Katzbach Mountains
The Katzbach Mountains or Kaczawskie Mountains ( pl, Góry Kaczawskie; german: Katzbachgebirge) are a mountain range, roughly 30 kilometres long, in the Western Sudetes in Poland. It is located within the Polish province of Lower Silesia. Its highest peak is the Melkgelte / Skopiec (724 m). To the north of the Katzbach Mountains are the Katzbach Foothills ( pl, Pogórze Kaczawskie; german: Bober-Katzbach-Vorgebirge). Location The ridge, which runs from northwest to southeast at heights between 400 and 700 metres, is a fold mountain range consisting of limestone, slate and dolomite. In the west the Bober separates the range from the Jizera Mountains and Jizera Foreland; to the north are the Katzbach Foothills; to the east the Raging Neisse / Nysa Szalona forms the boundary. In the southeast, the Katzbach Mountains merge into the Waldenburg/Walbrzyskie Highlands. To the south, the Landeshut Ridge / Rudawy Janowickie and Jelenia Gora Valley form the transition to the Giant ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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2006
File:2006 Events Collage V1.png, From top left, clockwise: The 2006 Winter Olympics open in Turin; Twitter is founded and launched by Jack Dorsey; The Nintendo Wii is released; Montenegro 2006 Montenegrin independence referendum, votes to declare independence from Serbia; The 2006 FIFA World Cup in Germany is won by Italy; Gol Transportes Aéreos Flight 1907 crashes in the Amazon rainforest after a mid-air collision with an Embraer Legacy 600 business jet; The 2006 Yogyakarta earthquake kills over 5,700 people; The IAU votes on the IAU definition of planet, definition of "planet", which demotes Pluto and other Kuiper belt objects and redefines them as "Dwarf planet, dwarf planets"., 300x300px, thumb rect 0 0 200 200 2006 Winter Olympics rect 200 0 400 200 Twitter rect 400 0 600 200 Nintendo Wii rect 0 200 300 400 IAU definition of planet rect 300 200 600 400 2006 Montenegrin independence referendum rect 0 400 200 600 2006 Yogyakarta earthquake rect 200 400 400 600 Gol Transportes A ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Jizera Mountains
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 area ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Giant Mountains
The Giant Mountains, Krkonoše or Karkonosze (Czech: , Polish: , german: Riesengebirge) are a mountain range located in the north of the Czech Republic and the south-west of Poland, part of the Sudetes mountain system (part of the Bohemian Massif). The Czech-Polish border, which divides the historic regions of Bohemia and Silesia, runs along the main ridge. The highest peak, Sněžka ( pl, Śnieżka, german: Schneekoppe), is the Czech Republic's highest point with an elevation of . On both sides of the border, large areas of the mountains are designated national parks (the Krkonoše National Park in the Czech Republic and the Karkonosze National Park in Poland), and these together constitute a cross-border biosphere reserve under the UNESCO Man and the Biosphere Programme. The source of the River Elbe is within the Giant Mountains. The range has a number of major ski resorts, and is a popular destination for tourists engaging in downhill and cross-country skiing, hiking, cycling a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Landeshut Ridge
The Rudawy Janowickie or Landeshut Ridge (german: Landeshuter Kamm, cs, Janovické rudohoří) is a mountain range in Sudetes in Poland. See also *Colourful lakelets Colourful lakelets (Polish "Kolorowe Jeziorka") is the name of three (sometimes four) artificial ponds formed in place of former mines at the slope of Wielka Kopa mountain (871 m) in Rudawy Janowickie, range in Sudetes Mountains, Poland. The bigg ... Sudetes Geography of Lower Silesian Voivodeship {{LowerSilesian-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Waldenburg Mountains
The Wałbrzyskie Mountains or Waldenburg Mountains ( pl, Góry Wałbrzyskie; german: Waldenburger Bergland), sometimes called the Wałbrzyskie Highlands or Waldenburg Highlands, is one of the three mountain ranges that form the western part of the Central Sudetes. The other ranges are the Owl Mountains and the Falcon Mountains. Geography The Wałbrzyskie Mountains lie almost entirely within Poland. Several southern ridges reach as far as the Czech Republic. The range extends to the west and southwest of the Lower Silesian town of Wałbrzych ''(Waldenburg)''. The Owl and Falcon Mountains to the southeast form a continuation of the Wałbrzyskie Highlands. To the west of the highlands in the Western Sudetes are the adjoining ranges of the Bober-Katzbach Mountains and the Landeshut Ridge. Division of the Wałbrzych Mountains The Wałbrzych Mountains are divided into three separate parts: * Trójgarb and Krąglak Massif * Chełmiec Massif * Black Mountains File:Sattelwald-Troj ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Nysa Szalona
The Raging NeisseDodge, Lt Col Theodore Ayrault. ''Napoleon: A History of the Art of War. Vol. IV'', 2014 ( pl, Nysa Szalona, or ''Jauersche Neiße'') is a river in Poland. It has a length of about and flows into the Kaczawa (Katzbach), which in turn flows into the Oder. Its largest tributary is the Little Neisse. The Raging Neisse rises at a height of on the western side of a mountain called the Kokosz on the Waldenburg Heights. It flows down through the lowlands among the foothills of the Sudetes and the heights of Hainau, through the towns of Bolków (''Bolkenhain'') and Jawor (''Jauer''). It then merges with the Kaczawa (''Katzbach'') at a height of not far from Jawor near the village of Slup (''Schlaup'') on the battlefield of the Battle of Katzbach. During heavy rain and due to its mountainous character, the water level of this small river can rise by up to 2.5 metres or about 8 feet, whence its name, the "Raging" Neisse. Napoleonic Wars The river became famo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Raging Neisse
The Raging NeisseDodge, Lt Col Theodore Ayrault. ''Napoleon: A History of the Art of War. Vol. IV'', 2014 ( pl, Nysa Szalona, or ''Jauersche Neiße'') is a river in Poland. It has a length of about and flows into the Kaczawa (Katzbach), which in turn flows into the Oder. Its largest tributary is the Little Neisse. The Raging Neisse rises at a height of on the western side of a mountain called the Kokosz on the Waldenburg Heights. It flows down through the lowlands among the foothills of the Sudetes and the heights of Hainau, through the towns of Bolków (''Bolkenhain'') and Jawor (''Jauer''). It then merges with the Kaczawa (''Katzbach'') at a height of not far from Jawor near the village of Slup (''Schlaup'') on the battlefield of the Battle of Katzbach. During heavy rain and due to its mountainous character, the water level of this small river can rise by up to 2.5 metres or about 8 feet, whence its name, the "Raging" Neisse. Napoleonic Wars The river became famous ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Jizera Foreland , a plateau
{{geodis ...
Jizera may refer to places in the Czech Republic: *Jizera (river), a river *Jizera Mountains, a mountain range *Jizera Table The Jizera Table ( cs, Jizerská tabule) is a plateau and a geomorphological mesoregion of the Czech Republic. It is located mostly in the Central Bohemian Region, northeast of Prague. Geomorphology The Jizera Table is a mesoregion of the Centra ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |