The instrument collected 26 readings in total during the Apollo 17 mission. Three instrument readings were taken to establish the thermal state of the instrument, once at the beginning of each EVA with no gravity readings collected. Measurements were taken in two different positional states to help "normal" other measurements. This included measurement with the instrument upside down and both on and off the lunar roving vehicle. 6 measurements were taken at the
Lunar module landing site with 11 measurements taken at a variety of locations during the missions 3 EVA's. Two locations also had repeat measurements taken with the instrument off the Lunar Roving Vehicle. The 25th measurement may have been disrupted due to a pallet swinging open and causing issues with the instrument.
Results The experiment found that the Lunar Module landing site had a gravity value of 162694.6 ± 5 mgal. The edges of the valley proximal to the landing site had gravity values around 25 mgal lower than the landing site. These results with interpreted to represent a 1km thick layer of volcanic basalt infilling the valley. This basalt was estimated to have a density that was 0.8g/cm3 greater than the surrounding valley walls. It was found that the instrument was particularly sensitive to impacts when the instrument was removed from the lunar rover and place on the lunar surface. These would produce notable shifts in the readings the instrument would provide and the effect was cumulative. == References ==