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Vocabulary flashcards covering key terms from Lecture 8b on absolute dating and early Earth time scales.
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Absolute dating
Determines numerical age of rocks/minerals using radioactive decay rather than relative age alone.
Radiometric dating
Method within absolute dating that uses decay of unstable isotopes to calculate age.
Half-life
Time required for half of a radioactive parent isotope to decay into its daughter.
Zircon
A durable mineral (ZrSiO4) that incorporates uranium and is used for U–Pb dating.
Parent isotope
The unstable radioactive isotope that decays to a daughter isotope.
Daughter isotope
The product formed when a parent isotope decays.
Carbon-14
Radioactive carbon isotope used to date organic material; half-life ~5730 years.
Potassium-40
Radioactive isotope that decays to Argon-40; used to date older rocks.
Argon-40
Daughter product of Potassium-40 decay; used in K–Ar dating.
Uranium-238
Radioactive isotope that decays to Lead-206; half-life ~4.5 billion years.
Lead-206
Daughter product in the Uranium-238 decay series.
Uranium-235
Radioactive isotope that decays to Lead-207; half-life ~710 million years.
Lead-207
Daughter product in the Uranium-235 decay series.
Hadean
Earliest Earth eon (about 4.6–4.0 Ga) with differentiation and Moon formation.
Archean
Geologic eon (about 4.0–2.5 Ga) featuring crust formation and early plate tectonics.
Phanerozoic
Eon from about 541 Ma to the present, marked by abundant visible life.
Eonothem
Chronostratigraphic term for the eon-level interval of time.
Erathem
Chronostratigraphic term for the era-level interval; corresponds to a major rock-formation interval.
System
Chronostratigraphic term for the period-level interval in the timescale.
Series
Chronostratigraphic term for the epoch-level interval (a subdivision of a period).
Stage
Chronostratigraphic term for the age-level interval within a Series.
GSSP
Global Boundary Stratotype Section and Point; reference section defining a boundary.
Chronostratigraphic chart
International chart mapping time divisions (eon to stage) to rock units.
Komatiite
Ultramafic volcanic rock common in Hadean–Archean; very high melting temperature.
Greenstone belt
Archean metamorphosed volcanic-sedimentary belts linked to early crust formation.
Acasta Gneiss
Oldest rock in Canada (~4.04 Ga); provides evidence for early crust.
Shield
Ancient, stable interior of a continent consisting of Precambrian crystalline rocks.
Platform
Younger sedimentary cover over a shield, forming the continental platform.
Craton
Stable interior of a continent comprising shield plus platform.
Nebular hypothesis
Theory that the Solar System formed from a rotating solar nebula, leading to planet formation.