and an area of 228.63 km². In October 2013, the town of Põlva (formerly a separate municipality) was merged into Põlva Parish, becoming the centre of it. In 2017, as part of the administrative reform, the neighbouring Ahja, Laheda, Mooste and Vastse-Kuuste parishes were merged with Põlva Parish. Settlements ;Town: Põlva ;Small boroughs: Ahja - Mooste - Vastse-Kuuste ;Villages: Aarna - Adiste - Akste - Andre - Eoste - Himma - Himmaste - Holvandi - Ibaste - Jaanimõisa - Joosu - Kaaru - Kadaja - Kanassaare - Karilatsi - Kastmekoja - Kauksi - Kiidjärve - Kiisa - Kiuma - Koorvere - Kosova - Kähri - Kärsa - Lahe - Laho - Leevijõe - Logina - Loko - Lootvina - Lutsu - Mammaste - Meemaste - Metste - Miiaste - Mustajõe - Mustakurmu - Mõtsküla - Naruski - Nooritsmetsa - Orajõe - Padari - Partsi - Pe ...
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Counties Of Estonia
Counties ( et, maakond, plural ') are the first-level administrative subdivisions of Estonia. Estonian territory is composed of 15 counties, including 13 on the mainland and 2 on islands. The government (') of each county is led by a ' (governor) who represents the national government (') at the regional level. Governors are appointed by the national government for a term of five years. Each county is further divided into municipalities of two types: urban municipalities (towns, ') and rural municipalities (parishes, '). The number and name of the counties were not affected. However, their borders were changed by the administrative reform at the municipal elections Sunday 15 October 2017, which brought the number of municipalities down from 213 to 79. List Population figures as of 1 January 2021. The sum total of the figures in the table is 42,644 km2, of which the land area is 42,388 km2, so that 256 km2 of water is included in the figures. History In the first ...
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Põlva County
Põlva County ( et, Põlva maakond or ''Põlvamaa'') is one of 15 counties of Estonia. It is situated in south-eastern part of the country and borders Tartu, Valga and Võru counties. 28,507 people live in Põlva County – constituting 2.3% of the total population in Estonia (as of January 2013). Government The County Government (Estonian: ''Maavalitsus'') is led by the Governor (Estonian: ''maavanem''), who is appointed by the Government of Estonia for a term of five years. Since 2007, the Governor position is held by Priit Sibul. Municipalities The county is subdivided into municipalities. There are 3 rural municipalities ( et, vallad – parishes) in Põlva County. Demographics 27,028 people live in Põlva County – constituting 2.1% of the total population in Estonia (as of January 2013). Gallery Ahja tiik 2.jpg, Ahja Pikajärve mõisa aitkuivati *.jpg, Pikajärve manor granary Aalupi järv 2013 08.jpg, Lake Aalupi Pikajärve mõisa peahoone2.jpg, Pikajä ...
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Eastern European Time
Eastern European Time (EET) is one of the names of UTC+02:00 time zone, 2 hours ahead of Coordinated Universal Time. The zone uses daylight saving time, so that it uses UTC+03:00 during the summer. A number of African countries use UTC+02:00 all year long, where it is called Central Africa Time (CAT), although Egypt and Libya also use the term ''Eastern European Time''. The most populous city in the Eastern European Time zone is Cairo, with the most populous EET city in Europe being Athens. Usage The following countries, parts of countries, and territories use Eastern European Time all year round: * Egypt, since 21 April 2015; used EEST ( UTC+02:00; UTC+03:00 with daylight saving time) from 1988–2010 and 16 May–26 September 2014. See also Egypt Standard Time. * Kaliningrad Oblast (Russia), since 26 October 2014; also used EET in years 1945 and 1991–2011. See also Kaliningrad Time. * Libya, since 27 October 2013; switched from Central European Time, which was u ...
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Eastern European Summer Time
Eastern European Summer Time (EEST) is one of the names of the UTC+03:00 time zone, which is 3 hours ahead of Coordinated Universal Time. It is used as a summer daylight saving time in some European and Middle Eastern countries, which makes it the same as Arabia Standard Time, East Africa Time, and Moscow Time. During the winter periods, Eastern European Time ( UTC+02:00) is used. Since 1996, European Summer Time has been applied from the last Sunday in March to the last Sunday in October. Previously, the rules were not uniform across the European Union. Usage The following countries and territories use Eastern European Summer Time during the summer: * Belarus, Moscow Summer Time in years 1981–89, regular EEST from 1991-2011 * Bulgaria, regular EEST since 1979 * Cyprus, regular EEST since 1979 ( Northern Cyprus stopped using EEST in September 2016, but returned to EEST in March 2018) * Estonia, Moscow Summer Time in years 1981–88, regular EEST since 1989 * Finland, regu ...
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Estonia
Estonia, formally the Republic of Estonia, is a country by the Baltic Sea in Northern Europe. It is bordered to the north by the Gulf of Finland across from Finland, to the west by the sea across from Sweden, to the south by Latvia, and to the east by Lake Peipus and Russia. The territory of Estonia consists of the mainland, the larger islands of Saaremaa and Hiiumaa, and over 2,200 other islands and islets on the eastern coast of the Baltic Sea, covering a total area of . The capital city Tallinn and Tartu are the two largest urban areas of the country. The Estonian language is the autochthonous and the official language of Estonia; it is the first language of the majority of its population, as well as the world's second most spoken Finnic language. The land of what is now modern Estonia has been inhabited by '' Homo sapiens'' since at least 9,000 BC. The medieval indigenous population of Estonia was one of the last " pagan" civilisations in Europe to adopt Ch ...
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Outcrop
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and build ...
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Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Railway Stop Near Taevaskoja Village
Rail transport (also known as train transport) is a means of transport that transfers passengers and goods on wheeled vehicles running on rails, which are incorporated in tracks. In contrast to road transport, where the vehicles run on a prepared flat surface, rail vehicles (rolling stock) are directionally guided by the tracks on which they run. Tracks usually consist of steel rails, installed on sleepers (ties) set in ballast, on which the rolling stock, usually fitted with metal wheels, moves. Other variations are also possible, such as "slab track", in which the rails are fastened to a concrete foundation resting on a prepared subsurface. Rolling stock in a rail transport system generally encounters lower frictional resistance than rubber-tyred road vehicles, so passenger and freight cars (carriages and wagons) can be coupled into longer trains. The operation is carried out by a railway company, providing transport between train stations or freight customer facili ...
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Villages In Põlva County
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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