RainmanTime
Super Moderator
Re: Rhythm of Time: Telluric Currents
Thought you might enjoy this article, as the relationship between the earth's core and the telluric currents is certainly a strong one:
http://wattsupwiththat.com/2010/12/17/first-measurement-of-magnetic-field-in-earths-core/
And especially this quote:
<font color="red"> The Earth’s magnetic field is produced in the outer two-thirds of the planet’s iron/nickel core. This outer core, about 1,400 miles thick, is liquid, while the inner core is a frozen iron and nickel wrecking ball with a radius of about 800 miles – roughly the size of the moon. The core is surrounded by a hot, gooey mantle and a rigid surface crust.
The cooling Earth originally captured its magnetic field from the planetary disk in which the solar system formed. That field would have disappeared within 10,000 years if not for the planet’s internal dynamo, which regenerates the field thanks to heat produced inside the planet. The heat makes the liquid outer core boil, or “convect,†and as the conducting metals rise and then sink through the existing magnetic field, they create electrical currents that maintain the magnetic field. This roiling dynamo produces a slowly shifting magnetic field at the surface.
“You get changes in the surface magnetic field that look a lot like gyres and flows in the oceans and the atmosphere, but these are being driven by fluid flow in the outer core,†Buffett said. [/COLOR]
Now, whether those currents contain enough power to warp spacetime (my informed supposition is they are not even close) is another matter altogether.
RMT
Thought you might enjoy this article, as the relationship between the earth's core and the telluric currents is certainly a strong one:
http://wattsupwiththat.com/2010/12/17/first-measurement-of-magnetic-field-in-earths-core/
And especially this quote:
<font color="red"> The Earth’s magnetic field is produced in the outer two-thirds of the planet’s iron/nickel core. This outer core, about 1,400 miles thick, is liquid, while the inner core is a frozen iron and nickel wrecking ball with a radius of about 800 miles – roughly the size of the moon. The core is surrounded by a hot, gooey mantle and a rigid surface crust.
The cooling Earth originally captured its magnetic field from the planetary disk in which the solar system formed. That field would have disappeared within 10,000 years if not for the planet’s internal dynamo, which regenerates the field thanks to heat produced inside the planet. The heat makes the liquid outer core boil, or “convect,†and as the conducting metals rise and then sink through the existing magnetic field, they create electrical currents that maintain the magnetic field. This roiling dynamo produces a slowly shifting magnetic field at the surface.
“You get changes in the surface magnetic field that look a lot like gyres and flows in the oceans and the atmosphere, but these are being driven by fluid flow in the outer core,†Buffett said. [/COLOR]
Now, whether those currents contain enough power to warp spacetime (my informed supposition is they are not even close) is another matter altogether.
RMT