- 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...
- 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...
- of KREEP) is
located within the
regions of Oce****
Procellarum and the
Imbrium basin, a
unique geochemical province now
referred to as the Procellarum...
- Ampère. The
Montes Apenninus were
formed by the
impact that
created Mare
Imbrium. The
mountain was
named after the
Dutch astronomer,
mathematician and physician...
-
fairly old. This
range forms the
southeastern border of the
large Mare
Imbrium lunar mare and the
northwestern border of the
Terra Nivium highland region...
- that a
large portion of
these might instead be
derived from the
Imbrium basin. The
Imbrium impact basin is the
youngest and
largest of the multi-ring basins...
- – 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...
- m****if in the
Montes Apenninus range,
along the
eastern edge of the Mare
Imbrium. It is
located to the west of the
crater Conon. To the west of this peak...
- "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...
