An Evolutionary Ring

Prometheus Bound to the F Ring at Saturn

F-ring at  Saturn

What happens when you put a small world orbiting through an ethereal pair of dust and ice particle rings, all encircling the planet Saturn? You get intricate whirled and kinked structure in the rings, as seen in this image from the Cassini Mission’s imaging subsystem.

It’s all in the gravity of the situation. Prometheus (which is a natural satellite (moon) of Saturn off to the right of the F ring (center)) does a little dance with the F ring, getting closer and farther away over a period of just under 15 hours. As this little oddly-shaped moon gets close to the ring particles, its gravitational interaction draws out a stream of material. The stream then gets more misshapen as it orbits around Saturn, forming the graceful loops and curves we see in this image. The Cassini Mission pages have many more images of this phenomenon, which is yet another good reason to study a planetary system over long periods of time. Snapshots give us a frozen moment in time; long-term observations tell us a more detailed and exacting story of just how things change on both large and small scales in the solar system.

For more fascinating images from the Cassini Mission, visit the Cassini-Huygens mission web pages and do a little browsing. You’ll learn more about Saturn, its moons (particularly fascinating Titan), and those glittery, wonderful rings that have so captivated planetary scientists.

It’s Not Dead, Jim

It’s Alive!!!! (In the Geological Sense, That Is…)

For those of you who thought Mars was a dead planet, this just in: there are avalanches out there, Captain!

The ongoing in situ exploration of Mars, which includes two rovers, and three orbiters (plus another spacecraft headed out to Mars by May of this year) is showing us a lot of Mars for our money. Just about every day, and more than once a day, you can log into the Mars missions web pages and see the latest from the Red Planet. And that doesn’t even count the great  images that Hubble Space Telescope gets every once in a while.

If you have been checking out Mars images pretty frequently, you’ll know that the place is far from being a dead planet. Sure, it has no biological life (that we know of , so far), but in every other way that counts, it is an evolving planet. The atmosphere changes with the seasons, its surface is constantly sculpted by winds and possibly the action of tectonic forces, and its polar caps grow and shrink throughout the year. If it had some liquid water on the surface, we’d probably see that change as the years go by. As it is, we are limited to watching what happens with ice and dust and rocks, but Mars hasn’t let us down. The Red Planet is giving us quite a show for our exploration money. And that’s the beauty of sending long-term missions to other planets: we get to see them change over time, which lets us understand them far better than if we only had snapshots to work from.

The latest in planetary surface modification at Mars comes to us from the High Resolution Imaging Science Experiment on the Mars Reconnaisance Orbiter. It caught a sequence of events on near the Martian north pole that are clearly action shots of an avalanche in progress. Dust and ice are tumbling down a 700-meter (2,300-foot) tall cliff and settling out on a gentler slope below. It’s pretty dramatic-looking, isn’t it?

Mars avalanche