This frame from a sequence of images shows a blast zone where the sky crane from NASA's Curiosity rover mission hit the ground after setting the rover down in August 2012. The images are from HiRISE on NASA's Mars Reconnaissance Orbiter.
This observation from NASA's Mars Reconnaissance Orbiter shows an interesting crater floor with what appear to be inverted channels, rounded lobe-like landforms, and light-toned layered deposits along the southern portion of the crater wall.
This image is of a portion of the Southern plains region within Hellas, the largest impact basin on Mars, with a diameter of about 2300 kilometers (1400 miles), as observed by NASA's Mars Reconnaissance Orbiter.
Eleven years and two months after its landing on Mars, the total driving distance of NASA's Mars Exploration Rover Opportunity surpassed the length of a marathon race: 26.219 miles (42.195 kilometers).
This image from NASA's Mars Reconnaissance Orbiter covers Raga Crater, the location of well-studied recurring slope lineae (RSL). RSL are dark flows that disappear and re-form every Mars year at certain locations.
Gullies and Layers in a Crater Near Mariner Crater
Gullies are commonly found in the southern mid-latitudes of Mars. In this image from NASA's Mars Reconnaissance Orbiter they start near top of a long ridge, and descend into an impact crater that lies at the bottom of the ridge.
This image from NASA's Mars Reconnaissance Orbiter shows dark dunes in the western Medusae Fossae. This image shows no large dunes, but many of the dark sand patches cover slopes up to discrete layers.
Bigbee is a 21 kilometer-diameter impact crater located on the northern rim of Holden crater in southern Margaritifer Terra, a region on Mars that is well known for its long record of water-rich activity as seen by NASA's Mars Reconnaissance Orbiter.
Taken in late southern spring and when Mars is near perihelion (closest distance to the Sun), this image from NASA's Mars Reconnaissance Orbiter shows the effects of dry ice sublimation on a longitudinal dune in the far Southern hemisphere.
In February 2015, NASA's Mars Exploration Rover Opportunity is approaching a cumulative driving distance on Mars equal to the length of a marathon race. This map shows the rover's position relative to where it could surpass that distance.
NASA's Curiosity Mars rover can be seen at the 'Pahrump Hills' area of Gale Crater in this view from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter.
The dark fans in this image are made up of small particles from the surface deposited on top of the seasonal layer of ice; carbon dioxide ice still covers much of the surface at this high latitude site observed by NASA's Mars Reconnaissance Orbiter.
This image from NASA's Mars Reconnaissance Orbiter shows two small craters (called 'tangential craters'), just touching on their rims, in the much larger Ptolmaeus Crater, which is located in the Martian Southern hemisphere.
The pits visible in this image from NASA's Mars Reconnaissance Orbiter aren't impact craters. The material they are embedded into is ejecta (stuff thrown out of an impact crater when it forms) from a large crater called Hale not seen in this image.
In this observation from NASA's Mars Reconnaissance Orbiter made for a study of ancient craters, we see the craters filled with smooth material that has subsequently degraded into scallops. These formations might be possibly due to ground ice sublimation.