| Large, Fluid Lava Flows
The Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 1998
confirmed that a vast region of Mars south of the Elysium volcanoes is
covered by a relatively young lava surface that was very fluid when it
erupted--so fluid that it ran more than a thousand kilometers (more
than 600 miles) across a region known as the Elysium Basin and a
channel named Marte Vallis. This result was initially reported by MOC
scientists in October 1998 (previous Elysium Basin release).
The picture above expands upon these results.
MOC image 38804 (above) shows a portion of Marte Vallis. Marte
Vallis has been thought by some to have been carved by a giant water
flood. However, the picture shown here does not have any flood
features. If there ever was a water flood, all of the evidence
in this
particular location (at 7.1°N latitude and 182.7°W longitude)
has been covered-up by a vast lava flow.
When it was forming, the lava flowed from the lower left, toward the
center right, then curved to the left and flowed toward the top-center
of the frame.
The center of the lava flow in image 38804 has a wide, shallow
channel bounded by steep, discontinuous walls--also known as levees.
Such leveed channels are commonly the conduit through which some of
the later stages of molten rock are transported along a lava flow. The
margins of the lava flow are broken into plates--some of them several
kilometers across. These plates were once part of a hard, rock crust
that floated on molten lava. As the lava flowed down Marte Vallis, huge
chunks of this crust broke off at the margins of the flow and floated a
few kilometers away from where they had originated. Long after the
lava had cooled and hardened, a distant meteorite impact splashed
ejecta across the martian surface such that a field of small
craters--known as secondary craters--formed on top of the lava flow
shown here.
MOC image 38804 was taken on June 25, 1998. This subframe
shows an area 15.8 km by 45.8 km (9.8 miles by 28.5 miles) in size.
The image here has a resolution of about 31 meters (101 feet) per pixel.
North is approximately up, illumination is from the right.
Malin Space Science Systems and the California Institute of
Technology built the MOC using spare hardware from the Mars Observer
mission. MSSS operates the camera from its facilities in San Diego, CA.
The Jet Propulsion Laboratory's Mars Surveyor Operations Project
operates the Mars Global Surveyor spacecraft with its industrial partner,
Lockheed Martin Astronautics, from facilities in Pasadena, CA and
Denver, CO.
Photo Credit: NASA/JPL/Malin Space Science Systems
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