By: Charles Q. Choi, OurAmazingPlanet Contributor
Published: 10/08/2012 12:35 PM EDT on OurAmazingPlanet
Published: 10/08/2012 12:35 PM EDT on OurAmazingPlanet
The entire outermost part of Earth may be wandering over the planet's whirling molten core, new research suggests.
Knowing whether the Earth's outer layers
are roaming in this manner is key to understanding the big picture of
how the planet's surface is evolving overall, scientists added.
At various times in Earth's history, the planet's solid exterior — its
crust and mantle layers — has apparently drifted over the planet's
spinning core. To picture this, imagine that a peach's flesh somehow
became detached from a peach's pit and was free to move about over it.
This movement of the Earth's outer layers is known as "true polar
wander." It differs from the motion of the individual tectonic plates
making up Earth's crust, known as tectonic drift, or the motions of
Earth's magnetic pole, called apparent polar wander.
'Hot spot' landmarks
Past research suggested the Earth experienced true polar wander during
the early Cretaceous period that lasted from 100 million to 120 million
years ago. Determining when, in which direction and at what rate true
polar wander is taking place depends on having stable landmarks against
which one can observe the motion of Earth's outer shell, much like one
can tell a cloud is moving by seeing if its position has changed
relative to its surroundings.
Volcanic "hot spots,"
or areas of recurrent volcanism, are one potential landmark. Geologists
have suggested these are created by mantle plumes, giant jets of hot
rock buoying straight upward from near the Earth's core. Mantle plumes
are thought to create long island chains such as the Hawaiian Islands as
they sear tectonic plates drifting overhead.
Scientists have
treated hot spots as stationary features for decades. The idea was that
material surrounding the mantle plumes roil about to form structures
known as convection cells that kept the plumes straight and fixed in
place. [50 Amazing Volcano Facts]
Later on, however, researchers began suggesting that mantle plumes
could move about slightly, caught as they are in the flowing mantle
layer under the crust. "From this point of view, the plumes are expected
to move, bend and get distorted by the 'mantle wind,' resulting in hot spot drift over geologic time," said researcher Pavel Doubrovine, a geophysicist at the University of Oslo in Norway.
By allowing hot spot positions to meander slowly, Doubrovine and his
colleagues have devised computer simulations that better match
observations of the chains of islands created by each hot spot.
"Estimating hot spot drift in the geological past is not a trivial
task," Doubrovine told OurAmazingPlanet. "It requires substantial
modeling efforts."
The scientists then compared the way the
Earth's outermost layers drifted in relation to the planet's axis of
spin. The Earth's magnetic field is aligned with the core's axis of
rotation, and researchers can tell how Earth's magnetic field was
oriented in the past by analyzing ancient rock. Magnetic minerals in
molten rock can behave like compasses, aligning with Earth's magnetic field lines, an orientation that gets frozen in place once the rock solidifies.
Current wandering
Using their simulations and the magnetic field rock record, the
scientists identified three new potential instances of true polar wander
over the past 90 million years. These include two cases in which the
Earth's solid outermost layers traveled back and forth by nearly 9
degrees off Earth's axis of spin
from 40 million to 90 million years ago. Moreover, the researchers
suggest that Earth's outer shell has been undergoing true polar wander
for the past 40 million years, slowly rotating at a rate of 0.2 degrees
every million years.
Researchers suspect true polar wander is
caused by shifting of matter within the mantle, due, for instance, to
variations in temperature and composition. However, "we don't know yet
what specific tectonic events may have triggered the specific episodes
of true polar wander that we identified," Doubrovine said.
These
new details regarding true polar wander could help shed light on what
triggers it. In the future, the researchers plan to look even further in
the past at how the planet's outermost layers have changed. Doubrovine
and his colleagues Bernhard Steinberger and Trond Torsvik detailed their
findings online Sept. 11 in the Journal of Geophysical Research — Solid
Earth.
from: Huffington Post