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Bodetal
The Bode Gorge (german: Bodetal) is a long ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, ''Bodetal'' (literally "Bode Valley"), is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode. At the Bode Gorge, the River Bode, which rises on the highest mountain in the Harz, the Brocken, has cut deeply into the hard Ramberg granite rock. The ravine is about 140 m deep at Treseburg and some 280 m deep at Thale where it breaks out into the Harz Foreland. The Bode Gorge was designated a nature reserve as early as 5 March 1937; its boundaries being subsequently expanded. With an area of, currently , it is one of the largest nature reserves in Saxony-Anhalt. Geology Apart from intrusions of Ramberg granite, which rose to the surface and solidified 300 million years ago in the Upper Carboniferous Period, and their associated veins of q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bodetal2
The Bode Gorge (german: Bodetal) is a long ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, ''Bodetal'' (literally "Bode Valley"), is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode. At the Bode Gorge, the River Bode, which rises on the highest mountain in the Harz, the Brocken, has cut deeply into the hard Ramberg granite rock. The ravine is about 140 m deep at Treseburg and some 280 m deep at Thale where it breaks out into the Harz Foreland. The Bode Gorge was designated a nature reserve as early as 5 March 1937; its boundaries being subsequently expanded. With an area of, currently , it is one of the largest nature reserves in Saxony-Anhalt. Geology Apart from intrusions of Ramberg granite, which rose to the surface and solidified 300 million years ago in the Upper Carboniferous Period, and their associated veins o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bodetal Ramberggranit
The Bode Gorge (german: Bodetal) is a long ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, ''Bodetal'' (literally "Bode Valley"), is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode. At the Bode Gorge, the River Bode, which rises on the highest mountain in the Harz, the Brocken, has cut deeply into the hard Ramberg granite rock. The ravine is about 140 m deep at Treseburg and some 280 m deep at Thale where it breaks out into the Harz Foreland. The Bode Gorge was designated a nature reserve as early as 5 March 1937; its boundaries being subsequently expanded. With an area of, currently , it is one of the largest nature reserves in Saxony-Anhalt. Geology Apart from intrusions of Ramberg granite, which rose to the surface and solidified 300 million years ago in the Upper Carboniferous Period, and their associated veins of q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bodetal
The Bode Gorge (german: Bodetal) is a long ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, ''Bodetal'' (literally "Bode Valley"), is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode. At the Bode Gorge, the River Bode, which rises on the highest mountain in the Harz, the Brocken, has cut deeply into the hard Ramberg granite rock. The ravine is about 140 m deep at Treseburg and some 280 m deep at Thale where it breaks out into the Harz Foreland. The Bode Gorge was designated a nature reserve as early as 5 March 1937; its boundaries being subsequently expanded. With an area of, currently , it is one of the largest nature reserves in Saxony-Anhalt. Geology Apart from intrusions of Ramberg granite, which rose to the surface and solidified 300 million years ago in the Upper Carboniferous Period, and their associated veins of q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Bode
The Bode is a river in the German state of Saxony-Anhalt, a left tributary of the Saale. It rises in the Harz mountains and drains them in a northerly direction. After it discharges into the Saale at Nienburg. The river is named after a legendary giant, the wild, rampaging, Bohemian, ''Prince Bodo'', who, according to the '' Rosstrappe'' legend changed into a marauding dog that guarded the crown of ''Princess Brunhilde'' in the ''Kronensumpf'' ("crown marsh") in the present-day Bode Gorge (german: Bodetal). The gorge is the narrow section of the Bode valley between Treseburg and Thale. The ''Bodo'' legend According to tradition, there was once a giant called ''Bodo'' who came from Thuringia to pursue ''Brunhilde'', the king's beautiful daughter, whom he wanted to marry against her will. ''Brunhilde'' fled on a white stallion (''Ross''), but they suddenly came to a deep ravine. With one bold leap she reached the rocks on the far side, but her pursuer fell into the abyss. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bode (river)
The Bode is a river in the German state of Saxony-Anhalt, a left tributary of the Saale. It rises in the Harz mountains and drains them in a northerly direction. After it discharges into the Saale at Nienburg. The river is named after a legendary giant, the wild, rampaging, Bohemian, ''Prince Bodo'', who, according to the '' Rosstrappe'' legend changed into a marauding dog that guarded the crown of ''Princess Brunhilde'' in the ''Kronensumpf'' ("crown marsh") in the present-day Bode Gorge (german: Bodetal). The gorge is the narrow section of the Bode valley between Treseburg and Thale. The ''Bodo'' legend According to tradition, there was once a giant called ''Bodo'' who came from Thuringia to pursue ''Brunhilde'', the king's beautiful daughter, whom he wanted to marry against her will. ''Brunhilde'' fled on a white stallion (''Ross''), but they suddenly came to a deep ravine. With one bold leap she reached the rocks on the far side, but her pursuer fell into the abyss. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thale
Thale () is a town in the Harz district in Saxony-Anhalt in central Germany. Located at the steep northeastern rim of the Harz mountain range, it is known for the scenic Bode Gorge stretching above the town centre. Geography The town is situated on the river Bode, approximately west of Quedlinburg. Served by Transdev Sachsen-Anhalt trains, Thale Hauptbahnhof is the terminus of the Magdeburg–Thale railway line. The town has access to the Bundesstraße 6n highway. Divisions The town Thale consists of Thale proper and the following ''Ortschaften'' or municipal divisions:Hauptsatzung der Stadt Thale December 2014. * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harz Foreland
The Harz () is a highland area in northern Germany. It has the highest elevations for that region, and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt, and Thuringia. The name ''Harz'' derives from the Middle High German word ''Hardt'' or ''Hart'' (hill forest). The name ''Hercynia'' derives from a Celtic name and could refer to other mountain forests, but has also been applied to the geology of the Harz. The Brocken is the highest summit in the Harz with an elevation of above sea level. The Wurmberg () is the highest peak located entirely within the state of Lower Saxony. Geography Location and extent The Harz has a length of , stretching from the town of Seesen in the northwest to Eisleben in the east, and a width of . It occupies an area of , and is divided into the Upper Harz (''Oberharz'') in the northwest, which is up to 800 m high, apart from the 1,100 m high Brocken massif, and the Lower Harz (''Unterharz'') in the east which is up to arou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harz Mountains
The Harz () is a highland area in northern Germany. It has the highest elevations for that region, and its rugged terrain extends across parts of Lower Saxony, Saxony-Anhalt, and Thuringia. The name ''Harz'' derives from the Middle High German word ''Hardt'' or ''Hart'' (hill forest). The name ''Hercynia'' derives from a Celtic name and could refer to other mountain forests, but has also been applied to the geology of the Harz. The Brocken is the highest summit in the Harz with an elevation of above sea level. The Wurmberg () is the highest peak located entirely within the state of Lower Saxony. Geography Location and extent The Harz has a length of , stretching from the town of Seesen in the northwest to Eisleben in the east, and a width of . It occupies an area of , and is divided into the Upper Harz (''Oberharz'') in the northwest, which is up to 800 m high, apart from the 1,100 m high Brocken massif, and the Lower Harz (''Unterharz'') in the east which is up to arou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphosed
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone ( sedimentary rocks) through lithification. Sediments are most often transported by water ( fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biotite
Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula . It is primarily a solid-solution series between the iron- endmember annite, and the magnesium-endmember phlogopite; more aluminous end-members include siderophyllite and eastonite. Biotite was regarded as a mineral ''species'' by the International Mineralogical Association until 1998, when its status was changed to a mineral ''group''. The term ''biotite'' is still used to describe unanalysed dark micas in the field. Biotite was named by J.F.L. Hausmann in 1847 in honor of the French physicist Jean-Baptiste Biot, who performed early research into the many optical properties of mica. Members of the biotite group are sheet silicates. Iron, magnesium, aluminium, silicon, oxygen, and hydrogen form sheets that are weakly bound together by potassium ions. The term "iron mica" is sometimes used for iron-rich biotite, but the term also refers to a flaky mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
