Laurence Soderblom, PhD (Former Employee)
Science and Products
Filter Total Items: 137
Preliminary geological mapping of Io Preliminary geological mapping of Io
Terrain units and their global distribution on Io are summarised. A map of the complex region of Io is also presented. ?? 1979 Nature Publishing Group.
Authors
H. Masursky, G. G. Schaber, L.A. Soderblom, R.G. Strom
The Jupiter system through the eyes of Voyager 1 The Jupiter system through the eyes of Voyager 1
The cameras aboard Voyager 1 have provided a closeup view of the Jupiter system, revealing heretofore unknown characteristics and phenomena associated with the planet's atmosphere and the surfaces of its five major satellites. On Jupiter itself, atmospheric motions—the interaction of cloud systems—display complex vorticity. On its dark side, lightning and auroras are observed. A ring was
Authors
B.A. Smith, L.A. Soderblom, T. V. Johnson, A.P. Ingersoll, S.A. Collins, E.M. Shoemaker, G.E. Hunt, H. Masursky, M. H. Carr, M. E. Davies, A.F. Cook, J. Boyce, G. E. Danielson, Tobias Owen, C. Sagan, R.F. Beebe, J. Veverka, R.G. Strom, J.F. McCauley, D. Morrison, G.A. Briggs, V.E. Suomi
Apollo over the Moon: A view from orbit Apollo over the Moon: A view from orbit
No abstract available.
Authors
Harold Masursky, G. W. Colton, Farouk El-Baz, Frederick J. Doyle, Richard E. Eggleton, Maurice J. Grolier, James W. Head, Carroll Ann Hodges, Keith A. Howard, Leon J. Kosofsky, Baerbel K. Lucchitta, Michael C. McEwen, Henry J. Moore, Gerald G. Schaber, David H. Scott, Laurence A. Soderblom, Mareta West, D.E. Wilhems
Global color variations on the Martian surface Global color variations on the Martian surface
Surface materials exposed throughout the equatorial region of Mars have been classified and mapped on the basis of spectral reflectance properties determined by the Viking II Orbiter vidicon cameras. Frames acquired at each of three wavelengths (0.45 ± 0.03 μm, 0.53 ± 0.05 μm, and 0.59 ± 0.05 μm) during the approach of Viking Orbiter II in Martian summer (Ls = 105°) were mosaicked by...
Authors
L.A. Soderblom, K. Edwards, E. M. Eliason, E.M. Sanchez, M.P. Charette
Possible fossil H2O liquid-ice interfaces in the Martian crust Possible fossil H2O liquid-ice interfaces in the Martian crust
Throughout the northern equatorial region of Mars, extensive areas have been uniformly stripped, roughly to a constant depth. These terrains vary widely in their relative ages. A model is described here to explain this phenomenon as reflecting the vertical distribution of H2O liquid and ice in the crust. Under present conditions the Martian equatorial regions are stratified in terms of...
Authors
L.A. Soderblom, D. B. Wenner
Voyager imaging experiment Voyager imaging experiment
The overall objective of this experiment is exploratory reconnaissance of Jupiter, Saturn, their satellites, and Saturn's rings. Such reconnaissance, at resolutions and phase angles unobtainable from Earth, can be expected to provide much new data relevant to the atmospheric and/or surface properties of these bodies. The experiment also has the following specific objectives: Observe and
Authors
B.A. Smith, G.A. Briggs, G. E. Danielson, A.F. Cook, M. E. Davies, G.E. Hunt, H. Masursky, L.A. Soderblom, T.C. Owen, C. Sagan, V.E. Suomi
Lunar surface chemistry: A new imaging technique Lunar surface chemistry: A new imaging technique
Detailed chemical maps of the lunar surface have been constructed by applying a new weighted-filter imaging technique to Apollo 15 and Apollo 16 x-ray fluorescence data. The data quality improvement is amply demonstrated by (i) modes in the frequency distribution, representing highland and mare soil suites, which are not evident before data filtering and (ii) numerous examples of...
Authors
C.G. Andre, M.J. Bielefeld, E. Eliason, L.A. Soderblom, I. Adler, J.A. Philpotts
Preliminary results from the Viking orbiter imaging experiment Preliminary results from the Viking orbiter imaging experiment
During its first 30 orbits around Mars, the Viking orbiter took approximately 1000 photographic frames of the surface of Mars with resolutions that ranged from 100 meters to a little more than 1 kilometer. Most were of potential landing sites in Chryse Planitia and Cydonia and near Capri Chasma. Contiguous high-resolution coverage in these areas has led to an increased understanding of...
Authors
M. H. Carr, H. Masursky, W.A. Baum, K.R. Blasius, G.A. Briggs, J.A. Cutts, T. Duxbury, R. Greeley, J. E. Guest, B.A. Smith, L.A. Soderblom, J. Veverka, J.B. Wellman
Viking orbital colorimetric images of mars: Preliminary results Viking orbital colorimetric images of mars: Preliminary results
Color reconstruction and ratios of orbital images of Mars confirm Earth-based measurements showing red/violet ratios for bright areas to be roughly 1.5 times greater than dark areas. The new results show complex variation among dark materials; dark streaks emanating from craters in southern cratered terrains are much bluer than dark materials of the north equatorial plains on which...
Authors
L.A. Soderblom
Origin of lunar light plains Origin of lunar light plains
Most Cayley-type Imbrian-age plains deposits and adjacent mantled slopes, including those at the Apollo 16 site, may be composed at least near the surface of ejecta from the Orientale basin, the youngest multiringed impact basin on the Moon. The distribution and apparent age of the plains deposits and preliminary data on the highly feldspathic breccias collected by the Apollo 16 crew...
Authors
E. C. T. Chao, Carroll Ann Hodges, J. M. Boyce, L.A. Soderblom
A summary of relative ages of lunar nearside and farside plains A summary of relative ages of lunar nearside and farside plains
This report contains a summary of the moon-wide distribution of relative ages of lunar plains units determined with Apollo and Lunar Orbiter photographs. Relative ages are expressed as the largest diameter of craters (DL, meters) in a mappable unit that are eroded to a slope of 1 ° by the net accumulated flux of small impacts. New data show that the technique used here generally requires...
Authors
Joseph M. Boyce, Arthur L. Dial, Laurence A. Soderblom
Simulated “true color” images from ERTS data Simulated “true color” images from ERTS data
No abstract available.
Authors
Eric M. Eliason, Pat S. Chavez, Laurence A. Soderblom
Science and Products
Filter Total Items: 137
Preliminary geological mapping of Io Preliminary geological mapping of Io
Terrain units and their global distribution on Io are summarised. A map of the complex region of Io is also presented. ?? 1979 Nature Publishing Group.
Authors
H. Masursky, G. G. Schaber, L.A. Soderblom, R.G. Strom
The Jupiter system through the eyes of Voyager 1 The Jupiter system through the eyes of Voyager 1
The cameras aboard Voyager 1 have provided a closeup view of the Jupiter system, revealing heretofore unknown characteristics and phenomena associated with the planet's atmosphere and the surfaces of its five major satellites. On Jupiter itself, atmospheric motions—the interaction of cloud systems—display complex vorticity. On its dark side, lightning and auroras are observed. A ring was
Authors
B.A. Smith, L.A. Soderblom, T. V. Johnson, A.P. Ingersoll, S.A. Collins, E.M. Shoemaker, G.E. Hunt, H. Masursky, M. H. Carr, M. E. Davies, A.F. Cook, J. Boyce, G. E. Danielson, Tobias Owen, C. Sagan, R.F. Beebe, J. Veverka, R.G. Strom, J.F. McCauley, D. Morrison, G.A. Briggs, V.E. Suomi
Apollo over the Moon: A view from orbit Apollo over the Moon: A view from orbit
No abstract available.
Authors
Harold Masursky, G. W. Colton, Farouk El-Baz, Frederick J. Doyle, Richard E. Eggleton, Maurice J. Grolier, James W. Head, Carroll Ann Hodges, Keith A. Howard, Leon J. Kosofsky, Baerbel K. Lucchitta, Michael C. McEwen, Henry J. Moore, Gerald G. Schaber, David H. Scott, Laurence A. Soderblom, Mareta West, D.E. Wilhems
Global color variations on the Martian surface Global color variations on the Martian surface
Surface materials exposed throughout the equatorial region of Mars have been classified and mapped on the basis of spectral reflectance properties determined by the Viking II Orbiter vidicon cameras. Frames acquired at each of three wavelengths (0.45 ± 0.03 μm, 0.53 ± 0.05 μm, and 0.59 ± 0.05 μm) during the approach of Viking Orbiter II in Martian summer (Ls = 105°) were mosaicked by...
Authors
L.A. Soderblom, K. Edwards, E. M. Eliason, E.M. Sanchez, M.P. Charette
Possible fossil H2O liquid-ice interfaces in the Martian crust Possible fossil H2O liquid-ice interfaces in the Martian crust
Throughout the northern equatorial region of Mars, extensive areas have been uniformly stripped, roughly to a constant depth. These terrains vary widely in their relative ages. A model is described here to explain this phenomenon as reflecting the vertical distribution of H2O liquid and ice in the crust. Under present conditions the Martian equatorial regions are stratified in terms of...
Authors
L.A. Soderblom, D. B. Wenner
Voyager imaging experiment Voyager imaging experiment
The overall objective of this experiment is exploratory reconnaissance of Jupiter, Saturn, their satellites, and Saturn's rings. Such reconnaissance, at resolutions and phase angles unobtainable from Earth, can be expected to provide much new data relevant to the atmospheric and/or surface properties of these bodies. The experiment also has the following specific objectives: Observe and
Authors
B.A. Smith, G.A. Briggs, G. E. Danielson, A.F. Cook, M. E. Davies, G.E. Hunt, H. Masursky, L.A. Soderblom, T.C. Owen, C. Sagan, V.E. Suomi
Lunar surface chemistry: A new imaging technique Lunar surface chemistry: A new imaging technique
Detailed chemical maps of the lunar surface have been constructed by applying a new weighted-filter imaging technique to Apollo 15 and Apollo 16 x-ray fluorescence data. The data quality improvement is amply demonstrated by (i) modes in the frequency distribution, representing highland and mare soil suites, which are not evident before data filtering and (ii) numerous examples of...
Authors
C.G. Andre, M.J. Bielefeld, E. Eliason, L.A. Soderblom, I. Adler, J.A. Philpotts
Preliminary results from the Viking orbiter imaging experiment Preliminary results from the Viking orbiter imaging experiment
During its first 30 orbits around Mars, the Viking orbiter took approximately 1000 photographic frames of the surface of Mars with resolutions that ranged from 100 meters to a little more than 1 kilometer. Most were of potential landing sites in Chryse Planitia and Cydonia and near Capri Chasma. Contiguous high-resolution coverage in these areas has led to an increased understanding of...
Authors
M. H. Carr, H. Masursky, W.A. Baum, K.R. Blasius, G.A. Briggs, J.A. Cutts, T. Duxbury, R. Greeley, J. E. Guest, B.A. Smith, L.A. Soderblom, J. Veverka, J.B. Wellman
Viking orbital colorimetric images of mars: Preliminary results Viking orbital colorimetric images of mars: Preliminary results
Color reconstruction and ratios of orbital images of Mars confirm Earth-based measurements showing red/violet ratios for bright areas to be roughly 1.5 times greater than dark areas. The new results show complex variation among dark materials; dark streaks emanating from craters in southern cratered terrains are much bluer than dark materials of the north equatorial plains on which...
Authors
L.A. Soderblom
Origin of lunar light plains Origin of lunar light plains
Most Cayley-type Imbrian-age plains deposits and adjacent mantled slopes, including those at the Apollo 16 site, may be composed at least near the surface of ejecta from the Orientale basin, the youngest multiringed impact basin on the Moon. The distribution and apparent age of the plains deposits and preliminary data on the highly feldspathic breccias collected by the Apollo 16 crew...
Authors
E. C. T. Chao, Carroll Ann Hodges, J. M. Boyce, L.A. Soderblom
A summary of relative ages of lunar nearside and farside plains A summary of relative ages of lunar nearside and farside plains
This report contains a summary of the moon-wide distribution of relative ages of lunar plains units determined with Apollo and Lunar Orbiter photographs. Relative ages are expressed as the largest diameter of craters (DL, meters) in a mappable unit that are eroded to a slope of 1 ° by the net accumulated flux of small impacts. New data show that the technique used here generally requires...
Authors
Joseph M. Boyce, Arthur L. Dial, Laurence A. Soderblom
Simulated “true color” images from ERTS data Simulated “true color” images from ERTS data
No abstract available.
Authors
Eric M. Eliason, Pat S. Chavez, Laurence A. Soderblom