Category Archives: MESSENGER

Another Side of Mercury

More Cool Planetary Science

A wide-angle camera view of Mercury
A wide-angle camera view of Mercury

Yesterday the MESSENGER mission did a close flyby of Mercury and began returning high-resolution images.  I’ll start with the last one first — it was was taken about 90 minutes after the spacecraft’s closest approach to the planet, while Messenger was on the way “out”.

The bright crater in the center is called “Kuiper” — named after Gerard Kuiper, a well-known planetary scientist.  This crater was first spotted in Mariner 10 images in the 1970s, but the real news is that this image shows terrain we haven’t seen before. Everything east of Kuiper (toward the limb (right edge) is new to our eyes. Notice the rays extending out across the whole right side of the image, emanating from a relatively fresh crater that had only been seen at low resolution from Earth using radar scanning techniques. This gives planetary scientists a whole new side of Mercury to interpret as they work to understand Mercury’s formation and cratering history.

A close-up of Mercury a few minutes after close approach.
A close-up of Mercury a few minutes after close approach.

Only a few minutes after closest approach, the spacecraft snapped this image of Mercury’s cratered, pitted surface. The last time anybody saw an image of this part of Mercury was from Mariner 10 in the 1970s. The largest impact feature at the top of the image is about 133 kilometers (83 miles) across and is named Polygnotus (who was a Greek painter who lived in the 5th century B.C.). It has a central peak ring and is surrounded by smooth plains material (which probably was molten rock that flowed and hardened after the impact). Another large crater at the top left of the image is called Boethius (after a 6th century Roman philosopher).  It also appears to be almost filled with smooth plains (probably formed the same way).  Sometime well after the impact which created the crater, the whole area was deformed during the formation of a prominent scarp (a cliff).

Never-before-seen terrain on Mercury
Never-before-seen terrain on Mercury

Finally, from a time about 58 minutes before closest approach, Messenger snapped this dynamic image, which I think gives a nifty 3D “feel” for those of us watching on flat screens. The features in the foreground, near the right side of the image, are close to the terminator, the line between the sunlit dayside and dark night side of the planet, so shadows are long and prominent.  You can make out two very long scarps that appear to cut across each other. One occurred first, and then sometime later, tectonic forces created the other one. The easternmost scarp also cuts through a crater, which means that it formed after the impact that created the crater. Other neighboring impact craters, such as in the upper left of this image, appear to be filled with smooth plains material (again, probably from molten rock that flowed after the impact and then cooled and hardened).

There will undoubtedly be more images coming from the MESSENGER mission. If you want to follow the action and get larger versions of all the images, point your browser to the MESSENGER website gallery. Mission scientists are examining images and putting them up as they do — so check frequently!

It’s Not Dead, says Jim

Mercury Continues to Surprise People

I’ve been reading up on the Mercury MESSENGER mission lately. Its findings are fascinating because they seem to refute the old “Mercury’s a dead planet” meme that was popular in planetary science circles for a while. MESSENGER’s measurements of Mercury’s magnetic field, for example, show that there is a dipole field (meaning it has north and south poles), and that it’s still being generated by a dynamo deep inside the planet.

In addition, images of the planet show that it was quite the poppin’ place back in the early days of the solar system. Its geologic history is much more complex than anybody thought, and it includes episodes of volcanic eruptions, particularly around the huge Caloris Basin impact crater site. Here’s what planetary scientist Jim Head had to say about Mercury’s turbulent past:

“By combining Mariner 10 [which first imaged and studied Mercury] and MESSENGER data, the science team was able to reconstruct a comprehensive geologic history of the entire basin interior,” explained James Head of Brown University, the lead author of one of several reports that were published earlier this summer in the journal Science. “The Caloris basin was formed from an impact by an asteroid or comet during the heavy bombardment period in the first billion years of Solar System history. As with the lunar maria, a period of volcanic activity produced lava flows that filled the basin interior. This volcanism produced the comparatively light, red material of the interior plains intermingled with impact crater deposits. Subsidence caused the surface of the Caloris floor to shorten, producing what we call wrinkle-ridges. The large troughs, or graben, then formed as a result of later uplift, and more recent impacts yielded newer craters.”

Mapping a Volcano

What I personally find fascinating are the volcanic vents that MESSENGER has imaged. This figure shows a mosaic of images taken of the largest volcano yet found on Mercury. The sketch map below identifies the major features in the image. The “irregularly-shaped depressions” probably correspond to volcanic vents. The “margin of the dome-like feature” shows the outer limits of lava flows from the vents. Those flows probably covered up the underlying surface of “hummocky plains” that existed earlier. The unlabeled double line outlines bright material associated with the volcano. That material could be pyroclastic deposits ejected during volcanic eruptions at the vents.

The “highly-embayed impact crater” seems to have had lava flow up to its rim; a more distant impact crater is “relatively fresh” and unchanged by any lava. (“Relatively fresh” means that it hasn’t been cratered over, and is younger than the surrounding terrain.) The volcano is located just inside the rim of the Caloris impact basin, labeled as “Caloris basin rim units” on this map.

This map (Credit: Figure 1 from Head et al., Science, 321, 69-72, 2008) and many others are what planetary scientists are using to understand the processes that have shaped Mercury since its formation.