8/28/2019 1407

Asiab geosite

Old Mill waterfall is located in 35 km east of Jolfa city, along the Jolfa-Siahrood road. In this location, near an abandoned watermill, there is a travertine spring that flows from a cleft in the rocks. The cleft, in fact, is the entry of a cave that long 150 m and end to a chamber where is the main appearance of the spring. Its water stream passing close to the abandoned watermill end to a waterfall with a height of 10 m, where dense hydrophilic plants are grown.

Beautiful folding stretched in Cretaceous flysch deposits on the left side slopes of Asiyab-kharabe valley. These chevron folds in the alternate sandstone-shale layers provide a wonderful perspective and attract the interest and curiosity of people. Fossils and various sedimentary structures in the base of sandstone beds complete this stunning picture, phenomena that represent bioactivity in the Neotethys seabed living near 70 million years ago and probably are ancestors of some of the present day animals.