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STARTER 1. Differentiate between focus and epicenter of an earthquake. 2. Name the two categories of seismic waves and tell the type of material they move.

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Presentation on theme: "STARTER 1. Differentiate between focus and epicenter of an earthquake. 2. Name the two categories of seismic waves and tell the type of material they move."— Presentation transcript:

1 STARTER 1. Differentiate between focus and epicenter of an earthquake. 2. Name the two categories of seismic waves and tell the type of material they move through. 3. The machine that records seismic activity is called a _______. The report produced by this machine is a ______. 4. Why are surface waves the most destructive seismic waves?

2 8.3 DESTRUCTION FROM EARTHQUAKES p. 76 Today, you will be able to: Describe the factors contributing to earthquake damage. Identify other dangers associated with earthquakes. Explain the potential for earthquake prediction.

3 8.3 DESTRUCTION FROM EARTHQUAKES Seismic Vibrations Seismic Vibrations  The damage to buildings and other structures from earthquake waves depends on several factors.  intensity and duration of the vibrations  material on which the structure is built  the design of the structure.

4 EARTHQUAKE DAMAGE

5 8.3 DESTRUCTION FROM EARTHQUAKES Seismic Vibrations Seismic Vibrations  Building Design Factors that determine structural damage - Intensity of the earthquake - Unreinforced stone or brick buildings are the most serious safety threats - Nature of the material upon which the structure rests - The design of the structure

6 8.3 DESTRUCTION FROM EARTHQUAKES Seismic Vibrations Seismic Vibrations  Liquefaction Saturated material turns fluid Underground objects may float to surface

7 EFFECTS OF SUBSIDENCE DUE TO LIQUEFACTION

8 8.3 DESTRUCTION FROM EARTHQUAKES Tsunamis Tsunamis  Cause of Tsunamis A tsunami caused by an earthquake occurs where a slab of the ocean floor is moved vertically along a fault. A tsunami also can occur when the vibration of a quake sets an underwater landslide into motion. Tsunami is the Japanese word for “seismic sea wave.”

9 MOVEMENT OF A TSUNAMI

10 8.3 DESTRUCTION FROM EARTHQUAKES Tsunamis Tsunamis  Tsunami Warning System Large earthquakes are reported to Hawaii from Pacific seismic stations. Although tsunamis travel quickly, there is sufficient time to evacuate all but the area closest to the epicenter.

11 DESTRUCTION FROM EARTHQUAKES Other Dangers Other Dangers  Landslides With many earthquakes, the greatest damage to structures is from landslides and ground subsidence, or the sinking of the ground triggered by vibrations.  Fire In the San Francisco earthquake of 1906, most of the destruction was caused by fires that started when gas and electrical lines were cut.

12 LANDSLIDE DAMAGE

13 8.3 DESTRUCTION FROM EARTHQUAKES Predicting Earthquakes Predicting Earthquakes  Short-Range Predictions So far, methods for short-range predictions of earthquakes have not been successful.  Long-Range Forecasts Scientists don’t yet understand enough about how and where earthquakes will occur to make accurate long-term predictions. A seismic gap is an area along a fault where there has not been any earthquake activity for a long period of time.

14 8.4 EARTH’S LAYERED STRUCTURE p.76 Today, you will be able to: List the layers of Earth based on composition and physical properties. Describe the composition of each layer of Earth.

15 EARTH’S LAYERED STRUCTURE Layers Defined by Composition Layers Defined by Composition  Earth’s interior consists of three major zones defined by their chemical composition—the crust, mantle, and core.  Crust Thin, rocky outer layer Varies in thickness - Roughly 7 km in oceanic regions (4.3 mi.) - Continental crust averages 8–40 km (4.97-24.8mi.) - Exceeds 70 km in mountainous regions (24.9mi.)

16 SEISMIC WAVES PATHS THROUGH THE EARTH

17 EARTH’S LAYERED STRUCTURE Layers Defined by Composition Layers Defined by Composition  Crust Continental crust - Upper crust composed of granitic rocks - Lower crust is more akin to basalt - Average density is about 2.7 g/cm 3 - Up to 4 billion years old

18 EARTH’S LAYERED STRUCTURE Layers Defined by Composition Layers Defined by Composition  Crust Oceanic crust - Basaltic composition - Density about 3.0 g/cm 3 - Younger (180 million years or less) than the continental crust

19 EARTH’S LAYERED STRUCTURE Layers Defined by Composition Layers Defined by Composition  Mantle Below crust to a depth of 2900 kilometers (1801.97 miles) Composition of the uppermost mantle is the igneous rock peridotite (changes at greater depths).

20 EARTH’S LAYERED STRUCTURE Layers Defined by Composition Layers Defined by Composition  Core Below mantle Sphere with a radius of 3486 kilometers (2466 miles) Composed of an iron-nickel alloy Average density of nearly 11 g/cm 3

21 EARTH’S LAYERED STRUCTURE Layers Defined by Physical Properties Layers Defined by Physical Properties  Lithosphere Crust and uppermost mantle (about 100 km thick) (62 miles) Cool, rigid, solid  Asthenosphere Beneath the lithosphere Upper mantle To a depth of about 660 kilometers (410 miles) Soft, weak layer that is easily deformed

22 EARTH’S LAYERED STRUCTURE Layers Defined by Physical Properties Layers Defined by Physical Properties  Lower Mantle 660–2900 km (410-1802 miles) More rigid layer Rocks are very hot and capable of gradual flow.

23 Layers Defined by Physical Properties Layers Defined by Physical Properties EARTH’S LAYERED STRUCTURE  Inner Core Sphere with a radius of 1216 km (755.6 miles) Behaves like a solid Thought to be solid iron  Outer Core Liquid layer 2270 km thick (1410.5 miles) Convective flow of metallic iron within generates Earth’s magnetic field

24 EARTH’S LAYERED STRUCTURE

25 EARTH’S INTERIOR SHOWING P AND S WAVE PATHS

26 EARTH’S LAYERED STRUCTURE Discovering Earth’s Composition Discovering Earth’s Composition  Crust Early seismic data and drilling technology indicate that the continental crust is mostly made of lighter, granitic rocks.  Mantle Composition is more speculative. Some of the lava that reaches Earth’s surface comes from asthenosphere within.

27 EARTH’S LAYERED STRUCTURE Discovering Earth’s Composition Discovering Earth’s Composition  Core Earth’s core is thought to be mainly dense iron and nickel, similar to metallic meteorites. The surrounding mantle is believed to be composed of rocks similar to stony meteorites.

28 STARTER : 11/20/14 1. ________________________ is when saturated material turns to fluid and underground objects may float. 2. A ___________ caused by an earthquake occurs where a slab of the ocean floor is moved vertically along a fault. 3. What are some other dangers that may be associated with an Earthquake? Answer Study Guide Questions on page 71& 72 of your ISN. Answer Study Guide Questions on page 71& 72 of your ISN.

29 PLATE BOUNDARIES (PAGE 61)

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32 SEISMIC RISK MAP (PAGE 65)

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34 STARTER : 1. ________________________ is when saturated material turns to fluid and underground objects may float. 2. A ___________ caused by an earthquake occurs where a slab of the ocean floor is moved vertically along a fault. 3. Earth’s interior consists of three major zones defined by their chemical composition—__________, ___________, ______________. Answer Study Guide Questions on page 67-68 of your ISN. Answer Study Guide Questions on page 67-68 of your ISN.

35 Use page 234 to identify the layers of the Earth and Chapter 8.4 to complete # 2.

36 Use page 234 to identify the layers of the Earth and Chapter 8.4 to complete # 2.


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