Built by a geologist
Mineral Magnetism Test Chart
Mineral magnetism is a useful screening property, not an identification verdict. Magnetite commonly gives a strong hand-magnet response, while pyrrhotite can range from weakly to readily magnetic. Hematite or ilmenite specimens may appear weakly magnetic when magnetite is intergrown or attached. A whole rock or sand is a mixture, so one magnetic grain can create a localized response. Use a small enclosed magnet near an intact surface without dragging it, record strong, weak, absent, or localized movement, and repeat the observation. Keep magnets away from implanted medical devices, magnetic storage and cards, compasses, and sensitive instruments; follow magnet and device manufacturer guidance. Magnetic attraction does not confirm a meteorite because terrestrial magnetite-rich rocks and industrial materials are much more common. Bubbles, a red or black streak, industrial context, interior texture, and qualified examination help test that explanation. GeoMiner's private lookup accepts only one of three bounded response categories, records no specimen name, free text, photo, location, magnet strength, or device information, and hands the observation to Quick ID without an account. Combine it with streak, hardness, lustre, cleavage, heft, texture, and geologic context.