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STS-1 anniversary event
This 25th anniversary celebration of the first space shuttle launch took place April 12 at Space Center Houston. Speakers included Johnson Space Center Director Mike Coats, NASA Administrator Mike Griffin, Congressman Tom DeLay, Senator Kay Bailey Hutchison, STS-1 commander John Young and pilot Bob Crippen.

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New lunar mission
During this NASA news conference on April 10, agency officials unveil the Lunar Crater Observation and Sensing Satellite, or LCROSS, that will launch piggyback with the Lunar Reconnaissance Orbiter spacecraft in October 2008. LCROSS will use the launch vehicle's spent upper stage to crash into the moon's south pole in an explosive search for water.

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LCROSS mission plan
Daniel Andrews, the LCROSS project manager from NASA's Ames Research Center, narrates this animation depicting the mission from launch through impact on the lunar surface.

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STS-1 crew looks back
In this highly entertaining program, commander John Young and pilot Bob Crippen of the first space shuttle crew tell stories and memories from STS-1. The two respected astronauts visited Kennedy Space Center on April 6 to mark the upcoming 25th anniversary of Columbia's maiden voyage.

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STS-41G crew film
The October 1984 flight of space shuttle Challenger featured a diverse set of accomplishments. The Earth Radiation Budget Satellite environmental spacecraft was deployed and a planet-mapping radar was tested. The seven-person crew was led by Bob Crippen and included the first Canadian in space, Marc Garneau, and the first time two women, Sally Ride and Kathryn Sullivan, had flown aboard one flight. Sullivan and Dave Leestma also conducted a spacewalk to demonstrate techniques for refueling satellites. The crew narrates this post-flight film of STS-41G.

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STS-37 anniversary
On April 5, 1991, space shuttle Atlantis lifted off from Kennedy Space Center carrying the Compton Gamma Ray Observatory -- NASA's second Great Observatory. Launch occurred at 9:23 a.m. from pad 39B.

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Crew news conference
The combined Expedition 12 and 13 crews, along with visiting Brazilian astronaut Marcos Pontes, hold this in-flight news conference with reporters in Houston, Cape Canaveral and Moscow on April 3. The crews are handing over duties during this week-long handover before Expedition 12 returns to Earth from the space station.

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Next station crew
Full coverage of the Expedition 13 crew's launch aboard a Russian Soyuz spacecraft to begin a six-month mission aboard the International Space Station.

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Mars Express orbiter spots possible sites for life
EUROPEAN SPACE AGENCY NEWS RELEASE
Posted: April 21, 2006

By mapping minerals on the surface of Mars using the European Space Agency's Mars Express spacecraft, scientists have discovered the three ages of Martian geological history - as reported in the latest issue of Science - and found valuable clues as to where life might have developed.

The new work shows that large bodies of standing water might only have been present on Mars in the remote past, before four thousand million years ago, if they were present at all. Within half a billion years, these conditions had faded away.

The results come from the Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activite (OMEGA) instrument on board Mars Express. In one Martian year (687 Earth days) of operation, OMEGA mapped 90 percent of the surface, allowing the identification of a variety of minerals and the processes by which they have been altered during the course of Martian history. The maps have allowed a team of scientists, led by Professor Jean-Pierre Bibring, Institut d'Astrophysique Spatiale (IAS), Orsay (France), to identify three geological eras for Mars.

The earliest, named by the authors as the Œphyllosian' era, occurred between 4.5-4.2 thousand million years ago, soon after the planet formed. The environment was possibly warm and moist at this time, allowing the formation of large-scale clay beds, many of which survive today.

The second era, the Œtheiikian', took place between 4.2 and 3.8 billion years ago. It was prompted by planet-wide volcanic eruptions that drove global climate change. In particular, the sulphur these eruptions belched into the atmosphere reacted with the water to produce acid rain, which altered the composition of the surface rocks where it fell.

Finally, there was the Œsiderikian', the longest lasting of the Martian eras. It began sometime around 3.8-3.5 billion years ago and continues today. There is little water involved in this era; instead, the rocks appear to have been altered during slow weathering by the tenuous Martian atmosphere. This process gave Mars its red colour.

The eras are named after the Greek words for the predominant minerals formed within them. The one most likely to have supported life was the phyllosian, when clay beds could have formed at the bottom of lakes and seas, providing the damp conditions in which the processes of life could begin.

However, there are still question marks. The team points out that the clay beds might have been formed underground, rather than in lakebeds.

"Hydrothermal activity below the surface, the impact of water-bearing asteroids, even the natural cooling of the planet could all have promoted the formation of clay below Mars's surface. If so, the surface conditions may always have been cold and dry," said Bibring.

After this initial period, water largely disappeared from the planet's surface either by seeping underground or being lost into space. Except for a few localised transient water events, Mars became the dry, cold desert seen by spacecraft today. This new identification of clay beds on Mars provides high-priority targets for future Mars landers that seek to investigate whether Mars once harboured life.

"If living organisms formed, the clay material would be where this biochemical development took place, offering exciting places for future exploration because the cold Martian conditions could have preserved most of the record of biological molecules up to the present day," concluded Bibring.

The full results are published in the 21 April issue of the journal Science. The article, ŒGlobal Mineralogical and Aqueous Mars History Derived from OMEGA/Mars Express Data', is by Jean-Pierre Bibring, Yves Langevin, Francois Poulet and Brigitte Gondet (Institut d'Astrophysique Spatiale - IAS, Orsay, France), John F. Mustard (Brown University, Providence, USA), Raymond Arvidson (Washington University, St.Louis, USA), Aline Gendrin (Institut d'Astrophysique Spatiale - IAS, Orsay, France & Brown University, Providence, USA), Nicolas Mangold (IDES, Orsay Campus, France), P. Pinet (Observatoire Midi-Pyrenees, Toulouse, France), F. Forget (LMD - Univ. Paris 6, France), and the Mars Express OMEGA team.