Csobanc

Csobanc is a hill in the Tapolca Basin, Hungary. Csobanc is one of the highlights of the region. Similar to the other hills inside the vicinity, it is of volcanic starting place. These hills are known as “Witness Hills”. The expression originates from the fact that those hills “witnessed” the decrease of the land surface level during volcanic activity millions of years ago. They maintain the original surface for the reason that Pliocene duration. Csobanc is one of the unique and atypical monadnocks of Tapolca Basin. It is a end result of basalt volcanism three.Five million years in the past.

Numerous rare habitats in want of protection were preserved because of the tremendously secluded and undisturbed area. The herbal assets of Csobanc granted the hill increased safety from the Balaton Uplands National Park and the Bakony-Balaton Geopark. Relatively sheltered habitat due to its inaccessible region along the rims of the plateau. Sensitive to being disturbed and trodded on. Paragliding can be a tremendous hazard to the habitat and its function species including the northern rock-cress and the particular livelong saxifrage, each growing at the northern rock partitions.