Page Type: | Mountain/Rock |
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Lat/Lon: | 50.73600°N / 15.74000°E |
Activities: | Hiking |
Season: | Spring, Summer, Fall, Winter |
Elevation: | 5259 ft / 1603 m |
Sněžka/Śnieżka (a feminine noun in both Czech and Polish, which can be translated as the Snowy One or Snow White; Schneekoppe in German) at an elevation of 1602 or – according to the latest Czech measurement – 1603m, is the highest summit in the Giant Mountains, in all of the Sudetes as well as Czechia. It has 1203m of prominence and, standing on the border between Czechia and Poland, rises nearly 200m above the main ridge of the Giant Mountains. This is due to the mountain's geologic make-up: unlike its surroundings, it is formed of hornfels, which is extremely resistant to erosion. Until the 19th century Śnieżka was also known as Rieseberg, that is the Giant Mountain. Sněžka's north and southwest sides are quite high and steep. They descend over 500m to the bottoms of the valleys of, respectively, Łomniczka and Úpa brooks. The gentler side is the southeast side. To the south Śnieżka sends out a lateral ridge which is named after Růžová hora (1390m), its first summit south of Sněžka. At the west foot of Śnieżka extends the undulating plateau – an ancient peneplain raised by tectonic forces - that forms what we call the main ridge of the Giant Mountains west from Sněžka. The main ridge of the Giant Mountains east of Śnieżka is much narrower and does look like a ridge. Between Sněžka and Svorová hora/Czarna Kopa at 1407m, the ridge - clad in dwarf mountain pine and talus - is called Obří hřeben (Giant Ridge)/Czarny Grzbiet (Black Ridge).
In the Ice Age, the upper parts of the valleys that begin at Sněžka cradled glaciers, which results in a couple of fine, albeit lakeless, corries sitting below Śnieżka on either side of the international border. These corries are notorious for avalanches.
Given the qualities of the rock which Śnieżka is composed of, it is no surprise that the upper slopes of the mountain are virtually devoid of vegetation and covered in talus. On the steep slopes of Sněžka and nearby mountains debris flows occur as well. In the summer of 1897, after two weeks of continuous rainfall, two most destructive debris flows rushed down the western slopes of Růžová hora to raze two buildings and claim the lives of seven people. Photographs from that time can be seen in a little chapel in Obří Důl.
As far as the climate is concerned, Sněžka can be called the Central European Mount Washington, especially with reference to the wind speed. The maximum wind speed recorded on Śnieżka was 345km/h in 1990 (Mount Washington 372km/h in 1934).
Sněžka has been climbed for nearly or even more than 500 years! In Obří důl (Giant Pit), the uppermost part of the Úpa Valley, metal ores were mined as early as the 16th century. The popularity of Śnieżka soared in the 19th century when it was the highpoint of Prussia. There are a few buildings on the summit, of which the chapel of St.Lawrence, built in 1681, is the oldest. The biggest is the Polish 'UFOs' from 1976, which used to house a weather station, a mountain hut and a restaurant. But in summer 2016 only a buffet was open on the ground floor. Another building is a Czech post office, where you can buy postcards and similar stuff. The fourth structure is the upper station of a Czech cable car.
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NB There are plenty of guesthouses and hotels as well as a few campsites on either side of the Giant Mountains.
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Czechia
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