The highest point is Prosečský hřeben at 593 metres (1,946ft) above sea level, located between the Czech cities of Liberec and Jablonec nad Nisou.[1]
Natural region divisions
Eastern Upper Lusatia in the geomophological system of the Czech RepublicEastern Upper Lusatia in the geomophological system of Poland
In the Czech Republic, the mesoregion has an area of 187km2 (72sqmi) and an average elevation of 384m (1,260ft).[2] It is further subdivided into the microregions of Liberec Valley and Hrádek Basin.[3]
In Poland the mesoregion has an area of about 240km2 (93sqmi).
According to the German division, the Eastern Upper Lusatia is divided as follows into mesogeochores and microgeochores and hills:[4]
12 Eastern Upper Lusatia
11002 Zittau Basin (65.04 km²)
Hirschfeld Neiße Valley
Olbersdorf Ridge
Northern Zittau Basin
Southern Zittau Basin
Zittau Neiße and Mandau Valley
Olbersdorf Open-Cast Mine (Olbersdorfer See)
11003 Großschönau Basin and Kuppenland (60.97 km² in SN; continues into the Czech Republic)
Spitzkunnersdorf Kuppen Region (Hofebusch and Richterberg (469.3m), Lindeberg 459.3m Forstenberg 454.8m, Pfaffenberg 418.1m, Wiedeberg 396.6m)
Seifhennersdorf Kuppen Region (border region of the otherwise entirely Czech southeastern part of the Lusatian Highlands; Frenzelsberg 468.2m)
Rotstein Ridge (Rotstein 453.7m, Hengstberg 421.3m, Georgenberg 396.5m, Horkenberg 331.9m; on the far side of the railway and B6: Rosenhainer Berg 307.9m)
Hochstein-Kämpferberg Ridge (397.2m und 415m; Königshain Hills)
Notes
↑Actually the 395.3m high main summit according to maps –like the clearly well known neighbour in the north – is called the Schafberg and the Jäckelberg at 388.5m and the Jäckelbaude is only the northern top. Locally the hill is better known as the Jäckelberg.
Landscape and geology
The natural region is very varied and characterized by hill ranges, isolated hills, plateau and basins alongside one another. Ice age ground moraines, meltwater sands and the overlying loess soils fill out the granite relief to varying degrees. The loess loam is generally only about 1 to 1.5m thick. As witnesses to the Tertiaryvolcanism of the area there are lava plains and isolated hills of basalt and phonolite. In the Zittau and Oderwitz Basin, as well as the Berzdorf Basin there are important deposits of brown coal in the sediments.
Climatically Eastern Upper Lusatia lies partially in the lee of the Upper Lusatian Highlands. For example, only 665mm of precipitation falls annually. The average annual temperature lies between 8 and 8.6°C. The potential natural vegetation here is Wood Bedstraw-Hornbeam-Oak forest with Small-leaved Limes.
Mannsfeld, K. und Syrbe, R.-U. (eds.): Naturräume in Sachsen mit Kartenbeilage "Naturräumliche Gliederung Sachsens", in: Forschungen zur deutschen Landeskunde (Vol. 257), Deutsche Akademie für Landeskunde, Selbstverlag, Leipzig, 2008, ISBN978-3-88143-078-4
This page is based on this Wikipedia article Text is available under the CC BY-SA 4.0 license; additional terms may apply. Images, videos and audio are available under their respective licenses.