Stay up to date with notifications from The Independent

Notifications can be managed in browser preferences.

Mars rover Curiosity finds evidence of ancient fast-moving streams on surface of red planet

Discovery of bedrock and rounded pebbles offer the most convincing evidence yet that there was water on the surface of Mars

Steve Connor
Friday 28 September 2012 17:19 BST
Comments

Your support helps us to tell the story

From reproductive rights to climate change to Big Tech, The Independent is on the ground when the story is developing. Whether it's investigating the financials of Elon Musk's pro-Trump PAC or producing our latest documentary, 'The A Word', which shines a light on the American women fighting for reproductive rights, we know how important it is to parse out the facts from the messaging.

At such a critical moment in US history, we need reporters on the ground. Your donation allows us to keep sending journalists to speak to both sides of the story.

The Independent is trusted by Americans across the entire political spectrum. And unlike many other quality news outlets, we choose not to lock Americans out of our reporting and analysis with paywalls. We believe quality journalism should be available to everyone, paid for by those who can afford it.

Your support makes all the difference.

A dried-up riverbed has been discovered on Mars which is the first direct evidence of an ancient network of fast-running streams on the Red Planet, scientists said today.

Although there has been strong indirect evidence that large amounts of water once existed on our neighbouring planet, the latest observations from Nasa's Curiosity rover confirm that Mars was once a watery world in which microbial life may once have thrived.

The rover, which is just a few weeks in to a two-year mission, has captured images showing gravel beds in the Martian rocks that have clearly been eroded away over many years to form smooth pebble-like stones just like those found in terrestrial riverbeds.

Scientists from the Jet Propulsion Laboratory (JPL) in Pasadena, California, estimated from the size and shape of the eroded rocks that fast-moving stream was up to several feet deep and could have existed for thousands and possibly millions of years for a period between 3.5 and 4 billion years ago.

“From the size of the gravels it carried, we can interpret the water was moving about three feet per second, with a depth somewhere between ankle and hip deep,” said William Dietrich of the University of California, Berkeley, the science co-investigator on the project.

“Plenty of [scientific] papers have been written about channels on Mars with many different hypotheses about the flows in them. This is the first time we're actually seeing water-transported gravel on Mars,” Dr Dietrich said.

“This is a transition from speculation about the size of streambed material to direct observation of it,” he said.

Curiosity, a six-wheeled mobile laboratory the size of a family car, has just begun its exploration of the north rim of the huge Gale Crate where it landed in August. It was examining two outcrops of rock, called Hottah and Link, when its mast-mounted cameras detected the distinctive gravel beds of a fast-moving stream.

“Hottah looks like someone jack-hammered up a slab of city sidewalk, but it's really a tilted block of an ancient streambed,” said John Grotzinger of the California Institute of Technology in Pasadena.

Both of the outcrops contain rounded pebbles embedded in stone to form what is known as rock conglomerates. The gravels in the conglomerates range in size from grains of sand to rocks the size of golf balls, and although some have sharp edges, many are rounded.

Nasa chose the Gale Crater as the landing site because it contains a large mountain in the middle, called Mount Sharp, where observations from orbiting space probes indicate the rocks have been formed by sedimentary processes, which are likely to preserve some geological signs of life.

Dr Grotzinger said that clay and sulphate minerals have been detected on the slopes of this mountain and these types of rocks are good preservers of carbon-based organic chemicals that are the potential ingredients for life.

Observations of the crater from orbit have also revealed the existence of an alluvial fan formed by watery material that had been washed down from the rim of the crater. Images show streaks of channels where large amounts of water once flowed.

“A long-flowing steam can be a habitable environment. It's not our top choice as an environment for preservation of organics, though. We're still going to Mount Sharp, but this is insurance that we have already found our first potentially habitable environment,” Dr Grotzinger said.

Curiosity is armed with toolbox of sophisticated instruments for analysing the chemical and physical composition of rocks but it is not designed to test for direct evidence of Martian life, he said. However, Nasa hopes that the rover will provide important scientific clues that could lead to the discovery of fossilised life forms, if they do indeed exist on Mars.

Life on Mars, in Utah

Mars rover Curiosity drills into Martian surface

Scientists claim new data is 'strongest evidence yet' that Mars may have supported life

Join our commenting forum

Join thought-provoking conversations, follow other Independent readers and see their replies

Comments

Thank you for registering

Please refresh the page or navigate to another page on the site to be automatically logged inPlease refresh your browser to be logged in