1977
DOI: 10.3133/pp880
|View full text |Cite
|
Sign up to set email alerts
|

Geology of the Apollo 14 landing site in the Fra Mauro highlands

Abstract: Cross-reference oflunar samples with locations, lunar-surface photographs, status of determining sample location and orientation, megascopic sample description, and comments by the astronaut crew during sample collection____ Usage of film on the lunar surface during the Apollo 14 mission________________________________________________ Sequential listing within each magazine of 60 mm Apollo

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
48
0

Year Published

1992
1992
2021
2021

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 34 publications
(50 citation statements)
references
References 10 publications
(21 reference statements)
2
48
0
Order By: Relevance
“…The landing site shows numerous subdued craters up to several hundreds of meters across and the regolith was estimated to be 10-20 m thick (Swann et al 1971). The geology of the Fra Mauro area is discussed in detail in Chapter 2 and by Chao (1973), Swann et al (1977), Hawke and Head (1977), and Simonds et al (1977).…”
Section: Apollo 14 (January-february 1971)mentioning
confidence: 98%
“…The landing site shows numerous subdued craters up to several hundreds of meters across and the regolith was estimated to be 10-20 m thick (Swann et al 1971). The geology of the Fra Mauro area is discussed in detail in Chapter 2 and by Chao (1973), Swann et al (1977), Hawke and Head (1977), and Simonds et al (1977).…”
Section: Apollo 14 (January-february 1971)mentioning
confidence: 98%
“…At the Apollo 14 site, much of the material in the Fra Mauro Formation probably consists of locally derived material excavated by secondary impacts related to the Imbrium event rather than primary Imbrium ejecta, however (Hawke and Head, 1977). Sample 14321 was collected on the rim of a 340-m diameter crater and is thought to represent Fra Mauro material derived from about 65 m below the surface (Swann et al, 1977).…”
Section: Apollo 14 Brecciamentioning
confidence: 99%
“…With the return of the Apollo 14 rocks and soils in 1971, the Preliminary Examination Team reported that the majority of the rocks were breccias (Swann et al 1977). Only four rocks were reported to be basalts: (1) 14310 and its smaller pair, 14073; and (2) 14053 and its smaller pair, 14072.…”
Section: Introductionmentioning
confidence: 97%
“…This sample was chipped from a large (~0.5 m long) boulder at station C2, about 130 m south of the rim of Cone crater, during EVA 2 of Apollo 14 (Swann et al 1977). Basalt 14053 is relatively coarse-grained, but otherwise is typical of other Apollo 14 high-Al basalts.…”
Section: Introductionmentioning
confidence: 99%