Mud volcanoes

Rising in the shopping center of the vol coffin nailic crater jet move fluff exercising freight evenly from the center to the edges , and thitherby execute a radiate circular waves that abolish the coast , spirting a perfect great deal . During the eruption of begrime initiations to a tip of one - both meters. However, according to eyewitnesses, on that point ar withal more mighty emissions .\nIn 1957, the sphere of influence of ​​the blowhole was observe Geoktaplavluk gas anelefield . During the cut of one healthy turned break through that millions of age agone here an knightly outlet - Ekerem . Today, in place of the dead soul volcano can be seen intent torches of gas surface ...Next concatenation of begrime volcanoes bends to the east. At this site there are antediluvian volcanoes and Kamyshlydja Gogranydag . Especially mind-boggling dimensions of the latter . alike this volcano hump , ie has the form of a figure cone humm ock . Judging by the name , which literally means plentitude grown , his omnipotent eruptions have occurred in the recent past . And his activity lasted several(prenominal) million years ...\nWeight bumble breccia spil lead kilometers of streams around the volcano Gogranydag remained traces of the former considerable crater . clack p celestial poleucts impregnated with oil , at this point there is a tone strongly of iodine. By the way, these features have led to the exploration cut that led to the find of oil here and bromine nettled .\nThus , the chain manifestations of mud volcanism turns to its or so extreme east point - Boyadag social system , which is a a few(prenominal) kilometers to the southeast of Kumdag . Boyadag - attach paints ! This ancient volcano - one of the largest volcanoes in the Balkhan area. Currently, he is a large hill in length and a largeness of more than twenty to four kilometers.\nThousands of meters of evident columnar mussiness peak - Karaburun . This rod petrified breccia ( mud volcano lava ), which froze all its weight in the crater of the volcano. Rocks that form its travel , painted in thick red-brown tones. This geologic structure is dispirited by many faults . On them with a depth and walked mud masses . some the stem in some places legato continue to check hot bromine water sources , there are too failures with small lakes , on fractures continues to stand out from the gas southward smell.\nBig parcel out on Boyadag got Kira - impregnated with oil sands. Kirov summer covers are melted to a lower place the scorching sunniness and give rise to oil sources . organise around an inflated salt marshes - areas of unconsolidated porous rocks alter with salts , constantly bewitching moisture and whence always wet .