Earthquakes Unit 12 2 Earthquake shaking of the

  • Slides: 24
Download presentation
Earthquakes Unit 12. 2

Earthquakes Unit 12. 2

Earthquake: shaking of the ground as a result of a ____________ sudden release of

Earthquake: shaking of the ground as a result of a ____________ sudden release of energy in Earth’s crust friction between moving tectonic plates that • often occurs as a result of _____ pressure builds-up ______ • about 80% of earthquakes occur in a ring bordering the ________ • the Juan de Fuca convergent plate boundary West of Vancouver Island has many earthquakes

Earthquake: shaking of the ground as a result of a ____________ sudden release of

Earthquake: shaking of the ground as a result of a ____________ sudden release of energy in Earth’s crust friction between moving tectonic plates that • often occurs as a result of _____ builds-up ______ pressure • about 80% of earthquakes occur in a ring bordering the ________ Pacific Ocean • the Juan de Fuca convergent plate boundary West of Vancouver Island has many earthquakes

Focus: _______ location where the pressure is finally released as an earthquake Epicenter: the

Focus: _______ location where the pressure is finally released as an earthquake Epicenter: the point on the ______ surface ______ directly _____ above the focus Earthquakes occur at various depths, depending on the plates involved. more damage • earthquakes at the surface usually cause ________ Classification of Earthquakes Classification Depth of Focus Shallow Focus 0 to 70 km Intermediate Focus 70 to 300 km Deep Greater than 300 km

Seismic wave: ________ vibration energy released by earthquakes source of an earthquake (where an

Seismic wave: ________ vibration energy released by earthquakes source of an earthquake (where an earthquake • can tell us the ______ happened) strength of an earthquake • can tell us the ______

primary wave Longitudinal wave (P wave) underground solids fastest 1 st same liquids gases

primary wave Longitudinal wave (P wave) underground solids fastest 1 st same liquids gases

secondary wave Transverse wave (S wave) underground solids slower 2 nd perpendicular to

secondary wave Transverse wave (S wave) underground solids slower 2 nd perpendicular to

surface only surface wave (L wave) solids slowest last (3 rd) perpendicular to structural

surface only surface wave (L wave) solids slowest last (3 rd) perpendicular to structural damage

composition and _____ size of Earth’s Seismic waves can tell us the ________ interior

composition and _____ size of Earth’s Seismic waves can tell us the ________ interior layers since they behave differently in different materials • some can travel underground • they travel _____ faster through solids than liquids

The velocity increases Since seismic waves travel faster through solids, this must mean that

The velocity increases Since seismic waves travel faster through solids, this must mean that the outer core is liquid

L P mantle S P

L P mantle S P

Seismometer: a machine that measures and records seismic wave energy Seismograph: a graph that

Seismometer: a machine that measures and records seismic wave energy Seismograph: a graph that shows arrival time of seismic waves • ________ long • how _____ an earthquake lasted • an earthquake’s ________ magnitude (strength)

5 min 3000 km

5 min 3000 km

The magnitude (size) of an earthquake is the size of the line on the

The magnitude (size) of an earthquake is the size of the line on the seismograph The magnitude is measured by the Richter Scale 10 x stronger 1 in magnitude = _______ • an increase of ____ 10 102 103