Presentation is loading. Please wait.

Presentation is loading. Please wait.

Earthquakes HOW AND WHERE EARTHQUAKES HAPPEN. Why Earthquakes Happen? Rocks along faults pressed tightly together. Rocks along faults pressed tightly.

Similar presentations


Presentation on theme: "Earthquakes HOW AND WHERE EARTHQUAKES HAPPEN. Why Earthquakes Happen? Rocks along faults pressed tightly together. Rocks along faults pressed tightly."— Presentation transcript:

1 Earthquakes HOW AND WHERE EARTHQUAKES HAPPEN

2 Why Earthquakes Happen? Rocks along faults pressed tightly together. Rocks along faults pressed tightly together. Stress occurs but friction prevents them from moving – fault is said to be locked. Stress occurs but friction prevents them from moving – fault is said to be locked. Rocks under stress suddenly shift along a fault Rocks under stress suddenly shift along a fault Fault – break in body of rock where one block slides relative to another Fault – break in body of rock where one block slides relative to another When rocks along a fault move, a sudden release of energy occurs causing movements on the ground... When rocks along a fault move, a sudden release of energy occurs causing movements on the ground...

3 ….This is an Earthquake

4 FOCUS Area along a fault where the slippage first occurs Area along a fault where the slippage first occurs Focus is beneath the earths surface Focus is beneath the earths surface The epicenter is directly above The epicenter is directly above The depth of the focus varies – 90% of continental earthquakes have shallow focus The depth of the focus varies – 90% of continental earthquakes have shallow focus Shallow foci – within 70km from surface Shallow foci – within 70km from surface Deep foci – subduction zones farther from plate boundaries than shallow quakes Deep foci – subduction zones farther from plate boundaries than shallow quakes

5 FOCUS DEPTH

6 FOCUS DEPTH OF EARTHQUAKES IN WASHINGTON

7 EPICENTER A point on the earths surface directly above the focus A point on the earths surface directly above the focus

8 What happens when rocks in motion release energy in the form of vibrations? Seismic Waves travel outward in all directions from focus

9 Seismic Waves Two types of waves produced from earthquakes : Two types of waves produced from earthquakes : Body waves – travel through body of a medium Surface waves – travel along surface of body rather than through middle

10 Surface Waves Form from motion along shallow fault or by energy transfer from P and S waves reaching earths surface. Form from motion along shallow fault or by energy transfer from P and S waves reaching earths surface. Slowest moving seismic waves Slowest moving seismic waves Cause greatest damage at surface Cause greatest damage at surface Two types : Love and Rayleigh Two types : Love and Rayleigh

11 Love and Rayleigh Waves Love waves – rock moves side-to-side and perpendicular to wave direction Love waves – rock moves side-to-side and perpendicular to wave direction Rayleigh waves – move ground in an elliptical rolling motion Rayleigh waves – move ground in an elliptical rolling motion

12 Earthquakes and Plate Tectonics Most earthquakes are located at or near tectonic plate boundaries Most earthquakes are located at or near tectonic plate boundaries

13 Convergent Oceanic Environments Plates move toward one another and collide Plates move toward one another and collide Subduction occurs as denser plate sinks under overriding plate - earthquakes occur Subduction occurs as denser plate sinks under overriding plate - earthquakes occur Oceanic-oceanic or oceanic-continental Oceanic-oceanic or oceanic-continental

14 Divergent Oceanic Environments Plates moving away from each other and mid-ocean ridge Plates moving away from each other and mid-ocean ridge Spreading motion causes earthquakes Spreading motion causes earthquakes

15 Continental Environments Two continental plates converge, diverge, or move horizontally to one another Two continental plates converge, diverge, or move horizontally to one another Rocks build up stress Rocks build up stress Mountains form and earthquakes occur Mountains form and earthquakes occur

16 MAJOR EARTHQUAKE ZONES Pacific Ring of Fire Pacific Ring of Fire Mid-ocean ridges Mid-ocean ridges Eurasian-Melanesian Mountain Belt Eurasian-Melanesian Mountain Belt

17 MAJOR EARTHQUAKES AREAS

18 Fault Zones Intense stress along plate boundaries create fault zones Intense stress along plate boundaries create fault zones Plates separate, collide, subduct or slide past one another Plates separate, collide, subduct or slide past one another Movement from stress buildup causes major earthquakes Movement from stress buildup causes major earthquakes

19 PUGET SOUND FAULT ZONES

20 Studying Earthquakes Ancient Chinese Method of Studying Earthquakes

21 Magnitude The measure of the strength of an earthquake, determined by measuring the amount of ground motion. The measure of the strength of an earthquake, determined by measuring the amount of ground motion.

22 Richter Scale Used for most of the 20 th century. Each number represents a factor of 30 (a 5 earthquake has 30 times the energy of a 4). We now prefer to use the…… Used for most of the 20 th century. Each number represents a factor of 30 (a 5 earthquake has 30 times the energy of a 4). We now prefer to use the……

23 Moment Magnitude Based on the size of the area of fault movement, the average distance that the fault blocks move, and the rigidity of the rocks in the fault zone. More accurate for large earthquakes. Based on the size of the area of fault movement, the average distance that the fault blocks move, and the rigidity of the rocks in the fault zone. More accurate for large earthquakes.

24 Intensity Based on an earthquakes effects. The Mercalli scale (p. 304) uses Roman numerals I-XII. Depends on magnitude, distance from the epicenter, local geology, earthquake duration, and human infrastructure. Based on an earthquakes effects. The Mercalli scale (p. 304) uses Roman numerals I-XII. Depends on magnitude, distance from the epicenter, local geology, earthquake duration, and human infrastructure. Charleston, SC

25 I & II Not felt except by a very few. Not felt except by a very few. Felt by a few persons on the upper floors of buildings. Felt by a few persons on the upper floors of buildings.

26 III & IV Felt indoors. Felt indoors. Hanging objects swing. Hanging objects swing.

27 V & VI Felt outdoors. Felt outdoors. Felt by all, many scared and run outdoors. Felt by all, many scared and run outdoors.

28 VII & VIII Difficult to stand. Difficult to stand. Damage slight in specially designed structures. Damage slight in specially designed structures.

29 IX & X Damage considerable in specially designed structures. Damage considerable in specially designed structures. Ground cracked, rails bent. Ground cracked, rails bent.

30 XI & XII Bridges destroyed, broad fissures in ground. Bridges destroyed, broad fissures in ground. Total destruction. Total destruction.

31 Earthquakes and Society Effects on Humans, Property & Infrastructure How to PREPARE for an Earthquake

32

33 MAJOR TSUNAMIS

34 Caused by an earthquake whose epicenter is on or below the ocean floor that causing: A rapid drop or rise in the ocean floor OR An underwater landslide that displaces a large volume of water

35 Much Safer To Be Out In The Open Most injuries result from the collapse of buildings, falling objects, and flying glass. Most injuries result from the collapse of buildings, falling objects, and flying glass.

36 Other Dangers Include Landslides Landslides Fires Fires Explosions (broken electric and gas lines) Explosions (broken electric and gas lines) Floods (from collapsing dams) Floods (from collapsing dams)

37 Ground Type Is Important Loose soil and rock can vibrate like Jell-O. Loose soil and rock can vibrate like Jell-O.

38 KOBE SEISMOGRAPH Top - Station on solid ground Right - Station on water saturated, soft ground KOBE SEISMOGRAPH Top - Station on solid ground Right - Station on water saturated, soft ground

39 LIQUEFACTION Kobe

40 Quake Duration A long duration moderate earthquake can cause more damage than a short one at a higher magnitude. A long duration moderate earthquake can cause more damage than a short one at a higher magnitude.

41 FIRES Kobe

42 Destruction to Buildings and Property

43 STRUCTURAL DAMAGE Kobe earthquake

44 CHILE – 1960 Largest Recorded 9.5

45 ALASKA

46 EARTHQUAKE SAFETY People who live near active faults should be ready to follow a few simple earthquake safety rules to help prevent death, injury, and property damage § BEFORE - Be prepared § DURING - Stay calm § AFTER - Stay cautious

47 Before an Earthquake Be prepared. Keep an adequate supply of food, water, batteries, flashlights and a radio. Be prepared. Keep an adequate supply of food, water, batteries, flashlights and a radio. Prepare an earthquake plan and discuss it with your family. Prepare an earthquake plan and discuss it with your family. Learn how to turn off the gas, water, and electricity in your home. Learn how to turn off the gas, water, and electricity in your home.

48 During an Earthquake Protect yourself by moving to a safe position. Protect yourself by moving to a safe position. Best way is the Triangle of Life (next slide-- ) Best way is the Triangle of Life (next slide-- ) Indoors – get under a table or if not possible in a inside door frame away from heavy furniture Indoors – get under a table or if not possible in a inside door frame away from heavy furniture Outdoors – get away from tall buildings, tunnels, power lines or bridges out in the open Outdoors – get away from tall buildings, tunnels, power lines or bridges out in the open

49 Triangle of Life during a Quake Newest research shows your first best position to get into during a quake is next to and below the level of a heavy object – table or furniture Newest research shows your first best position to get into during a quake is next to and below the level of a heavy object – table or furniture Cover your head in bracing position (like shown on a plane) Cover your head in bracing position (like shown on a plane) Any falling debris will hit table or furniture and arc over you and you will be protected Any falling debris will hit table or furniture and arc over you and you will be protected

50 Bracing Under a Table Especially at School

51 Earthquake Warnings and Forecasts Scientists study past earthquakes to predict where future earthquakes will occur. There is currently no way to predict exactly when an earthquake will occur.

52 Seismic Gaps – Areas along a fault where stress has built up due to a decrease in seismic activity recently but where strong earthquakes occurred in the past

53 Dont be Scared, Be Prepared ! 3 Days, 3 Ways Earthquake Preparedness Starts NOW! 3days3ways.org Mr. K will show you how starting Tuesday!


Download ppt "Earthquakes HOW AND WHERE EARTHQUAKES HAPPEN. Why Earthquakes Happen? Rocks along faults pressed tightly together. Rocks along faults pressed tightly."

Similar presentations


Ads by Google