Lunar Topography in False Color

  • Released Friday, April 17, 2009
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An updated version of this animation is available here.

This animation is a brief tour of several prominent features of the Moon's terrain: Tycho crater, the south pole, and the South Pole-Aitken basin. The height of the terrain is color-coded, with blues and greens representing low altitudes and reds representing high altitudes. The view is match-moved to a companion piece showing the Moon in natural colors.

The elevation map comprises low-resolution data from a number of sources, including the Clementine and JAXA/SELENE spacecraft, combined with high-resolution insets for Tycho and the region near the south pole. One of the goals of the Lunar Reconnaissance Orbiter mission is the creation of a high-resolution elevation map of the entire surface of the Moon.

Moon false color topo flyover

Elevation key

Elevation key

Tycho crater and its bright ejecta rays are among the youngest and most recognizable features on the Moon. The crater is 85 kilometers (50 miles) wide and 4700 meters (15,400 feet) deep. The central peak is 2400 meters (7900 feet) above the crater floor.

Tycho crater and its bright ejecta rays are among the youngest and most recognizable features on the Moon. The crater is 85 kilometers (50 miles) wide and 4700 meters (15,400 feet) deep. The central peak is 2400 meters (7900 feet) above the crater floor.

The floors of deep craters near the poles, including bowl-shaped Shackleton near the center of this view of the south pole, are in permanent shadow and therefore cold and dark enough to harbor potential deposits of water ice.

The floors of deep craters near the poles, including bowl-shaped Shackleton near the center of this view of the south pole, are in permanent shadow and therefore cold and dark enough to harbor potential deposits of water ice.

The South Pole-Aitken basin, roughly 2100 kilometers (1300 miles) wide and 10 kilometers (6 miles) deep, is perhaps the largest impact feature in the solar system. It lies on the far side of the Moon, the hemisphere never visible from Earth, and was found only after spacecraft began visiting the Moon in the 1960s.

The South Pole-Aitken basin, roughly 2100 kilometers (1300 miles) wide and 10 kilometers (6 miles) deep, is perhaps the largest impact feature in the solar system. It lies on the far side of the Moon, the hemisphere never visible from Earth, and was found only after spacecraft began visiting the Moon in the 1960s.

For More Information

See http://www.nasa.gov/lro

Credits

Please give credit for this item to:
NASA/Goddard Space Flight Center Scientific Visualization Studio. Some elevation data provided by JAXA/SELENE.

This page was originally published on Friday, April 17, 2009.
This page was last updated on Wednesday, May 3, 2023 at 1:54 PM EDT.

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Tapes

The media on this page originally appeared on the following tapes:
  • LRO Pre-Launch Resource Tape (ID: 2009030)
    Tuesday, April 7, 2009 at 4:00AM
    Produced by - Andy Acuna (Hughes STX)

Datasets used

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