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Using various radioactive decay dating techniques to assign ages in years before the present to rocks
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An uncomformity below which older rocks dip at a different angle (usually steeper) than overlying strata.
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An association of sedimentary rocks defined its fossil content.
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An association of sedimentary rocks defined its fossil content.
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| Carbon 14 dating technique |
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Absolute dating technique relying on the ratio of C14 to C12 in an organic substance, useful back to about 70,000 years ago.
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Demonstration of the physical continuity of rock units or biostratigraphic units, or demonstration of time equivalence as in time-stratigraphic correlation.
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A boundary across which seismic wave velocity or direction of travel changes abruptly, such as the mantle-core boudary.
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The absolute dating proccess in which small linear tracks (fission tracks) resulting from alpha decay are counted in mineral crystals.
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An easily identifiable fossil with an extensive geographic distribution and short geologic range useful for determining the relative ages of rocks in different areas.
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The time neccessary for half of the original number of radioactive atoms of an element to decay to a stable daughter product; for example, the half-life for potassium 40 is 1.3 billion yrs.
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A body of rock, such as a formation, defined solely by its physical attributes.
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An unfconformity in which stratified sedimentary rocks overlie an erosion surface cut into igneous or metamorphic rocks.
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| Principle of cross-cutting relationships |
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A principle holding that an igneous intrusion or fault must be younger than the rocks it intrudes or cuts across.
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| Principle of fossil succession |
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A principle holding that fossils and especially groups or assemblages of fossils, succeed one another through time in a regular and predictable order.
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A principle holding that inclusions or fragmentsin a rock unit are older than the rock unit itself; for example,granite inclusions in sandstone are older than the standstone
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| principle of lateral continuity |
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A principle holding that rock layers extend outward in all directions until they terminate
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The planets orbit the sun. The Geo-centric theory vs. Hylio centric theory We are the center of the earth, everything went around us.
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Planets revolve around the earth 1st and 2nd law of motion - body in motion stays in motion, body in rest stays at rest; strength of materials
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The universe never has a beginning nor end; scienctific method; water cycle
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Law of; Superposition, original horizontality, lateral continuity
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Cross-cutting Relationships, uniformatarianism
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Determined earth's age by meltingan iron ball-75,000 yrs
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All rocks owe their origins to the oceans; Neptunism
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| Principle of original horizontality |
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according to this principle, sediments are deposited in horizontal or nearly horizontal layers.
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| Principle of Superposition |
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a principle holding that in a vertical sequence of undeformed sedimentary rocks, the relative ages of the rocks can be determinded by their position in sequence-oldest at the bottom followed by successively younger layers.
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| Principle of uniformitarianism |
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A principle holding that we can interpret past events by understanding present day processes, based on the idea that natural processes have always operated in the same way.
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The spontaneous change of an atom to an atom of a different element by emission of a particle from its nucleus (alpha and beta decay) or by election capture
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The process of determining the age of an event; involves placing geologic events in their correct chronological order but does not involve consideration of when the events occurred in number of years ago.
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A body of strata that was deposited during a specific interval of geologic time; for example, the Devonian system was deposited during the Devonian period
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Any of the units such as eon, era, period, epoch, and age used to refer to specific intervals of geologic time.
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The process of determining the age of a tree or wood in a structure by counting the number of annual growth rings.
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A break in the geologic record represented by an erosional surface seperating younger strata from older rocks.
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