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Posts tagged ‘geology’

the Sistine Chapel of crystals…

Giant Crystal Cave Comes to Light

National Geographic News, April 9, 2007—Geologist Juan Manuel García-Ruiz calls it “the Sistine Chapel of crystals,” but Superman could call it home.

A sort of south-of-the-border Fortress of Solitude, Mexico‘s Cueva de los Cristales (Cave of Crystals) contains some of the world’s largest known natural crystals—translucent beams of gypsum as long as 36 feet (11 meters).

How did the crystals reach such superheroic proportions?

In the new issue of the journal Geology, García-Ruiz reports that for millennia the crystals thrived in the cave’s extremely rare and stable natural environment. Temperatures hovered consistently around a steamy 136 degrees Fahrenheit (58 degrees Celsius), and the cave was filled with mineral-rich water that drove the crystals’ growth.

Modern-day mining operations exposed the natural wonder by pumping water out of the 30-by-90-foot (10-by-30-meter) cave, which was found in 2000 near the town of Delicias (Chihuahua state map). Now García-Ruiz is advising the mining company to preserve the caves.

“There is no other place on the planet,” García-Ruiz said, “where the mineral world reveals itself in such beauty.”

Read the full story of the new discovery.

—Stefan Lovgren and Ted Chamberlain

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beauty, nature, science & technology

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rockin’ through the ages

The Earth is very old—4.5 billion years or more according to scientific estimates. Most of the evidence for an ancient Earth is contained in the rocks that form the Earth’s crust. The rock layers themselves—like pages in a long and complicated history—record the events of the past, and buried within them are the remains of life—the plants and animals that evolved from organic structures that existed 3 billion years ago.

Also contained in rocks once molten are radioactive elements whose isotopes provide Earth with an atomic clock. Within these rocks, “parent” isotopes decay at a predictable rate to form “daughter” isotopes. By determining the relative amounts of parent and daughter isotopes, the age of these rocks can be calculated.

Thus, the scientific evidence from rock layers, from fossils, and from the ages of rocks as measured by atomic clocks attests to a very old Earth.

See USGS Fact Sheet 2007-3015 at http://pubs.usgs.gov/fs/2007/3015/ for ages of geologic time periods. Ages in the spiral have been rounded from the age estimates in the Fact Sheet. B.Y., billion years; M.Y., million years. For more information, see the booklet on Geologic Time at http://pubs.usgs.gov/gip/geotime/.

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nature

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