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Albínovská Hora
Albínovská hora, sometimes also Albínovská hôrka (translated to English as ''Albinov Hill'' or ''Albinov Mountain'', in local dialect ''Baňa''—Mine from Hungarian ''Bánya'') is a hill located on the west part of Sub-Slanec Hills, division of Eastern Slovak Hills, in eastern Slovakia. The hill is high and it is located in the administrative area of Sečovce, north of the residential area. Remains of Tertiary volcanic activity in the area (see Slanské Hills) is andesite and characteristic tuff, covered under layers by Neogene sedimentary rocks – gravel, sand, kaolin Kaolinite ( ) is a clay mineral, with the chemical composition Al2 Si2 O5( OH)4. It is an important industrial mineral. It is a layered silicate mineral, with one tetrahedral sheet of silica () linked through oxygen atoms to one octahedral ... etc.Magyar, Július (2009), Prírodné podmienky, in Ordoš, Ján, edi. ''Sečovce'', 2nd edition, Prešov: L.I.M., pp. 7–24, , p.13 Footnotes Mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sečovce
Sečovce (; hu, Gálszécs; uk, Сечівці) is a town in the Trebišov District in the Košice Region of south-eastern Slovakia. History The town was first mentioned in year 1255 on the list of king Béla IV of Hungary. In 1494, a Roman Catholic church was built in the Gothic architecture style. Since the 15th century, there was gradual development of trade, including markets with shoemakers, saddlers, potters and furriers. The first post-office was opened in 1783, telegraph office in 1868, telephone office in 1890, train station in 1904, and museum in 1954, which was moved to Trebišov in 1981. Geography The town lies at an altitude of , which rises to on Albínovská hora. It covers an area of and has a population of about 8,000. Demographics According to the 2001 census, it had 7,819 inhabitants - 95.89% of whom were Slovak, 2.17% Roma, 0.47% Czech, and 0.22% Hungarian. The religious makeup was 47.05% Roman Catholic, 25.71% Greek Catholic, 18.11% with no religiou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovakia
Slovakia (; sk, Slovensko ), officially the Slovak Republic ( sk, Slovenská republika, links=no ), is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the southwest, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , with a population of over 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of present-day Slovakia in the fifth and sixth centuries. In the seventh century, they played a significant role in the creation of Samo's Empire. In the ninth century, they established the Principality of Nitra, which was later conquered by the Principality of Moravia to establish Great Moravia. In the 10th century, after the dissolution of Great Moravia, the territory was integrated into the Principality of Hungary, which then became the Kingdom of Hungary in 1000. In 1241 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Slovak Hills
The East(ern) Slovak Hills (Slovak: ''Východoslovenská pahorkatina''), also translated as Eastern Slovak Upland, is the higher, mountain-like part of the Eastern Slovak Lowland. It is a strip of hilly land surrounding the Eastern Slovak Flat along the neighbouring volcanic mountains of the Carpathians. It covers an area of 735 km², and the highest point is Dúbravka at 397 m. Important towns: Michaľany, Dargov, Vranov nad Topľou, Strážske, Michalovce. Division: #Podslanská pahorkatina (Sub-Slanec Hills) #Toplianska niva (Topľa River Plain) #Vranovská pahorkatina (Vranov Hills) #Ondavská niva (Ondava River Plain) #Pozdišovský chrbát (Pozdišovce Ridge) #Laborecká niva (Laborec River Plain) #Podvihorlatská pahorkatina (Sub-Vihorlat Hills) #Zálužická pahorkatina (Zálužica Hills) #Petrovské podhorie (Petrovce Piedmont) An important recreation area is the Zemplínska šírava Dam. Alkaline salty springs can be found at the Byšta Byšta ( hu, Biste) is a vill ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yosemite Decimal System
The Yosemite Decimal System (YDS) is a three-part system used for rating the difficulty of walks, hikes, and climbs, primarily used by mountaineers in the United States and Canada. It was first devised by members of the Sierra Club in Southern California in the 1950s as a refinement of earlier systems, particularly those developed in Yosemite Valley, and quickly spread throughout North America. Description The class 5 portion of the class scale is primarily a rock climbing classification system, while classes 1–2 are used mainly in hiking and trail running. Class 3 describes easy and moderate climbing (i.e. scrambling), with varying amounts of exposure (length of a possible fall). Class 4 is an "in-between" rating that describes a very exposed scramble, corresponding roughly to the IFAS classification of PD+. Climbers, specifically those involved with technical class 5 climbing, often abbreviate "class 3" and "class 4" to "3rd" and "4th" respectively. Originally the system was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harmanec
Harmanec ( hu, Hermánd) is a village and municipality in Banská Bystrica District in the Banská Bystrica Region of central Slovakia. History The village first appears in historical records circa 1540. Geography The municipality lies at an altitude of 486 metres and covers an area of 7.757 km². It has a population Population typically refers to the number of people in a single area, whether it be a city or town, region, country, continent, or the world. Governments typically quantify the size of the resident population within their jurisdiction using a ... of about 918 people. Sights The village is located close to the Harmanec Cave. References External links * https://www.harmanec.sk/ Villages and municipalities in Banská Bystrica District {{BanskaBystrica-geo-stub ... [...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] |
Slanské Hills
The Slanské Hills (in Slovak, ''Slanské vrchy'') is a range of mountains in eastern Slovakia, one segment of the Mátra-Slanec Area of the Inner Western Carpathians. Overview The area is named after the nearest town in the southern portion, Slanec. The range is approximately long, side, and extends southeast of the city of Prešov, between the and the Eastern Slovak Lowland. The mountains average high, with the highest elevation at , (where 700 healthy, mature elms were discovered in 1998). The mountains are forested, with several mineral springs, and resources such as gold, silver, and antimony. Passes through the mountains include the Herľany Pass and Dargov Pass (''Dargovský priesmyk''), site of a significant World War II battle. Geology and formation The Slanské Hills are a chain of andesite volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma cham ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaolin
Kaolinite ( ) is a clay mineral, with the chemical composition Al2 Si2 O5( OH)4. It is an important industrial mineral. It is a layered silicate mineral, with one tetrahedral sheet of silica () linked through oxygen atoms to one octahedral sheet of alumina () octahedra. Rocks that are rich in kaolinite are known as kaolin () or china clay. Kaolin is occasionally referred to by the antiquated term lithomarge, from the Ancient Greek ''litho-'' and Latin ''marga'', meaning 'stone of marl'. Presently the name lithomarge can refer to a compacted, massive form of kaolin. The name ''kaolin'' is derived from Gaoling (), a Chinese village near Jingdezhen in southeastern China's Jiangxi Province. The name entered English in 1727 from the French version of the word: , following François Xavier d'Entrecolles's reports on the making of Jingdezhen porcelain. Kaolinite has a low shrink–swell capacity and a low cation-exchange capacity (1–15 meq/100 g). It is a soft, earthy, usu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
