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37 Cards in this Set

  • Front
  • Back

Define an earthquake

a vibration of the ground

elastic rebound theory

if stress is applied to rock, rock undergoes elastic deformation. if enough stress is applied, rock ruptures and energy is released as earthquake vibrations and rock returns to original non stressful state.

list the types of seismic waves

Primary (p) wave, Secondary (S) wave, Surface Wave



how are earthquakes measured

mercalli scale, richter scale, moment magnitude scale

name various ways that earthquakes can cause damage on the surface of the earth

ground shaking, landslides, liquefaction, fires, tsunamis

name the 4 primary layers of the earth

crust, mantle, outercore, innercore

secondary layers of the earth

lithosphere- surface (100 km), solid, rigid and brittle


asthenosphere- 100 km-700 km, weak, plastic, gooey, capable of flow

describe the theory of plate tectonics

Pangea- supercontinent, continental drift by


alfred wegener

three types of plate boundaries

divergent, convergent, and transform



name the geographical locations where the plate boundaries are located

divergent- mid atlantic ridge, mid indian ridge, east pacific rise

convergent- cascade mountains, andes mountains


transform- san Andreas fault, pakistan


Primary (P) Wave

type of seismic wave, propagates via compression and expansion, travels 16000 mph, can travel through all mediums


Secondary (S) Wave

types of seismic wave, propagates via shearing motion, travels 10,000 mph, only travels through solids

Surface Wave

type of seismic wave, propagates similar to an S wave, slowest (few 1000 mph), causes most damage

Mercalli Scale

based on amount of damage the earthquake caused, ranges from I to XII

Richter Scale

based on amplitude of seismic wave, ranges from 1 to 10. logarithmic scale- for every unit on the scale, intensity increases by 10X, energy increases by 30X, poorly assesses large EQ's

Moment Magnitude Scale

based on amount of displacement along fault, most accurate to date, best estimates intensity of large EQ's, best estimates energy released, verified in the field

Crust

outermost, thinnest, two types: continental crust and oceanic crust


continental- up to 70 km composed of felsic


oceanic- 5-6 km thick, composed of mafic igneous rock (basalt)

Mantle

2900 km thick, composed of peridotite (ultra mafic)

Outercore

2300 km thick, composed of iron, believed to be liquid

innercore

1200 km radius, solid very dense, composed of iron and nickel

hot spot

weak zone in the crust that allows magma to reach the surface (example: hawaii)

paleomagnetic evidence of plate tectonics

magnetic reversals- show flip flopping of earth's magnetic field and supports divergent plate activity

driving mechanism for plate tectonics

convection- migration of warm material into cool material

features of a volcano

mountain formed by extrusion of molten rock, lava

types of material expelled during volcanic eruptions

pyroclastic material- broken rock fragments classified by size: ash (smallest), lapilli (walnut size), blocks/bombs (largest)

three types of volcanoes

1.shield: largest, gently sloping slides, composed of basaltic lava


2. stratovolcano: moderate size, moderately sloping sides, composed of pyroclastics and lava


3. cinder cone: smallest, steep sides, composed of pyroclastics

features associated with volcanic activity

caldera- large depression formed by a collapsed volcano


volcanic neck- erosional remnant of a former volcano

major water bodies on the surface of the earth

pacific ocean, atlantic ocean, indian ocean, arctic ocean, southern ocean

pacific ocean

largest ocean, largest geographical feature on earth, 13,000 ft avg

atlantic ocean

about half the size of the pacific, bounded by almost parallel continent, 12000 ft

indian ocean

slightly smaller than atlantic but has roughly same average ft, mostly in southern hemisphere

arctic ocean

only 7% the size of the pacific, 2500 ft avg

southern ocean

found below 50 degrees south parallel, encircles antarctica, distinguished by changes in temp, salinity and fauna

active continental margin

associated with plate boundary, EQ's and volcanoes, narrow band of highly disturbed sediment

passive continental margin

not associated with a plate boundary, little to not EQ's and volcanoes, thick wedge of undisturbed sediment. flat slope

mid ocean ridge

represent areas of divergence 46000 miles, high compared to rest of ocean floor (volcanic activity pushes surface upward)

sea floor sediments

terrigeneous, biogeneous, hydrogenous, oil and natural gas, gas hydrates, sand and gravel, manganese nodules