Contains:  Solar system body or event
One evening in Lunar Copernicus, Astroavani - Avani Soares

One evening in Lunar Copernicus

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Description

Copernicus is a prominent impact crater located on the eastern Oceanus Procellarum. The crater Copernicus is estimated to be about 800 million years old, the time marking the start of the Copernican era in the Lunar geologic timescale. Due to its relative youth, the crater has received very little erosion and it remains sharp and well-defined.

The circular rim has a discernable hexagonal form, with a terraced inner wall and a 30-km wide, sloping rampart that descends nearly a kilometer to the surrounding maria. There are three distinct terraces visible, and arc-shaped landslides due to slumping of the inner wall as the crater debris subsided.

Most likely due to its recent formation, the crater floor has not been flooded by lava. The terrain along the bottom is hilly in the southern half while the north is relatively smooth. The central peaks consist of three isolated mountainous rises climbing as high as 1.2 km above the floor. These peaks are separated from each other by valleys, and they form a rough line along an east-west axis. Infrared observations of these peaks during the 1980s determined that they were primarily composed of the mafic form of Olivine.

The crater rays from Copernicus spread as far as 800 kilometers across the surrounding maria, overlaying rays from the Aristarchus and Kepler craters. The rays are less distinct than the long, linear rays about Tycho crater, instead forming a nebulous pattern with plumy markings. In multiple locations the rays lay at glancing angles, instead of forming a true radial dispersal. An extensive pattern of smaller secondary craters can also be observed surrounding Copernicus, a detail that was depicted in a map by Giovanni Cassini in 1680. Some of these secondary craters form sinuous chains in the ejecta.

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One evening in Lunar Copernicus, Astroavani - Avani Soares