The changes are most visible in the Afar region of northeastern Ethiopia. Scientists say that the Gulf of Aden and the Red ...
A study on tectonic plates that converge on the Tibetan Plateau has shown that Earth's fault lines are far weaker and the ...
WCBD Charleston on MSN
Examining South Carolina’s earthquake history and activity
CHARLESTON, S.C. (WCBD) – With recent earthquakes felt in parts of Dorchester County and the Midlands in recent weeks, we ...
All around the world, from the Red Sea to the deep ocean ridges of the Atlantic, lurk more than a dozen geological misfits.
It turns out that continental breakups are just as messy as human ones, with the events leaving fragments scattered far from home ...
Times-Standard on MSN
Lori Dengler | The sea is not level
"The ocean surface is definitely not flat. It is constantly changing as wind, waves and swells produce surface undulations, daily tidal fluctuations raise and lower the average height." ...
What are the main theories about the true nature and location of Atlantis? Was it on Sardinia, Crete, Africa, or was it just an allegory?
Morning Overview on MSN
NASA supercomputer reveals chilling timeline for life on Earth
Earth’s oxygen-rich atmosphere, the very thing that allows complex life to exist, may not last forever. Coupled biogeochemistry and climate simulations estimate that the planet’s breathable air could ...
Empire Sports Media on MSN
7 Mets prospects appear in Baseball Prospectus’ list of 101: Get to know them all
Forget the pinstripes across town or the big-spending Dodgers for a second. If you want to see where the real […] ...
Green Matters on MSN
Ocean Fossils Keep Turning Up on Top of Mount Everest. Scientists Say There’s a Good Reason for It
Conspiracy theories on the internet attribute these fossils to everything from a 'great flood' to a prank of Gandalf monster.
Precious metals may be escaping from the planet’s core. This hotly debated subject could help us understand Earth’s evolution and determine whether life exists elsewhere in the Universe ...
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