Planetary Sciences 206
Homework #4

Solution

1.  In this picture of the full Moon one can see several "rayed craters", most notably the bright crater Tycho at the bottom of the picture.  Rays from Tycho extend for many hundreds of kilometers outward from its center.

full Moon (Luc
      Viatour) Image by Luc Viatour from Wikipedia

Go to the Messenger website and find at least two examples of rayed cratera on Mercury.  Print out images of these rayed Mercury craters along with their identifications, and turn these in with this homework assignment.

There are many spectacular examples of rayed craters on the Messenger site.  Here is crater Kuiper, first observed and named by the Mariner 10 team shortly after G. P. Kuiper's death:

crater Kuiper
This crater is 62 km in diameter and its rays extend for hundreds of kilometers in all directions.  Note the central peak.

Here is a whole-disk image of Mercury from Messenger, showing intersecting ray systems:
whole-disk image of
      Mercury
The bright crater just south of the center of the image is Kuiper.

2.  Go to
http://en.wikipedia.org/wiki/Impact_crater

and click on the impact movie under "Crater formation."  The movie shows a high-speed digital sequence of a vertical impact by a copper sphere traveling at 4.5 km/sec into porous pumice (density of about 1g/cc).   Ejecta are launched out of the target and only gravity limits how far they can travel beyond the rim on ballistic trajectories.

impact_still image by P.H. Schultz, Brown University and J.P. Wiens

Based on such impact experiments and the discussion given in lecture about orbital and suborbital (ICBM) trajectories, discuss how rayed craters are formed.

As we can see from these experiments, a high-velocity impact launches a conical sheet of material moving outward from the impact site.  If the impacted surface is not perfectly smooth but has irregularities, these irregularities may cause the ejected sheet to not be a perfect cone, but have "rays" (corresponding to low spots in the impact site).  Depending on the energy of the impact, some of the sheet material can travel for very long distances, and if the material is ejected at close to orbital velocity, it can even travel a trajectory to very distant points on the planet:
sub-orbital