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37 Cards in this Set

  • Front
  • Back

Structure

rock type, structural geology, stratigraphy

Process

external forces form landscape (rain, wind, water)

Time

process act on a geologic structure with the passage of time

System

collection of objects and the interactions between them

closed system

reaches a static equilibrium

open system

reach dynamic equilibrium and remain transient

gradient

change in the value of a quantity with change in a given variable (distance)

Common types of gradient

Chemical, thermal, hydraulic. Important because it drives change on earth

Relative dating

determining the age of a rock, fossil, or event using other rocks, fossils, or events

Biostratigraphy

correlation of units with fossils

tephrachronology

using volcanic eruptions to date rocks


Numeric dating

using different methods to determine the age of a rock. usually in years

radioactive decay

the nucleus of an unstable atom loses energy then releases heat and emits alpha, beta, or gamma particles

Cenozoic years

0-65mya

Mesozoic years

70-25mya

Paleozoic years

260-540mya

Precambrian years

750-4000mya

Orogeny

process of mountain formation at convergent boundaries

Epirogeny

process of continent formation

Glacial Isostacy

regional subsidence occurs because of mass of ice

Orogenic Types (Oceanic crust-Oceanic crust)

forms island arcs and trenches

Cordillean

where oceanic lithosphere subducts under continental lithosphere. ex. Andes mtns

Collisional

where convergence and subduction have brought an island arc or another plate of continental crust into contact with the overlying. Ex. Himalayas

Extensional mtn belts

comes from divergence

tectonic landform

landforms that result from crustal movement

scarp

shortened form of escarpment

fault scarp

when a fault displaces the ground surface so one side of the fault is higher than the other

grabben

the depressed fault block bound by normal faults

half-grabben

asymmetrical valleys or basins caused by 2 fault blocks that tilted the same direction along a normal fault

landforms from folding

syncline, aniticline, monocline

tectonic domes

form from shallow intrusion (igneous domes, laccoliths, shallow igneous sills)

volcano

area of earth where hot gas, liquid molten rock and shattered rock fragments are forcibly or rapidly ejected onto the surface

Exhalative volcanic activity

discharge of water, steam or gas. Hot springs, geysers

Explosive activity

solid volcanic ejecta. rock becomes fragmented by sudden loss of volitiles, abrupt contact with the ground, water or abrasion in the volcanic neck. Most dangerous kind.

Effusive activity

copious outpouring of lava from a vent or fissure

Felsic

silica rich, more viscous

Mafic

Silica poor, less viscous