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57 Cards in this Set

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