Publications
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Photogrammetry and altimetry: Part C: frequency distributions of lunar slopes Photogrammetry and altimetry: Part C: frequency distributions of lunar slopes
The metric and panoramic cameras aboard the Apollo 16 spacecraft provided photographs on which photogrammetric techniques may be used to obtain precise measurements of horizontal distances and elevations. These measurements of horizontal distances and elevations. These measurements may in turn be used to obtain slope-frequency distributions of lunar surfaces at various slope lengths and...
Authors
Sherman S.C. Wu, H. J. Moore
Photogeology: Part W: Apollo 16 landing site: summary of Earth-based remote sensing data Photogeology: Part W: Apollo 16 landing site: summary of Earth-based remote sensing data
The purpose of the infrared (IR) and radar study of the Apollo data is to establish lunar surface conditions in the vicinity of the orbital tracks of the Apollo command modules during the J-series missions. Correlations and comparisons between the Earth-based radar observations, IR observations, and other data will be plotted on photomaps produced from the mapping and panoramic cameras...
Authors
S.H. Zisk, Harold Masursky, D.J. Milton, G. G. Schaber, R.W. Shorthill, T.W. Thompson
Photogeology: Part S: mare ridges and arches in southern Oceanus Procellarum Photogeology: Part S: mare ridges and arches in southern Oceanus Procellarum
Low-relief mare features such as ridges and arches are best studied by using stereoscopic photographs taken at low Sun angles. Apollo 16 metric camera photography of the southern Oceanus Procellarum east of Letronne Crater reveals a diversity of subtle features (fig. 29-125) and adds significantly to an understanding of the forms of mare ridges and arches their relative ages, and their...
Authors
George W. Colton, Keith A. Howard, Henry J. Moore
Photogeology: Part Y: physical and geological aspects of heiligenschein measurements Photogeology: Part Y: physical and geological aspects of heiligenschein measurements
Heiligenschein is the upsurge in reflected brightness as zero-phase angle is approached. For the first time, an effort has been made to investigate the diagnostic value of the heiligenschein photometric magnitude on a statistically significant scale. This investigation was performed by using the vertical photography of the Apollo 16 metric camera. The brightness surge of reflected light...
Authors
Robert L. Wildey
Photogeology: Part X: calibration of radar data from Apollo 16 results Photogeology: Part X: calibration of radar data from Apollo 16 results
Orbital and surface photography collected during the Apollo 16 mission can be used to calibrate existing Earth-based, high-resolution radar maps of the lunar surface. The absence of any theoretical treatment of the radar backscatter from irregular rocks has prevented the assignment of radar-echo cross sections to specific size distributions of rocks. This gap will now be filled with the...
Authors
S.H. Zisk, H. J. Moore
Photogrammetry and altimetry: Part B: photogrammetry using Apollo 16 orbital photography Photogrammetry and altimetry: Part B: photogrammetry using Apollo 16 orbital photography
The Apollo 15 and 16 metric and panoramic cameras have provided photographs for accurate topographic portrayal of the lunar surface using photogrammetric methods. In turn, quantitative morphologic analyses of topographic results are invaluable aids in the interpretation of the geologic processes.
Authors
Sherman S.C. Wu, Francis J. Schafer, Raymond Jordan, Gary M. Nakata
Orbital-science investigation: Part C: photogrammetry of Apollo 15 photography Orbital-science investigation: Part C: photogrammetry of Apollo 15 photography
Mapping of large areas of the Moon by photogrammetric methods was not seriously considered until the Apollo 15 mission. In this mission, a mapping camera system and a 61-cm optical-bar high-resolution panoramic camera, as well as a laser altimeter, were used. The mapping camera system comprises a 7.6-cm metric terrain camera and a 7.6-cm stellar camera mounted in a fixed angular...
Authors
Sherman S.C. Wu, Francis J. Schafer, Raymond Jordan, Gary M. Nakata, James L. Derick
Orbital-science investigation: Part G: lineaments that are artifacts of lighting Orbital-science investigation: Part G: lineaments that are artifacts of lighting
Many Apollo 15 orbital photographs, particularly those taken at low Sun-elevation angles, reveal grid patterns of lineaments. In some circumstances, the grid pattern is present in areas where structural control seems unlikely. For example, in an oblique view (fig. 25-52), the ejecta blankets of two fresh impact craters seem to have two intersecting sets of lineaments. Because previous...
Authors
Keith A. Howard, Bradley R. Larsen
Geological, geophysical, and engineering investigations of the Loveland Basin landslide, Clear Creek County, Colorado, 1963-65 Geological, geophysical, and engineering investigations of the Loveland Basin landslide, Clear Creek County, Colorado, 1963-65
No abstract available.
Authors
Charles Sherwood Robinson, Fitzhugh T. Lee, R.W. Moore, R. D. Carroll, J. H. Scott, J.D. Post, C. S. Robinson, R.A. Bohman
Photogeology: Part G: structural aspects of Imbrium sculpture Photogeology: Part G: structural aspects of Imbrium sculpture
Apollo 16 metric photographs taken at low to high Sun angles (from approximately 7° to 40°) provide the first stereographic coverage of the distinctive landforms collectively referred to as "Imbrium sculpture" (refs. 29-40 and 29-41). The sculpture consists of a series of nearly linear ridges and troughs extending radially outward for more than 1000 km from the rim of the Imbrium Basin...
Authors
David H. Scott
Orbital-science investigation: Part B: photogrammetric analysis of Apollo 15 records Orbital-science investigation: Part B: photogrammetric analysis of Apollo 15 records
The three cameras—stellar, mapping, and panoramic—together with the laser altimeter, all included in the scientific instrument module (SIM) bay, represent an integrated photogrammatric system with extraordinary potential for extending knowledge of the lunar figure, surface configuration, and geological structure.
Authors
Frederick J. Doyle
Photogeology: Part B: Cayley Formation interpreted as basin ejecta Photogeology: Part B: Cayley Formation interpreted as basin ejecta
The discovery that samples returned from the Cayley Formation at the Apollo 16 landing site consist mainly of nonvolcanic breccias (secs. 6 and 7 of this report) suggests that the hypothesis in which light plains-forming materials may be ejecta from multi-ring basins should be reevaluated (refs 29-15 to 29-17). Improved information on the morphology and distribution of the Cayley...
Authors
R. E. Eggleton, G. G. Schaber