HISTORICAL GEOLOGY

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Created by:

ekirman  on April 27, 2011

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Combined Historical Geology Set

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spiffy science, Earth and Space Science

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HISTORICAL GEOLOGY

geologic time scale
a record of the geologic events and life forms in Earth's history
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Terms

Definitions

geologic time scale a record of the geologic events and life forms in Earth's history
eon the longest division of geological time
era a unit of geologic time that includes two or more periods
periods subdivisions of an era in geologic time
epochs smallest and 4th largest divisions of geologic time
Phanerozoic the period from about 5,400 million years ago until the present, means "visible life"
Paleozoic means "ancient life", spans from 544 million to about 230 million years ago
Mesozoic means "middle life" from 230 million to 63 million years ago
Cenozoic means "recent life" approximately the last 63 million years
Precambrian name for the time in earths early history that accounts for ninety percent of earth's time, but only cellular organisms lived
radioactivity the process by which an unstable nucleus gives off nuclear radiation
half-life the time required for one half of the atoms of a radioisotope to emit radiation an decay products
radiometric dating process used to calculate the absolute age of rock by measuring the ratio of parent isotope to daughter product in a mineral and knowing the half-life of the parent
radiocarbon dating method measuring the decay rate of carbon isotopes in organic matter to provide dates for organic materials like wood or fiber
parent element The unstable or starting radioactive element.
daughter element the unstable or starting radiactive element decays into this product
alpha emission the process in which two protons and two neutrons that are bound together and are emitted from the nucleus during some kinds of radioactive decay
beta emission release of an electron from the nucleus
electron capture the process in which an inner orbital electron is captured by the nucleus of the atom that contains the electron
radioactive isotope an isotope that is unstable; the nucleus decays spontaneously, giving off detectable particles and energy
carbon 14 taken up by living things while they are alive--when an organism dies, it decays to form nitrogen 14.used to date fossils younger than 60,000 years. half life=5370 years.
uranium 238 the radioactive isotope of uranium having an atomic mass of 238 and a half-life of 4.5 billion years
carbon 12 stable isotope used to measure the age of organic material
fossil preserved remains or evidence of an ancient organism
trace fossil a type of fossil that provides evidence of the activities of ancient organisms, includes the footprints, tracks, trails, and burrows made by living things
index fossil a fossil known to have lived in a particular geologic age that can be used to date the rock layer in which it is found
petrified remains fossils that form when some of the original materials that made up the organisms are replaced with minerals
cast a type of body fossil that forms when crystals fill a mold or sediments wash into a mold and harden into rock
mold a fossil formed when an organism buried in sediment dissolves, leaving a hollow area
amber hardened tree sap, often a source of insect fossils
unaltered remains fossil retains the organism's original structure and composition; it remains unchanged such as a complete insect in amber
altered remains fossils changed structurally or chemically; minerals may seep into the pores or cavities of an organism's bones, teeth, and shells
gastrolith fossilized stone from the digestive system of a dinosaur
trilobite organism with a three-lobed exoskeleton that was abundant in Paleozoic oceans and is considered to be an index fossil, PA state fossil
law of superposition in undisturbed rock layers, the oldest rocks are on the bottom and the youngest rocks are on the top
uniformitarianism is the idea that the geologic processes that operate today also operated in the past
relative dating method to determine the order of events and relative age of rocks by examining the position of rocks in a sequence
principal of cross-cutting relationships a feature that cuts a layer of rock is younger than the rock itself
unconformity gap in the rock layer that is due to erosion or periods without any deposition
principle of original horizontality layers of sediment are generally deposited in a horizontal position
correlation establishing the equivalence of rocks of similar age in different areas
fault a crack in the earth's crust resulting from the displacement of one side with respect to the other
fold a bend in layers of rock
angular unconformities an unconformity that exists between horizontal sedimentary rock layers and folded or tilted layers of rock
disconformities formed as an erosion surface between parallel layers of sedimentary rock
nonconformities exists where horizontal sedimentary rock layers lie on top of an eroded surface or older metamorphic rock or igneous rock
dike a slab of volcanic rock formed when magma forces itself across rock layers
sill igneous rock feature formed when magma is squeezed into a horizontal crack between layers of rock and hardens underground
anticline a fold in rock that bends upward into an arch
syncline a fold in rock that bends downward to form a valley
James Hutton known as the Father of Modern Geology, is known for creating the theory of Uniformitarianism

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