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This Apollo 15 photograph depicts the sinuous Hadley Rille, the Apennine
Mountains trending from lower left to upper right, and the smooth surface
of Palus Putredinus (Marsh of Decay) in the upper left quarter. The Apollo
15 landing site at 26.4° N, 3.7° E (arrow) was selected because
of the variety of important lunar surface features concentrated in the
small area. The Apennine Mountains, with almost 5 km of relief in the area
pictured, are a part of a ring of mountains that surrounds the Imbrium
basin and in which very old rocks are thought to be exposed. The smooth
lava flows of Palus Putredinus formed later, and Hadley Rille, sharply
etched in the mare surface, is thought to be one of the youngest rilles
on the Moon. The V shaped rille originates in a cleft at the base of the
mountains in the south and gradually becomes shallower and less distinct
to the north and west. Layered rocks crop out in its walls at several places.
Near the landing site, the width of the rille is 1.5 km and its depth is
more than 300 m. M.C.M.
Report Source: NASA SP-362, Page 193, Figure 202
This web page was created by Francis Ridge
for The Lunascan Project
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