Latest Mud volcano Stories
A powerful earthquake that struck the southwestern province of Baluchistan, Pakistan Tuesday afternoon, killing hundreds of people, has given rise to a new island off the coast of the country's Gwadar Port.
In 2006 the island of Java, Indonesia was struck by a devastating earthquake followed by the onset of a mud eruption to the east, flooding villages over several square kilometers and that continues to erupt today.
Scientists said Thursday that a mud volcano in Indonesia is responsible for displacing more than 13,000 families, and shows no sign of stopping for the better part of the next quarter century.
New data provides the strongest evidence to date that the world's biggest mud volcano, which killed 13 people in 2006 and displaced thirty thousand people in East Java, Indonesia, was not caused by an earthquake.
U.S. scientists say they've completed the first study of microbes living in deep sea volcanoes, where conditions may resemble extraterrestrial environments. The Gulf of Mexico study was led by Professor Samantha Joye of the University of Georgia.
Scientists study how microbes survive and thrive in deep, dark, noxious, oxygen-depleted, super-salty ecosystems that may resemble primordial environments.
The answer to whether or not Mars is hospitable to life could lie beneath the surface, experts from NASA's Johnson Space Center in Houston said on Thursday.
World scientists conclude drilling, not earthquake, was the cause of east Java mud volcano at international debate.
A linear string of mud pots and mud volcanoes suggest surface evidence for a southern extension of the San Andreas Fault that runs through the Salton Sea, according to a paper published in the August issue of the Bulletin of the Seismological Society of America (BSSA).
A mud-spewing fissure in the ocean floor has given birth to a tiny Caribbean island and is posing a threat to small boats.
Scoria is a term used by geologists to describe an igneous rock containing many gas bubbles, or vesicules. Scoria forms when magma rich in dissolved gases is vented. As the magma encounters lower pressures, the gasses are able to escape and form bubbles. These bubbles are trapped when the magma cools and solidifies. Volcanic cones of scoria can be left behind after eruptions, usually forming mountains with a crater at the summit. An example is Mount Wellington, Auckland in New Zealand....
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