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| central portion of the earth believed to be composed mainly of iron and nickel in a molten state |
| slow movement of water through the pores in soil or permeable rock |
| rubidium-strontium dating | |
| —n | |
| a technique for determining the age of minerals based on the occurrence in natural rubidium of a fixed amount of the radioisotope 87Rb which decays to the stable strontium isotope 87Sr with a half-life of 4.7 × 1011 years. Measurement of the ratio of these isotopes thus gives the age of a mineral, for ages of up to about 4 × 109 years | |