Geological studies of Krivenkovskoe field
27.03.2015
Mountain Neveb composed of Upper Jurassic and Lower Cretaceous deposits, which began to be studied further in the early 20th century. One of the first researchers of the geology of the region in the 20th century was the future director of the Geological Committee of Russia - VSEGEI (1914-1917.) well known geologist K.I. Bogdanovich, who considered that the deposits belong to the upper Callovian deposits or Lower Oxfordian (border deposits Middle and Upper Jurassic), based on data collected in 1906 under.Interesting Geology
27.03.2015
Mountain Web is located on the south-western outskirts of Krivenkovckaya village Tuapse district of the Krasnodar Territory. Composed of rocks of two of the most interesting geological periods - Jurassic and Cretaceous. A period when the planet - on land and under water was dominated by huge reptiles while shallow harbor and reefs were swarming with ammonites and Belemnites, the remains of which we find today in the form of fossilized shells. It was then that the sediment in the bottom of the Tethys Ocean formed rock mountain Neveb, standing proudly on the southern slope of the Greater Caucasus.