The Děčínský Sněžník ( German : Hoher Schneeberg ) is a mountain in the Czech Republic . At 723.5 m (2,374 ft) above sea level, it is the highest peak of the Elbe Sandstone Mountains .
99-670: Děčínský Sněžník is located in the Elbe Sandstone Mountains in the Ústí nad Labem Region . It is located mostly in the Jílové municipality, only the eastern slopes are located in the territory of Děčín . The mountain is the highest mesa in the Czech Republic. One of the first historical figures to visit Děčínský Sněžník was Emperor Joseph II of Habsburg , who climbed the peak in September 1779. The Sněžník
198-707: A Hercynian block tilted so as to present a steep scarp face towards Bohemia and a gentle slope on the German side. They were formed during a lengthy process. During the folding of the Variscan orogeny , metamorphism occurred deep underground, forming slate and gneiss . In addition, granite plutons intruded into the metamorphic rocks. By the end of the Palaeozoic era, the mountains had been eroded into gently undulating hills (the Permian massif ), exposing
297-453: A loamy , rapidly weathered gneiss in the east of the mountains producing a light soil. As a result of the subsoils based on granite and rhyolite, the land is mostly covered in forest ; on the gneiss soils it was possible to grow and cultivate flax in earlier centuries and, later, rye , oats and potatoes up to the highlands. Today the land is predominantly used for pasture . But it is not uncommon to see near-natural mountain meadows. To
396-530: A mountain range straddling the border between the state of Saxony in southeastern Germany and the North Bohemian region of the Czech Republic , with about three-quarters of the area lying on the German side. In both countries, core parts of the mountain range have been declared a national park. The name derives from the sandstone which was carved by erosion. The river Elbe breaks through
495-686: A cover up for the Eastern Bloc's highly secretive uranium mining. For the third time in history, thousands of people poured into the Ore Mountains to build a new life. The principal mining areas were located around Johanngeorgenstadt , Schlema and Aue . Uranium ore deposits were also exploited for the Soviet Union in Bohemian Jáchymov (St. Joachimsthal). Its processing was associated with serious health consequences for
594-548: A height of 807 m above sea level (NN) on the mountain of Komáří vížka which lies on the Czech side, east of Zinnwald-Georgenfeld , right on the edge of the fault block. Consequently, it is a fault-block mountain range, which has been incised by a whole range of river valleys whose rivers drain southwards into the Ohře and northwards into the Mulde or directly into
693-504: A height of 922 m above sea level (NN) , on average only about 140 frost-free days per year are observed. Based on reports of earlier chroniclers, the climate of the upper Ore Mountains in past centuries must have been even harsher than it is today. Historic sources describe hard winters in which cattle froze to death in their stables, and occasionally houses and cellars were snowed in even after snowfalls in April. The population
792-528: A large number of Bohemian Protestants then fled into the neighbouring Electorate of Saxony . As a result, many Bohemian villages became devastated and desolate, while on the Saxon side new places were founded by these migrants, such as the mining town of Johanngeorgenstadt . Ore mining largely came to a standstill in the 17th century, especially after the Thirty Years' War . Due to the very sharp decline of
891-488: A leading centre of wood and toy manufacturing. Here, wooden smoking figures , nutcrackers , hand-carved wooden trees ( Spanbäume ), candle arches , ( Schwibbogen ), Christmas pyramids and music boxes are made. Up to the last third of the 20th century, Coal was mined near Zwickau until 1978, around Lugau and Oelsnitz until 1971 and in the Döhlen Basin near Freital until 1989. The mountains that until
990-438: A length of 120 km. The eastern Ore Mountains are protected landscape. Other smaller areas on the German and Czech sides are protected as nature reserves and natural monuments. On the ridges there are also several larger raised bogs that are only fed by rainwater. The mountains are popular for hiking and there are winter sports areas at higher elevations. In 2019, the region became a UNESCO World Heritage Site . In English,
1089-454: A literal translation of the German name, and Vyšehory , meaning "high mountains". In Upper Sorbian the mountains are known as the Rudne horiny . The German and Upper Sorbian names, as well as the historical Czech Rudohoří , literally mean "ore mountains". The Ore Mountains are geologically considered to be one of the most heavily researched mountain ranges in the world. The Ore Mountains are
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#17327768159931188-704: A long time, so that for about 100 years the blue colour works had a worldwide monopoly. From about 1820 in Johanngeorgenstadt, uranium was also extracted and was then used to colour glass, amongst other things. Even richer deposits of uranium ore were found in St. Joachimsthal. St. Andrew's White Earth Mine ( Weißerdenzeche St. Andreas ) at Aue supplied kaolin to the Meissen Porcelain Factory in Meissen for nearly 150 years. Its export from
1287-483: A result of long-term tectonic stresses on the entire sandstone platform of the mountain range. This network of clefts runs through the sandstone beds in a relatively regular way, but in different directions in two regions of the range. Subsequent weathering processes of very different forms and simultaneous complex deposition (leaching, frost and salt wedging , wind , solution weathering with sintering as well as biogenic and microbial effects) have further changed
1386-546: A result of settlement in the early 12th century at the northern edge of the Ore Mountains, the first silver ore was discovered in the vicinity of present-day Freiberg , resulting in the First Berggeschrey or mining rush. Almost simultaneously, the first tin ore was discovered on the southern edge of the mountains in Bohemia. In the 13th century, colonization of the mountains took place only sporadically along
1485-423: A result of the climatic influences of the ice ages. The mineral composition of the sandstone beds has a direct effect on the morphology of the terrain. The fine-grained form with clayey-silty cement between the quartz grains causes banks and slopes with terracing. The beds of sandstone with siliceous cement are typically the basis of the formation of rock faces and crags. Small variations in the cement composition of
1584-669: A rock face or when dressing the rough blocks of stone. The sandstone of this region is a sought-after building material used for example, for imposing city edifices such as the Church of Our Lady in Dresden . Large parts of the Elbe Sandstone Mountains are under statutory protection. In Germany there is the national park region of Saxon Switzerland, which consists two elements: Saxon Switzerland National Park itself, founded in 1990 and covered an area of 93 km²; and
1683-465: A second trending north–south from Freiberg through Marienberg, Annaberg, Niederschlag, Joachimsthal, and Schlaggenwald. Late Tertiary faulting and volcanism gave rise to basalt and phonolite dikes . Ore veins include iron, copper, tin, tungsten, lead, silver, cobalt, bismuth, uranium, plus iron and manganese oxides. The most important rocks occurring in the Ore Mountains are schist , phyllite and granite with contact metamorphic zones in
1782-476: A source of building material, the tower was finished in autumn 1864. Originally used by geodesists, the view attracted many visitors and in 1865 the local forest administration decided to build a small hostelry for them. The observation tower at Děčínský Sněžník has remained a popular tourist attraction and lasted, with small modifications, for more than 80 years. After the Second World War the hostelry
1881-660: Is Krušné hory , derived from an old Czech expression krušec , meaning "ore". The mountains are sometimes divided into the Saxon Ore Mountains and Bohemian Ore Mountains. A similarly named range in Slovakia is usually known as the Slovak Ore Mountains . Europe's earliest mining district appears to be located in Erzgebirge, dated to 2500 BC. From there tin was traded north to
1980-592: Is a stop on the E3 European long distance path . Ascents may be made from the town of Jílové or from the German municipality of Rosenthal-Bielatal to the north. Elbe Sandstone Mountains The Elbe Sandstone Mountains , also called the Elbe Sandstone Highlands ( German : Elbsandsteingebirge , pronounced [ɛlpˈz̥antʃtaɪnɡəˌbɪʁɡə] ; Czech : Děčinská vrchovina , pronounced [ˈɟɛtʃɪnskaː ˈvr̩xovɪna] ), are
2079-617: Is formed by sandstones, planers and other rocks as well as basal conglomerates of older origin. Several erosion relics from Reinhardtsgrimma through Dippoldiswalde and the Tharandt Forest to Siebenlehn form isolated examples south of Dresden. They are mainly characterised by sandstones. On the Bohemian side the sandstone beds continue and form part of the North Bohemian Cretaceous. The chalk sediments of
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#17327768159932178-402: Is seen historically as part of the Ore Mountains, Chemnitz is seen historically as just lying outside them, but Freiberg is included. The supposed limit of the Ore Mountains continues southwest of Dresden towards the Elbe Sandstone Mountains . From this perspective, its main characteristics, i.e., gently sloping plateaus climbing up to the ridgeline incised by V-shaped valleys , continue to
2277-988: Is the Děčínský Sněžník in Bohemian Switzerland on the left bank of the river in Bohemian Switzerland north of Děčín. The mountain range links the Ore Mountains in the west with the Lusatian Highlands range of the Sudetes in the east. Saxon Switzerland and the Zittau Mountains of the Lusatian Mountains form the Saxon-Bohemian Chalk Sandstone Region . The most striking characteristic of this deeply dissected rocky mountain range
2376-548: Is the extraordinary variety of terrain within the smallest area. Unique amongst the Central European Uplands are the constant changes between plains , ravines , table mountains and rocky regions with undeveloped areas of forest. This diversity is ecologically significant. The variety of different locations, each with its own conditions in terms of soil and microclimate , has produced an enormous richness of species . The numbers of ferns and mosses alone
2475-560: Is unmatched by any other of the German central uplands . The occurrence of Elbe sandstones and hence the Elbe Sandstone Mountains themselves is related to widespread deposition by a former sea in the Upper Cretaceous epoch. On the Saxon side of the border the term "Elbe Valley Cretaceous" is used, referring to a region stretching from Meißen - Oberau in the northwest through Dresden and Pirna into Saxon Switzerland, and which
2574-793: The Baltic Sea and south to the Mediterranean following the Amber Road trading route, of great importance in the Bronze Age . Tin mining knowledge spread to other European tin mining districts from Erzgebirge and evidence of tin mining begins to appear in Brittany , Devon and Cornwall , and in the Iberian Peninsula around 2000 BC. These deposits saw greater exploitation when they fell under Roman control between
2673-691: The Elbe . The main geologic feature in the Ore Mountains is the Late Paleozoic Eibenstock granite pluton , which is exposed for 25 miles along its northwest–southeast axis and up to 15 miles in width. This pluton is surrounded by progressive zones of contact metamorphism in which Paleozoic slates and phyllites have been changed to spotted hornfels , andalusite hornfels, and quartzites . Two key mineral centres intersect this pluton at Joachimsthal, one trending northwesterly from Schneeberg through Johanngeorgenstadt to Joachimsthal, and
2772-591: The Königstein Fortress , Pravčická brána , the Schrammsteine , Pfaffenstein , and the valleys of the Kirnitzsch and Kamenice rivers. There are some 14,000 climbing routes via which mountain climbers can conquer 1100 free-standing peaks. Visitors can experience the natural scenes on the asphalt Elbe cycle path, or on board a steam paddleboat that is part of the oldest fleet of its kind in
2871-419: The Lusatian Mountains was shaped and affected by intense volcanism ; but individual intrusions of magma also forced their way through the sandstone platform of the Elbe Sandstone Mountains. The most striking evidence of this phase in the earth's history are the conical basaltic hills of Růžovský vrch , Cottaer Spitzberg and Raumberg , but also Großer and Kleiner Winterberg . At its southwestern edge
2970-706: The Lusatian Mountains , the Iser Mountains , the Giant Mountains and the Inner-Bohemian Mountains . At the same time it forms a y-shaped mountain chain, along with the Upper Palatine Forest, Bohemian Forest, Fichtel Mountains , Franconian Forest , Thuringian Slate Mountains and Thuringian Forest , that has no unique name but is characterised by a rather homogeneous climate. According to cultural tradition, Zwickau
3069-717: The Western , Central and Eastern Ore Mountains , separated by the valleys of the Schwarzwasser and Zwickauer Mulde and the Flöha (" Flöha Line "), the division of the western section along the River Schwarzwasser is of a more recent date. The Eastern Ore Mountains mainly comprise large, gently climbing plateaux, in contrast with the steeper and higher-lying western and central areas, and are dissected by river valleys that frequently change direction. The crest of
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3168-800: The Zittau Basin are counted as part of the latter due to their regional-geological relationships. The sedimentary sequences of the Cretaceous sea continue across a wide area of the Czech Republic to Moravia. Together these beds form the Saxon-Bohemian Cretaceous Zone. In Czech geological circles, the Elbe Valley Cretaceous is described as the foothills of the Bohemian Cretaceous Basin. The eroded sandstone landscape of this region
3267-420: The discovery of large ore deposits the area was further renamed in the 16th century. Petrus Albinus used the name Erzgebirge ("Ore Mountains") for the first time in 1589, in his chronicle. In the early 17th century, the name Meißener Berge ("Meissen Mountains") was temporarily used. A quarter of a century later the names Erzgebirge in German and Rudohoří in Czech became established. The Czech toponym
3366-414: The engineering and textile industries . In 1789 the chemical element uranium was discovered in St. Joachimsthal; then in pitchblende from the same area, radium was discovered by Marie Curie in 1898. In the late 1930s, following the discovery of the nuclear fission , uranium ore became of particular interest for military purposes. After the incorporation of Sudetenland into Germany in 1938 all
3465-703: The loess hill country to the north between Zwickau and Chemnitz is referred to as the Ore Mountain Basin ; that from the Eastern Ore Mountains as the Ore Mountain Foreland . Between Freital and Pirna , the area is called the Dresden Ore Mountain Foreland ( Dresdner Erzgebirgsvorland ) or Bannewitz-Possendorf-Burkhardswald Plateau ( Bannewitz-Possendorf-Burkhardswalder Plateau ). Geologically
3564-861: The protected area surrounding it that was founded in 1956 and covers 287 km². The German part of the range was also designated in May 2006 as one of the 77 most important national geotopes in Germany by the Academy of Geosciences in Hanover. In the Bohemian part of the range there has been a protected landscape area in the northeastern region since 1972 called the Elbe Sandstone Protected Landscape Area with an area of 324 km . In 2000, Bohemian Switzerland National Park
3663-426: The 12th century onwards, and even the forests owned by the nobility could not cover the growing demand for wood. In the 18th century, industries were encouraged to use coal as fuel instead of timber in order to preserve the forests, and this was enforced in the 19th century. In the early 1960s the first signs of forest dieback were seen in the Eastern Ore Mountains near Altenberg and Reitzenhain , after local damage to
3762-664: The 21st century, the working group Naturhaushalt und Gebietscharakter of the Saxon Academy of Sciences ( Sächsische Akademie der Wissenschaften ) in Leipzig merged the Ore Mountains with the major unit group of Vogtland to the west and the major landscape units of Saxon Switzerland , Lusatian Highlands and Zittau Mountains to the east into one overarching unit, the Saxon Highlands and Uplands . In addition, its internal divisions were changed. Former major unit 420
3861-469: The 9th century, were only used in a general sense for the vast forests of the Central Uplands. Frequently the term Miriquidi is used to refer directly to the Ore Mountains, but it only surfaces twice in the 10th and early 11th centuries, and these sources do not permit a clear identification with the ancient forest that formerly covered the whole of the Ore Mountains and its foreland. Following
3960-472: The Bohemian Way ( antiqua Bohemiae semita ). It was here that Sayda was built, a station on the trade route from Freiberg via Einsiedl , Johnsdorf and Brüx to Prague. In Sayda it joined the so-called salt road that ran from Halle via Oederan and onto Prague. Glass-making was introduced into the region from the second half of the 13th century. The emergence of this branch of trade benefited from
4059-411: The Bohemian mining town of Graupen (Czech Krupka ) its name. With the further settlement of the Ore Mountains in the 15th century, new, rich, ore deposits were eventually discovered around Schneeberg Annaberg and St. Joachimsthal . The Second Berggeschrey started and triggered a massive wave of colonization. In quick succession, new, planned, mining towns were built across the Ore Mountains in
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4158-556: The Czech Republic and Saxony in Germany. The highest peaks are the Klínovec in the Czech Republic (German: Keilberg ) at 1,244 metres (4,081 ft) above sea level and the Fichtelberg in Germany at 1,215 metres (3,986 ft). The Ore Mountains have been intensively reshaped by human intervention and a diverse cultural landscape has developed. Mining in particular, with its tips, dams, ditches and sinkholes, directly shaped
4257-468: The Czech side, is actually the highest town in Central Europe . Only on the relatively inaccessible, less climatically favourable ridges are there still large, contiguous forests, but since the 18th century these have been managed economically. Due to the high demand for timber by the mining and smelting industries, where it was needed for pit props and fuel, large-scale deforestation took place from
4356-716: The Eastern Ore Mountains by narrow fingers of the aforementioned basin. South(east) of the Western Ore Mountains lie the Sokolov Basin , the Eger Graben and the Doupov Mountains . To the north the boundary is less sharply defined because the Ore Mountains, a typical example of a fault-block , descend very gradually. The topographical transition from the Western and Central Ore Mountains to
4455-589: The Eastern Ore Mountains. Here, the artisans were required by Prince-Elector Augustus under the Timber Act of 1560, to buy their wood in Bohemia. Wood from the Saxon Ore Mountains was still needed for the mines and smelters in Freiberg. This export of timber led, among other things, to the construction of an artificial cross-border rafting channel, the Neugrabenflöße , along the river Flöha . Because of
4554-458: The Elbe Sandstone Mountains are the furrows with parallel ridges between them ( grykes and clints ) that look like cart ruts and which are particularly common, as well as extensive cave systems. They are occasionally described by the term pseudokarst . The application of the concept to several erosion formations in the sandstone of this mountain range is however contentious. Czech geologists have identified in quartzite-cemented sandstone areas in
4653-429: The Elbe Valley zone. The western part of the Ore Mountains is home to the two highest peaks of the range: Klínovec , located in the Czech part, with an altitude of 1,244 metres (4,081 ft) and Fichtelberg , the highest mountain of Saxony, Germany, at 1,214 metres (3,983 ft). The Ore Mountains are part of a larger mountain system and adjoin the Fichtel Mountains to the west and the Elbe Sandstone Mountains to
4752-413: The Elbe made the deepest incision. Later the Lusatian granodiorite was uplifted over the 600 metre thick sandstone slab along the Lusatian Fault and pushed it downwards until it fractured. This northern boundary of the sandstone deposit lies roughly along the line Pillnitz – Hohnstein – Hinterhermsdorf – Krásná Lípa . In the Tertiary period, the adjacent region of the Central Bohemian Uplands and
4851-491: The Ore / ɔːr / Mountains are sometimes referred to as the Ore Mountain Range , but are also sometimes called the Erzgebirge [ˈeːɐ̯tsɡəˌbɪʁɡə] or Erz Mountains / ɛər t s , ɜːr t s / after their German name or the Krušné Mountains / ˈ k r ʊ ʃ n i , - n eɪ / after their Czech name. In Czech they are the Krušné hory [ˈkruʃnɛː ˈhorɪ] , from old Czech krušec , meaning "piece of ore", and were historically known as Rudohoří ,
4950-412: The Ore Mountains reach the city limits of Dresden at the Windberg hill near Freital and the Karsdorf Fault . The V-shaped valleys of the Ore Mountains break through this fault and the shoulder of the Dresden Basin . The Ore Mountains belong to the Bohemian Massif within Europe's Central Uplands, a massif that also includes the Upper Palatine Forest , the Bohemian Forest , the Bavarian Forest ,
5049-428: The Ore Mountains remains unchanged under the title of Southern Ore Mountains ( Süderzgebirge ). The climate of the higher regions of the Ore Mountains is characterised as distinctly harsh. Temperatures are considerably lower all year round than in the lowlands, and the summer is noticeably shorter and cool days are frequent. The average annual temperatures only reach values of 3 to 5 °C. In Oberwiesenthal , at
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#17327768159935148-410: The Ore Mountains was given new life during the First and Second World Wars in order to supply raw materials. Nazi Germany also saw the resumption of silver mining. Afterwards the people returned to the manufacture of wooden products and toys , especially in the Eastern Ore Mountains. The clock industry is centred on Glashütte . In the Western Ore Mountains, economic alternatives were offered by
5247-444: The abundance of excess timber, which was created by clearings and new settlements and which was able to meet the high demand of the glassworks. Monks from Waldsassen Abbey brought a knowledge of the glass manufacture to the Ore Mountains. Most glassworks were located in the vicinity of Moldau , Brandau and the Frauenbach valley . The oldest glassworks site is Ulmbach . This timber-hungry industry lost its importance, however, with
5346-405: The boom in mining, which also enjoyed royal patronage. Mining on the Bohemian side of the mountains probably began in the 14th century. An indication of this is a contract between Boresch of Riesenburg and the Ossegg abbot, Gerwig, in which the division of revenue derived from ore was agreed. Grains of tin ( Zinnkörner or Graupen ) were obtained at that time in the Seiffen mining area and gave
5445-409: The border. From west to east: In the division of Germany into natural regions that was carried out Germany-wide in the 1950s the Ore Mountains formed major unit group 42: Even after the reclassification of natural regions by the Federal Agency for Nature Conservation in 1994 the Ore Mountains, region D16 , remained a major unit group with almost unchanged boundaries. However, at the beginning of
5544-481: The crest of the mountains, such as the Freiberg Mines Water Management System or the Reitzenhainer Zeuggraben . Only a few mines remained profitable over a long period. Amongst them was the Himmelsfürst Fundgrube near Erbisdorf , whose 50 continuous years of profitable operation were commemorated in 1818 with the issue of a commemorative coin ( Ausbeutetaler ) and which went on to make a profit continuously until 1848. Thanks to discoveries of rich ore seams it became
5643-409: The decline in industrial production in that period, people without any ties migrated to the interior of Germany or Bohemia. After the discovery of the cobalt blue pigments the mining industry experienced a revival. Cobalt was extracted especially in Schneeberg, and processed in the state paintworks to produce cobalt blue paints and dyes. They succeeded in keeping the method of production secret for
5742-431: The description Quader Sandstone.". Quader is German for an ashlar or block of stone, hence the name "Square Sandstone" is also used in English. The term Quader Sandstone Mountains or Square Sandstone Mountains , introduced by Hanns Bruno Geinitz in 1849, is an historical, geological term for similar sandstone deposits, but was also used in connection with the Elbe Sandstone Mountains. The fissures were formed as
5841-422: The early 1990s. In St. Egidien and Aue there were important nickel smelting sites. In Pöhla in the Western Ore Mountains, during exploratory work for SDAG Wismut new, rich lodes of tin ore were discovered in the 1980s. The test workings of that time are now considered the largest tin finds in Europe. Another well-known place of tin production was Seiffen . The village in the Eastern Ore Mountains has become
5940-408: The east. Past the River Elbe , the mountain chain continues as the Lusatian Mountains . While the mountains slope gently away in the northern (German) part, the southern (Czech) slopes are rather steep. The Ore Mountains are oriented in a southwest–northeast direction and are about 150 km long and, on average, about 40 km wide. From a geomorphological perspective the range is divided into
6039-433: The forests had become apparent since the 19th century as a result of smelter smoke ( Hüttenrauch ). The German population of the Bohemian part of the Ore Mountains was expelled in 1945 in accordance with to the Beneš decrees . The upper western part of the Ore Mountains, known in German as Erzgebirge , belongs to the Ore Mountains/Vogtland Nature Park . The eastern part, called the Eastern Ore Mountains ( Osterzgebirge ),
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#17327768159936138-431: The formation of sandstone beds. Its stratification is characterized by variations in the horizontal structure (deposits of clay minerals, grain sizes of quartz, differences in the grain-cement) as well as a typical but fairly small fossil presence and variably porous strata. After the Cretaceous sea had retreated ( marine regression ), the surface of the land was shaped by weathering influences and watercourses, of which
6237-423: The greatest cretaceous sandstone erosion complex in Europe. Human-induced changes caused by nearly 1,000 years of continual sandstone quarrying have also contributed in parts of the sandstone highlands to the appearance of the landscape today. The fissures (called Loose by the quarrymen) played an important role here, because they provided in effect natural divisions in the rock that were helpful when demolishing
6336-420: The hard rocks. In the Tertiary period these mountain remnants came under heavy pressure as a result of plate tectonic processes during which the Alps were formed and the North American and Eurasian plates were separated. As the rock of the Ore Mountains was too brittle to be folded, it shattered into an independent fault block which was uplifted and tilted to the northwest. This can be very clearly seen at
6435-517: The heartland of the Central European mining industry. New ore discoveries attracted more and more people, and the number of residents on the Saxon side of the mountains continued to rise rapidly. Bohemia, in addition to migration from within the country, also received migration from elsewhere, mainly of German miners, who settled in the mountain villages and in the towns at the edge of the mountains. Under Emperor Ferdinand II an unprecedented Re-Catholicization began in Bohemia from 1624 to 1626, whereupon
6534-409: The heavy amounts of snow a natural Dwarf Mountain Pine region is found near Satzung , near the border to Bohemia at just under 900 m above sea level (NN) . By comparison, in the Alps these pines do not occur until 1,600 to 1,800 m above sea level (NN) . The term Saltusbohemicus ("Bohemian Forest") for the region emerged in the 12th century. In the German language
6633-484: The landscape and the habitats of plants and animals in many places. The region was also the setting of the earliest stages of the early modern transformation of mining and metallurgy from a craft to a large-scale industry, a process that preceded and enabled the later Industrial Revolution . The higher altitudes from around 500 m above sea level on the German side belong to the Ore Mountains/Vogtland Nature Park – the largest of its kind in Germany with
6732-400: The late 11th (and early 12th century) were covered in dense forests were almost completely transformed into a cultural landscape by the mining industry and by settlement . The population density is high right up into the upper regions of the mountains. For example, Oberwiesenthal , the highest town in Germany, lies in the Ore Mountains, and neighbouring Boží Dar (German: Gottesgab ) on
6831-479: The miners. In addition a dam burst in 1954 at Lengenfeld at a uranium mining waste lake; 50,000 cubic metres of waste water poured down 4 kilometres into the valley. Until 1991 uranium ore was also mined in Aue- Alberoda and Pöhla . Mining operations in Freiberg that had begun in 1168 finally ceased in 1968 after 800 years. In Altenberg and Ehrenfriedersdorf tin mining continued to 1991. The smelting of these ores took place mainly in Muldenhütten until
6930-428: The mining industry and because the search for new ore deposits proved fruitless, the population had to resort to other occupations. Agricultural yields were low, however, and also the demand for wood was reduced by the closure of smelteries. Many people were already active at that time in textile production. However, since that was not enough for subsistence, the manufacture of wooden goods and toys developed, especially in
7029-402: The mining industry. Settlement in the Ore Mountains was slow to begin with, especially on the Bohemian side. The harsh climate and short growing seasons hindered the cultivation of agricultural products. Nevertheless, settlements were supported by the aristocratic Hrabischitz family and established mainly at the foot of the mountains and along mountain streams into the deep woods. In 1168, as
7128-556: The most productive Freiberg mine of the 19th century. But even the excavation of the Rothschönberger Stolln , the largest and most important Saxon drainage adit, which drained the entire Freiberg district, could not stop the decline of mining. Because even before the completion of this technical achievement the German Empire introduced the gold standard in 1871, the price of silver dropped rapidly and led to
7227-478: The mountain range in a steep and narrow valley. The Saxon Switzerland and Bohemian Switzerland national parks, known also as Saxon-Bohemian Switzerland, are located within the territory of Elbe Sandstone Mountains. The Elbe Sandstone Mountains extend on both sides of the Elbe from the Saxon town of Pirna in the northwest toward Bohemian Děčín in the southeast. Their highest peak with 723 m (2,372 ft)
7326-743: The mountains themselves forms, in all three regions, a succession of plateaux and individual peaks. To the east it is adjoined by the Elbe Sandstone Mountains and, to the west, by the Elster Mountains and other Saxon parts of the Vogtland . South(east) of the Central and Eastern Ore Mountains lies the North Bohemian Basin and, immediately east of that, the Bohemian Central Uplands which are separated from
7425-456: The names Böhmischer Wald , Beheimer Wald , Behmerwald or Böhmerwald were used, in Czech the name Český les . The last-mentioned names are used today for the mountain range along the Czech Republic's southwestern border ( see: Bohemian Forest ). From earlier research, other names for the Ore Mountains have also appeared in a few older written records. However, the names Hircanus Saltus ( Hercynian Forest) or Fergunna , which appeared in
7524-449: The nature of the rock surface. For example, collapse caves , small hole-like cavities ( honeycomb weathering ) with hourglass-shaped pillars, chimneys , crevices and mighty, rugged rock faces. Many morphological formations in the rocky landscape of the Elbe Sandstone Mountains are suspected to have been formed as a consequence of karstification . Important indicators of such processes in the polygenetic and polymorphic erosion landscape of
7623-405: The north of the Ore Mountains, west of Chemnitz and around Zwickau lies the Ore Mountain Basin which is only really known geologically. Here there are deposits of stone coal where mining has already been abandoned. A similar but smaller basin with abandoned coal deposits, the Döhlen Basin , is located southwest of Dresden on the northern edge of the Ore Mountains. It forms the transition to
7722-433: The northern part of the Bohemian Cretaceous Basin, karst features in the shape of spherical caverns and cave formations. According to them, these emerged as a result of solution processes by water in complex interactions with iron compounds from neighbouring or intrusive magmatic-volcanic rocks. The variation in relief in these sandstone regions is explained on the basis of these processes. The Elbe Sandstone Mountains are
7821-588: The range. The highest elevation on the Saxon side is the 1,215-metre-high Fichtelberg , which was the highest mountain in East Germany . The Ore Mountains contain about thirty summits with a height over 1,000 m above sea level (NN) , but not all are clearly defined mountains. Most of them occur around the Klínovec and the Fichtelberg. About a third of them are located on the Saxon side of
7920-457: The rock can have a visible impact on the landscape. Elbe Sandstone gets its characteristic cuboid appearance from its thick horizontal strata ( massive bedding ) and its vertical fissures . In 1839 Bernhard Cotta wrote about this in his comments on the geognostic map : "Vertical fissures and cracks cut through, often virtually at right angles, the horizontal layers and, as a result, parallelepiped bodies are formed, that have given rise to
8019-491: The sandstone landscape is a result of the subsequent chemical and physical erosion and biological processes acting on the rocks formed from those sands laid down during the Cretaceous Period. The inlets of a Cretaceous sea, together with marine currents, carried away sand over a very long period of time into a shallow zone of the sea and then the diagenetic processes at differing pressure regimes resulted in
8118-529: The sandstone plate was uplifted by over 200 metres at the Karsdorf Fault , whereby the slab was tilted even more and increased the gradient of the Elbe River. The water masses cut valleys into the rock with their streambeds and contributed in places to the formation of the rock faces. Over time the gradients reduced, the streambed of the Elbe widened out and changed its course time and again, partly as
8217-591: The southern edge of the Dresden Basin . North of the Ore Mountains the landscape gradually transitions into the Saxon Lowland and Saxon Elbeland . Its cultural-geographical transition to Saxon Switzerland in the area of the Müglitz and Gottleuba valleys is not sharply defined. The highest mountain in the Ore Mountains is the Klínovec (German: Keilberg ), at 1,244 metres, in the Bohemian part of
8316-502: The state, however, was prohibited by the Prince-electors under threat of severe punishment or even death. Towards the end of the 19th century, mining slowly declined again. Drainage costs increased, from the mid-19th century, led to a steady decrease in yield, despite sinking of deeper galleries ( Erbstollen ) and the expansion of ditch and tunnel ( Rösche ) systems for supplying the necessary water for overshot wheels from
8415-592: The third century BC and the first century AD. Demand for tin created a large and thriving network amongst Mediterranean cultures of Classical times . By the Medieval period, Iberia's and Germany's deposits lost importance and were largely forgotten while Devon and Cornwall began dominating the European tin market. From the time of the first wave of settlement, the history of the Ore Mountains has been heavily influenced by its economic development, especially that of
8514-413: The tower, and this was followed by the erection of a new inn. Since summer 1992 the tower at Děčínský Sněžník has again been open to the public and the peak is once again a popular tourist destination. The observation tower is 33 m (108 ft) high, 153 steps lead to the observation deck. The tower offers a panoramic view over Bohemian and Saxon Switzerland , and Lusatian Mountains . The summit
8613-418: The unprofitability of the entire Ore Mountain silver mining industry. This situation was not altered even by short-term discoveries of rich deposits in various mines nor the state's purchase of all the Freiberg mines and their incorporation into the state-owned enterprise, Oberdirektion der Königlichen Erzbergwerke , founded in 1886. In 1913, the last silver mines closed and the company was disbanded. Mining in
8712-484: The upper reaches of the mountains. Since a large part of the precipitation falls as snow , in many years a thick and permanent layer of snow remains until April. The ridges of the Ore Mountains are one of the snowiest areas in the German Central Uplands . Foehn winds, and also the so-called Bohemian Wind may occur during certain specific southerly weather conditions. As a result of the climate and
8811-467: The uranium production facilities were commandeered for the development of nuclear weapons. After the American atomic bomb was dropped on Japan in 1945, Soviet experts searched for evidence of the German nuclear energy project to support Soviet atomic bomb development . Shortly thereafter, the processing of uranium ore for the Soviet Union began in the Ore Mountains under the code name SAG Wismut ,
8910-399: The vicinity of newly discovered ore deposits. Typical examples are the towns of Marienberg , Oberwiesenthal , Gottesgab ( Boží Dar ), Sebastiansberg ( Hora Sv. Šebestiána ) and Platten ( Horní Blatná ). Economically, however, only silver and tin ores were used. From that time, the wealth of Saxony was built on the silver mines of the Ore Mountains. As a metal used for coinage, silver
9009-480: The west, basalt as remnants in the Plešivec (Pleßberg), Scheibenberg , Bärenstein , Pöhlberg , Velký Špičák ( Großer Spitzberg or Schmiedeberger Spitzberg ), Jelení hora ( Haßberg ) and Geisingberg as well as gneisses and rhyolite ( Kahleberg ) in the east. The soils consist of rapidly leaching grus . In the western and central areas of the mountains it is formed from weathered granite. Phyllite results in
9108-550: The world. The Elbe Sandstone Mountains have numerous facilities for cure and rehabilitation. The discovery of ferrous and sulphurous sources in Bad Schandau in 1730 led to its development as a health resort and the building of swimming baths . Ore Mountains The Ore Mountains ( German : Erzgebirge , Czech : Krušné hory ) lie along the Czech–German border, separating the historical regions of Bohemia in
9207-482: Was abandoned as it had to be pulled down. Likewise the tower deteriorated and, by the 1980s, was in poor condition. Vandals contributed to the degradation of the tower, and its masonry started to collapse. The tower was assigned to the monument fund of the State Monument Preservation, but this formal step did not bring any improvement. In 1992 two million CZK were collected for the renovation of
9306-607: Was considered an important geodetic point for triangulation and cartographers asked the owner of the principality of Děčín, Prince Franz of Thun and Hohenstein , for permission to establish the peak as a triangulation point. Prince Franz contracted the Dresden architect, Karl Moritz Haenel, to design a stone observation tower . The construction of the Neo-gothic tower at the summit of the Sněžník began in 1863. A nearby fault line
9405-475: Was established with an area of 79 km , bringing around 700 km of the range under protection as a natural and cultural landscape. The Elbe Sandstone mountains have been a popular destination for tourists for more than 200 years, and for climbers for more than 100 years. It is also a popular recreation area for the nearby Saxon capital Dresden . Places of interest include the Bastei cliffs near Rathen ,
9504-501: Was formed from depositions that accumulated on the bottom of the sea millions of years ago. Large rivers carried sand and other eroded debris into the Cretaceous sea. Rough quartz sand, clay and fine marl sank and became lithified layer by layer. A compact sandstone sequence developed, about 20 x 30 kilometres wide and up to 600 metres thick dating to the lower Cenomanian to Santonian stages . The tremendous variety of shapes in
9603-548: Was grouped with the western part of major units 421 and 423 to form a new major unit, the Western Ore Mountains ( Westerzgebirge ), the eastern part of major units 421 and 423 became the Central Ore Mountains ( Mittelerzgebirge ) and major units 422 and 424 became the Eastern Ore Mountains ( Osterzgebirge ). The current division therefore looks as follows: The geographic unit of the Southern Slopes of
9702-517: Was minted on site in the mountain towns into money. The Joachimsthaler coins, minted in the valley of Joachimsthal , became famous and gave their name to the medieval coin known as the Thaler from which the word " dollar " is derived. After the end of the Hussite Wars , the economy in Bohemia, which had been disrupted by the conflict, recovered. In the 16th century the Ore Mountains became
9801-431: Was regularly cut off from the outside world. The upper Ore Mountains was therefore nicknamed Saxon Siberia already in the 18th century. The fault block mountain range that climbs from northwest to southeast, and which enables prolonged rain to fall as orographic rain when weather systems drive in from the west and northwest, gives rise to twice as much precipitation as in the lowlands which exceeds 1,100 mm on
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