The age of a rock compared to the ages of rock layers
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numerical age
age of a feature given in years
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absolute age
The age of a rock given as the number of years since the rock formed.
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Principle of Uniformitarianism
Earth processes occurring today are similar to those that occurred in the past
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Principle of Original Horizontality
layers of sediment are generally deposited in a horizontal position
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Principle of Superposition
When artifacts are found in rock or earth that is layered, the deeper layers hold the older artifacts. Sediments need a layer of substate to accumulate on top of.
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Principle of Lateral Continuity
Beds originate as continuous layers that extend in all directions until they eventually thin out or grade into a different sediment type
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principle of cross-cutting relationships
younger features cut across older features
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Unconformity
A break in the geologic record created when rock layers are eroded or when sediment is not deposited for a long period of time.
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angular unconformity
tilted rocks are overlain by flat-lying rocks
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Nonconformity
A type of unconformity in which layered sedimentary rocks lie on an erosion surface cut into igneous or metamorphic rocks
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Disconformity
a type of unconformity in which the sedimentary layers above and below the unconformity are parallel
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angular unconformity (diagram)
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nonconformity (diagram)
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Disconformity (diagram)
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geologic contact
the boundary between two adjacent rock units
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stratigraphic column
A diagram representing a series of rock layers
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geologic map
A map showing the distribution of rock units and structures across a region.
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geologic column
an arrangement of rock layers in which the oldest rocks are at the bottom
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Eons
the largest division of geologic time
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Precambrian
Name for the time in earths early history that accounts for ninety percent of earth's time, but only cellular organisms lived. (Hadean, Archean,Proterozoic, Phanerozoic)
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era
a long and distinct period of history with a particular feature or characteristic.
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period
further divided era of time
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epoch
further divided period of time
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isotopic dating
the use of naturally occurring radioactive elements to determine the ages of rocks
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Geochronology
study of the ages of geologic events
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Isotopes
Atoms of the same element that have different numbers of neutrons
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radioactive decay
A spontaneous process in which unstable nuclei lose energy by emitting radiation
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Parent Atom
the atom that undergoes radioactive decay in a nuclear reaction
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Daughter Atom
the product atom from the radioactive decay of a parent atom
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half-life
length of time required for half of the radioactive atoms in a sample to decay
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closure temperature
the temperature below which isotopes are no longer free to move
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metamorphic rock
A type of rock that forms from an existing rock that is changed by heat, pressure, or chemical reactions.
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Protolith
the original rock from which a metamorphic rock formed
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Metamorphism
the process in which one type of rock changes into metamorphic rock because of chemical processes or changes in temperature and pressure
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metamorphic minerals
new minerals that grow in place within the solid rock only under metamorphic temperatures and pressures
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Metamorphic textures
foliated and non-foliated
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metamorphic foliation
A fabric defined by parallel surfaces or layers that develop in a rock as a result of metamorphism; schistocity and gneissic layering are examples.
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differential stress
when stress is applied unequally in different directions
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preferred orientation
The metamorphic texture that exists where platy grains lie parallel to one another and/or elongate grains align in the same direction.
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Metasomatism
the process by which a rock's overall chemical composition changes during metamorphism because of reactions with hot water that bring in or remove elements
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Foliation
An arrangement of minerals in flat or wavy parallel bands.
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slate
A type of Metamorphic rock that was once shale rock formed by heat and pressure.
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Phyllite
A fine-grained metamorphic rock with a foliation caused by the preferred orientation of very fine-grained mica.
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Schist
Metamorphic, Foliated
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Metaconglomerate
A metamorphic rock produced by metamorphism of a conglomerate; typically, it contains flattened pebbles and cobbles.
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Gneiss
A metamorphic rock that has ribbon like layers. It was made from other rocks that have been squeezed and heated a long time in the Earth.
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Migmatite
A rock formed when gneiss is heated high enough so that it begins to partially melt, creating layers, or lenses, of new igneous rock that mix with layers of the relict gneiss.
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Hornfels
Rock that undergoes metamorphism simply because of a change in temperature, without being subjected to differential stress.
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Quartzite
a metamorphic rock composed of quartz and transformed from a protolith of quartz sandstone
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marble
metamorphic rock that was once limestone
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metamorphic grade
the degree to which the parent rock changes during metamorphism
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metamorphic facies
A set of metamorphic mineral assemblages indicative of metamorphism under a specific range of pressures and temperatures.
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metamorphic zone
The region between two metamorphic isograds, typically named after an index mineral found within the region.
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metamorphic aureole
The region around a pluton, stretching tens to hundreds of meters out, in which heat transferred into the country rock and metamorphosed the country rock.
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thermal metamorphism
metamorphism caused by heat conducted into country rock from an igneous intrusion
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contact metamorphism
A change in the texture, structure, or chemical composition of a rock due to contact with magma.
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burial metamorphism
metamorphism due only to the consequences of very deep burial
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dynamic metamorphism
metamorphism that occurs as a consequence of shearing alone, with no change in temperature or pressure
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dynamothermal metamorphism
Metamorphism that involves heat, pressure, and shearing.
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regional metamorphism
formation of metamorphic rock bodies that are hundreds of square kilometers in size
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hydrothermal metamorphism
occurs when very hot water reacts with rock, altering its mineralogy and chemistry
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shock metamorphism
the changes that can occur in a rock due to the passage of a shock wave, generally resulting from a meteorite impact
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exhumation
The process (involving uplift and erosion) that returns deeply buried rocks to the surface.
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shield
broad region of long lived, stable continental crust where sedimentary cover either was not deposited or has been eroded away so that precambrian basement rocks are exposed.
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Mountain belts/orogens
a linear range of mountains
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Mountain Building
Major geological event that occurs when continental plates of equal density converge, resulting in mountain chains.
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Orogeny
a process in which a section of the earth's crust is folded and deformed by lateral compression to form a mountain range.
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distortion
a change in the shape, size, or position of a place when it is shown on a map
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ductile deformation
A type of solid-state flow that produces a change in the size and shape of a rock body without fracturing. Occurs at depths where temperatures and confining pressures are high.
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Stress
A force that acts on rock to change its shape or volume
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faults
Breaks in Earth's crust where rocks have slipped past each other.
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strike-slip fault
a type of fault where rocks on either side move past each other sideways with little up or down motion
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dip
angle of the planes slope
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plunge
angle between a line and horizontal in the vertical plane that contains the line
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bearing
compass heading of the line, meaning the angle between the projection of the line on the horizontal plane and the direction to true north
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reverse fault
a type of fault where the hanging wall slides upward; caused by compression in the crust
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thrust fault
a reverse fault in which the hanging wall slides over to the foot wall.
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normal fault
A type of fault where the hanging wall slides downward; caused by tension in the crust
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oblique-slip fault
A fault with both strike-slip and dip-slip components.
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fault scarp
a small step on the ground surface where one side of a fault has moved vertically with respect to the other
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slickensides
The polished surface of a fault caused by slip on the fault; lineated slickensides also have grooves that indicate the direction of fault movement.
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Rock fold
occurs when one or a stack of originally flat and planar surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation
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limbs
the two sides of a fold
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hinge
refers to a line along which the curvature of the fold is greatest
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axial surface
the imaginary surface that encompasses the hinges of successive layers of a fold
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Anticline
an upward fold in rock formed by compression of Earth's crust
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Syncline
A downward fold in rock formed by compression in Earth's crust
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Monocline
a large steplike fold in otherwise horizontal sedimentary strata
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nonplunging fold
has a horizontal hinge
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plunging fold
A fold in which the hinge line (or axis) is not horizontal.
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dome
a fold with the shape of an overturned bowl
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basin
a natural depression in the surface of the land often with a lake at the bottom of it
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Foliation
An arrangement of minerals in flat or wavy parallel bands.
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suture
the boundary between blocks that have been separate before the collision
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accretion
growth in size or increase in amount
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Global Positioning System (GPS)
A system that determines the precise position of something on Earth through a series of satellites, tracking stations, and receivers.
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Isostasy
The balancing of the downward force of the crust and the upward force of the mantle.
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crustal root
low-density crustal rock that protrudes downward beneath a mountain range