On 7 December 1972, the Apollo 17 mission launched from the Kennedy Space Centre, marking the final crewed lunar landing of the Apollo programme. As the concluding expedition of this historic series, the mission represented the culmination of years of lunar exploration and technological advancement.

A significant aspect of this mission was the inclusion of Harrison Schmitt, a professional geologist. His presence on the crew ensured that scientific fieldwork and geological research became a central focus of the expedition, allowing for a more detailed analysis of the lunar surface than had been possible on previous flights.

The mission objectives were designed to maximise the scientific return from the Moon, with the crew conducting extensive geological surveys and deploying various experiments. The success of Apollo 17 provided invaluable data that continues to inform our understanding of lunar history and the evolution of the solar system.

Key highlights of the Apollo 17 mission included:

• The final crewed lunar landing of the Apollo programme.
• The inclusion of geologist Harrison Schmitt to lead scientific fieldwork.
• The collection of a diverse range of lunar rock and soil samples.
• The deployment of sophisticated surface experiments.
• The safe return of the crew to Earth, concluding the Apollo era.

By prioritising rigorous scientific investigation, the Apollo 17 mission left a lasting legacy in the field of planetary science. It remains a landmark achievement in human spaceflight, demonstrating the capacity for complex geological research in the challenging environment of the lunar landscape.