February 11, 2013

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More Evidence

images from Ashley et al, 2013, LPSC #2504.

Forty years ago lunar red spots were discovered. These are small volcanic features, like the Gruithuisen domes, that absorb in the ultraviolet and hence look bright at the red end of the spectrum. Some are cones, a few are steep domes and others are just odd pieces of old terrain. Their steep sides and conical shapes have been suggested as evidence that they were made of materials more viscous than normal mare lavas. Scientists working with LRO data have brought to light new information about the Lassell Massif, a red spot just east of 9 km wide Lassell C. It is a hilly ridge of older material surrounded by younger lavas of Mare Nubium. The LRO mosaic depicts the area, the chart labeled "a" shows the topography of half of Lassell C and the Massif, and "b" presents an interpretive geologic map. Lassell G & K are suggested to perhaps be volcanic pits or explosion craters. The image at the far right was constructed from LRO's Diviner infra-red data with the purple-blue representing material that is silica-rich. This is strong support for the idea that this red spot does represent eruptions of magmas more evolved than mare lavas.

Chuck Wood

Related Links
Rükl plate 54
21st Century Atlas chart 16.

Yesterday's LPOD: Hidden Roughness

Tomorrow's LPOD: Four Worlds


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