Jizera Mountains | |
Range | |
Frýdlantské cimbuří, a granite formation above Bílý Potok
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Countries | Czech Republic, Poland |
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States | Bohemia, Lower Silesia |
Part of | Western Sudetes |
Highest point | Wysoka Kopa |
- elevation | 1,127 m (3,698 ft) |
- coordinates | |
Geology | Granite, Basalt |
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Jizera Mountains (Czech: Jizerské hory; German: Isergebirge; Polish: Góry Izerskie), or Izera Mountains, are part of the Western Sudetes on the border between the Czech Republic and Poland. The major part is formed from granite, with some areas formed from basalt. The mountains got their name from the Jizera River, which rises at the southern base of Smrk Mountain (German: Tafelfichte).
The weather conditions are characterized by above-average annual precipitation. On 30 July 1897, the measuring station at Nová Louka recorded a daily precipitation amounting to 345.1 mm (13.6 inches), still an unbroken European record. The Jizera Mountains comprise the sources of the Jizera river, the Kwisa and the Lusatian Neisse.
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The highest peak is Wysoka Kopa (Hinterberg, 1,127 m, 3,698 feet) near the town of Szklarska Poręba in Poland. Other mountains include Smrk (1124 m, 3,688 feet), with a recently rebuilt look-out tower, Jizera (1,122 m, 3,681 feet) and Stóg Izerski (Heufuder, 1,107 m, 3,632). The peaks in order of elevation:
The first settlements in the area date back to prehistory. Later on, Celts, German tribes resides in the valleys until they left in 5th century. Later came Lusatian Sorbs. In the 14th century, German-speaking colonists came and started clearing of the dense primeval forests. Permanent settlements were established. In the 16th century, several glass works were founded. Glassmaking had a profound effect on the ecosystem. The primeval forest was gradually replaced by fast-growing spruce monoculture. Other important industries included tin-mining, metallurgy and textile. The Tabulový kámen (German: Tafelstein), 1072 m) on the northern edge of the Smrk Mountain marked the border between the properties of the Counts of Gallas in Friedland, Bohemia, the von Gersdorff family from Meffersdorf, Upper Lusatia, and the Counts of Schaffgotsch from Schreiberhau, Silesia.
In the second half of the 20 century the character of the Jizera Mountains changed completely. The German population of the area was expelled in 1945 and replaced by Poles on the now Polish and Czechs on the Czechoslovakian side of the mountains. The ecosystem was badly hit by emissions, produced by lignite fired power stations located in the Zittau basin. Weakened spruce forest, less resistant against various types of parasites, were on the verge of extinction. The higher parts of the mountains, once densely wooded, became largely treeless, in part also because of excessive deforestation. New roads cut through the once secluded landscape. The situation improved only after the fall of communism in 1989. Open-pit coal mines in the former East Germany were closed, as well as several major power plants. Emission filters were installed at the immense Turów power station in Bogatynia on the Polish side of Lusatian Neisse. At the same time large-scale reforestation projects were started.
The Jizera Mountains are an attractive location for winter sports, cycling and hiking. The centre for both downhill skiing and ski run is Bedřichov. The international cross-country races Jizerská 50 and Bieg Piastów (in Polana Jakuszycka) take place there. Its summer MTB counterpart is also gaining popularity.
The towns surrounding the mountains include Liberec, Frýdlant v Čechách, Nové Město pod Smrkem, Świeradów Zdrój, Szklarska Poręba, Desná, Tanvald and Jablonec nad Nisou.