Your Everyday Destination for Science News & Research Articles

Similar-Looking Ridges On Mars Have Diverse Origins

View from the HiRISE camera on NASA’s Mars Reconnaissance Orbiter shows part of an area on Mars where narrow rock ridges, some as tall as a 16-story building, intersect at angles forming corners of polygons. Credit: NASA/JPL-Caltech/Univ. of Arizona

Thin, blade-like walls, some as tall as a 16-story building, dominate a previously undocumented network of intersecting ridges on Mars, found in images from NASA’s Mars Reconnaissance Orbiter.

The simplest explanation for these impressive ridges is that lava flowed into pre-existing fractures in the ground and later resisted erosion better than material around them.

A new survey of polygon-forming ridges on Mars examines this network in the Medusae Fossae region straddling the planet’s equator and similar-looking networks in other regions of the Red Planet.

“Finding these ridges in the Medusae Fossae region set me on a quest to find all the types of polygonal ridges on Mars,” said Laura Kerber of NASA’s Jet Propulsion Laboratory, Pasadena, California, lead author of the survey report published this month in the journal Icarus.

The pattern is sometimes called boxwork ridges. Raised lines intersect as the outlines of multiple adjoining rectangles, pentagons, triangles or other polygons. Despite the similarity in shape, these networks differ in origin and vary in scale from inches to miles.

Small and Large Examples:

Mars rover missions have found small versions they have been able to inspect up close. Some of these polygonal ridges, such as at “Garden City” seen by Curiosity, are veins deposited by mineral-laden groundwater moving through underground fissures, long before erosion exposed the veins. Curiosity recently also imaged small boxwork ridges that likely originated as mud cracks.
This stereo view shows an area on Mars where narrow rock ridges intersect at angles forming corners of polygons. It combines two observations from the HiRISE camera on NASA’s Mars Reconnaissance Orbiter and appears three-dimensional when viewed through red-blue glasses with the red lens on the left.
Credit: NASA/JPL-Caltech/Univ. of Arizona
[ads-post][right-side]
At the other end of the size scale, ridges outline several rectangles each more than a mile (more than 2 kilometers) wide at a location called “Inca City” near Mars’ south pole. These may have resulted from impact-related faults underground, with fractures filled by rising lava that hardened and was later exposed by erosion.

“Polygonal ridges can be formed in several different ways, and some of them are really key to understanding the history of early Mars,” Kerber said. “Many of these ridges are mineral veins, and mineral veins tell us that water was circulating underground.”

Polygonal ridges in the Nilosyrtis Mensae region of northern Mars may hold clues about ancient wet, possibly warm environments. Examples of them found so far tend to be in the same areas as water-related clues such as minerals that form in hot springs, clay-mineral layers and channels carved by ancient streams. A larger sample is needed to test this hypothesis.

Materials provided by ICARUS & NASA-Jet Propulsion Laboratory
Opinions
Retriving Opinions From Visitors...

This website uses cookies to improve your experience. We'll assume you're ok with this, but you can opt-out if you wish. Accept Read More