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Home > Holt Earth Science Chapter 12, Section 12.3

Holt Earth Science Chapter 12, Section 12.3

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Environmental Science [1]
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Chemistry [2]
Physics [3]
Nature [4]
Nuclear physics [5]
Radioactivity [6]
Nuclear chemistry [7]
Isotopes [8]
Radioactive decay [9]
Radiometric dating [10]
Neutron [11]
Atom [12]
Radionuclide [13]

Dating With Radioactivity It is possible to measure numerical values for the age of Earth?s geologic activities - in billions and millions of years - by using radiometric dating. A. Reviewing Basic Atomic Structure An atom has a nucleus with protons (positive) and neutrons (proton+electron combined = neutral) orbited by electrons (negative charge). Atomic Number = number of protons in the nucleus; each element?s Atomic Number differs. Atoms of the same element have the same number of protons. 99.9% of an atom?s mass is in the nucleus - electrons have hardly any mass. By adding together the number of protons and neutrons, the atomic mass of an atom is obtained. The number of neutrons varies (called isotopes; have different atomic masses).

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