It's a bit of fun, even if for the vast majority the answer was "somewhere in an ocean". But would it be possible to dig ...
Over the past 250 million years, periods when coral reef growth has peaked have coincided with big rises in sea temperatures ...
Researchers found that eroded lava rubble beneath the South Atlantic can trap enormous amounts of CO2 for tens of millions of ...
Smithsonian Magazine on MSN
For More Than 250 Million Years, Coral Reefs Have Had a Major Influence on Earth’s Changing Climate
The planet has been flipping between two main modes of carbon recovery depending on the state of coral reefs, new research ...
The Express Tribune on MSN
What caused the 5.2-magnitude earthquake that jolted Karachi?
Expert urges quake preparedness for Karachi, says city sits near three-plate junction and multiple fault lines ...
Interesting Engineering on MSN
How an invisible fire beneath the surface is generating clean power day and night
Geothermal energy delivers constant power using heat from beneath the Earth. Here’s how it works and why it matters.
One of the oldest unsolved riddles in planetary science concerns the origin of the moon. Over a century ago, George Darwin ...
The Santa Monica and San Gabriel mountains formed millions of years ago. Within both of them lies a fascinating world of rocks, gemstones, crystals and minerals. Here's how to start identifying them.
China begins drilling a six-mile-deep scientific well named Shendi Take 1 to explore the depths of the Earth and its secrets.
Netflix’s shocking $72 billion bid to buy Warner Bros. and HBO is the rare corporate mega-merger that can shift the tectonic plates of an entire industry and permanently change the way all of its ...
The discovery of organisms that have been alive for many thousands of years requires a revolution in how we understand life ...
Map of significant earthquakes (greater than magnitude 4) in the UK Credit: British Geological Survey/UKRI News of a 3.3-magnitude earthquake in the north-west of England overnight may have left you ...
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