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Multiple craters with dark
haloes. Credit: NASA/JPL/Northwestern University
Jul 31, 2008
More from Mercury
The latest images by the MESSENGER
spacecraft indicate how similar Mercury is to other bodies
in the solar system that have been scarred by electric arcs.
On August 3, 2004, NASA launched the Mercury Surface, Space Environment,
Geochemistry and Ranging (MESSENGER) experiment from the
Cape Canaveral
facility on a 7-year mission to study the solar system’s innermost planet. On
January 14, 2008, MESSENGER performed an initial flyby of
Mercury, coming
within 200 kilometers of the torrid world.
Since interplanetary probes are designed with power conservation in mind, they
use a highly compressed stream of data, which takes time to decode. Some of the
images are as late as February 27, 2008, with more coming. Once the
spacecraft settles into orbit around its target world, a long-term study of
Mercury’s plasmasphere, its magnetic field and its surface materials will begin.
Meanwhile, the geology of Mercury is intriguing to space scientists because it
provides them with a number of “mysteries” and “processes that have yet to be
understood.” Complex
chains of craters and melted pits extend outward from terraced depressions
over 60 kilometers wide. The flat bottoms and the vertical sidewalls have been
presented in past Picture of the Day articles as signs that they were created
through electric discharge machining (EDM) and not because of meteor impacts on
the surface.
Although large pieces of rock impacting the surface of Mercury is not an
unreasonable theory, the signs of EDM are
more prevalent than the signs of kinetic shock through the strata. Most of
the debris on the surface of Mercury appears to be chunks of fallback material
that was blown out by the explosive energies of plasma discharges. Ordinarily,
as in the image at the top of the page, the craters have little if any ejecta
surrounding them. The crater field shown above is generally lacking in boulders
or smaller breccias despite the surrounding haloes of blackened terrain.
Indeed, a close examination of some of those concentrations of craters reveals
them to be woven together in patterns that criss-cross and braid themselves over
and under one another. They all lie along the path of
flat-topped mesas that rise above deep chasms cutting across the landscape
without regard to the elevation. Many times the chasms slice right through the
middle of a crater and its central mountain peak as if they weren’t even there.
Giant escarpments rise above V-shaped canyons and continue their way along
the mountain tops and hundred-kilometer ridges that hulk around the planet. The
long cliffs of Mercury are a feature that can also be found on Saturn’s moon
Dione.
Whether it is on Dione, Mercury,
Ganymede, Mars or Venus – whenever we send satellites or rovers to examine
the geology of other celestial objects, more and more evidence mounts in support
of the Electric Universe and the electric discharges that have shaped the
surfaces of solid bodies.
Mercury’s magnetic field is
another enigma for NASA investigators. It is believed that
Mercury generates a magnetic field in the same way as the
Earth does, through a rotating “dynamo” at the core of the
planet. Mercury is unique in that it has such a weak field
for the size of its core – less that 1% as strong as Earth’s
magnetic field. One theory is that Mercury has a solid outer
shell that prevents the core from turning freely, thus
reducing its momentum transfer into electromagnetism.
Another theory suggests that Mercury’s slow rotation keeps
the magnetic field in a weakened state. Mercury rotates in
59 Earth days, making it the planet with the slowest
rotation next to Venus. It is more likely that the
problematic 'dynamo' theory of planetary magnetism is
wrong.' A charged, slowly rotating body will produce a weak
dipole magnetic field
By Stephen Smith
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