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here for larger, original NASA image
Click
here for lunar chart showing location
In contrast to figure 45, which is an oblique view looking southward,
this is a vertical view arranged for stereoscopic viewing. North is at
the top and the crater Descartes (D) is partly visible at the lower edge.
The craters North Ray (N) and South Ray (S) are prominent landmarks used
during the planning and conduct of the mission. The LM landed between the
two. The age of South Ray is discussed in more detail in figure 105. The
smooth materials filling most topographically low areas are mapped as the
Cayley Formation. Samples of the Cayley excavated from the craters were
collected by the astronauts. Most of the samples consisted of feldspar
rich breccia. This is consistent with an early interpretation (Eggleton
and Marshall, 1962) that the Cayley accumulated as ejecta from large multiringed
basins, probably Imbrium (1400 km to the northwest) and Orientale (2800
km to the west). The more rugged material immediately east of the landing
site is designated as the Descartes Formation. Originally interpreted as
volcanic deposits, it is now thought to consist mostly of breccia, although
the samples collected may not be representative of the entire formation.
From the evidence presently available, its origin as basin ejecta, possibly
from the Nectaris basin 450 km to the east, seems to be the most likely
explanation. -G.G.S.
Report Source: NASA SP-362, Page 58, Figure 46
This web page was created by Francis Ridge
for The Lunascan Project
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