A mud volcano or mud dome is a landform created by the eruption of mud or slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. Mud volcanoes may range in size from merely 1 or 2 meters high and 1 or 2 meters wide, to 700 meters high and 10 kilometers wide. Smaller mud exudations are sometimes referred to as mud-pots.
Hydrate-bearing sediments, which often are associated with mud volcano activity. Source: USGS, 1996.
On top of Gekpatlawuk mud volcano, Western Turkmenistan
Two mud volcanoes on the Taman Peninsula near Taman Stanitsa, Russia
Akpatlawuk mud volcano, western Turkmenistan
A petroleum seep is a place where natural liquid or gaseous hydrocarbons escape to the Earth's atmosphere and surface, normally under low pressure or flow. Seeps generally occur above either terrestrial or offshore petroleum accumulation structures. The hydrocarbons may escape along geological layers, or across them through fractures and fissures in the rock, or directly from an outcrop of oil-bearing rock.
Naturally occurring oil seep near McKittrick, California, United States.
Petroleum seep near the Korňa in northern Slovakia.
Tar "volcano" in the Carpinteria, California, asphalt mine. Oil exudes from joint cracks in the petroliferous shale forming the floor of mine. 1906 photo, U.S. Geological Survey Bulletin 321
Tar bubble at La Brea Tar Pits, California