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Volhynian Upland
The Volhynian Upland ( uk, Волинська височина, ''volynska vysochyna'') is an upland in western Ukraine, with its small northwestern part stretching into eastern Poland. The Podolian Upland and the Volhynian Upland are sometimes grouped together as the Volhynian-Podolian Upland. It should be known that both uplands are separated by a plain called "Little Polesia" ( uk, Мале Полісся). Volhynian Upland lays between Western Bug and Korchyk River which is a tributary of Sluch River. It stretches for over with a width around . Average elevation is with the maximum being Mizoch Ridge . Its surface is weakly wavy dissected by wide river valleys and gulches. Geologically, it consists of Paleozoic deposits overlapped with rocks of Cretaceous system. There are karst forms of relief and in karstic depressions there exist small lakes. Among minerals there are chalk, black coal, peat, pegmatites, clays. Widespread there are peat bogs. The geographic region ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ukraine Volin Highland En
Ukraine ( uk, Україна, Ukraïna, ) is a country in Eastern Europe. It is the List of European countries by area, second-largest European country after Russia, which it borders Russia–Ukraine border, to the east and northeast. Ukraine covers approximately . Prior to the ongoing 2022 Russian invasion of Ukraine, Russian invasion, it was the List of European countries by population, eighth-most populous country in Europe, with a population of around 41 million people. It is also bordered by Belarus to the north; by Poland, Slovakia, and Hungary to the west; and by Romania and Moldova to the southwest; with a coastline along the Black Sea and the Sea of Azov to the south and southeast. Kyiv is the nation's capital and List of cities in Ukraine, largest city. Ukraine's official language, state language is Ukrainian language, Ukrainian; Russian language in Ukraine, Russian is also widely spoken, especially in the Eastern Ukraine, east and Southern Ukraine, south. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic Deposits
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean but e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of Ukraine
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ukrainian Soviet Encyclopedia
The ''Ukrainian Soviet Encyclopedia'' ( uk, Українська радянська енциклопедія, ''Ukrayinska radyanska entsyklopediya'') was a multi-purpose encyclopedia of Ukraine, issued in the USSR. First attempt Following the publication of the first volume of the in Lviv, then in Poland, in 1930, the ''Ukrainian Soviet Encyclopedia'' (''USE'') was commissioned by Mykola Skrypnyk. During his chairmanship in Kharkiv the editorial board of the ''USE'' was established, enlisting the help of over 100 professionals. Printing began in early 1933, but Moscow censors decried the encyclopedia as being nationalist. Of the 20 planned volumes only three were produced. In the same year Skrypnyk committed suicide, and was succeeded by Volodymyr Zatonsky. The printed copies were destroyed, and plans for the November 1934 edition of USE dissolved. First edition In early 1948, interest in the ''USE'' returned as a response the publication of the '' Encyclopedia of Ukrainia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peat Bog
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A baygall is another type of bog found in the forest of the Gulf Coast states in the United States.Watson, Geraldine Ellis (2000) ''Big Thicket Plant Ecology: An Introduction'', Third Edition (Temple Big Thicket Series #5). University of North Texas Press. Denton, Texas. 152 pp. Texas Parks and Wildlife. Ecological Mapping systems of Texas: West Gulf Coastal Plain Seepage Swamp and Baygall'. Retrieved 7 July 2020 They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink. Bogs occur where the water at the ground surface is acidic and low in nutrients. In contrast to fens, they derive most of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pegmatites
A pegmatite is an igneous rock showing a very coarse texture, with large interlocking crystals usually greater in size than and sometimes greater than . Most pegmatites are composed of quartz, feldspar, and mica, having a similar silicic composition to granite. However, rarer intermediate composition and mafic pegmatites are known. Many of the world's largest crystals are found within pegmatites. These include crystals of microcline, quartz, mica, spodumene, beryl, and tourmaline. Some individual crystals are over long. Most pegmatites are thought to form from the last fluid fraction of a large crystallizing magma body. This residual fluid is highly enriched in volatiles and trace elements, and its very low viscosity allows molecules to migrate rapidly to join an existing crystal rather than coming together to form new crystals. This allows a few very large crystals to form. While most pegmatites have a simple composition of minerals common in ordinary igneous rock, a few pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, 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 hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous System
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mizoch Ridge
Mizoch ( uk, Мізоч, russian: Мизоч, pl, Mizocz, yi, מיזאָטש) is an urban-type settlement in Zdolbuniv Raion, Rivne Oblast, Ukraine, 30 km far from Rivne. Its population was . History The first written record goes back to 1322. The confirmation of the city's legal status dates from 1429. In 1761, the King Augustus III of Poland granted Mizocz the Magdeburg Rights. The civic self-government placed the city Velykyi Mizoch (Greater Mizoch) in the Luts'k district. Between world wars, Mizocz was a multi-ethnic community like many others in eastern Poland, inhabited by Jews, Poles, and Ukrainians. There was a military school in Mizocz for the officer cadets of the Battalion 11 of the Polish Army's First Brigade; the Karwicki Palace (built in 1790, partly destroyed by the Bolsheviks in 1917), Hotel Barmocha Fuksa, a Catholic and an Orthodox church, and a Synagogue. The nearest major city was Równo. In World War II, the town was invaded twice. It fell under the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upland (geology)
Highlands or uplands are areas of high elevation such as a mountainous region, elevated mountainous plateau or high hills. Generally speaking, upland (or uplands) refers to ranges of hills, typically from up to while highland (or highlands) is usually reserved for ranges of low mountains. However, the two terms are sometimes interchangeable. Highlands internationally Probably the best-known area officially or unofficially referred to as ''highlands'' in the Anglosphere is the Scottish Highlands in northern Scotland, the mountainous region north and west of the Highland Boundary Fault. The Highland council area is a local government area in the Scottish Highlands and Britain's largest local government area. Other highland or upland areas reaching 400-500 m or higher in the United Kingdom include the Southern Uplands in Scotland, the Pennines, North York Moors, Dartmoor and Exmoor in England, and the Cambrian Mountains in Wales. Many countries and regions also have areas refe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sluch River (Ukraine)
The Sluch or Southern Sluch (, , , ) is a river, a right tributary of the Horyn, which flows through Ukraine. It has a length of 451 km and a drainage basin of 13,800 km2. The Sluch river takes its source in the Ukrainian province of Khmelnytskyi, and then flows through the Zhytomyr and Rivne oblasts, and flows briefly along the Ukrainian-Belarusian border before finally emptying into the Horyn. Cities and towns located on the Sluch river include: Zviahel, Berezne, and Sarny. Geography Slugs near Gubkov Starts in the Podolian Upland; it flows from a small lake near the village of Chervony Sluch of Galchynetska village council of Theophyll district of the Khmelnytsky region. In the lower reaches in the Polis lowland. First, it flows east, then gradually returns to the north, then to the northwest, and from the city of Sarny - again to the north. Falls to Horyn, south of Velyun village. Large settlements on the Cases: Krasilov, Starokonstantinov, Lyubar, Miropol, Pershot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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