Studying
the number of impact craters to calculate the age of these regions on the surface, scientists estimated that the planet's magnetic field is very ancient — at least 3.7 billion to 3.9 billion years old.
Scientists record the size and
number of impact craters — and how eroded they are — to determine the ages and histories of different planetary surfaces.
Not exact matches
That's potentially problematic, because planetary scientists use the
number of small
impact craters to estimate the age
of the lunar surface.
«By comparing the measured
craters to the
number and spatial distribution
of large
impact basins on Mercury, we found that they started to accumulate at about the same time, suggesting that the resetting
of Mercury's surface was global and likely due to volcanism,» said lead author Dr. Simone Marchi, who has a joint appointment between two
of NASA's Lunar Science Institutes, one at the SwRI in Boulder and another at the Lunar and Planetary Institute in Houston.
The
number of new
craters found by Speyerer and colleagues is greater than anticipated by standard
impact - modeling rates used by lunar scientists.
«In addition to the new
impact craters and starburst debris patterns, we observed a surprising
number of small surface changes which we call splotches,» Speyerer said.
Stothers, R.B., 1998: Galactic disc dark matter, terrestrial
impact cratering and the law
of large
numbers.