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Hostýn
Hostýn (or Svatý Hostýn, i.e. Saint Hostýn) is a hill in Chvalčov in the Zlín Region of the Czech Republic. It is part of the Hostýn-Vsetín Mountains and has an elevation of . It is an important Marian place of pilgrimage. The pilgrimage comes from a legend that describes a miracle made by the Virgin Mary. Legend According to a traditional legend, first recorded in 1665 by the writer Bohuslav Balbín in his work ''Diva Montis Sancti'', during the disastrous raid of the "Tartars" in the 13th century, people who were seeking asylum here lacked water and they prayed Mary for help. It is said that a stream of water came out of the ground and a powerful storm forced Tatars to retreat. History On the hilltop is an ancient hill fort with a ditch and defensive wall made of earth and stone, which is 4–8 metres high. The fortification was first built by the people of the Lusatian culture circa 1200 BCE. In later centuries it was destroyed and rebuilt several times, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hostýn-Vsetín Mountains
Hostýn-Vsetín Mountains ( cs, Hostýnsko-vsetínská hornatina) is a mountain range in the Zlín Region of the Czech Republic. The mountains are densely forested mainly by secondary spruce plantations. Most visited are the bordering Rožnovská Bečva river valley in the north (with Valašské Meziříčí and Rožnov pod Radhoštěm towns and Dolní, Prostřední and Horní (i.e. ''Lower, Middle'' and ''Upper'') Bečva resorts) and the southern Vsetínská Bečva river valley starting in the town of Vsetín with the resort of Velké Karlovice. The Hostýn-Vsetín Mountains are part of the Western Carpathians, it is divided by the Bečva River valley into the lower eastern ''Hostýnské vrchy'' and the higher western ''Vsetínské vrchy'' which are a part of the Beskydy Landscape Protected Area. They are built mainly of flysch Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zlín Region
Zlín Region ( cs, Zlínský kraj; , ) is an administrative unit ( cs, kraj) of the Czech Republic, located in the south-eastern part of the historical region of Moravia. It is named after its capital Zlín. Together with the Olomouc Region it forms a cohesion area of Central Moravia. It is located in the eastern part of the Czech Republic, where the borders with Slovakia (Trenčín and Žilina Regions) are formed by its eastern edge. It borders the South Moravian Region in the southwest, the Olomouc Region in the northwest and the Moravian-Silesian Region in the north. Culturally, the region is composed of parts of three traditional Moravian regions: Hanakia, the Moravian Slovakia and the Moravian Wallachia, as the city of Zlín lies roughly at their tripoint. Administrative divisions The Zlín Region is divided into 4 districts: The Zlín Region was established on 1 January 2000 on the basis of the constitutional act No. 347 from 3 December 1997 on foundation of higher self- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kroměříž District
Kroměříž District ( cs, okres Kroměříž) is a district ('' okres'') within the Zlín Region of the Czech Republic. Its capital is the town of Kroměříž. List of municipalities Bařice-Velké Těšany - Bezměrov - Blazice - Bořenovice - Brusné - Břest - Bystřice pod Hostýnem - Cetechovice - Chomýž - Chropyně - Chvalčov - Chvalnov-Lísky - Dřínov - Holešov - Honětice - Horní Lapač - Hoštice - Hulín - Jankovice - Jarohněvice - Karolín - Komárno - Koryčany - Kostelany - Kostelec u Holešova - Kroměříž Kroměříž (; german: Kremsier) is a town in the Zlín Region of the Czech Republic. It has about 28,000 inhabitants. It is known for the Kroměříž Castle with castle gardens, which are a UNESCO World Heritage Site. The town centre with the ... - Kunkovice - Kurovice - Kvasice - Kyselovice - Lechotice - '' Litenčice'' - Loukov - Lubná - Ludslavice - Lutopecny - Martinice - Míškovice - Morkovice-Slížany - M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chvalčov
Chvalčov is a municipality and village in Kroměříž District in the Zlín Region of the Czech Republic. It has about 1,600 inhabitants. Chvalčov lies approximately north-east of Kroměříž, north of Zlín, and east of Prague. History The first written mention of Chvalčov is from 1369. Sights The Hostýn Hostýn (or Svatý Hostýn, i.e. Saint Hostýn) is a hill in Chvalčov in the Zlín Region of the Czech Republic. It is part of the Hostýn-Vsetín Mountains and has an elevation of . It is an important Marian place of pilgrimage. The pilgrim ... hill, a Catholic pilgrimage site, lies in the municipal territory of Chvalčov. There is also the ruin of Obřany Castle on the eponymous hill. References Villages in Kroměříž District {{Zlín-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust ( pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Czech Republic
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deluvial
Diluvium is an archaic term applied during the 1800s to widespread surficial deposits of sediments that could not be explained by the historic action of rivers and seas. Diluvium was initially argued to have been deposited by the action of extraordinary floods of vast extent, specifically the Noachian Flood.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Kotlyakov, V. and Komarova, A., 2006. ''Elsevier's dictionary of geography: in English, Russian, French, Spanish and German.'' New York, Elsevier Scientific Publishing. 1072 pp. In 1822 and 1823, William Buckland published the term ''diluvium'' in his monograph ''Reliquiae Diluvianae ''Buckland, W., 1823. ''Reliquiae Diluvianae, or Observations on the Organic Remains Contained in Caves, Fissures, and Diluvial Gravel, and on Other Geological Phenomena, Attesting the Action of an Universal Deluge.'' 1st ed. John Murray, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 relate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago ( Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of the Cretaceous–Paleogene extinction event that ended the preceding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pius X
Pope Pius X ( it, Pio X; born Giuseppe Melchiorre Sarto; 2 June 1835 – 20 August 1914) was head of the Catholic Church from 4 August 1903 to his death in August 1914. Pius X is known for vigorously opposing modernist interpretations of Catholic doctrine, and for promoting liturgical reforms and scholastic theology. He initiated the preparation of the 1917 Code of Canon Law, the first comprehensive and systemic work of its kind. He is venerated as a saint in the Catholic Church and is the namesake of the traditionalist Catholic Priestly Fraternity of Saint Pius X. Pius X was devoted to the Blessed Virgin Mary under the title of Our Lady of Confidence; while his papal encyclical ''Ad diem illum'' took on a sense of renewal that was reflected in the motto of his pontificate. He advanced the Liturgical Movement by formulating the principle of ''participatio actuosa'' (active participation of the faithful) in his motu proprio, ''Tra le sollecitudini'' (1903). He encouraged ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rome
, established_title = Founded , established_date = 753 BC , founder = King Romulus (legendary) , image_map = Map of comune of Rome (metropolitan city of Capital Rome, region Lazio, Italy).svg , map_caption = The territory of the ''comune'' (''Roma Capitale'', in red) inside the Metropolitan City of Rome (''Città Metropolitana di Roma'', in yellow). The white spot in the centre is Vatican City. , pushpin_map = Italy#Europe , pushpin_map_caption = Location within Italy##Location within Europe , pushpin_relief = yes , coordinates = , coor_pinpoint = , subdivision_type = Country , subdivision_name = Italy , subdivision_type2 = Region , subdivision_name2 = Lazio , subdivision_type3 = Metropolitan city , subdivision_name3 = Rome Capital , government_footnotes= , government_type = Strong Mayor–Council , leader_title2 = Legislature , leader_name2 = Capitoline Assembl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
