Hold on to your hats, because
scientists have found more evidence that Earth tips over from time to time. We know that the continents are moving slowly due to plate tectonics, but continental drift only pushes the tectonic plates past each other. It has been debated for the past few decades whether the outer, solid shell of the Earth can wobble about, or even tip over relative to the spin axis. Such a shift of Earth is called "true polar wander", but the evidence for this process has been contentious. New research published in
Nature Communications, led by the Earth-Life Science Institute (ELSI) at Tokyo Institute of Technology's Principle Investigator Joe Kirschvink (also a Professor at Caltech) and Prof. Ross Mitchell at the Institute of Geology and Geophysics in Beijing, provides some of the most convincing evidence to date that
such planetary tipping has indeed occurred in Earth's past.

© Ross Mitchell
Figure 1.
Scaglia Rossa Limestone exposed near Furlo, Italy, in the Northern Apennine Mountains. Limestone at this locality accumulated on the bottom of a shallow sea, in an arm of the ancient Mediterranean ocean nearly 85 million years ago, during what is called Late Cretaceous time.
True polar wander bears some dissecting. The Earth is a stratified ball, with a solid metal inner core, a liquid metal outer core, and a solid mantle and overriding crust at the surface which we live on. All of this is spinning like a top, once per day. Because the Earth's outer core is liquid, the solid mantle and crust are able to slide around on top of it. Relatively dense structures, such as subducting oceanic plates and massive volcanoes like Hawaii, prefer to be near the Equator, in the same way that your arms like to be out to your side when you are spinning around in an office chair.
Despite this wandering of the crust, Earth' magnetic field is generated by electrical currents in the convecting liquid Ni-Fe metal of the outer core. On long time scales, the overlying wander of the mantle and crust does not affect the core, because those overlying rock layers are transparent to Earth's magnetic field. In contrast, the convection patterns in this outer core are actually forced to dance around Earth's rotation axis, which means that the overall pattern of Earth's magnetic field is predictable, spreading out in the same fashion as iron filings lining up over a small bar magnet. Hence, these data provide excellent information about the direction of the North and South geographic poles, and the tilt gives the distance from the poles (a vertical field means you are at the pole, horizontal tells us it was on the Equator). Many rocks actually record the direction of the local magnetic field as they form, in much the same way that a magnetic tape records your music. For example, tiny crystals of the mineral magnetite produced by some bacteria actually line up like tiny compass needles, and get trapped in the sediments when the rock solidifies. This, "fossil" magnetism can be used to track where the spin axis is wandering relative to the crust.
Comment: In Of Flash Frozen Mammoths and Cosmic Catastrophes , Pierre Lescaudron details just how ''woolly' mammoths were perhaps not so woolly after, that they were likely were temperate creatures, not polar ones, and what these points, along with various other fascinating insights and theories, perhaps reveals about mammoths, their demise, and the great shifts our planet has undergone over the last 15,000 years: See also:
- The Seven Destructive Earth Passes of Comet Venus
- Last mammoths plagued by genetic defects
- 26,000 year old, most northerly settlement of Palaeolithic era found on Kotelny island in the Arctic, evidence of butchered mammoth bones found
- Evolution of extinct miniature elephants of Sicily revealed through first-ever DNA recovered
- Woolly mammoths lived alongside first humans in New England
- 45,000 year old lion statuette found in Denisova Cave may be world's oldest
- America Before by Graham Hancock - Book review
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