
"NASA 1970's Mars penetrator mission concept. The carrier spacecraft would launch the penetrator by rocket from a tube. An umbrella-like deployable fabric decelerator would be used to slow and stabilize the penetrator, which would leave an aftbody antenna at the surface."
The above, although associated with a black & white diagram of the image I've posted in the comments section, still aptly pertains to the striking view portrayed by Ken Hodges:
www.lpl.arizona.edu/~rlorenz/penetrators_asr.pdf
Credit: College of Science/Lunar & Planetary Laboratory/The University of Arizona website
AND!
“…A Mars Science Working Group (MSWG) chaired by Thomas Mutch was established by NASA to develop a science strategy for a future mission (Mars Science Working Group, 1977). It met four times in 1977. The plan assumed two Space Shuttle launches in December 1983 or January 1984, each carrying a spacecraft consisting of an orbiter, a lander with rover, and three penetrators, set to arrive at Mars in September or October 1984. The penetrators would be deployed just before arrival, but the rovers would wait in orbit until the dust storm season was over. Highly elliptical initial orbits would permit magnetospheric studies. After the rovers landed, the orbiters would enter circular orbits, one near-polar at 500 km altitude for global mapping and communication with the penetrators, the other 1000 km high with about a 30° inclination for rover communications. As the rovers might each deploy an instrument station with a seismometer, there could be ten simultaneously operating landed components.
As each orbiter neared the planet, it would deploy three penetrators which would fall on a circle around the centre of the planet’s disk as seen from the approach direction. After deployment the orbiters would be deflected off the approach path to enter orbit. The six penetrators, carrying seismometers and soil and atmospheric analysis equipment, would form a global array. Three would be placed about 500 km apart in an area likely to be seismically active, such as Tharsis. The other three would be spaced about 5000 km apart to give global coverage. Two additional and more sophisticated seismometers would be deployed by the rovers in areas partly shielded from the wind. Latitudes between 50° N and 87° S would be accessible, and the landing ellipses were 200-km-diameter circles. Slopes would have to be less than 45° at the impact point. Site selection was reported in a Penetrator Site Studies document preserved in Tim Mutch’s papers at Brown University. One potential array design was described (Table 36), along with four deployment options which include several additional sites (Table 37). Option 1 was the potential array described in Table 36. The penetrator sites in Table 37 were also described in Manning (1977), in which the site selection work was attributed to T. E. Bunch and Ronald Greeley.
The rover landing ellipses were roughly 50 by 80 km across. Five landing sites were studied using Viking data, in addition to the four sites previously considered by USGS for the Viking Rover (Figures 109 and 110). Only two sites were identified in the MSWG report, Capri and Candor (Table 38, Figures 111 and 112). The other sites were identified in Working Group documents among Tim Mutch’s papers in the archives at Brown University.
The rover landing ellipses in these documents were 65 by 40 km across. The polar orbiter would be able to deploy its rover from orbit at latitudes between 30° N and 50° N (this range could vary, depending on the launch date), whereas the low-inclination orbit could deliver a rover to latitudes between 20° S and 20° N.
Six rover landing sites were identified in a Rover Site Studies report prepared for the Working Group (Table 38a, Figure 111). Most derived from work done earlier for Viking or the Viking rover study, including proposals to land near Viking 1 and visit it or to explore the abandoned A-1 site with its complex geology. In a memorandum dated 9 May 1977, Hal Masursky followed up on discussions at a meeting of the Mars 1984 Mission Study Group held on 1 April. He asked Tim Mutch to request high-resolution stereoscopic Viking imaging coverage of four of these sites, using slightly different coordinates (Table 38b). These, he said, ‘were sites for which we have made traverse plans’. He added that ‘a backup smoother site near B-1’ at Cydonia had also been studied. Eventually the Capri and Candor sites were chosen, and detailed mission plans were prepared (Figure 109). Traverses near the Chryse sites were also prepared, including those in Figure 114.
The Capri site provided access to cratered uplands, crater ejecta and a fluvial channel. Candor was on the floor of the canyon system, with access to thick-layered deposits, canyon wall materials and, at the end of the extended mission, possibly the volcanic plateau surrounding the canyon. Alba had fractured volcanic plains and crater ejecta, but also small channels.
The Mars 1984 rovers had three traverse modes. Mode 1 was for detailed site investigations and involved only short, precise drives as needed for science operations. Mode 2, the ‘survey traverse mode’, would cover about 400 m per sol and could include some observations along the route. Mode 3, the ‘fast traverse mode’, could cover as much as 800 m per sol, including travel at night. The goal was to cover about 200 km during one Mars year and up to 200 km more in an extended mission in the second Mars year.
On 13 May 1977, Carl Pilcher, Hal Masursky and Ron Greeley suggested a variation on the role of penetrators in this mission. Two penetrators would be dropped in the lander target ellipse, carrying beacons to help guide the rover to a precision landing. After the landing they would operate with instruments on the lander itself as a local area seismic network.
The Mars 1984 orbiters would carry cameras, spectrometers for surface composition, infrared and microwave radiometers, a magnetometer, a plasma probe, a radar altimeter and communication relay equipment.
The relationship between Mars 1984 and other missions was considered by the Working Group. If Viking Lander 1 survived long enough, it might provide useful meteorological data for a Mars 1984 landing at Chryse, if that site was chosen. Conversely, Mars 1984 might be reconfigured to gather samples for collection by a sample return mission in about 1990.
Mars 1984 was not funded, probably in part because significant opposition to it arose in the science community. Jim Arnold and Mike Duke objected publicly that the final report of the Working Group did not reflect the group discussions, particularly in its assertions that the rovers were the only realistic option, that they were essential for future Mars Sample Return missions, and that simpler missions (orbiters, hard landers) were ‘a step backwards’. The report also suggested that only Mars rovers would command broad public interest, whereas missions such as Voyager, Jupiter Orbiter/Probe (Galileo) and the Lunar Polar Orbiter would not. This mention of Voyager refers to the outer planet spacecraft, not the earliest version of Viking (Table 2), and the suggestion that it would attract little public interest turned out to be the opposite of the truth. Elbert King (University of Houston) wrote to Mutch on 29 August 1977, stating emphatically that Mars 1984 ‘would only ensure a repeat of the very limited scientific success of Viking – providing mostly only costly clues and ambiguous answers to the important scientific questions’. He argued that only sample return was justified by the cost. This dismal assessment of Viking’s scientific worth stems from its failure to detect life, or to definitively rule it out, but overlooks its detailed characterization of surface and atmospheric composition, meteorology and landing site geology, not to mention the mission’s orbital data…”
WOW, I say again, WOW. The above phenomenal excerpt from “The International Atlas of Mars Exploration”, written by Philip J. Stooke, and most graciously made available by Cambridge Core/Cambridge University Press, at.
Wait one, maybe NOT so gracious.
Apparently, like everybody/place else, one is required to be registered or possibly possess an esteemed enough pedigree in order to be granted access...I apparently burned my one gratis peek:
www.cambridge.org/core/books/international-atlas-of-mars-...
We've come quite a way, eh? From dropping Jarts from orbit to flying a helicopter!
See also:
spaceflighthistory.blogspot.com/2017/08/prelude-to-mars-s...
spaceflighthistory.blogspot.com/2017/08/prelude-to-mars-s...
Both above credit: David S. F. Portree/"No Shortage of Dreams" blogspot
Last, but NOT least. This is a wonderful find, with a lot of fantastic imagery, to include this one. AND, it's still free, with no login/registration required...HOT-DAMN:
rpif.asu.edu/slides_mission_concepts/
Specifically:
rpif.asu.edu/slide_sets/future_mission_concepts/Mars_Pene...
Credit: Ronald Greeley Center for Planetary Studies/Arizona State University website