Physical Geology Chapter 9

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caratoon  on April 14, 2012

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Physical Geology Chapter 9

Law of Superposition
*Developed by Steno in 1669
*Oldest rock on the bottom
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Law of Superposition *Developed by Steno in 1669
*Oldest rock on the bottom
Principle of Original Horizontality *Layers of sediment are generally deposited in horizontal position
*Rock layers that are flat
Principle of Cross Cutting Younger cuts through old
Inclusion *A piece of rock that is enclosed within another rock
*Rock containing inclusion is younger
Unconformity *Break in rock record produced by erosion/non deposition of rock units
Angular Unconformity Tilted rocks are overlain by flat lying rocks
Disconformity Strata on either side of unconformity are parallel
Nonconformity Metamorphic/Igneous in contact with sediment strata
Paleontology *Study of fossils
*Reamins are now preserved in rocks gen. in sediment
Types of Fossils *Remains of recent organisms (teeth)
*Entire animal, flesh included
*Petrified
*Molds and Casts
Permineralization *Mineral grow in cells of organisms remains
*Cell wall remain intact (silica, pyrite, and carbonate)
Impressions *Left by the bones-- Internal structure
*Result of compression
Mold Hollow imprint left by organism
Cast Replica of organism
Carbonization Remains smashed causing disassembly
Conditions for Favoring Preservation *Rapid Burial
*Possession of hard parts
Correlation Match rocks of similar age in different regions- rely on fossils
Principle of Fossil Succession Fossil organisms succeed one another in a definite and determinable order. Therefore, any time period can be recognized by its fossil content.
Index Fossil Geographically widespread fossil limited to short span of geologic time
Proton Positive charge
Neutron Neutral
Electron Negative charge
Atomic Number *Elements identifying number
*Equal to number of protons
Mass Number Sum of number of protons and neutrons
Isotope *Variant of same parent atom
*Differs in number of neutrons
*Different mass number of parent
Radioactivity Spontaneous changes in structure of nucleus
Beta Emission *Electron (beta particle) ejected from nucleus
*Mass number unchanged
*Atomic number increased by 1
Alpha Emission *Emission of 2 protons and 2 neutrons
*Mass number is reduced by 4
*Atomic number 2 less
Electron Capture Electron captured by nucleus and combine w proton to form neutron-Mass # unchanged, Atomic # minus 1
Parent Unstable radioactive isotope
Daughter Result from decay of parent
Half Life Time needed for half sample to decay--size does NOT matter
Radiometric Dating *Percentage of radioactive atoms that decay during half is always the same
*Compare ratio of parent to daughter
Sources of Error *Closed system required
*Want fresh, unweathered samples--igneous
Geologic Time Scale *Adam S and Roderick M named Cambrian, Silurian, and Devonian
*Had fight
Charles Lapworth Added Ordovician
Eon Greatest expanse of time
Phanerozoic, Proterozoic, Archean, Hadean
Phanerozoic Visible life, most recent eon
Proterozoic Tiny fossils
Hadean Oldest Eons
Era Subdivision of an eon
Cenozoic, Mesozoic, Paleozoic
Cenozoic Recent Life
Mesozoic Middle life
Paleozoic Ancient life
Eras are subdivided into Period
Period divided into Epochs
Precambrian Nearly 4 billion years before cambrian
Not divided into smaller units b/c details unknown
Big Bang Theory 13.7 by a
Debris condensed and cooled down
Genesis 1
Nuclear Fusion Nuclei join together, form one heavy nucleus
Release energy in form of heat
Supernova Death of very large stars

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