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Pictures of Mercury from MESSENGER Spacecraft


Geology, Basins, Craters, Ejecta, Faults, Scarps and Lava Flows


mercury planet
NASA's MESSENGER spacecraft was launched on August 3, 2004 and has been on a voyage to observe Venus and Mercury. MESSENGER observed Venus in 2006 and 2007, acquiring images and a wealth of data. In early January, 2008, MESSENGER made its first flyby of Mercury and started obtaining detailed images of the planet's surface. The images and captions shown on this page are from NASA news releases of the mission.

The image at right was taken on January 15, 2008 at a distance of about 17,000 miles. It shows the previously unseen side of Mercury. As expected this side of Mercury is heavily cratered and blanketed with ejecta. The light area in the upper right has been named the Caloris Basin. It is believed to have been formed by the impact of a large asteroid or comet. It is one of the largest and youngest impact basins in our solar system.



Mercury's Cratered Surface

mercury surface
This is one of the first images of Mercury acquired by the MESSENGER spacecraft. It shows Mercury's heavily cratered surface. The craters range in age from very old to very young. Older craters can be recognized because numerous younger craters can be seen within them or cutting their rims. The rough surface surrounding the large crater in the lower right corner of the image is ejecta (debris blasted from the crater at the time of impact). Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.


Lava Flows on Mercury

mercury lava
This image reveals some of the geologic history of Mercury. Note how many of the craters have been filled by lava flows, producing a flat surface. These lava surfaces have a much younger age that the surrounding landscape and are shown with the letter "L" on the supplemental image. Their younger age can be determined because they have a low density of impact craters. A large fault is visible in this image and marked with a dashed line on the supplemental image. Note how it cuts across the medium size crater in the upper left of this images. This reveals that the fault was active after the crater had formed. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.


Mercury's Ejecta Features

mercury ejecta
This image shows more of Mercury's heavily cratered surface. This image shows a relatively young crater with bright "rays" of ejected material extending outwards in all directions from the crater's center. The bright rays are shown as dashed lines on the supplemental image. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.


Impact Craters

mercury craters
This image shows a large, relatively recent impact crater. The walls of this crater were very steep when it formed but afterwards slumping of the steep walls produced a terraced crater rim. When the impact occurred, the blast launched large volumes of ejecta into the air. These blanketed the surface with debris and the larger fragments of ejecta produced hundreds of smaller craters around the parent crater. The cratered surface of Mercury is complex. It has many craters caused by direct impacts and many craters produced by the infall of ejecta. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.


Fault Scarp

mercury fault
This image was captured by MESSENGER during its closest approach to Mercury. It shows some craters as small as 300 yards across. It also shows one of the highest and longest fault scarps discovered on the planet. Forces within the planet produced the fault by lifting the terrain on the left side of the image. Later a younger impact crater obliterated a portion of the scarp. The region shown in this image is about 100 miles across. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington.

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