A Seafloor Shaped by Gas
Off the eastern coast of Borneo, the seabed of the Makassar Strait is an area of mounds and pockmarks. This is the Berau Delta, a region where geologic structures known as mud volcanoes and cold seeps release a steady flow of methane gas from deep within the Earth. These are not volcanoes in the traditional sense; they do not erupt molten lava. Instead, These features carry over-pressured fluids, mud, and gas that have been forced upward through fractures in the rock. The gas erupting is primarily methane.
The mud volcanoes are situated within the Kutai Basin, Indonesia's largest and deepest basin of Tertiary age (from 66 million to 2.58 million years ago). This basin contains sedimentary rock layers up to 15 kilometers thick. Tectonic compression has created a network of faults and anticlines, upward-arching rock folds, across the basin. These geological structures are pathways for gas and fluids trapped in deep, over-pressured shale formations to escape to the seafloor. The source material for the seeps originates miles underground, driven to the surface by immense pressure.