Map. Credit: NASA/GSFC/Arizona State University Although large boulders are not rare on the Moon, in-place bedrock is a rarity. LROC NAC close-up of light-toned bedrock exposed within the central structural uplift of Copernicus crater (~93-km diameter). During the mission of Apollo 17 in december 1972, crater Copernicus and its system of central peaks was photographed A prominent impact site anchored in the lunar Oceanus Procellarum, Copernicus crater is at the center of this telescopic portrait in light and shadow. Estos cráteres se cree que son de origen volcánico y no el resultado de impactos. Caught in stacked and sharpened video frames recorded on April 14 at 3:30am UTC, the lunar terminator, or boundary between night and day, cuts across the middle of the 93 kilometer diameter crater. Eudoxus (67 km) The mosaic was created by combining 24 high resolution images taken by Lunar Orbiter V on 16 August 1967. Stratigraphy is the science of determining relative ages of geologic materials by observing overlapping relationships between …

Eratosthenes (58 km) well formed crater with group of central mountains. Interactive Moon Map. notable for its collection of large internal impact craters. Rays of North Ray and South Ray craters cross near the Apollo 16 site in the Descartes Highlands and a ray from Tycho crater can be traced across the Apollo 17 site in the Taurus-Littrow Valley … Copernicus and its satellite crater "H" are included in ALPO list of bright ray craters; Copernicus H is a dark halo crater of Copernican age.

Copernicus H, un típico cráter de "halo oscuro", fue un objetivo de observación de la nave Lunar Orbiter 5 en 1967. Copernicus crater also plays an important role in our understanding of the lunar geologic timescale. Copernicus crater played a key role as pioneering lunar geologists Gene Shoemaker and Robert Hackman unraveled the basic stratigraphy of the Moon fifty years ago. Scientists use the basic principles of stratigraphy and superposition to define relative ages for geologic terrains and features. For a tablet or mobile device, touch an area of interest for about one second. Seeing the Copernicus crater close up mustered Space Age feelings of wonder. Rays are young lunar features, and any geologic unit covered by a ray of Copernicus must be relatively older than the crater itself. In general, ray craters are relatively young as their rays overlay the lunar terrain. Endymion (125 km) foreshortened crater with dark smooth floor. Copernicus is a classic example of a well-preserved, relatively young (less than 1 billion years old) lunar impact crater. This area lies just to the south of Mare Imbrium in the northwest quadrant of the side of the Moon … Map.

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