What’s Really Waiting to be Mined on the Moon
Warwick Grey
– April 15, 2026
4 min read

The Moon holds vast, untapped resources that could fuel future space exploration, industrial activities, and energy production. As humanity looks to establish a permanent presence in space, these resources, found in the Moon’s surface regolith (the term for the soil found on the Moon, Mars, and other solid bodies in the Solar System), and in its polar ice deposits, will play a crucial role. Understanding these resources, their locations, and how they can be extracted will lay the foundation for long-term lunar development.
The most immediately valuable resource on the Moon is water ice, found primarily in the permanently shadowed craters near the lunar poles, especially at the lunar South Pole, in areas like Shackleton Crater. Water is critical for sustaining human life and powering space exploration. Early findings, such as those from the Lunar Crater Observation and Sensing Satellite mission, launched by the American National Aeronautics and Space Administration (NASA) in 2009, estimate water ice concentrations as high as 6.3% by mass (this means that there is 6.3g of water ice per 100g of other material) in the Shackleton Crater. This is significant because even small amounts of water on the Moon can be converted into rocket propellant (hydrogen and oxygen) and life-support oxygen. If we can mine lunar ice efficiently, it will drastically reduce the cost of transporting water, oxygen, and fuel from Earth, providing a critical resource for space missions, especially for long-term lunar habitation.
Another critical lunar resource is regolith, the fine dust and broken rock that covers the Moon’s surface. Lunar regolith contains valuable materials like silica, aluminium oxide, iron oxide, magnesium oxide, and titanium oxide, which are essential for construction, manufacturing, and oxygen production.
The regolith’s composition varies across the lunar surface, but it remains an abundant and accessible resource. For example, the maria (dark, flat volcanic plains) are particularly rich in iron and titanium, while the highlands (lighter, older, and more cratered regions) are more abundant in silica and aluminium. The maria are primarily found on the near side of the Moon, facing Earth, while the highlands are distributed across both the near side and far side of the Moon. Regolith will be primarily used as a construction material to build the infrastructure needed for a sustainable lunar base. By heating and fusing regolith, it can be transformed into durable building materials, including landing pads, radiation shielding, and structural components for habitats.
Helium-3, a rare isotope of helium, is another resource found on the Moon that has long captured the imagination of scientists. Deposited over billions of years by the solar wind, helium-3 is present in the regolith, particularly in the maria regions, and its concentration is about 30 parts per million. While this concentration might seem low, it is far higher than on Earth, where helium-3 is extremely rare. Helium-3 is theorised to be suitable as a potential fuel for nuclear fusion, a form of energy generation that would be cleaner and more efficient than traditional nuclear fission. The presence of helium-3 on the Moon makes it a valuable long-term resource, but its practical use in energy production is still decades away, dependent on the further development of fusion technology.
The Moon also contains a variety of critical minerals, including rare earth elements (REEs), such as neodymium, lanthanum, and cerium. These materials are found within the regolith and particularly in the maria regions of the Moon.
The concentrations of REEs in lunar regolith are lower than on Earth, but they are still valuable. Basalts from the Mare Tranquillitatis (Sea of Tranquility), the region of the Moon where Neil Armstrong and Buzz Aldrin landed in 1969, are particularly rich in neodymium and lanthanum, essential for manufacturing high-tech devices and magnets. These elements are also crucial for producing electric vehicles, wind turbines, and batteries, and will play a key role in the development of space-based technologies as well. REEs have substantial demand on Earth for alternative energy technologies and electronics, meaning lunar REEs could provide a sustainable supply of these critical resources, helping to reduce Earth’s reliance on terrestrial mining.
Titanium, another critical metal, is abundant in lunar basalts, particularly in regions such as the Mare Imbrium (Sea of Rains), where concentrations of titanium oxide reach up to 10% by mass. Put simply, if we harvest 100 grams of lunar regolith, 10 grams of it would be titanium oxide. This makes the Moon a rich source of titanium, a metal used extensively in aerospace for its strength, light weight, and resistance to corrosion. Titanium will be essential for the construction of durable space vehicles, habitats, and other infrastructure on the Moon and in space.
Our knowledge of lunar resources is evolving but still incomplete. While remote sensing missions, such as those by NASA and the Chinese Chang’e programme, have provided invaluable data, direct exploration is still limited.
Lunar mining will require advanced technology to identify, extract, and process these valuable resources. Robotic systems will likely play a crucial role in early mining operations, with autonomous excavation machines designed to harvest regolith, extract water ice, and process materials. Magnetic smelting and electromagnetic levitation techniques will enable the extraction of metals from the regolith and its conversion into useful materials for construction and manufacturing.
In the early stages, the Moon’s resources will be used primarily to support space operations. Lunar water and oxygen will be processed into fuel and life support for lunar bases and space missions. Regolith will be turned into construction materials for building the infrastructure needed to sustain human life on the Moon. Only later, when more complex industrial capabilities are developed, will the Moon’s resources begin to flow back to Earth, either for commercial use or to supply deep space missions.