|
Partnachklamm
The Partnach Gorge (german: Partnachklamm) is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal (Wetterstein), Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is long and, in places, over deep. It was designated a natural monument in 1912. Geology and origin In the Triassic, about 240 million years ago, on the bed of a shallow sea, dark grey, relatively hard layers of Alpine muschelkalk, so-called ''Wurstelkalk'', were laid down in the area of the present day Partnach Gorge. On the bead-like strata of this rock the traces of the burrowing and feeding of marine animals can still be seen. Importantly, about 5 million years later, softer marls were deposited in the same marine basin, which today are known as Partnach Strata (''Partnach-schichten''). In the course of the subsequent Alpine mountain folding the so-called Warnberg Saddle (''Warnberger Sattel'') was formed from these rock strata. The erosion force ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnachklamm
The Partnach Gorge (german: Partnachklamm) is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal (Wetterstein), Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is long and, in places, over deep. It was designated a natural monument in 1912. Geology and origin In the Triassic, about 240 million years ago, on the bed of a shallow sea, dark grey, relatively hard layers of Alpine muschelkalk, so-called ''Wurstelkalk'', were laid down in the area of the present day Partnach Gorge. On the bead-like strata of this rock the traces of the burrowing and feeding of marine animals can still be seen. Importantly, about 5 million years later, softer marls were deposited in the same marine basin, which today are known as Partnach Strata (''Partnach-schichten''). In the course of the subsequent Alpine mountain folding the so-called Warnberg Saddle (''Warnberger Sattel'') was formed from these rock strata. The erosion force ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnachklamm Um 1900
The Partnach Gorge (german: Partnachklamm) is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is long and, in places, over deep. It was designated a natural monument in 1912. Geology and origin In the Triassic, about 240 million years ago, on the bed of a shallow sea, dark grey, relatively hard layers of Alpine muschelkalk, so-called ''Wurstelkalk'', were laid down in the area of the present day Partnach Gorge. On the bead-like strata of this rock the traces of the burrowing and feeding of marine animals can still be seen. Importantly, about 5 million years later, softer marls were deposited in the same marine basin, which today are known as Partnach Strata (''Partnach-schichten''). In the course of the subsequent Alpine mountain folding the so-called Warnberg Saddle (''Warnberger Sattel'') was formed from these rock strata. The erosion force of the Partnach stre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnachklamm Rb
The Partnach Gorge (german: Partnachklamm) is a deep gorge that has been incised by a mountain stream, the Partnach, in the Reintal valley near the south German town of Garmisch-Partenkirchen. The gorge is long and, in places, over deep. It was designated a natural monument in 1912. Geology and origin In the Triassic, about 240 million years ago, on the bed of a shallow sea, dark grey, relatively hard layers of Alpine muschelkalk, so-called ''Wurstelkalk'', were laid down in the area of the present day Partnach Gorge. On the bead-like strata of this rock the traces of the burrowing and feeding of marine animals can still be seen. Importantly, about 5 million years later, softer marls were deposited in the same marine basin, which today are known as Partnach Strata (''Partnach-schichten''). In the course of the subsequent Alpine mountain folding the so-called Warnberg Saddle (''Warnberger Sattel'') was formed from these rock strata. The erosion force of the Partnach stre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partnach
The Partnach is an mountain river in Bavaria, Germany. It rises at a height of on the Zugspitze Massif. The Partnach is fed by meltwaters from the Schneeferner glacier some higher up. The glacier's meltwaters seep into the karsty bedrock and reach the surface again near the source of the Partnach. The Partnach then flows down the Reintal valley. Until 2005 there were two mountain lakes here – the Vordere Blaue Gumpe and the Hintere Blaue Gumpe. At the first lake the water of the Partnach was impounded by scree from rock slides. As a result of heavy rain the natural dam, caused by rockfalls, was partially carried away and the lake was completed filled with sediment. As a result, the Blaue Gumpe does not exist any longer today. Tributaries The Partnach has the following tributaries which join it at or near the river kilometre shown in brackets: *Kanker (0.9) *Boddenberggraben (3.2) *Hornschlittengraben (4.1) *Eselsberggraben (4.4) *Wildsaugraben (4.7) *Graseckgraben (4.8) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zugspitzplatt
The Zugspitze (), at above sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Southern Schneeferner which covers 8.4 hectares. The Zugspitze was first climbed on 27 August 1820 by Josef Naus, his survey assistant, Maier, and mountain guide, Johann Georg Tauschl. Today there are three normal routes to the summit: one from the Höllental valley to the northeast; another out of the Reintal valley to the southeast; and the third from the west over the Austrian Cirque (''Österreichische Schneekar''). One of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reintal (Wetterstein)
The Reintal ("Rein Valley") is the name given to the upper and lower valleys of the River Partnach between the ''Zugspitzplatt'' plateau and the Partnachklamm gorge. A hiking route to Germany's highest mountain, the Zugspitze runs through the valley. The valley was formed during the Würm Ice Age by the Reintal Glacier and then deepened by the Partnach in the post-ice age period after the retreat of the glacier to the periphery of the Schneefernerkopf mountain. The upper Reintal, which was shaped by the glacier and today forms a U-shaped glacial valley, ends between the ''Hohe Gaifkopf'' in the west and the Schachen in the east. The lower Reintal lies in the area of the former glacial lake of the Loisach Glacier, into which the Reintal Glacier flowed from the southwest. It is a V-shaped valley and has been predominantly shaped by the Partnach river. Together with the Höllental valley to the north, the Reintal divides the Wetterstein Mountains into several ridges. The north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Bavaria
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slot Canyons
Slot, the slot or Slots may refer to: People * Arne Slot (born 1978), Dutch footballer * Gerrie Slot (born 1954), Dutch cyclist * Hanke Bruins Slot (born 1977), Dutch politician * Tonny Bruins Slot (born 1947), Dutch association football coach who is known for his analyses of matches and opponents * Jørgen Slots, a Danish-born periodontist in the United States * Margareta Slots (died 1669), Dutch-born mistress of Gustav II Adolf of Sweden Arts, entertainment, and media * Slot (band), a Russian alternative/nu metal band * Slot, abbreviation of St. Laurence O'Toole Pipe Band, a pipe band based in Dublin, Ireland * Dance slot, an imaginary narrow rectangle along which a follower moves back and forth with respect to the leader * ''The Slot'' (TV series), an Australian television series Sport * Slot (ice hockey), the area on the hockey rink directly ahead of the goaltender between the faceoff circles on each side * Slot, a space within a formation during a game of American foo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Germany
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grainau
Grainau is a municipality in the district of Garmisch-Partenkirchen, in southern Bavaria, Germany. It is located at the foot of the Zugspitze mountain, the tallest mountain in Germany in the sub-mountain range of the Wetterstein Alps which is a branch off the main mountain range it is connected to, the Alps. Lake Eibsee in Grainau lies at the foot of the Zugspitze surrounded by forest. Geography Grainau lies at the foot of the Zugspitze in the Wetterstein Mountains. It is part of the seven municipalities of the former County of Werdenfels, along with Garmisch-Partenkirchen, Farchant, Mittenwald, Krün and Wallgau. Grainau is also home to two mountain lakes, the Badersee and the Eibsee. Waxenstein mountain sits to the south, while the Kramerspitz mountain and Ammergau Alps sit to the north. The district of Grainau is made up of: * Obergrainau (parish village) * Untergrainau and Hammersbach (church village) * Schmölz (village) * Eibsee (hamlet) Notable people * Lorenz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfalls In Germany
This list of notable waterfalls of the world is sorted by continent, then country, then province, state or territory. A waterfall is included if it has an existing article specifically for it on Wikipedia, and it is at least high, or the falls have some historical significance based on multiple reliable references. There is no standard way to measure the height or width of a waterfall. No ranking of waterfalls should be assumed because of the heights or widths provided in the list. Many numbers are estimated and measurements may be imprecise. See additional lists of waterfalls by height, flow rate and type. Africa Angola * Kalandula Falls – high Burundi * Kagera Falls * Rusumo Falls Central African Republic * Boali Falls Chad * Gauthiot Falls Democratic Republic of the Congo * Boyoma Falls – formerly known as Stanley Falls; highest flow rate in the world * Inga Falls * Livingstone Falls * Lofoi Falls – high Ethiopia * Blue Nile Falls ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dracula
''Dracula'' is a novel by Bram Stoker, published in 1897. As an epistolary novel, the narrative is related through letters, diary entries, and newspaper articles. It has no single protagonist, but opens with solicitor Jonathan Harker taking a business trip to stay at the castle of a Transylvanian nobleman, Count Dracula. Harker escapes the castle after discovering that Dracula is a vampire, and the Count moves to England and plagues the seaside town of Whitby. A small group, led by Abraham Van Helsing, hunt Dracula and, in the end, kill him. ''Dracula'' was mostly written in the 1890s. Stoker produced over a hundred pages of notes for the novel, drawing extensively from Transylvanian folklore and history. Some scholars have suggested that the character of Dracula was inspired by historical figures like the Wallachian prince Vlad the Impaler or the countess Elizabeth Báthory, but there is widespread disagreement. Stoker's notes mention neither figure. He found the name ''D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Landforms Of Bavaria")
