Lunar Reconnaissance Orbiter Camera

Dark Wisps in Copernicus

Dark streaks ornament a slope along the Copernicus crater rim (9.3°N, 21.5°W). Down-slope is to the right. NAC image M11735067L, incidence angle 32°, Sun is from the east, north is up, image is ~400 meters across [NASA/GSFC/Arizona State University].

What are these low-reflectance (dark), wispy streaks? The differences in color among lunar deposits is often understood in terms of composition and/or intensity of space weathering (which can discolor soils over time). When they become mixed (often from cratering events), they can produce areas of high color contrast. Most of them seem to have the lowest reflectance at the points highest in elevation on the crater wall (to the left), and become more reflective down-slope (to the right). The features in this image seem to cluster near a promontory that has its own streak of material, emanating as a fan-shaped curtain (see context image below).

There are several possible explanations for how the smaller, low-reflectance features formed. For example, these dark patches may represent mare basalts that were buried and re-exposed by the formation of Copernicus and subsequent mass wasting. Another possibility is that the low-reflectance materials are dikes or sills (intrusive igneous bodies) that pre-date the Copernicus impact and are now weathering out. Still a third possibility is that mare basalt debris were ejected by a nearby impact and deposited here, perhaps encouraging the erosion of the promontory in the process - or landing near the promontory by coincidence. In this later scenario, each block of ejecta might then have fragmented upon impact and migrated down-slope as individual debris aprons. There are several nearby, relatively recent craters outside of the Copernicus rim that could be responsible for this type of deposition. Are there any additional clues that could be looked for to further solve this mystery?

A wider view of NAC image M11735067L shows the association of a promontory's location with the occurrence of the dark deposits. Image is ~2.2 km across, downsampled from 50 cm/pixel to ~2.3 m/pixel [NASA/GSFC/Arizona State University].

The context image below provides a sense for how steep the outermost walls of Copernicus crater are, and show the location of today's Featured Image.

WAC mosaic context image showing Copernicus crater and Featured Image location. Image is ~108 km across [NASA/GSFC/Arizona State University].

Review the full NAC image below to look for more examples.

Related posts include: Dark streaks in Diophantus crater


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