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The Devil's Nest
The Devil's Nest (Pirunpesä) is an eroded cavity located in the village Ylivalli in the municipality Jalasjärvi in Southern Ostrobothnia, Finland. It is 14 meters wide and 23 meters deep, and the deepest earth erosion in Europe. Formation The evolution of the Devil’s Nest can be explained in three stages: during the Tertiary period, the Ice Age and the present time. Clearly, it took over million years to turn into the way it is now. During Tertiary the area was very dry and vulnerable to erosion. The surface of the mountain was eroded many meters, forming an erosion layer. At the same time, a vertical cut was formed in the surface which was filled with eroded material. This was the first stage of the Devil’s Nest. During the Ice Age period (about 2 million years ago) there have been 4 glacial events and between them, interglacial periods that were comparable to the present climate. These glaciers overrode the area several times, removing the eroded surface layer down to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Municipalities Of Finland
The municipalities ( fi, kunta; sv, kommun) represent the local level of administration in Finland and act as the fundamental, self-governing administrative units of the country. The entire country is incorporated into municipalities and legally, all municipalities are equal, although certain municipalities are called cities or towns ( fi, kaupunki; sv, stad). Municipalities have the right to levy a flat percentual income tax, which is between 16 and 22 percent, and they provide two thirds of public services. Municipalities control many community services, such as schools, health care and the water supply, and local streets. They do not maintain highways, set laws or keep police forces, which are responsibilities of the central government. Government Municipalities have council-manager government: they are governed by an elected council (, ), which is legally autonomous and answers only to the voters. The size of the council is proportional to the population, the extremes bein ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jalasjärvi
Jalasjärvi is a former municipality of Finland. It was merged to the town of Kurikka on 1 January 2016. It is located in the province of Western Finland and is part of the Southern Ostrobothnia region. The population of Jalasjärvi was (30 June 2015) and covered a land area of . The population density was . The municipality was unilingually Finnish. Villages Alavalli, Hirvijärvi, Ilvesjoki, Jalasjärvi, Jokipii, Keskikylä, Koskue, Luopajärvi, Sikakylä, Taivalmaa and Ylivalli. Sights * The Devil's Nest, the deepest ground erosion in Europe * The Local Heritage Museum of Jalasjärvi, one of the largest local museum A local museum or local history museum is a type of museum that shows the historical development of a place/region (local history) using exhibits. These museums usually maintain a collection of historic three-dimensional objects which are exh ...s in Finland, consisting of over 25 rural buildings and a collection of exhibits approaching nearly 30 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Ostrobothnia
South Ostrobothnia ( fi, Etelä-Pohjanmaa; sv, Södra Österbotten) is one of the 19 regions of Finland. It borders the regions of Ostrobothnia, Central Ostrobothnia, Central Finland, Pirkanmaa, and Satakunta. Among the Finnish regions, South Ostrobothnia is the ninth largest in terms of population. Seinäjoki is the regional centre and by far the largest city in the area. As a cultural area, South Ostrobothnia is larger than its current regional borders and includes the region of Ostrobothnia as well. Historical provinces Municipalities The region of South Ostrobothnia is made up of 18 municipalities, of which eight have city status (marked in bold). Järviseutu sub-region: * Alajärvi (10,277) * Evijärvi (2,686) * Lappajärvi (3,394) * Vimpeli (3,212) Kuusiokunnat sub-region: * Alavus (12,354) * Kuortane (3,870) * Soini (2,367) * Ähtäri (6,394) Seinäjoki sub-region: * Ilmajoki (12,165) * Isokyrö () * Kauhava (17,206) * Kurikka (21,734) * Lapua (14,698) * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary Glaciation
The Quaternary glaciation, also known as the Pleistocene glaciation, is an alternating series of glacial and interglacial periods during the Quaternary period that began 2.58 Ma (million years ago) and is ongoing. Although geologists describe this entire period up to the present as an "ice age", in popular culture this term usually refers to the most recent glacial period, or to the Pleistocene epoch in general. Since Earth still has polar ice sheets, geologists consider the Quaternary glaciation to be ongoing, though currently in an interglacial period. During the Quaternary glaciation, ice sheets appeared, expanding during glacial periods and contracting during interglacial periods. Since the end of the last glacial period, only the Antarctic and Greenland ice sheets have survived, with other sheets formed during glacial periods, such as the Laurentide Ice Sheet, having completely melted. The major effects of the Quaternary glaciation have been the continental erosion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interglacial Period
An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age. The current Holocene interglacial began at the end of the Pleistocene, about 11,700 years ago. Pleistocene During the 2.5 million years of the Pleistocene, numerous glacials, or significant advances of continental ice sheets, in North America and Europe, occurred at intervals of approximately 40,000 to 100,000 years. The long glacial periods were separated by more temperate and shorter interglacials. During interglacials, such as the present one, the climate warms and the tundra recedes polewards following the ice sheets. Forests return to areas that once supported tundra vegetation. Interglacials are identified on land or in shallow epicontinental seas by their paleontology. Floral and faunal remains of species pointing to temperate climate and indicating a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devil
A devil is the personification of evil as it is conceived in various cultures and religious traditions. It is seen as the objectification of a hostile and destructive force. Jeffrey Burton Russell states that the different conceptions of the devil can be summed up as 1) a principle of evil independent from God, 2) an aspect of God, 3) a created being turning evil (a ''fallen angel''), and 4) a symbol of human evil. Each tradition, culture, and religion with a devil in its mythos offers a different lens on manifestations of evil.Jeffrey Burton Russell, ''The Devil: Perceptions of Evil from Antiquity to Primitive Christianity'', Cornell University Press 1987 , pp. 41–75 The history of these perspectives intertwines with theology, mythology, psychiatry, art, and literature developing independently within each of the traditions. It occurs historically in many contexts and cultures, and is given many different names— Satan, Lucifer, Beelzebub, Mephistopheles, Iblis—and at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seinäjoki
Seinäjoki (; "Wall River"; la, Wegelia, formerly sv, Östermyra) is a city located in South Ostrobothnia, Finland; east of Vaasa, north of Tampere, west of Jyväskylä and southwest of Oulu. Seinäjoki originated around the Östermyra bruk iron and gunpowder factories founded in 1798. Seinäjoki became a municipality in 1868, market town in 1931 and town in 1960. In 2005, the municipality of Peräseinäjoki was merged into Seinäjoki, and in the beginning of 2009, the neighbouring municipalities of Nurmo and Ylistaro were consolidated with Seinäjoki. Seinäjoki is one of the fastest growing regional centers in Finland. The city hall, city library, Lakeuden Risti Church and other public buildings were designed by Alvar Aalto. Seinäjoki was historically called ' in Swedish. Today this name, which never was official, is very seldom used even among the Swedish speakers. Seinäjoki Airport is located in the neighbouring municipality of Ilmajoki, south of the Seinäjoki c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Finland
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of South Ostrobothnia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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