Moravian-Silesian Beskids
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Moravian-Silesian Beskids
Moravian-Silesian Beskids
Moravskoslezské Beskydy
Smrk (Moravian-Silesian Beskids, CZE) - mountain in early spring.jpg
Smrk mountain in early spring
Highest point
PeakLysá hora
Elevation1,323 m (4,341 ft)
Coordinates49°32?45?N 18°26?51?E / 49.54583°N 18.44750°E / 49.54583; 18.44750Coordinates: 49°32?45?N 18°26?51?E / 49.54583°N 18.44750°E / 49.54583; 18.44750
Geography
Moravian-Silesian Beskids is located in Czech Republic
Moravian-Silesian Beskids
Moravian-Silesian Beskids
CountriesCzech Republic and Slovakia
States/ProvincesMoravian-Silesian (Czech Repub.) and ?ilina (Slovakia)
Parent rangeWestern Beskids, Western Carpathians
Geology
OrogenyAlpine
Age of rockMiocene
Type of rockGodulian sandstone

The Moravian-Silesian Beskids (Czech: About this soundMoravskoslezské Beskydy, Slovak: Moravsko-sliezske Beskydy) is a mountain range in the Czech Republic with a small part reaching to Slovakia. It lies on the historical division between Moravia and Silesia, hence the name. It is part of the Western Beskids, which is in turn part of the Outer Western Carpathians.

Geography

The mountains were created during the Alpine Orogeny in the Cenozoic. Geologically, they consist mainly of flysch deposits. In the north, they steeply rise nearly 1,000 m (3,300 ft) over a rather flat landscape; in the south, they slowly merge with the Javorníky. In the south-west, they are separated from the Vsetínské vrchy by the Ro?novská Be?va valley; in the north-east, the Jablunkov Pass separates them from the Silesian Beskids.

?eladenka River in Moravian-Silesian Beskids

The highest point is Lysá hora mountain at 1,323 m (4,341 ft), which is one of the rainiest places in the Czech Republic with around 1,500 mm (59 in) of precipitation a year. Many legends are bound to Radho Mountain, 1,129 m (3,704 ft), which is one of the most visited places in the mountains together with the nearby Pustevny resort.

Smrk, with a height of 1,276 m (4,186 ft), is the second highest summit of the range. Its northern slope steeply rises from the surrounding lowlands and is separated from the rest of the mountains by the deep Ostravice River (in the east) and ?eladenka (in the west) river valleys; in the south, it merges in the lower Zadní hory (i.e. Rear mountains) area.

The Moravian-Silesian Beskids create the largest part of the Beskydy Landscape Protected Area (Czech: Chrán?ná krajinná oblast Beskydy or Czech: CHKO Beskydy for short). The mountains are 80% forested, though mainly by plantations of spruce which were in some parts severely damaged by emissions from the Ostrava industrial region. Originally, the mountains were covered by mixed forest with dominant beech which are preserved in many places. Recently, permanent occurrence of all three large Central European carnivores - lynx, bear and wolf - have been confirmed in the area.

?ance Reservoir on the Ostravice River in the Moravian-Silesian Beskids

There are many popular holiday resorts for both winter and summer activities, with centers in the towns under the mountains (Frýdlant nad Ostravicí, Fren?tát pod Radho?t?m, Ro?nov pod Radho?t?m) and also in smaller resorts, hamlets and chalets throughout the mountains, especially on the ridges. Parts of two euroregions, the Beskydy/Beskidy and Tínské Slezsko/?l?sk Cieszy?ski, reach into the Moravian-Silesian Beskids.

References

  • Ludvík, Marcel (1987). Beskydy, Turistický pr?vodce ?SSR. Praha: Olympia. 27-031-87.
  • Rohlík, Ji?í (2001). Moravskoslezské Beskydy, Soubor turistických map 1:50 000. Praha: TRASA, s.r.o. ISBN 80-85999-29-3.
  • CHKO Beskydy Management. "CHKO Beskydy". Retrieved .

  This article uses material from the Wikipedia page available here. It is released under the Creative Commons Attribution-Share-Alike License 3.0.

Moravian-Silesian_Beskids
 



 

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