Map of Austria

Geography

The Grossglockner lies on the border between the Austrian states of Carinthia and Tyrol (East Tyrol). The peak is part of the Glocknerkamm ridge in the Glockner Group that branches off the main chain of the Alps at Eiskögele, heading in a southeasterly direction and forming the boundary between the East Tyrolean municipality of Kals am Großglockner, about 8 km (5.0 mi) in the southwest at 1,324 m (4,344 ft), and Carinthian Heiligenblut, about 12 km (7.5 mi) in the northeast at 1,291 m (4,236 ft). This boundary is also the watershed between the Kals Valley and its Teischnitz and Ködnitz side valleys on the Tyrolean side and the Möll Valley with the Pasterze glacier on the Carinthian side.

History

The French-born natural scientist Belsazar Hacquet, from 1773 professor of anatomy at the Academy of Ljubljana, travelled the Eastern Alps from 1779 to 1781 and published an itinerary in 1783, describing the Glokner mountain and stating that it had not been climbed yet. He estimated the mountain's height as 3,793 m (12,444 ft), and created an engraving illustrating Grossglockner and Pasterze, the first known depiction of the mountain.

Inspired by Hacquet's book and by the first ascent of the Mont Blanc in 1786, the Gurk prince-bishop Count Franz Xaver of Salm (1749–1822) together with his vicar general Sigismund Ernst Hohenwart (1745–1825) and Baron Franz Xaver von Wulfen (1728–1805) started efforts for a Grossglockner expedition.

Geography

The Zugspitze belongs to the Wetterstein range of the Northern Limestone Alps. The Austria–Germany border goes right over the mountain. There used to be a border checkpoint at the summit but, since Germany and Austria are now both part of the Schengen zone, the border crossing is no longer staffed.

The exact height of the Zugspitze was a matter of debate for quite a while. Given figures ranged from 2,690–2,970 metres (8,830–9,740 ft), but it is now generally accepted that the peak is 2,962 m (9,718 ft) above sea level as a result of a survey carried out by the Bavarian State Survey Office. The lounge at the new café is named "2962" for this reason.

At 2,962 metres (9,718 ft) (eastern peak) the Zugspitze is the highest mountain of the Zugspitze massif.

History

The first recorded ascent to the summit was accomplished by a team of land surveyors on 27 August 1820. The team was led by Lieutenant Josef Naus, who was accompanied by two men named Maier and G. Deutschl. However, local people had conquered the peak over 50 years earlier, according to a 1770 map discovered by the Alpenverein.

According to one legend, the northern part of the Zugspitze was given to Bavaria as a present by Emperor of Austria and Apostolic King of Hungary Franz Joseph I as a marriage present to his wife Princess Elisabeth ("Sisi") in 1854. This would have made the Zugspitze the highest mountain in Bavaria and later Germany.

Tourism

For those wishing to reach the summit under their own power, various hiking and ski trails can be followed to the top. Hiking to the top from the base takes between one and two days, or a few hours for the very fit. Food and lodging is available on some trails. In winter the Zugspitze is a popular skiing and snowboarding destination, with several slopes on both sides. The Zugspitzplatt is Germany's highest ski resort, and thus normally has sufficient snow throughout the winter.

At the Zugspitze's summit is the Münchner Haus, a mountain hut (Alpenhütte), a facility built by the German Alpine Club (Deutscher Alpenverein). For more than a hundred years, the summit has also had a weather station, which nowadays also gathers data for the Global Atmosphere Watch.

Geography

Lake Constance is located in the foothills of the Alps. The shore length of both main lakes is 273 kilometres (170 mi) long. Of this, 173 kilometres (107 mi) are located in Germany (Baden-Württemberg 155 kilometres or 96 miles, Bavaria 18 kilometres or 11 miles), 28 kilometres (17 mi) run through Austria and 72 kilometres (45 mi) through Switzerland. If the upper and lower lakes are combined, Lake Constance has a total area of 536 km2 (207 sq mi), the third largest lake in Central Europe by area after Lake Balaton (594 km2 or 229 sq mi) and Lake Geneva (580 km2 or 220 sq mi).

History

Lake Constance was formed by the Rhine Glacier during the Quaternary glaciation ice age and is a Zungenbecken or Tongue lake. After the end of the last glacial period, about 10,000 years ago, the Obersee and Untersee still formed a single lake. The downward erosion of the High Rhine caused the lake level to gradually sink and a sill, the Konstanzer Schwelle, to emerge.

The Rhine, the Bregenzer Ach, and the Dornbirner Ach carry sediments from the Alps to the lake, thus gradually decreasing the depth and reducing the extension of the lake in the southeast.

In antiquity, the two lakes had different names; later, for reasons which are unknown, they came to have the same name.

In the 19th century, there were five different local time zones around Lake Constance.

Ecology

Until the 19th century, Lake Constance was a natural lake. Since then, nature has been heavily influenced by clearing and the cultivation of much of the land around its shores. However, some near-natural areas have been largely conserved, especially in the nature reserves, or were re-naturalised. As a result, the Lake Constance region has some unusual ecological features. These include the large forested area on the Bodanrück, the occurrence of marsh gentian and orchids of the genera Dactylorhiza and Orchis in the Wollmatinger Ried, and the Siberian iris (Iris sibirica) in the Eriskircher Ried, which was therefore given its own name.

Description

Lake Constance is located along the Rhine between the Alpine Rhine, its main tributary, and the High Rhine, its outflow. It is the third largest freshwater lake by surface area in Central and Western Europe (and the second largest in volume), after Lake Geneva and (in surface area) Lake Balaton.

It is 63 km (39 mi) long, and, nearly 14 km (8.7 mi) at its widest point. It covers about 536 km2 (207 sq mi), and is 395 m (1,296 ft) above sea level. Its greatest depth is 252 metres (827 ft), exactly in the middle of the Upper Lake. Its volume is about 48 km3 (12 cu mi).

The lake has two parts.

Geography

The Alps are a crescent shaped geographic feature of central Europe that ranges in an 800 km (500 mi) arc (curved line) from east to west and is 200 km (120 mi) in width. The mean height of the mountain peaks is 2.5 km (1.6 mi). The range stretches from the Mediterranean Sea north above the Po basin, extending through France from Grenoble, and stretching eastward through mid and southern Switzerland. The range continues onward toward Vienna, Austria, and southeast to the Adriatic Sea and Slovenia. Depending on the definitions used, the Alpokalja foothills in western Hungary may also qualify as part of the Alps.

To the south it dips into northern Italy and to the north extends to the southern border of Bavaria in Germany.

Geology

Important geological concepts were established as naturalists began studying the rock formations of the Alps in the 18th century. In the mid-19th century, the now-defunct idea of geosynclines was used to explain the presence of "folded" mountain chains. This theory was replaced in the mid-20th century by the theory of plate tectonics.

The formation of the Alps (the Alpine orogeny) was an episodic process that began about 300 million years ago. In the Paleozoic Era the Pangaean supercontinent consisted of a single tectonic plate; it broke into separate plates during the Mesozoic Era and the Tethys sea developed between Laurasia and Gondwana during the Jurassic Period.

Ecology

Thirteen thousand species of plants have been identified in the Alpine regions. Alpine plants are grouped by habitat and soil type which can be limestone or non-calcareous. The habitats range from meadows, bogs, and woodland (deciduous and coniferous) areas to soil-less scree and moraines, and rock faces and ridges. A natural vegetation limit with altitude is given by the presence of the chief deciduous trees—oak, beech, ash and sycamore maple. These do not reach the same elevation, nor are they often found growing together, but their upper limit corresponds accurately enough to the change from a temperate to a colder climate that is further proved by a change in the presence of wild herbaceous vegetation.

History

When the ice melted after the Würm glaciation, Paleolithic settlements were established along the lake shores and in cave systems. Evidence of human habitation has been found in caves near the Vercors Cave System, close to Grenoble and Echirolles. In Austria, the Mondsee lake shows evidence of houses built on piles. Standing stones have been found in the Alpine areas of France and Italy. About 200,000 drawings and etchings have been documented, and are known as the Rock Drawings in Valcamonica.

A mummy of a Neolithic human, known as Ötzi, was discovered on the Similaun.

Geography

The Bohemian Forest consists of densely forested mountains with an average elevation of 800–1,400 metres (2,600–4,600 ft). On the Bavarian side, the highest peak is Großer Arber at 1,456 metres (4,777 ft). On the Bohemian and Austrian side, the highest peak is the Plöckenstein or Plechý in Czech at 1,378 metres (4,521 ft). The most eastern peak is the Sternstein at 1,125 metres (3,691 ft). The range is one of the oldest in Europe, and its mountains have eroded into round forms with few rocky parts. Typical for the Bohemian Forest are plateaus of about 1,000–1,200 metres (3,300–3,900 ft) elevation with fairly harsh climatic condictions and numerous peat bogs.

History

According to archaeological findings, the Bohemian Forest was not significantly populated during the Paleolithic era or the Stone Age, dating as far back as 9000 BC. Initial settlements of a more permanent character first appeared in southwest Bohemia during the Bronze Age between 3,000 and 1,000 years BC. In the 1st century AD, the northern part of the forest was inhabited by Gallo-Romans and by Germanic tribes.

The Celts were gradually forced out by Germanic tribes (the Marcomanni), and Celtic settlements fell in disrepair. With the subsequent departure of the Marcomanni, the Bohemian Forest continued to evolve without human influence. The forests only changed their character after the arrival of the Slavs in the region in the 6th century, who sought refuge there.