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Jizerské Hory
Jizera Mountains ( cz, Jizerské hory), or Izera Mountains ( pl, Góry Izerskie; german: Isergebirge), are part of the Western Sudetes on the border between the Czech Republic and Poland. The range got its name from the Jizera River, which rises at the southern base of the Smrk massif. The beech forests within the Jizera Mountains were added to the UNESCO World Heritage Site known as Ancient and Primeval Beech Forests of the Carpathians and Other Regions of Europe, because of their outstanding preservation and testimony to the ecological history of Europe (and the beech family specifically) since the Last Glacial Period. Geography The range stretches from the Lusatian Mountains (Zittau Mountains) in the northwest to the Krkonoše in the southeast. The Jizera Mountains comprise the sources of the Jizera river, as well as of the Kwisa and the Lusatian Neisse. The major part in the south is formed from granite, in the northern part from gneisses and mica schists, with some areas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liberec
Liberec (; german: Reichenberg ) is a city in the Czech Republic. It has about 103,000 inhabitants and it is the fifth-largest city in the country. It lies on the Lusatian Neisse, in a basin surrounded by mountains. The city centre is well preserved and is protected by law as an urban monument zone. Liberec was once home to a thriving textile industry and hence nicknamed the "Manchester of Bohemia". For many Czechs, Liberec is mostly associated with the city's dominant Ještěd Tower. Since the end of the 19th century, the city has been a conurbation with the suburb of Vratislavice nad Nisou and the neighbouring city of Jablonec nad Nisou. Therefore, the total area with suburbs encompasses 150,000 inhabitants. Administrative parts Liberec is made up of 32 city parts and one self-governing borough (Vratislavice nad Nisou). *Liberec I-Staré Město *Liberec II-Nové Město *Liberec III-Jeřáb *Liberec IV-Perštýn *Liberec V-Kristiánov *Liberec VI-Rochlice *Liberec VII-Horní ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lusatian Mountains
The Lusatian Mountains ( cs, Lužické hory; german: Lausitzer Gebirge; pl, Góry Łużyckie) are a mountain range of the Western Sudetes on the southeastern border of Germany with the Czech Republic. They are a continuation of the Ore Mountains range west of the Elbe valley. The mountains of the northern, German, part are called the Zittau Mountains. Geography The range is among the westernmost extensions of the Sudetes, which stretch along the border between the historic region of Silesia in the north, and Bohemia and Moravia in the south up to the Moravian Gate in the east, where they join the Carpathian Mountains. The northwestern foothills of the Lusatian Mountains are called the Lusatian Highlands; in the southwest the range borders on the České Středohoří mountains. The range is largely made up of sandstone sedimentary rocks leaning on a Precambrian crystalline Basement (geology), basement. The northern ridge is marked by the Lusatian Fault, a geological disturban ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smrk
Smrk may refer to: * Smrk (Jizera Mountains), the highest mountain in the Jizera Mountains of Bohemia, Czech Republic at 1124m * Smrk (Moravian-Silesian Beskids) Smrk is a massif and a mountain in the Moravian-Silesian Beskids range in the Czech Republic. With a height of it is the second highest summit of the range after Lysá hora. Its Northern slope steeply rises from the surrounding lowlands and is ..., a mountain in the Moravian-Silesian Beskids range in the Czech Republic * Smrk (Třebíč District), Vysočina, Czech Republic {{disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tafelfichte Clean
Smrk ( pl, Smrek; german: Tafelfichte) is the highest mountain in the Czech part of the Jizera Mountains. Rising , it is sometimes known as "The King of the Jizera Mountains". Geography The top of the mountain lies in the municipal territory of Lázně Libverda in the Liberec Region of northern Bohemia. On the eastern rim of the plateau is the boundary with Poland; the Polish summit west of Świeradów-Zdrój reaches a height of . The summit offers a panoramic view to the prominent Sněžka peak of the Giant Mountains in the east, as well as to the Lusatian Highlands beyond the German border in the west up to the cooling towers of Boxberg Power Station. History The "Tabulový kámen" (''Tafelstein'') stone monument on the northern slope marks the site, which since the Middle Ages formed the historic tripoint between * the Upper Lusatian lordship of ''Meffersdorf'' (Polish: Unięcice, in present-day Pobiedna) * the Lower Silesian duchy of Jawor, where the lands around Szklar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nová Louka
Nová Louka (german: Neuwiese or ) is a mountain meadow in Jizera Mountains (in Czech Jizerské hory) near the city of Bedřichov, district of Jablonec nad Nisou. It is situated in the north of the Czech Republic, approximately 130 km from Prague. There is Blatny brook (in Czech Blatný potok) flowing through the meadow. Nová Louka is an important cross-road of tourist paths in Jizera Mountains. There is sometimes used an alternative, less common name for the meadow which is Šámalova louka after the Czech politician Přemysl Šámal who resided in the house on the meadow. Šámal was the head of the Office of the President of Czechoslovakia during the First Czechoslovak Republic; he took part in resistance movements during World War I and II, and ultimately died in the Nazi prison in Moabit, Berlin. The meadow is a protected area with peat moor and several protected plants, including hellebore. It was created in 1630 when the trees were cut for the construction of hous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mica
Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists, and "books" (large individual crystals) of mica several feet across have been found in some pegmatites. Micas are used in products such as drywalls, paints, fillers, especially in parts for automobiles, roofing and shingles, as well as in electronics. The mineral is used in cosmetics and food to add "shimmer" or "frost." Properties and structure The mica group is composed of 37 phyllosilicate minerals. All crystallize in the monoclinic system, with a tendency towards pseudohexagonal crystals, and are similar in structure but vary in chemical composition. Micas are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lusatian Neisse
The Lusatian Neisse (german: Lausitzer Neiße; pl, Nysa Łużycka; cs, Lužická Nisa; Upper Sorbian: ''Łužiska Nysa''; Lower Sorbian: ''Łužyska Nysa''), or Western Neisse, is a river in northern Central Europe.''Neisse River'' at www.britannica.com. Retrieved 4 Feb 2011. at http://eagri.cz/public. Retrieved 4 Feb 2011. It rises in the , near |
