Mystery of the 'veins of Mars': Curiosity spots strange mineral deposits on the red planet that may hold clues to its watery past
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Curiosity Rover has discovered strange, multi-coloured veins on Mars that could give astronomers new insights into the red planet's watery past.
The mineral veins were found at a site called 'Garden City' on the slopes of Mount Sharp and stick up from the rock by up to 6cm (2.5 inches).
Scientists believe the bizarre network of ridges formed in Mars' wet past billions of years ago above the now eroded, much softer bedrock.
This March 18, view from the Mast Camera on the Curiosity rover shows a network of two-tone mineral veins. Scientists believe the bizarre formed in Mars' wet past billions of years ago above the now eroded bedrock
The ridges contain both bright and dark material. While Curiosity has found brightly coloured veins before, the darker ones remain have stumped scientists.
'Some of them look like ice-cream sandwiches: dark on both edges and white in the middle,' said Linda Kah, a Curiosity science-team member at the University of Tennessee, Knoxville.
'These materials tell us about secondary fluids that were transported through the region after the host rock formed.'
Veins such as these form where fluids move through cracked rock and leave minerals in the fractures, often affecting the chemistry of the rock surrounding the fractures.
This view from the Mars Hand Lens Imager on the arm of Curiosity rover is a close-up of a two-tone mineral vein at a site called 'Garden City' on lower Mount Sharp. It was taken during night, illuminated by LEDs
Kah said, 'At least two secondary fluids have left evidence here.
'We want to understand the chemistry of the different fluids that were here and the sequence of events. How have later fluids affected the host rock?'
Some of the sequence is known: Mud that formed lake-bed mudstones must have dried and hardened before the fractures formed.
The dark material that lines the fracture walls reflects an earlier episode of fluid flow than the white, calcium-sulphate-rich veins do - although both flows occurred after the cracks formed.
Curiosity has been studying rocky areas since landing on the Martian surface in 2012.
Garden City is about 39 feet (12 meters) higher than the bottom edge of the 'Pahrump Hills' outcrop of the bedrock forming the basal layer of Mount Sharp, at the center of Mars' Gale Crater.
'We investigated Pahrump Hills the way a field geologist would, looking over the whole outcrop first to choose the best samples to collect, and it paid off,' said David Blake of Nasa's Ames Research Center.
Analysis is still in its early stages, but the three drilled samples from Pahrump Hills have clear differences in mineral ingredients.
It seems that the two-toned minerals were created from two distinctive wet periods on the planet.
Curiosity is now exploring different layers of Mount Sharp in the hope of finding more clues to the red planet's history.
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