LATE-CAINOZOIC VOLCANISM IN THE NORTH AREA OF EASTERN CAUCASUS OROGEN (DAGHESTAN)
The article is devoted to detection of volcanic ashes on the territory of Central Daghestan in the limits of Daghestan Wedge structure. The accompanying processes (formation of red color rocks, carry out of clays of grey, green and grey color, bulks of silica etc.) are the evidence of local origin of ashes, and therefore, of late-Cainozoic volcanism existence on the territory of Eastern Caucasus (Daghestan).