Scientists are using ultra-sensitive underground particle detectors around the world to track geoneutrinos—subatomic particles generated deep within the planet by the radioactive decay of elements like uranium and thorium. By detecting these “ghostly” particles, researchers are beginning to map and understand the radioactive heat engine driving Earth’s plate tectonics, mantle convection, and magnetic field.
* Deep Underground Observatories: To catch geoneutrinos, detectors must be shielded from background cosmic rays.
Experiments like SNO+ (located 2 km underground in Sudbury, Canada) and the JUNO experiment in China utilize thousands of tons of ultrapure liquid and light sensors buried deep in rock mines to capture the faint flashes of light produced when neutrinos hit the detectors.
* Probing Earth’s Hidden Heat: A significant portion of the heat driving Earth’s interior processes comes from radioactive decay within the crust and mantle. Because neutrinos pass through solid rock unhindered, geoneutrinos provide a direct line of sight into inaccessible regions thousands of kilometers below the surface.
* Building a Global Map: A growing network of underground detectors is gathering substantial new measurement data, helping geoscientists test and refine models of Earth’s mantle composition, thermal budget, and volatile internal dynamics.
1. What are Geoneutrinos?
Neutrinos are extremely lightweight, subatomic particles that rarely interact with ordinary matter. Geoneutrinos are specifically the electron antineutrinos produced when radioactive isotopes—primarily uranium, thorium, and potassium—decay deep within Earth’s crust and mantle.








