Curiosity, a one-ton geochemistry lab on wheels, landed on Mars in August. Its goal is to see if the crater at one time could have been hospitable for simple forms of organic life. Curiosity has spent the past six months exercising its suite of 10 instruments and its seven-foot robotic arm in a series of tests aimed at ensuring all the hardware is working well before the rover heads for Mt. Sharp, its ultimate destination.
The rover probably won't begin to explore Mt. Sharp for another year.
Curiosity has traveled slightly more than a quarter of a mile, as the crow flies, since landing. Along the way, however, scientists have chosen targets for instrument tests that have already provided insights into the crater's geologic past – including evidence for an ancient stream bed.
Yellowknife Bay, a portion of a larger feature the team dubbed Glenelg, is the lowest, hence oldest, formation the rover has explored. It hosts a number of clues that point to a watery past. [Editor's note: The original version of this paragraph gave an incorrect relative age for the Yellowknife Bay formation.]
- Using the equivalent of a geologist's magnifying glass on the end of the the robotic arm, researchers identified a wide variety of rock textures. These range "from conglomerate to sandstone to siltstone" and all "are sedimentary rocks, meaning that other rocks had to be broken down into fragments and transported elsewhere," says Aileen Yingst, a researcher with the Planetary Science Institute in Tucson and deputy principle investigator for the robotic hand lens, known as MAHLI. How were they transported? Many of the fragments are too big to have traveled on the Martian wind, suggesting water.
- A layered, rock outcrop the team has named the Shaler Unit indicates a stream flowed through the area, shifting small sediment dunes on the stream bed in ways that formed the layers.
- The composition of the white minerals in rock veins is consistent with calcium sulfate, plus a fair bit of hydrogen. The relatively high levels of hydrogen suggest the minerals precipitated out of water flowing through the fissures.