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Hohenbol
The Hohenbol is a mountain of Baden-Württemberg, Germany. *Hohenbol (Baden-Württemberg) *Type Witnesses Mountain of volcanic origin The Hohenbol is a high mountain 2 kilometers from the town of Owen in the district of Esslingen in Baden-Württemberg. The Hohenbol is a foothill of the Teckberg and upstrimes this northwest. The Teckberg and the summit of Hohenbol (above the orchard slope) are a nature reserve protected area. The Hohenbol is a witness mountain of volcanic origin. He is one of the 355 volcanoes that are known from the "Urach volcanic area". Geology It is originated in the Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ..., when one of the volcanic vents of the Swabian volcano forced its way through the surrounding rock. Through erosion of Hohenbol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenbol - Gipfel
The Hohenbol is a mountain of Baden-Württemberg, Germany. *Hohenbol (Baden-Württemberg) *Type Witnesses Mountain of volcanic origin The Hohenbol is a high mountain 2 kilometers from the town of Owen in the district of Esslingen in Baden-Württemberg. The Hohenbol is a foothill of the Teckberg and upstrimes this northwest. The Teckberg and the summit of Hohenbol (above the orchard slope) are a nature reserve protected area. The Hohenbol is a witness mountain of volcanic origin. He is one of the 355 volcanoes that are known from the "Urach volcanic area". Geology It is originated in the Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ..., when one of the volcanic vents of the Swabian volcano forced its way through the surrounding rock. Through erosion of Hohenbol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenbol Und Teckberg
The Hohenbol is a mountain of Baden-Württemberg, Germany. *Hohenbol (Baden-Württemberg) *Type Witnesses Mountain of volcanic origin The Hohenbol is a high mountain 2 kilometers from the town of Owen in the district of Esslingen in Baden-Württemberg. The Hohenbol is a foothill of the Teckberg and upstrimes this northwest. The Teckberg and the summit of Hohenbol (above the orchard slope) are a nature reserve protected area. The Hohenbol is a witness mountain of volcanic origin. He is one of the 355 volcanoes that are known from the "Urach volcanic area". Geology It is originated in the Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ..., when one of the volcanic vents of the Swabian volcano forced its way through the surrounding rock. Through erosion of Hohenbol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teckberg
Teckberg is a mountain at ''Landkreis Esslingen'' in Baden-Württemberg, Germany, with an elevation of 775 metres. Situated on top is castle Teck. Geography The Teckberg jumps from Swabian Jura edge from about 3 km towards the north front and overlooks the Albvorland to 350 m, the Lauter (Neckar) valley to 400 m. He is flanked of the approximately 602 m high foothills Hörnle and Hohenbol north and northwest. Both Foothills include smokestacks of the Swabian volcano. North below the Hörnle is the glider area Teck (between Dettingen unter Teck and Bissingen an der Teck). The slope of the Teckberg formed by the Yellow Rock, a Schwammriff the Jura sea of bright lime. Under the "Gelber Fels", is the 31 m long and 45 m high Veronikahöhle, which is connected through columns with Verena-Beutlins-Loch. East of the Gelber Fels (Yellow Rock) three grave mounds indicate from the Hallstatt period (800-400 BC) the early settlement of the Teckberg. Under the castle Teck is the 35 m long an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baden-Württemberg
Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a total area of nearly , it is the third-largest German state by both area (behind Bavaria and Lower Saxony) and population (behind North Rhine-Westphalia and Bavaria). As a federated state, Baden-Württemberg is a partly-sovereign parliamentary republic. The largest city in Baden-Württemberg is the state capital of Stuttgart, followed by Mannheim and Karlsruhe. Other major cities are Freiburg im Breisgau, Heidelberg, Heilbronn, Pforzheim, Reutlingen, Tübingen, and Ulm. What is now Baden-Württemberg was formerly the historical territories of Baden, Prussian Hohenzollern, and Württemberg. Baden-Württemberg became a state of West Germany in April 1952 by the merger of Württemberg-Baden, South Baden, and Württemberg-Hohenzollern. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Owen, Germany
Owen (, see below) is a town in the district of Esslingen in Baden-Württemberg in southern Germany. It is located southeast of Stuttgart and south of Kirchheim unter Teck. Pronunciation The name's pronunciation contradicts ordinary German orthographic rules and is more similar to English standard pronunciation. The name derives from the old word "Aue", meaning floodplain, and kept its ancient pronunciation. Traffic Owen is connected to the railway-system by the Teckbahn ( Wendlingen– Oberlenningen). The Königlich Württembergischen Staats-Eisenbahnen built the station in 1899. There are bus connections to the neighbour communities. Through Owen leads A-Road B 465 from Kirchheim unter Teck to Blaubeuren Blaubeuren () is a town in the district of Alb-Donau near Ulm in Baden-Württemberg, Germany. it had 11,963 inhabitants. Geography Geographical location The core city Blaubeuren lies at the foot of the Swabian Jura, west of Ulm. Neighborin .... Highway A 8 is t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Baden-Württemberg
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Under 1000 Metres
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
