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Broumov Highlands

Broumov Highlands
View of Božanov
Highest point
PeakKrálovecký Špičák
Elevation881 m (2,890 ft)
Dimensions
Area535 km2 (207 mi2)
Geography
Broumov Highlands in the geomorphological system of the Czech Republic
Countries
Czech Republic, Poland
Hradec Králové
Range coordinates
50°35′N 16°11′E / 50.583°N 16.183°E / 50.583; 16.183
Parent rangeCentral Sudetes
Geology
Rock type(s)Sandstone, marlstone

The Broumov Highlands (Czech: Broumovská vrchovina) are highlands and a geomorphological mesoregion of the Czech Republic. It is located in the Hradec Králové Region. It is a part of the Central Sudetes macroregion and the highest peak is Královecký Špičák at 881 m (2,890 ft) above sea level. Most of the highlands is protected as the Broumovsko Protected Landscape Area.

Geomorphology

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The Broumov Highlands is a mesoregion of the Central Sudetes within the Bohemian Massif. Common landform features include mesas, cuestas and rock towns.[1] The mesoregion is further subdivided into the microregions of Žacléř Highlands, Police Highlands and Meziměstí Highlands.[2]

The highest peaks of the Broumov Highlands are:

  • Královecký Špičák, 881 m (2,890 ft)
  • Ruprechtický Špičák, 880 m (2,887 ft)
  • Szeroka, 845 m (2,772 ft)
  • Mravenčí vrch, 842 m (2,762 ft)[a]
  • Široký vrch, 841 m (2,759 ft)
  • Mravenčí vrch, 840 m (2,756 ft)[a]
  • Kopica, 803 m (2,635 ft)
  • Světlina, 797 m (2,615 ft)
  • Kozina, 796 m (2,612 ft)
  • Čertův vrch, 790 m (2,592 ft)

Geology

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Adršpach-Teplice Rocks

The Broumov Highlands is valuable because there is a great diversity of rocks in a small area. There are terrestrial and marine sedimentary rocks from the Carboniferous, Triassic and Cretaceous periods (sandstone, marlstone), and rocks originating from Permian volcanic activity. Subsequent tectonic uplift and erosion shaped the present-day relief. A common feature in the relief are rock towns modelled in Cretaceous sandstones. The area of the rock towns is known as Adršpach-Teplice Rocks. The Broumov Highlands are also known for underground pseudo-karst phenomena, caves and chasms.[3][4]

Geography

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The Broumov Highlands has an area of 535 km2 (207 sq mi) and an average elevation of 527 m (1,729 ft).[5]

The area is drained mainly by the rivers Ścinawka and Metuje. There are significant reserves of groundwater here, from which the region is supplied with drinking water.[4]

The most populated settlements in the territory are Broumov, Police nad Metují and Žacléř.

Protection of nature

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Broumovské stěny National Nature Reserve

Most of the Broumov Highlands is protected as the Broumovsko Protected Landscape Area due to their unique geological and ecological value. The protected landscape area was established in 1991 and borders the Stołowe Mountains National Park in Poland. The wider area of 570 km2 (220 sq mi) is also protected as the Broumovsko National Geopark.[4]

The most valuable part of the Broumov Higlands and the Broumovsko Protected Landscape Area are the national nature reserves of Broumovské stěny and Adršpach-Teplice Rocks.

Notes

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  1. 1 2 two different peaks with the same name

References

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  1. "Charakteristika oblasti: Horniny a reliéf". CHKO Broumovsko (in Czech). Nature Conservation Agency of the Czech Republic. Retrieved 2026-04-28.
  2. "Geomorfologické oblasti, celky a podcelky v ČR - dnes přijímané geomorfologické členění České republiky". Treking.cz (in Czech). Retrieved 2026-04-28.
  3. Ostradecká, Kateřina (2015-02-09). "Geologie Broumovska je mimořádná z více důvodů, říká speleolog Jiří Kopecký". Novinky.cz (in Czech). Retrieved 2026-04-28.
  4. 1 2 3 "Geoparky" (in Czech). Nature Conservation Agency of the Czech Republic. Retrieved 2026-04-28.
  5. "Geomorfologické celky ČR podle rozlohy – v Čechách, na Moravě a ve Slezsku v km2". Treking.cz (in Czech). 2009-12-15. Retrieved 2026-04-28.
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