Vértes is a mountain range in north-western Hungary, in the Central Transdanubian region, between the ranges Bakony and Gerecse. The Vértes Mountains are part of the Transdanubian Mountains.
The area of the Vértes occupies 314km2 (121sqmi). It is about 30km long and 10–15km wide. The average altitude is above sea level is 350meters; its highest points are 487m (Nagy-Csákány), 480m (Körtvélyes) and 479m (Csóka-hegy). Geologically the Vértes constitute a fairly uniform structure. On the surface of the entire mountain there are no older rocks than those of the mid-Triassic. The main rock is dolomite—CaMg(CO3)2—from the upper Triassic. All the layers are ancient marine deposits.
The Vértes possesses a well-developed valley network (1260km), but in spite of this spring and rivers are very rare in the mountain. Yearly sunshine duration is around 1950–2000hours. The average annual temperature above the height of 350meters is 8.5°C (in January, −3°C). The average annual precipitation is between 600 and 700millimeters. In winter the land is usually snow-covered.
History
According to a legend documented in mediaeval Hungarian chronicles, the Vértes mountains were named after a historical incident: during the unsuccessful campaign of 1051–1052, the withdrawing German troops of Henry III, emperor of the Holy Roman Empire, scattered their armours to ease their escape through the mountains; hence the name Vértes (cf. vért, Hungarian for armour).
Gallery
Vitány castle
Várgesztes castle
Csákvár
Gánt - bauxite mine
Csókakő
Sources
Béni Kornél–Viszló Levente: A Vértes hegység és környéke, 1996 ISBN963-04-6683-X
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