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A research team at the University of Illinois (UI) has just used the rumbles from quakes to more closely examine the core of our planet, and what they found there was quite a surprise. It seems our Earth's core has another core that measures about half the diameter of the original core.
What demarcates this "inner-inner core" is that the iron crystals it contains are oriented on an east-west axis, unlike the iron crystals in the "outer-inner core" which organize along a north-south axis.
"People have noticed differences in the way seismic waves travel through the outer parts of the inner core and its innermost reaches before, but never before have they suggested that the alignment of crystalline iron that makes up this region is completely askew compared to the outermost parts," said Prof. Simon Redfern from the University of Cambridge.
"If this is true, it would imply that something very substantial happened to flip the orientation of the core to turn the alignment of crystals in the inner core north-south as is seen today in its outer parts,"
... Can you explain to me the practical application of this?
originally posted by: Indigent
a reply to: PsychoEmperor
... Can you explain to me the practical application of this?
Scientist analyzed in a different way quake data and found out the solid ball we think the core was is actually 2 balls, not really practicals applications or anything, its like going from standard definition to HD and seeing all the wrinkles in actors, nothing new is going on, just better technology allow us to see more.
originally posted by: stirling
Yep exactly what went through my mind too....
Perhaps this opposite alignment has other purposes not yet understood....
Magnetic fields produce electricity....
Maybe even some influence upon gravity?
Or a stabilising effect on the mantle?
IDK, but there are ramifications here...
The inner core of the Earth may be melting, scientists now find.
This melting could actually be linked to activity at the Earth's surface, the researchers said, and added that the discovery could help explain how the core generates the planet's magnetic field.
As the Earth cools from the inside out, the molten outer core is slowly freezing. This is leading the solid inner core to grow at a rate of approximately 1 millimeter per year. However, scientists now find that the inner core might be melting at the same time. "The standard view has been that the inner core is freezing all over and growing out progressively, but it appears that there are regions where the core is actually melting," said researcher Sebastian Rost, a seismologist at the University of Leeds in England. "The net flow of heat from core to mantle ensures that there's still overall freezing of outer core material and it's still growing over time, but by no means is this a uniform process." As the Earth's interior cools, relatively hot and cold matter churns around inside the planet, a process known as convection. The roiling of material in the core, coupled with the spinning of the Earth, is what generates the planet's magnetic field.
For instance, when it comes to large regions under Africa and the Pacific where the lowermost mantle is hotter than average, the outer core below those areas can become hot enough to start melting the inner core. On the other hand, beneath seismically active regions around the so-called "Ring of Fire"— a zone encircling the Pacific high in volcanic and earthquake activity — the cold remnants of oceanic plates sucked to the bottom of the mantle are drawing a lot of heat from the core, helping it freeze.
These findings suggest "that the whole dynamics of the Earth's core are in some way linked to plate tectonics, which isn't at all obvious from surface observations," Mound said.
This model could also explain seismic anomalies past research detected that have suggested there is a dense layer of liquid surrounding the inner core. "The localized melting theory could also explain other seismic observations — for example, why seismic waves from earthquakes travel faster through some parts of the core than others," Rost said.
"The origins of Earth's magnetic field remain a mystery to scientists," Mound noted. "If our model is verified, it's a big step towards understanding how the inner core formed, which in turn helps us understand how the core generates the Earth's magnetic field."
Earthquakes (and nuclear tests) cause seismic waves that travel through the Earth's interior, but these waves travel at different speeds depending on what kind of material they are traveling through. By having listening posts scattered around the planet, we can deduce what layers the Earth's interior to possess based on how long it takes for these waves to reach the listening post from the earthquake that produced them. We then can match the speed of these seismic waves with materials we are familiar with and identify what the Earth's interior is made of - at least in theory.
originally posted by: Darkblade71
Is it just me?
That kind of reminds me of a gyroscope the way the out core and inner core are facing n/s e/w.
originally posted by: Darkblade71
That kind of reminds me of a gyroscope the way the out core and inner core are facing n/s e/w.
He stretcheth out the north over the empty place, and hangeth the earth upon nothing.
Job 26:7