Vértes Hills

The area of the Vértes occupies 314 km² (121 sq mi). It is about 30 km long and 10–15 km wide. The average altitude is above sea level is 350 meters; its highest points are 487 m (Nagy-Csákány), 480 m (Körtvélyes) and 479 m (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 (1260 km), but in spite of this spring and rivers are very rare in the mountain. Yearly sunshine duration is around 1950–2000 hours. The average annual temperature above the height of 350 meters is 8.5 °C (in January, −3 °C). The average annual precipitation is between 600 and 700 millimeters. In winter the land is usually snow-covered.

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).

• 
  Vitány castle
• 
  Várgesztes castle
• 
  Csákvár
• 
  Gánt - bauxite mine
• 
  Csókakő

Béni Kornél–Viszló Levente: A Vértes hegység és környéke, 1996 ISBN 963-04-6683-X

• Transdanubian Mountains
• Geography of Hungary

• KirándulóBlog - Lőrinci Nagykönyvtár túraköre / Farkas Ferenc at the Wayback Machine (archived November 12, 2007)
• Geology of the Carpathian Region, p. 325, at Google Books