Wednesday, April 23, 2014

The Biggest Mysteries of Our Planet

When the first Earth Day was held in 1970, geologists were still putting the finishing touches on plate tectonics, the model that explains how the Earth's surface takes shape. More than 40 years later, many riddles still remain when it comes to our planet.
An image of the Earth taken by the Russian weather satellite Elektro-L No.1.
For instance, dozens of spacecraft have mapped the surface of Mars more accurately than Earth's ocean depths. For today's Earth day, here are some of Earth's biggest unsolved mysteries.
1. Where did the water come from?
Scientists think Earth was a dry rock after it coalesced 4.5 billion years ago. So where did this essential chemical, H2O, come from? Perhaps an interstellar delivery system, in the form of massive impacts about 4 billion years ago. Pummeled by icy asteroids, the Earth could have replenished its water reservoirs during the period, called the Late Heavy Bombardment. But the beginnings of Earth's water are shrouded in mystery because so little rock evidence remains from this time period.  

2. What's down there in the core?
The stuff of legend and lore, Earth's core has long fascinated writers as well as scientists. For a while, the composition of Earth's unreachable core was a solved mystery … at least in the 1940s. With meteorites as proxy, scientists gauged the planet's original balance of essential minerals, and noted which were missing. The iron and nickel absent in Earth's crust must be in the core, they surmised. But gravity measurements in the 1950s revealed those estimates were incorrect. The core was too light.
Today, researchers continue to guess at which elements account for the density deficit beneath our feet. They're also puzzled by the periodic reversals in Earth's magnetic field, which is generated by the outer core's flowing liquid iron.

3. How did the moon get here?
Did a titanic collision between the Earth and a Mars-size protoplanet form the moon? There's no universal consensus on this giant impactor theory, because some details don't pan out. For example, the chemical composition of both rocky bodies matches so closely it suggests the moon was born from Earth, not a separate impactor. But a fast-spinning young Earth could have flung off enough molten rock during impact to form a chemically similar moon, other models suggest. And is there a relationship between these events and the rise of life on Earth, wondered Kevin McKeegan, a geochemist at the University of California, Los Angeles. "These are important planetary issues as we consider the possible histories of Earth-like exoplanets in the habitable zone," McKeegan said. 

4. Where did all the oxygen come from?
We owe our existence to cyanobacteria, microscopic creatures that helped to radically transform Earth's atmosphere. They pumped out oxygen as waste, and filled the skies with oxygen for the first time about 2.4 billion years ago. But rocks reveal oxygen levels cruised up and down like a roller coaster for 3 billion years, until they stabilized around the Cambrian Period about 541 million years ago. So did bacteria spike the air, or was there another contributing factor? Understanding the shift to an oxygen-rich Earth is a key factor in decoding the history of life on our planet.
5. Will we ever predict earthquakes?
At best, statistical models can tease out a forecast of future earthquake probability, similar to weather experts who warn of coming rain. But that hasn't kept people from trying to predict when the next one will hit — with no success. Even the biggest experiment failed by 12 years, when geologists predicted an earthquake at Parkfield, Calif., by 1994, and set up instruments to catch the coming temblor. The actual quake hit in 2004. One of the biggest hurdles is that geologists still don't understand why earthquakes start and stop. But there have been advances in predicting aftershocks and man made earthquakes, such as those linked to waste water injection wells (as used in fracking).
article taken from Live Science (original link)



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