It's official: The next Mars rover will explore a 5-kilometre-high mountain of sediment inside a crater called Gale, NASA announced today.
The Curiosity rover is scheduled to
launch between 25 November and 18 December. It will examine Martian
rocks and soil to learn about the history of the planet's climate and to
look for chemical traces of life.
There has been vigorous debate about where to send the rover. At a meeting in May, competing camps made their final arguments for each of the four sites then on the shortlist.
"These are all like different flavours of ice cream – all fantastic but slightly different," said John Grant
of the National Air and Space Museum in Washington DC, one of the
organisers of the May meeting, at a NASA press conference today.
In recent weeks, NASA said it had narrowed that list to two craters: Gale and Eberswalde.
Runner-up
Eberswalde contains a beautifully
preserved fan of sediment from an ancient river delta. On Earth, organic
material gets concentrated in such sediment, so this would be a good
place to look for signs of past life on Mars.
But on Friday, NASA announced it will send Curiosity, also known as the Mars Science Laboratory (MSL), to Gale crater instead.
There, a giant mound of layered
sediment rises 5 kilometres from the crater floor. It is not known
exactly how it got there, but the sediment contains clays, a sure sign
that it was exposed to liquid water at some point.
"If you start at the bottom of the pile of layers and you go to the top, it's like reading a novel," said John Grotzinger,
the rover's project scientist at the California Institute of Technology
in Pasadena. "And we think Gale crater is going to be a great novel
about the early environmental evolution of Mars."
Multiple sites
It is too dangerous to land on the
mountain itself, so Curiosity will touch down on a flatter part of the
crater floor, then drive up the mountain.
But first, it will take a look at
sediment deposited at the landing site by a river that once flowed into
the crater. That sediment and the clays in the mountain are two of the
places in Gale that may have been habitable and left organics behind.
But organics could also be preserved
in several other places where life may once have existed. One is an
ancient river canyon that cuts into the mountain. There are also layers
in the mountain containing sulphate minerals, which require water to
form. And there are also cracks in the mountain that appear to have been
waterlogged in the past.
"There was a real preference for Gale
in that it's not a one-trick pony," said Michael Meyer of NASA
Headquarters in Washington DC. "There's several different environmental
settings that can be explored [there], any one of which might have some
possibility of preserving organics."
Organic hunt
Grotzinger agrees: "It has
exceptionally high diversity for different kinds of habitable
environments and it is possible that some of those might preserve
organic carbon."
"Organic carbon" means any complex
carbon-based molecules, whether they come from living things or some
other source. For example, Mars has probably received organic carbon
from meteorite impacts.
Grotzinger noted that finding organic
carbon will be "a very, very difficult challenge" based on experience
with Earth geology. Even though life is abundant on our home planet,
ancient rocks very rarely preserve organic material, he says.
"We hope to be able to look for
organic carbon," he said. "What we can promise to deliver with MSL is an
understanding of the environmental history of Mars."
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