All right, it's Wednesday, and that means a new post for Eyes Turned Skywards. This week: Apollo 18. (Topic for discussion: would they end up making a slasher movie called
Apollo 19 ITTL? Might it be any good?) I'd like to thank everyone who put in names for the Apollo 18 CM/LM, and to those people who helped me figure out where the CM would end up. Anyway, without further ado, this week's installment of Eyes Turned Skyward:
Eyes Turned Skyward, Post #5:
Over the course of 1970, the slow death of the Apollo Applications Program, combined with an increasing focus by NASA on a space- station following the Apollo missions and the continuing budget cuts by a Congress hostile to continued space exploration began to take its toll on the Moon landing program. Originally, there were to be 14 manned Block II flights, Apollos 7-20, with the last 13 of those requiring the Saturn V, and the last 10 landing on the Moon. Further, these would be proceeded by two test flights of the Saturn V, Apollo 4 and Apollo 6, leading to the use of 15 Saturn Vs in all, exactly the size of the first production run. All very fine on paper, but events proved that this plan was unworkable when the second production run of Saturn Vs was canceled in late 1968, at the same time that Skylab was reworked into the dry workshop configuration, and now required a Saturn V for launch. Apollo 20 ended up sacrificed on the alter of Skylab as a result. As the year proceeded, even the reduced program so created became increasingly untenable. With the perceived need in NASA to have a Skylab follow-up ready for launch when Skylab itself ended--something that would clearly require another Saturn V to be available--and further budget cuts (threatened and imposed) by Congress, it became necessary to save another Saturn V in reserve, sacrificing another lunar mission. Despite earlier proposals to cancel then-Apollo 19 as well, or even all future lunar missions, only Apollo 15 ended up having to take the bullet for the rest of the program thanks to shrewd negotiation by NASA's management, the support of OMB Deputy Director Caspar Weinberger, and pressure from the scientific community.
Thus, even as preparations for the Skylab stations and improved hardware continued, NASA wrapped up the Apollo program with the fourth and final J-class mission, Apollo 18’s trip to Hyginus Crater. Like Apollo 15, 16, and 17, Apollo 18 would feature a lunar rover, and continue to push the Lunar Module to its absolute limits. However, fighting these goals to get the most out of the final Apollo mission was the feeling among many in the NASA structure that conservative planning was required. By 1973, spaceflights to the moon had become routine, almost to the level that a well-executed mission would not play in the public eye at all. However, if a mission was to be another dramatic failure, like Apollo 13 or worse, it could endanger the future of all of NASA’s programs.
This balancing act between a scientifically focused mission and one that would not take unnecessary risks was perhaps best embodied in the crew. The Commander selected was Richard Gordon Jr, a space veteran who had flown with Pete Conrad on Gemini 11 and as Comand Module Pilot on Apollo 12. Apollo 18 would be his second visit to lunar space. Joining him, though, were two astronauts on their first flights. Vince D. Brand was similarly a test pilot, and though his flight to the moon as Command Module Pilot of Apollo 18 would be his first, he had acted as backup for several other missions and played a role in ground-testing of Apollo hardware. The Apollo 18 Lunar Module Pilot, though, was an embodiment of the boundaries later Apollo missions were pushing. Harrison Schmidt was not a test pilot by trade, but a geologist, the first of a class of “scientist-astronauts.” While his training and experience with the Apollo equipment was in no means lacking, his lack of military flying background made him an exception. Though the results returned on previous missions with geology-trained pilots were acceptable, many scientists looked forward to seeing the flight of a flight-trained geologist. Indeed, this desire was so strong that when the cancellation of the Apollo 19 mission was considered along with the original Apollo 15, there was a serious push inside NASA to have Joseph Engle bumped from his flight to make room for Schmitt.
With mission goals that would strike a balance between stretching the Apollo capabilities in pursuit of science and the worries about avoiding a very public failure on the final moon launch, Apollo 18 flew skyward in a trouble-free launch in July, 1973. The Apollo hardware demonstrated its maturity: no serious issues were encountered with the Saturn V, the Apollo capsule
Windjammer, or the Lunar Module
Polaris, and the mission managed to slightly edge out Apollo 17 to set new records for duration on the surface, EVA times, and mass returned as engineers fine-tuned the Apollo system to realize every gain that could be made without risking the mission. Schmitt performed all his flight tasks perfectly, and the only complaint from the scientists was that the single TV camera per mission meant Schmitt’s investigations could only be heard over the radio, with camera focus only on the most interesting finds.
The geologic potential of the mission were astounding. The landing site, Hyginus Crater and the associated rille, were interesting in several senses. First, Hyginus itself was an anomaly among the multitude of craters scattered over the lunar surface: it lacked the traditional raised outer rim, indicating a possible volcanic origin. If confirmed, and especially with additional data about the many theories for rille origins, it could reveal fascinating new insights into the moon’s volcanic history. Schmitt’s mission would be a geologist’s playground, with a landing on the flat lunar surface at 7*32’47” N, 6*26’20” E. The first rover traverse would cover 15 km, including a drive along the rim of both the crater and the rille, the second would cover another 15 km venturing into the crater, while the final traverse would cover only 11 km but cover several km of the rille bottom.
The mission achieved every major objective, and the geologic results helped form a better picture of the moon’s volcanic features. The crater was revealed to have indeed been formed volcanically, and the discoveries made from analysis of the rille included the possibility of lunar lava tubes. In addition to the intriguing speculations this created about the moon’s history, this also fueled the trend of “tube colonies” that made an appearance in many science fiction stories of the late 70s and 80s, though the first actual lava tube (in the Marius Hills) would not be confirmed for several decades.
The Apollo 18 Command Module
Windjammer was initially displayed at the Luftwaffenmuseum der Bundeswehr, but in 1983 it returned to the United States and is now on display in the space gallery of the Museum of Flight in Seattle.