Curiosity Rover is Climbing By way of Dramatic Striped Terrain on Mars

Nearly day by day we right here on Earth get a wide ranging image of Mars’s terrain despatched again by a rover. However, the view from area will be fairly wonderful, too. The Mars Reconnaissance Orbiter (MRO) simply despatched again a thought-provoking image of Curiosity because it makes its method up a steep ridge on Mount Sharp.

The rover is a tiny black dot within the heart of the picture, which provides feeling for what MRO’s HiRISE digicam achieved. For scale, the rover is concerning the measurement of a dinner desk, sitting in a area of alternating darkish and lightweight bands of fabric on the Crimson Planet.

NASA's Curiosity Mars rover appears as a dark speck in this image captured from directly overhead by the agency's Mars Reconnaissance Orbiter, or MRO. Credit: NASA/JPL-Caltech/University of Arizona — NASA’s Curiosity Mars rover seems as a darkish speck on this picture captured from immediately overhead by the company’s Mars Reconnaissance Orbiter, or MRO. Credit score: NASA/JPL-Caltech/College of Arizona

The place’s Curiosity?

The Curiosity rover is exploring an historical ridge on the aspect of Mount Sharp, which is the height of a crater on Mars. It’s sitting on the aspect of a characteristic referred to as Gediz Vallis Ridge, and the terrains and supplies protect a file of what issues had been like when water final flowed there. That occurred about three billion years in the past. The pressure of the circulate introduced important quantities of rocks and particles by way of the area. They piled as much as type the ridge. So, a lot of what you see right here is the desiccated stays of that flooding.

Particles flows are fairly widespread right here on Earth, significantly within the aftermath of floods, volcanic eruptions, tsunamis, and different actions. We are able to see them wherever materials floods by way of a area or down a slope. In a flood-based circulate, the pace of the water combines with gravity and the diploma of slope to ship materials dashing throughout the floor. A particles circulate may also be a dry landslide, and people can happen just about anyplace on Earth the place the situations are proper. One other sort of particles circulate comes from volcanic exercise. That happens when materials erupts from a volcano, or when earthquakes mixed with an eruption collapse materials into the aspect of the mountain. That ends in what’s referred to as a “lahar”. People in North America would possibly recall the Mount St. Helens eruption in 1980; it resulted in a number of lahars that buried components of the encompassing terrain.

Now that scientists see similar-seeming areas on Mars, they wish to know a number of issues. How did they type? Have been they created by the identical processes that make them on Earth? And, how way back did they start to type? Curiosity and Perseverance and different rovers and landers have been despatched to Mars to assist reply these questions.

Understanding the Particles Ridge

Did any of those actions occur on Mars? The proof is fairly sturdy, which is why Gediz Vallis itself is a serious exploration aim for the rover. It’s a canyon that stretches throughout 9 kilometers of the Martian floor and is carved about 140 meters deep. Gediz was seemingly carved by so-called “fluvial” exercise (that means flowing motion) at first. Later floods deposited a wide range of fine-grained sands and rocks. Over time, winds have blown quite a lot of that materials away, abandoning protected pockets of supplies left behind by the flooding. The scale of the rocks tells one thing concerning the pace of the flows that deposited all the fabric. Geological research of these rocks will reveal their mineral compositions, together with their publicity to water over time.

The Gediz Vallis ridge resulted from the motion of water pushing rocks and filth round to construct it up over time. Planetary scientists now want to determine the sequence of occasions that created it. The clues lie within the scattered rocks within the area and the encompassing terrain. Mount Sharp itself (formally often known as Aeolis Mons), is about 5 kilometers excessive and is, primarily, a stack of layered sedimentary rocks. As Curiosity makes its method up the mountain, it explores youthful and youthful supplies.

NASA’s Curiosity captured this 360-degree panorama while parked below Gediz Vallis Ridge (seen at right), a formation that preserves a record of one of the last wet periods seen on this part of Mars. After previous attempts, the rover finally reached the ridge on its fourth try. Credits: NASA/JPL-Caltech/MSSS. — NASA’s Curiosity captured this 360-degree panorama whereas parked beneath Gediz Vallis Ridge (seen at proper), a formation that preserves a file of one of many final moist intervals seen on this a part of Mars. After earlier makes an attempt, the rover lastly reached the ridge on its fourth strive. Credit: NASA/JPL-Caltech/MSSS.

Curiosity’s Mission at Gediz

To place all this on a bigger scale, Mount Sharp is the central peak of Gale Crater. It fashioned some 3.5 to three.8 billion years in the past from an impression. As time glided by, water flooded the crater a number of occasions. It flowed out and finally disappeared as Mars’s local weather modified it to the dusty desert we see at the moment.

Winds additionally performed a task in filling the crater with mud and sand deposits. This so-called aeolian exercise additionally helped carve out Mount Sharp. This historical past of wind- and water-based deposition and erosion made Gale Crater a really engaging place to discover. That’s why Curiosity was despatched there and continues its journey up Mount Sharp.