LUNAR SURFACE ACTIVITY

Because the astronauts who landed on the Moon would be required to act as field geologists, a series of lectures and laboratory exercises were given in 1964 by the US Geological Survey (USGS) in a ramshackle shed of Second World War vintage at Ellington Air Force Base, which served as the airport for the Manned Spacecraft Center. On being introduced to the vocabulary of geology and basic mineralogy, the astronauts were taught how to describe rocks and to characterise a geological setting in terms of the granularity and bearing strength of its surface. Some of the astronauts – mainly those of the first group who were still active,[10] but also some of the second group – argued that there was no requirement for such training because the rocks they returned would be studied by the scientists. But other members of the second group and most of the third group, aware that they were unlikely to be assigned the first landing, looked ahead to the later missions on which science was certain to be a significant factor and reasoned that by taking the subject seriously they would improve their chances of a flight assignment.

The first geology field trip was to the Grand Canyon, incised into the Arizona Plateau by the Colorado River to a depth of some 6,000 feet. Viewing the strata exposed in the canyon wall was undoubtedly awe inspiring, but most of it was sedimentary and (the nomenclature for the lunar features notwithstanding) there were no rivers on the Moon. Later trips included Meteor Crater in Arizona, which seemed more relevant because the Moon was pocked by craters. Since there was at that time no consensus as to whether lunar craters were formed by impacts or by volcanism, trips were also made to a wide variety of volcanic features across the American southwest. Jack Schmitt, who joined NASA in 1965 as one of the first group of scientist-astronauts, and had a doctorate in geology from Harvard, was assigned to assist in geological training. He encouraged Armstrong and Aldrin to find time to make field trips. At a volcanic field near Cinder Lake in Arizona, the Astrogeology Branch of the USGS blasted a simulated lunar landscape based on a picture of a potential landing site taken by a Lunar Orbiter. Geologists then made ‘traverses’ wearing training space suits to evaluate procedures, test the tools that the astronauts were to employ, and determine what could reasonably be done in the time

Using a mockup of the LM hatch, porch and upper ladder. Buzz Aldrin undergoes one-sixth gravity training in a KC-135 on 10 July 1969Г

available to the first moonwalk. A crude LM was constructed as a perch from which to make visual observations. On his Mercury mission, Wally Schirra had been given an off-the-shelf Hasselblad 500C camera manufactured by the Victor Hasselblad Company in Sweden. NASA later asked the company to supply it with a modified version. The mechanism had to be capable of 5,000 ‘working cycles’ in Earth’s atmosphere, in pure oxygen, and in a vacuum; accommodate a magazine with a capacity of 160 exposures of 70-millimetre ‘thin’ film; and incorporate an electric motor to advance the film.[11] This camera was introduced on Gemini, and carried over to Apollo. The geologists conducted tests using a Hasselblad 500EL Data Camera configured for use by a suited astronaut, notably with its view sight deleted. The results were studied to determine how much of what was known of the terrain could be inferred from just the visual observations and photographs. The trials, conducted early in 1968, were led by Arnold Brokaw, chief of the surface planetary exploration section of the Astrogeology Branch. The conclusions were fed to Houston by Eugene M. Shoemaker, the branch chief, who was seconded to NASA. Shortly prior to the mission, Brokaw visited Armstrong to emphasise the value of photographing rocks, irrespective of whether these were sampled: ‘‘ft is important to us how a rock got where it is, how and where it lay, how it relates to other things in the area; we can determine a lot about its mineralogy simply from photographs.” Aldrin was inspired by geology, because it ‘‘opened my eyes to the immensity of time’’. Collins was not, ‘‘f hate geology – maybe that’s why they won’t let me get out on the Moon.’’ Armstrong, displaying an impishness worthy of Pete Conrad, later admitted that he had been ‘‘very tempted to sneak a piece of limestone up’’ and place it into a rock box as a sample, to see what the scientists would make of it.

The training for lunar surface activities was undertaken in Building 9 of the Manned Spacecraft Center campus, where there was a mockup LM. The astronauts suited up and donned all the extravehicular paraphernalia and, while attended by technicians from the crew systems division and the suppliers of the miscellaneous apparatus, they tested egress and ingress procedures, surface sampling tools, and the deployment of the scientific packages. The scientific community wanted the maximum work from Armstrong and Aldrin while they were on the lunar surface. Each task was timed during training, and integrated into the overall time line. A significant milestone was attained on 18 June 1969 by a full ‘walk through’ which included deploying the EASEP instruments. However, while the technical fidelity was high, this training was done in full Earth gravity. To familiarise themselves with lunar gravity – which is one-sixth that of Earth – the astronauts flew in a KC-135 aircraft (the military version of the Boeing 707) with its cabin deck cleared and padded. This aircraft would fly a precise arc, zooming, cresting and falling in order to simulate the desired gravitational load. During the climb the suited astronaut was held in position by technicians, and when the desired gravity was reached he had to

Neil Armstrong and Buzz Aldrin rehearse ‘documented’ (photographed) sampling using a scoop, a gnomon and individual sample bags.

Buzz Aldrin, having deployed the SWC.

Neil Armstrong starts to deploy the LRRR.

Buzz Aldrin documents the site with a panoramic sequence around the horizon.

The simulation over, Neil Armstrong prepares to ascend the ladder.

set up, conduct the test and then be restrained once more against the load of three gravities as the aircraft pulled out of its dive. The cabin was voluminous, but with technicians, film crew and Air Force supervisors lending assistance it soon became crowded. The aircraft would make several dozen arcs over a period of hours, flying a roller-coaster path through the sky. Inevitably someone would vomit.3 While this training was valuable, the fact that it simulated lunar gravity for no more than 30 seconds per time meant that it was possible only to test specific tasks, such as using a pair of tongs to lift a rock and pop it into a bag. To rehearse long sequences of tasks, systems using cables and pulleys were built – in some cases with the astronaut operating at an angle against a tilted surface. As Armstrong observed of these ‘Peter Pan’ rigs: ‘‘You had the feeling of being able to jump very high – a very light feeling. You also had the feeling that things were happening slowly, which indeed they were. It was a sort of floating sensation.’’ On the other hand, he was confident, ‘‘The lunar setting will become a very easy place to work, I think.’’