- In undeformed sedimentary rock, Each layer is older than the one above and younger than the one below - Applied to layers of lava flows and layer of volcanic ash
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What is the principle of original horizontality?
- Most sedimentary rocks formed in layers that are horizontal or close to horizontal - This is because lakes and sea surfaces are horizontal - Cross-bedding can occur up to 15 degrees
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What are the principles of cross-cutting relationships?
- Intrusions are younger than the rocks they intrude - A fault is younger than the rock that is fracture
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What is the principle of inclusions?
- Inclusions are fragments of one rock unit that are enclosed in another - Layer containing inclusions must be younger than the inclusions
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What is unconformity?
- The boundary between igneous rock and sedimentary rock - Represents missing time in the geological record
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What is a nonconformity?
- contacts between sedimentary and igneous rocks - exposure, weathering and erosion of intrusive igneous rock being filled with the deposition of sedimentary rock
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What is an intrusion?
- Layers which include intrusions are younger - Pieces of sedimentary rocks fall into magma and become inclusions within rock
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What is an angular uncomformity?
- the difference in angle between rocks of different ages - Time is missing from geological history recorded - evidence of past mountain building
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What is a disconformity?
- Sub-parallel strata on each side - difficult to recognize - Sedimentary rock above and below
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What is the process of formation of disconformity?
1. Deposition of limestone (below sea level) 2. Erosion of limestone (presumably above sea level) 3. Deposition of sandstone 4. Tilting of whole package
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What is a non-conformity?
- older metamorphic or igneous rocks below - younger sedimentary rock above - evidence of crustal movements - inclusions can help identify these feature
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What is the principle of correlation of rock layers?
- Relative dating can be applied to the local area - We must correlate rock layers from one location to another - Can be correlated using physical characteristics - method can not easily link the rock sequences in separate continents - fossils provide a method to correlate rock layers that are widely separated
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What is the principal of fossil succession?
- distribution of fossils over time is not random or constant - this allows for the cross referencing to reduce the age of a rock
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What are index fossils?
- fossils present in a wide geographic range and short time span - used for determining ages of rocks
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What were some initial theories of the age of the earth?
1. James Usher (based on timing of bible) - 4004 B.C 2. James Hutton - no beginning and no end 3. John Joly (Based on how long it would take to make the sea salty for no salt) - 80-100 Ma 4. Lord Kelvin - estimated that
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What was James Ushers age of the earth?
- 4004 B.C - based timing on historical events recorded in the bible
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What was James Hutton age of the earth?
- stated that the earth had no beginning nor end
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What was John Joly age of the earth?
- estimated 80-100 Ma - studied the amount of salt required to make the sea that salty - assumed that salt wasn't being taken out and that the ocean wasn't already salty
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What was Lord Kelvin age of the earth?
- Estimated 20-400 Ma - Estimated the rate of which a sphere would cool by the conduction of heat - Did not realize that the heat is transported by both convection and conduction - Heat was also generated by radioactive decay
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What is an element?
- A substance composed of atoms that all have the same properties
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What is an Isotope?
- An element that behaves the same chemically but has different atomic mass numbers -some isotopes are radioactive and decay
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What is radioactive decay?
- The process where an unstable atomic nucleus is transformed into an atomic nucleus of a different element - does not depend on molecule/compound or pressure or temperature - Exponential process
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How can we measure radioactivity?
- Measurements are made using a mass spectrometer - vaporizes sample and accelerates through a magnet (heavier ions deflect less)