ScienceIQ.com

The Mineral Chalcedony

Chalcedony is a catch all term that includes many well known varieties of cryptocrystalline quartz gemstones. They are found in all 50 States, in many colors and color combinations, and in sedimentary, igneous, and metamorphic rocks. Chalcedony includes carnelian, sard, plasma, prase, bloodstone, onyx, sardonyx, chrysoprase, thundereggs, agate, ...

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TheMineralChalcedony
Engineering

How Many Cows Does It Take To String A Tennis Racquet?

How many cows does it take to string a tennis racquet? According to Professor Rod Cross of the University of Sydney, an expert on the physics and technology of tennis, the answer is 3. Many top ... Continue reading

TennisRacquet
Engineering

The Right Stuff for Super Spaceships

Revolutions in technology - like the Industrial Revolution that replaced horses with cars - can make what seems impossible today commonplace tomorrow. ... Continue reading

SuperSpaceships
Biology

Did You Smell Something?

There's not a moment of our lives when smells -- or, more precisely, odor molecules -- aren't impacting our brain. It's been estimated that it takes at least 40 molecules of a given odor for us to be ... Continue reading

Smell
Astronomy

Two Face? Absolutely!

During the Viking missions to Mars in the mid 1970s, the planet was imaged from orbit by the Viking 1 and 2 Orbiters. These spacecraft returned images of regions of the planet that, while similar to ... Continue reading

TwoFaceAbsolutely

Devils Postpile National Monument

DevilsPostpileNationalMonumentEstablished in 1911 by presidential proclamation, Devils Postpile National Monument protects and preserves the Devils Postpile formation, the 101-foot Rainbow Falls, and the pristine mountain scenery. The Devils Postpile formation is a rare sight in the geologic world and ranks as one of the world's finest examples of columnar basalt. Its columns tower 60-feet high and display an unusual symmetry. Another wonder is in store just downstream from the Postpile at Rainbow Falls, once called 'a gem unique and worthy of its name'. When the sun is overhead, a bright rainbow highlights the spectacular Falls.

Fewer than 100,000 years ago, basalt lava erupted two miles upstream from today's postpile. The lava flowed into the valley and pooled to a depth of 400 feet. The mass of molten lava then began to cool uniformly from top to bottom. As it cooled and contracted, stresses built up in the basalt rock causing it to fracture. Each crack branched when it reached a length of about 10 inches, joining other cracks to form a pattern on the surface of the flow. Under ideal conditions, surface cracks deepened to create the vertical, hexagonal columns you see today. Some 10,000 years ago a glacier flowed down the Middle Fork of the San Joaquin River and overrode the Postpile formation. The moving ice quarried away one side of the postpile, exposing a sheer wall of columns 60 feet high. Evidence of the glacier - the polishing and scratches of glacial ice - remains atop the postpile.

The monument is also a portal to the High Sierra backcountry, with some 75% included in the Ansel Adams Wilderness. At 800 acres, Devils Postpile National Monument may be considered small by some, yet its natural and recreational values abound.