This image of sulfate deposits, including gypsum, in the Olympia Undae
region of Mars was taken by the Compact Reconnaissance Imaging
Spectrometer for Mars (CRISM) at 0026 UTC on November 18, 2006 (7:26 p.m.
EDT on November 17, 2006) near 80 degrees north latitude, 245 degrees east
longitude. CRISM's image was taken in 544 colors covering 0.36-3.92
micrometers, and shows features as small as 20 meters (66 feet) across.
Named for a classic albedo feature, Olympia Undae is a large dune field
that stretches some 1,100 kilometers (684 miles) across the northern polar
regions of Mars, just south of the ice cap.
In 2005 CRISM's sibling instrument, OMEGA, on board Mars Express, captured
data revealing that Olympia Undae’s dunes hold sulfate minerals including
gypsum. With more than five times the spatial resolution of OMEGA, CRISM
has captured greater detail of this region.
The top image reveals the location of CRISM data on a Mars Orbiter Laser
Altimeter (MOLA) map. The area from which CRISM data were gathered is
roughly 12 degrees north and 11 degrees east of the region where Phoenix
recently landed.
The lower left image is an infrared, false-color image that reveals dark
colored dunes overlying a lighter, rust-colored substrate. CRISM spectral
data (lower right image) shows the region is inundated with sulfates. It
also reveals that the darker dune material holds a higher concentration of
the water-bearing calcium sulfate mineral gypsum. A full resolution
targeted CRISM image taken just five degrees west of the image above,
revealed greater gypsum concentrations along the dunes’ crests
(Gypsum at Olympia Undae).
On Earth, gypsum is the most common sulfate mineral and is widely found in
sedimentary rocks. It’s frequently associated with evaporite salts and is
often found as a thick layer beneath halite or rock salt. Although most
often associated with evaporites, gypsum can also occur in layers with
limestone and shale. Most people are familiar with gypsum in the form of
plaster of Paris.
CRISM is one of six science instruments on NASA's Mars Reconnaissance
Orbiter. Led by The Johns Hopkins University Applied Physics Laboratory,
Laurel, Md., the CRISM team includes expertise from universities,
government agencies and small businesses in the United States and abroad.
NASA's Jet Propulsion Laboratory, a division of the California Institute
of Technology in Pasadena, manages the Mars Reconnaissance Orbiter and the
Mars Science Laboratory for NASA's Science Mission Directorate,
Washington. Lockheed Martin Space Systems, Denver, built the orbiter.