The Moon Revealed
LRO
The biggest revelation uncovered by researchers in recent years is the discovery of water on the moon, in ice and rocks, across huge craters and vast lunar plains. LRO helped discover the moon's hidden water by watching its partner probe LCROSS crash into the lunar surface in October 2009. LRO and other spacecraft ultimately found evidence of tons of water ice at the moon's north pole and elsewhere.Two Lunar Pits
LRO has now collected the most detailed images yet of at least two lunar pits, giant holes in the moon. Scientists believe these holes form when the ceiling of a subterranean lava tube collapses, possibly due to a meteorite strike. The image shows the Mare Ingenii pit, which surprisingly lies in an area with relatively few volcanic features. This pit is 426 feet (130 m) in diameter.
Hermite Crater
Far Side of the Moon
One side of the moon always faces toward our planet. The side that faces away should be referred to as the "far side of the moon"
instead of the "dark side of the moon," as it receives just as much
sunlight as the side that faces us. This image shows the moon's
topography from LRO's LOLA instruments with the highest elevations in
red and the lowest areas in blue.
Moon's Axis
The moon's axis tilts only slightly, so there
are areas of high elevation at its poles that remain almost constantly
exposed to the sun. Using LRO's precise measurements of topography,
scientists have been able to map illumination in detail, finding some
areas with up to 96% solar visibility. Such sites would have continuous
sun for approximately 243 days a year and never have a period of total
darkness for more than 24 hours.
A11
Images of the Apollo 11 landing site
taken by LRO clearly show where the descent stage (about 12 feet in
diameter) was left behind, as well as the astronauts' tracks and
equipment deployed. This LRO data has important scientific value, as it
provides context for the returned Apollo samples.
Lunar Mountains
On the moon, unlike on the Earth, even the largest lunar mountains
were formed in minutes or less as asteroids and comets slammed into the
surface, displacing and uplifting enough crust to create peaks that
easily rival those found on Earth.
Rilles
Rilles look like river channels on the lunar
surface. Researchers call the type shown here a "sinuous" rille,
exhibiting strong meanders. The formation of lunar rilles
remains a mystery. It is believed there may be many different formation
mechanisms including ancient magma flows and the collapse of
subterranean lava tubes.
Rover Lunokhod 1
Russian robotic rover Lunokhod 1
landed on the moon in 1970, and traveled about 6 miles (10 km) before
vanishing from detection in September 1971. This past March however, the
LROC team announced they had spotted it, miles from its supposed
location. A laser pulse was sent to Lunokhod 1, and contact was made
with the rover for the first time in nearly four decades. Lunokhod 1's
retroreflector returned a signal actually about five times better than
returned by Lunokhod 2.
Moon Zoo
The LRO Camera (LROC)
has a resolution about ten times better than any previous lunar orbiter
mission. LROC gathers 100 pixels to other spacecrafts' single pixel.
Researchers can now see detailed craters and individual boulders, some
measuring only a few feet on the lunar surface. Further, the public can
get involved by doing crater and boulder counts to aid in the research
at the "Moon Zoo" (http://www.moonzoo.org).
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