The Bernese Alps are a mountain range of the Alps, located in western Switzerland. Although the name suggests that they are located in the Berner Oberland region of the canton of Bern, portions of the Bernese Alps are in the adjacent cantons of Valais, Fribourg and Vaud, the latter being usually named Fribourg Alps and Vaud Alps respectively. The highest mountain in the range, the Finsteraarhorn, is also the highest point in the canton of Bern.
The Bavarian Forest is a wooded, low-mountain region in Bavaria, Germany that is about 100 kilometres long. It runs along the Czech border and is continued on the Czech side by the Bohemian Forest. Most of the Bavarian Forest lies within the province of Lower Bavaria, but the northern part lies within Upper Palatinate. In the south it reaches the border with Upper Austria.
The Zugspitze, at 2,962 m (9,718 ft) above sea level, is the highest peak of the Wetterstein Mountains and the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen in Bavaria, and the Austria–Germany border is on its western summit. South of the mountain is the Zugspitzplatt, a high karst plateau with numerous caves. On the flanks of the Zugspitze are two glaciers, the largest in Germany: the Northern Schneeferner with an area of 30.7 hectares and Höllentalferner with an area of 24.7 hectares. Shrinking of the Southern Schneeferner led to the loss of glacier status in 2022.
The Würm glaciation or Würm stage, usually referred to in the literature as the Würm, was the last glacial period in the Alpine region. It is the youngest of the major glaciations of the region that extended beyond the Alps themselves. Like most of the other ice ages of the Pleistocene epoch, it is named after a river, in this case the Würm in Bavaria, a tributary of the Amper.
The Riss glaciation, Riss Glaciation, Riss ice age, Riss Ice Age, Riss glacial or Riss Glacial is the second youngest glaciation of the Pleistocene epoch in the traditional, quadripartite glacial classification of the Alps. The literature variously dates it to between about 300,000 to 130,000 years ago and 347,000 to 128,000 years ago. It coincides with the Saale glaciation of North Germany. The name goes back to Albrecht Penck and Eduard Brückner who named this cold period after the river Riss in Upper Swabia in their three-volume work Die Alpen im Eiszeitalter published between 1901 and 1909.
The Swiss Plateau or Central Plateau is one of the three major landscapes in Switzerland, lying between the Jura Mountains and the Swiss Alps. It covers about 30% of the Swiss surface area, and is partly flat but mostly hilly. The average height is between 400 metres (1,300 ft) and 700 metres (2,300 ft) AMSL. It is by far the most densely populated region of Switzerland, the center of economy and important transportation.
Hoher Dachstein is a strongly karstic mountain in central Austria and the second-highest mountain in the Northern Limestone Alps. It is situated at the border of Upper Austria and Styria, and is the highest point in each of those states. Parts of the massif also lie in the state of Salzburg, leading to the mountain being referred to as the Drei-Länder-Berg.
Hohenpeißenberg is a municipality in the Weilheim-Schongau district, in Bavaria, Germany. Hohenpeißenberg is situated in the Bavarian Oberland, in the Alpine Foreland.
The Allgäu Alps are a mountain range in the Northern Limestone Alps, located in Bavaria and Baden-Württemberg in Germany and Tyrol and Vorarlberg in Austria. The range lies directly east of Lake Constance.
Mount Blum, or Mount Bald, is a 7,685-foot (2,342 m) summit of the North Cascades range in Washington state, on the western edge of North Cascades National Park. It is the highest summit of a string of mountain peaks located east of Mount Shuksan and west of the Picket Range. Two small active glaciers rest on its northern flank. Mount Blum was named after John Blum, a United States Forest Service fire patrol pilot who perished in a plane crash near Snoqualmie Pass in 1931.
The Phlegra Montes are a system of eroded Hesperian–Noachian-aged massifs and knobby terrain in the mid-latitudes of the northern lowlands of Mars, extending northwards from the Elysium Rise towards Vastitas Borealis for nearly 1,400 km (870 mi). The mountain ranges separate the large plains provinces of Utopia Planitia (west) and Amazonis Planitia (east), and were named in the 1970s after a classical albedo feature. The massif terrains are flanked by numerous parallel wrinkle ridges known as the Phlegra Dorsa.
Buckner Mountain is a tall peak in the North Cascades of Washington state and in the Stephen Mather Wilderness of North Cascades National Park. At 9,114 feet (2,778 m) in elevation it is the highest in Skagit County and one of about ten of Washington's non-volcanic peaks above 9,000 feet high. It is ranked as the 14th highest peak in the state, and the third highest peak in North Cascades National Park.
The Alpine Foreland, less commonly called the Bavarian Foreland, Bavarian Plateau or Bavarian Alpine Foreland, refers to a triangular region of plateau and rolling foothills in Southern Germany, stretching from Lake Constance in the west to beyond Linz on the Danube in the east, with the Bavarian Alps forming its south boundary and the Danube its northern extent.
The Ammergau Alps are a mountain range in the Northern Limestone Alps in the states of Bavaria (Germany) and Tyrol (Austria). They cover an area of about 30 x 30 km and begin at the outer edge of the Alps. The highest summit is the Daniel which has a height of 2,340 metres (7,680 ft).
The Forggensee, also called the Roßhaupten Reservoir, is a reservoir located north of Füssen in the county of Ostallgäu in Bavaria, Germany and one of many lakes in the region around Hohenschwangau and Neuschwanstein castles. With a surface area of 15.2 km², it is the fifth-largest lake in Bavaria and the largest reservoir in Germany by area. The River Lech flows through it. The Forggensee is known primarily as a tourist destination for aquatic sports and recreation. Besides Füssen, other settlements on the lake include Halblech, Rieden am Forggensee and Roßhaupten. The lake takes its name from the former hamlet of Forggen which has been submerged by the reservoir.
The Mieming(er) Range, Mieminger Chain or Mieminger Mountains, is a mountain range of the Northern Limestone Alps in the Eastern Alps. It is located entirely in Austria within the state of Tyrol. This sub-group is somewhat in the shadows of its more famous neighbour, the Wetterstein to the north. Whilst the region around the Coburger Hut and the lakes of Seebensee and Drachensee in the west and the Hohe Munde in the extreme east receive large numbers of visitors, the less developed central area remains very quiet. The Hohe Munde is also a popular and challenging ski touring destination.
An alpentor in geology is the point where an entire glacier forced its way through to the Alpine Foreland from the Alps during the ice age.
The geology of Germany is heavily influenced by several phases of orogeny in the Paleozoic and the Cenozoic, by sedimentation in shelf seas and epicontinental seas and on plains in the Permian and Mesozoic as well as by the Quaternary glaciations.
The geology of Austria consists of Precambrian rocks and minerals together with younger marine sedimentary rocks uplifted by the Alpine orogeny.
The Munich gravel plain is an outwash plain in Upper Bavaria, Germany, formed during Late Pleistocene glacial periods. Characterized by its very wide extension, it comprises sandur terraces and the floodplain of the Isar river. These most recent deposits overlie the Neogene Molasse basin of the Alpine Foreland, which in contrast comprises fine-grained fluviatile and lacustrine facies.
