Water flow on Mars suggests ancient life on planet
Top Stories
- Anti-corruption unit will now monitor access to players: BCCI
- Counter-terrorism to top Indo-US Security dialogue agenda: Sushilkumar Shinde
- IPL 2013 LIVE SCORE: Pune Warriors vs Delhi Daredevils
- Chinese Premier Li Keqiang arrives today, PM to seek early revival of border talks
- Telangana very much part of UPA national agenda: P C Chacko

Narrow ridges found in Martian craters may actually be fossilised remnants of underground cracks through which water once flowed on the red planet, a new study claims.
Water flowing beneath the surface of ancient Mars suggests life may once have been possible on the Red planet, according to a new analysis by researchers from Brown University.
The study, published in the journal Geophysical Research Letters, bolsters the idea that the subsurface environment on Mars once had an active hydrology and could be a good place to search for evidence of past life.
The study conducted by Lee Saper and Jack Mustard suggest the ridges, many of them hundreds of meters in length and a few meters wide, had been noted in previous research, but how they had formed was not known.
Saper and Mustard thought they might once have been faults and fractures that formed underground when impact events rattled the planet's crust.
Water, if present in the subsurface, would have circulated through the cracks, slowly filling them in with mineral deposits, which would have been harder than the surrounding rocks. As those surrounding rocks eroded away over millions of years, the seams of mineral-hardened material would remain in place, forming the ridges seen today.
Using high-resolution images from NASA's Mars Reconnaissance Orbiter, the researchers noted the orientations of the ridges and composition of the surrounding rocks.
The orientation data is consistent with the idea that the ridges started out as fractures formed by impact events.
Importantly, researchers also found that the ridges exist exclusively in areas where the surrounding rock is rich in iron-magnesium clay, a mineral considered to be a telltale sign that water had once been present in the rocks.
"The association with these hydrated materials suggests there was a water source available. That water would have flowed along the path of least resistance, which in this case would have been these fracture conduits," Saper said.
... contd.
Editors’ Pick
- Quake-hit and shaken, Bhaderwah spends nights in the open
- UP blast accused dies on way to jail, govt wanted to drop case against him
- Former civil aviation secy changes mind, seeks airport security exemption as EC
- BCCI suspects Gujarat players in other teams were also approached
- Police on money trail, Sreesanth in fresh trouble
- Chhattisgarh 'encounter' leaves 8 villagers dead, no Maoist link yet
- Chinese Premier Li Keqiang arrives today, PM to seek early revival of border talks


YouTube starts paid subscription service
ESA's gen-next satellite to monitor Earth's forests
Nokia launches Asha 501 globally from India, aims to take on Android smartphones
Singapore mobile app flushes out clean and dirty toilets




















