Dating Methods /
Essential Question How can scientists determine the ages of geologic material?
What are strata? Layers of rock
Strata
Folded strata
What is an angular unconformity? When rock deposited in horizontal layers is folded or tilted, then eroded, and then covered by more horizontal layering
Angular unconformity
What is the law of cross-cutting relationships? The fault or igneous intrusion is always younger than the rock layer it cuts through.
Cross-cutting relationship
What are nonconformities? Unstratified igneous or metamorphic rock is eroded and then covered by layers of sediment.
Nonconformity
What are disconformities? The boundary between younger sedimentary rock layers deposited on an eroded layer of older sedimentary rock
disconformity
What are faults? A break or crack in Earth’s crust along which rocks shift their positions
Fault
Earth history in 24 hours scale: 1 sec = 52,000 years 1 min = 3,125, 000 yrs 1 hour = 187,500,000 yrs
What is correlation? Matching geologic materials from different regions to ages
Correlating tree rings
Rates of erosion and deposition Measure the recent rates Estimate age of geologic feature –Becomes less reliable as age increases –Most reliable within last 10,000-20,000 years
Niagara Falls
Varve count Similar to counting tree rings Count annual layers of sediment Common in glacial lake beds Distinguished by layers of dark fine particals and light heavy particles
Radiometric dating A method of determining the absolute age of an object by comparing the relative percentages of a radioactive (parent) isotope and a stable (daughter) isotope. Atoms of the same element with different numbers of neutrons are called isotopes.
Radioactivity and radiometric dating Radiometric dating Half-life – the time for one-half of the radioactive nuclei to decay Requires a closed system Cross-checks are used for accuracy Complex procedure Yields numerical dates
The radioactive decay curve
Dating sedimentary strata using radiometric dating
Radioactivity and radiometric dating Carbon-14 dating Half-life of only 5730 years Used to date very recent events Carbon-14 produced in upper atmosphere Incorporated into carbon dioxide Absorbed by living matter Useful tool for anthropologists, archeologists, historians, and geologists who study very recent Earth history