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57 Cards in this Set
- Front
- Back
Metamorphic Rock
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Formed from pre-existing rock by adding heat and pressure
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Fault Scarp
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Small step on the ground where one side of a fault has moved vertically with respect to the other
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Epicenter
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The point on the surface of the earth directly above hypocenter
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Recrystallization
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Minerals change size and shape
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Phase Change
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Same chemical formula and different crystal structure
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Neocrystaliztion
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New minerals with pressure or temp change
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Pressure Solution
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Mineral grains partially dissolve
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Plastic Deformation
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Mineral grains soften and deform
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Differential Stress
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Pressure that is greater in one orientation
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Fault
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Large fracture on which sliding occurs
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Metamorphic Rock
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Formed from pre-existing rock by adding heat and pressure
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Fault Scarp
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Small step on the ground where one side of a fault has moved vertically with respect to the other
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Epicenter
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The point on the surface of the earth directly above hypocenter
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Recrystallization
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Minerals change size and shape
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Phase Change
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Same chemical formula and different crystal structure
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Neocrystaliztion
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New minerals with pressure or temp change
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Pressure Solution
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Mineral grains partially dissolve
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Plastic Deformation
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Mineral grains soften and deform
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Differential Stress
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Pressure that is greater in one orientation
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Fault
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Large fracture on which sliding occurs
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Hypocenter
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The focus of the earthquake
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Hydrothermal Metamorphism
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Alteration by hot, chemically aggressive water
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Subduction Metamorphism
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Creates Blue schist
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Exhumation
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metamorphic rocks returning to the surrface
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Shields
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eroded remnants of orogenic belts
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Deadliest Earthquake
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China 1557 830,000 killed
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Largest Earthquake on East Coast
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South Carolina 1886
6.7 magnitude |
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Liquefaction
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Water-saturated sediment turn into a mobile fluid
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Recurrence Interval
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Average time between events
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Seismic Gaps
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Places that havent slipped recently, most likely canidates for earthquake
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unconformity
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time gap in the rock record due to non deposition or erosion
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sequence
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relative order in which rock occur
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Hadean Eon
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Formations of Oceans
4.6-3.8 Ga |
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Archean Eon
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Birth of Continents, First life forms 3.8-2.5 Ga
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Proterozoic Eon
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Techtonic plates form, first traces of ozone 2.5-.542 Ga
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Phanerozoic Eon
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Continents break up, first visible life 542 Ma-Present
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Paleozoic Era
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Life diversified rapidly
542-251 Ma |
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Mesozoic Era
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Age of Dinosaurs
251-65.5 Ma |
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Cenozoic Era
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Age of mammals
65.5 Ma-Present |
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Relative Humidity
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Amount of water in the air divided by he amount of water it could hold
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Water Shed
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The region that collects water that feeds into a given drainage network
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Dendritic Drainage Network
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Branching, treelike
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Radial Drainage Network
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Outward from a central point
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Rectangular Drainage Network
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Bend at right angles, controlled by jointed rocks
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Field Capacity
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The amount of water the ground can hold when it is fully drained
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Hydrograph
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Velocity of a stream as a function of time
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Rill Erosion
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Water concentrated into innumerable closley spaced small channels and cut vertically and horizontally if left unchecked
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Gullies
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Steep-Sided trenches formed by connected rills
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Rain-Splash
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erosion caused by impact of water striking earths surface
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Displacement
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amount of slip on the fault
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Stress
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Push, pull, or shear of a rock
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Stick-slip behavior
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stop-start movement along a fault plane caused by friction, which prevents movement until stress builds up sufficiently
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Fault Creep
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When movement on a fault line happens without generating earthquakes
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Foliation
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Planar fabric from aligned materials
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Dynamic Metamorphism
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Shearing at fault zones break rocks
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Regional Metamorphism
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Tectonic collisions deform huge mobile belts
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Prolith
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Parent Rock
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