|
Kräuterin
The Kräuterin is a karst massif with a size of 10 km by 12 km, located in the Ybbstal Alps, Austria Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous .... Its highest peak is the Hochstadl, at 1919 meters above sea level. Mountain ranges of Styria Karst {{austria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hochstadl
The Hochstadl is a mountain of the Ybbstal Alps located in Styria, Austria, belonging to the Kräuterin karst massif. It is the highest summit of the Northern Lower Austria Alps. Geography Administratively the mountain belongs to the Austrian state of Styria. Access to the summit The suggested route for the mountain starts from Dürradmer and reaches the top through the Kräuterinhütte (Kräuterin mountain hut) at 1,394 m.''Kräuterinhütte (1394 m)'', article owww.tourensuche.eu (accessed in May 2012) References {{reflist External links * Article in German German(s) may refer to: * Germany (of or related to) **Germania (historical use) * Germans, citizens of Germany, people of German ancestry, or native speakers of the German language ** For citizens of Germany, see also German nationality law **Ger ... obergkraxler.heimat.eu One-thousanders of Austria Mountains of the Alps Mountains of Styria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ybbstal Alps
The Ybbstal Alps (german: Ybbstaler Alpen) are a mountain range of the Northern Limestone Alps and part of the Eastern Alps, located in Austria. They occupy an area along the borders of the states of Upper Austria, Lower Austria and Styria. The range includes the eastern part of the Eisenwurzen, as well as the Göstling Alps and the Kräuterin in the south. The Göstling Alps are home to the popular skiing area at Hochkar Hochkar (1,808 m) is a mountain and a ski area located from Vienna. Located near the small resort of Göstling an der Ybbs on the Steiermark and Lower Austria border, it is popular among skiers who want to leave Vienna for a day, being about a ... (1,808 metres). Their highest peak is the Hochstadl, at above sea level. Another popular mountain is the Dürrenstein at 1,878 m. References Northern Limestone Alps Mountain ranges of the Alps Mountain ranges of Lower Austria Mountain ranges of Upper Austria Mountain ranges of Styria {{Au ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Massif
In geology, a massif ( or ) is a section of a planet's crust that is demarcated by faults or flexures. In the movement of the crust, a massif tends to retain its internal structure while being displaced as a whole. The term also refers to a group of mountains formed by such a structure. In mountaineering and climbing literature, a massif is frequently used to denote the main mass of an individual mountain. The massif is a smaller structural unit of the crust than a tectonic plate, and is considered the fourth-largest driving force in geomorphology. The word is taken from French (in which the word also means "massive"), where it is used to refer a large mountain mass or compact group of connected mountains forming an independent portion of a range. One of the most notable European examples of a massif is the Massif Central of the Auvergne region of France. The Face on Mars is an example of an extraterrestrial massif. Massifs may also form underwater, as with the Atlanti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Styria
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Karst")
