One of the sites of the Berca Mud Volcanoes, this site has generally has fewer tourists, andmore volcanoes than at Paclele Mari. The mud volcanoes are caused by gases that flow from 3,000 metres deep towards the surface, through the underground layers of clay and water. They push up underground salty water and mud, until they overflow through the mouths of the volcanoes, where the gas emerges as bubbles. The mud constantly flows and changes the landscape causing amazing troughs and canals. Also since you're walking on a crust of dried mud access is only permitted on dry days.
📍 Explore on PIXEO Map →
scenicnatureruralgeological
