Finally, a Solid Look at Earth's Core
By Robert Roy Britt, LiveScience Senior Writerposted: 14 April 2005 02:04 pm ET
Scientists have long thought Earth's core is solid. Now they have some solid evidence.
The core is thought to be a two-part construction. The inner core is solid iron, and that's surrounding by a molten core, theory holds. Around the core is the mantle, and near the planet's surface is a thin crust -- the part that breaks now and then and creates earthquakes.
The core was discovered in 1936 by monitoring the internal rumbles of earthquakes, which send seismic waves rippling through the planet. The waves, which are much like sound waves, are bent when they pass through layers of differing densities, just as light is bent as it enters water. By noting a wave's travel time, much can be inferred about the Earth's insides.
Yet for more than 60 years, the solidity of the core has remained in the realm of theory.
A study announced today involved complex monitoring of seismic waves passing through the planet. The technique is not new, but this is the first time it's been employed so effectively to probe the heart of our world.
First, some jargon:
P is what scientists call the wave
K stands for the outer core
J is the inner core
Path of a PKJKP wave.
© Science
So a wave that rolls through it all is called PKJKP.
An earthquake sends seismic waves in all directions. The surface waves are sometimes frighteningly obvious. Seismic waves passing through the mantle and traversing much of the planet's interior are routinely studied when they reach another continent. But no PKJKP wave has ever been reliably detected until now.
Aimin Cao of the University of California-Berkeley and colleagues studied archived data from about 20 large earthquakes, all monitored by an array of German seismic detectors back in the 1980s and '90s.
The trick to detecting a PKJKP wave is in noting the changes it goes through as it rattles from one side of the planet to the other. What starts out as a compression wave changes to what scientists call a shear wave (explanations and animations of these are here).
"A PKJKP traverses the inner core as a shear wave, so this is the direct evidence that the inner core is solid," Cao told LiveScience, "because only in the solid material the shear wave can exist. In the liquid material, say water, only the compressional wave can travel through."
The arrival time and slowness of the waves agree with theoretical predictions of PKJKP waves, which indicates a solid core. The results were published today online by the journal Science.
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What's Down There
The Earth's radius is about 4,000 miles (6,400 kilometers). The main layers of its interior are in descending order: crust, mantle and core.
The crust thickness averages about 18 miles (30 kilometers) under the continents, but is only about 3 miles (5 kilometers) under the oceans. It is light and brittle and can break. In fact it's fractured into more than a dozen major plates and several minor ones. It is where most earthquakes originate.
The mantle is more flexible - it flows instead of fractures. It extends down to about 1,800 miles (2,900 kilometers) below the surface.
The core consists of a solid inner core and a fluid outer core. The fluid contains iron, which, as it moves, generates the Earth's magnetic field. The crust and upper mantle form the lithosphere, which is broken up into several plates that float on top of the hot molten mantle below.
SOURCE: LiveScience reporting
http://www.livescience.com/environment/050414_earth_core.html
