- Mare
Imbrium /ˈɪmbriəm/ (Latin
imbrium, the "Sea of Showers" or "Sea of Rains") is a vast lava
plain within the
Imbrium Basin on the Moon and is one of...
- of KREEP) is
located within the
regions of Oce****
Procellarum and the
Imbrium basin, a
unique geochemical province now
referred to as the Procellarum...
- been
formed from ejecta, or debris, from the
impact which formed Mare
Imbrium.
During Apollo 14, the crew
members sampled ejecta from Cone crater, a...
-
impact of the
South Pole–Aitken basin.
Other large impact basins such as
Imbrium, Serenitatis, Crisium, Smythii, and
Orientale possess regionally low elevations...
-
Montes Apenninus is the most
prominent remnant of the
outer ring of the
Imbrium basin,
which also
includes Montes Carpatus to its
south and
Montes Caucasus...
-
formed by the
impact that
created Mare
Imbrium. Mons
Huygens rises 5,300 m (17,380 ft) from its Mare
Imbrium base, per
altimetry data from the Lunar...
-
believed to
contain much
material spattered by the
impact that had
filled the
Imbrium basin early in the Moon's history.
Dating it
would provide information...
- – Lunokhod-1
rover traveled 10.5 km (6.5 mi)
across lunar surface Mare
Imbrium 038.28N 325.00E Luna-18 5,750
Proton 2
September 1971
Sample return Failure...
-
terrain found in
lunar highlands. The
period ended with the
formation of the
Imbrium basin,
which initiated the
Imbrian Period.
Magnetic anomalies found in...
- "J-missions", in July 1971. The site is
located on the
eastern edge of Mare
Imbrium on a lava
plain known as
Palus Putredinis. Hadley–Apennine is bordered...
