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EXPLORING EARTH'S INNER CORE/MOON

机译:探索地球的内心/月球

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Far below your feet—about 3,219 miles down—is Earth's other moon. Rotating independently of the planet, turning at a different speed within a fluid outer core, this solid, satellite-size sphere holds clues to understanding Earth's earliest history and perhaps even life on the planet. For 300 years, little was added to the pos-tulation that Earth had at its center a homogeneous ball of pure iron. But in the past decade or so, geophysicists, using new data and laboratory simulations, have started to map and analyze it. Every year, more features are discerned from seismic evidence. Scientists don't yet agree on what all the information means, but one thing is becoming dear: Earth's center is far more varied and unusual than anyone had previously thought.
机译:地球的另一个卫星位于您的脚下,下方约3,219英里。这种坚固的,卫星大小的球体独立于行星旋转,在流体外核内以不同的速度旋转,为了解地球最早的历史甚至行星上的生命提供了线索。 300年以来,几乎没有人认为地球的中心有一个均匀的纯铁球。但是在过去的十年左右的时间里,地球物理学家利用新的数据和实验室模拟,开始对其进行制图和分析。每年,从地震证据中都可以发现更多的特征。科学家们尚未就所有信息的含义达成共识,但一件事情变得越来越珍贵:地球中心比以前任何人都想像的更加多样化和异常。

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