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Earthquakes and Mountain Building Presented by Mrs.Tonya
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Earthquakes and Mountain Building

Jan 04, 2016

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Earthquakes and Mountain Building. Presented by Mrs.Tonya. Layers of the Earth. Crust. Mantle. Inner Core. Outer Core. Crust. 20 miles thick below continents 6.5 miles thick below oceans Thin outer layer that surrounds the mantle Rocky and brittle Less than 1% of earth’s volume. - PowerPoint PPT Presentation
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Page 1: Earthquakes and Mountain Building

Earthquakes and Mountain Building

Presented by Mrs.Tonya

Page 2: Earthquakes and Mountain Building

Layers of the EarthCrust

Mantle

Outer CoreInner Core

Page 3: Earthquakes and Mountain Building

Crust

• 20 miles thick below continents

• 6.5 miles thick below oceans

• Thin outer layer that surrounds the mantle

• Rocky and brittle• Less than 1% of

earth’s volume

Page 4: Earthquakes and Mountain Building

Mantle

• 1,800 miles thick• Mostly solid but can

slowly deform(plastic)• 84% of earth’s

volume• 1000oC

Page 5: Earthquakes and Mountain Building

Core

Inner Core• 758 miles in radius• Solid • 4300oC

Outer Core• 1,400 miles thick• Liquid layer• 3700oC

Page 6: Earthquakes and Mountain Building

Math Trivia

• The crust is 1% of the earth’s volume and the mantle is 84% of the earth’s volume. What percentage of the earth’s volume is the core?

Answer: 15%

Page 7: Earthquakes and Mountain Building

Egg Model

Page 8: Earthquakes and Mountain Building

Tectonic Plates

• Pieces of the crust and uppermost mantle that make up the lithosphere

• Interconnecting pieces that fit together like a puzzle

Page 9: Earthquakes and Mountain Building

Is it possible that all of the continents were connected to

form one landmass? Tectonic plate activity

Page 10: Earthquakes and Mountain Building

Theory

• Similar species (fossils)

• Matching layers of rock

• Coastlines appearing to fit together

Page 11: Earthquakes and Mountain Building

Movement of tectonic plates

• Caused by convection currents(theory)

• 3 types of movement

Page 12: Earthquakes and Mountain Building

Normal fault

• Tectonic plates are moving apart

• Lithosphere is stretching

Page 13: Earthquakes and Mountain Building

Reverse fault

• Tectonic plates are moving towards one another

Page 14: Earthquakes and Mountain Building

Strike Slip fault

• Tectonic plates slide past one another

Page 15: Earthquakes and Mountain Building

What causes mountains to be formed?

• 2 tectonic plates collide

• Slabs pile into one another

• Causes crust to deform and elevate

• Oreo demo

Page 16: Earthquakes and Mountain Building

What causes a volcano?

• 2 tectonic plates collide• 1 plate boundary is

subducted or forced deeper into earth

• Causes other slab to fold deeply

• Hot magma can seep to surface of earth

• Spreading of two plates can cause hot magma to rise to surface

Page 17: Earthquakes and Mountain Building

What causes an earthquake?

• The release of stored up energy as the plates move past each other

• The energy moves outward from the fault in all directions in the form of waves

• When the waves reach the earth’s surface this causes the ground to shake

Page 18: Earthquakes and Mountain Building

Primary waves

• Compression waves

• Push and pull

• Slinky demo

• The fastest seismic wave

Page 19: Earthquakes and Mountain Building

Secondary waves

• Shear waves

• Side to side motion

• Slinky demo

• Slower than primary wave

Page 20: Earthquakes and Mountain Building

Love waves

• Surface waves

• Cause the most damage to buildings

• Travel the slowest of all seismic waves

Page 21: Earthquakes and Mountain Building

How far is the earthquake?

• Detect p-waves and s-waves on a seismograph

• Calculate difference between waves

Page 22: Earthquakes and Mountain Building

• Calculate distance to earthquake

• Distance = rate X time

• Example

You are traveling 30 miles/hour and you travel for 2 hours. What distance have you traveled?

Distance = (30 miles/hour)x(2 hours)

= 60 miles

Page 23: Earthquakes and Mountain Building

3 locations to determine where earthquake is located

Page 24: Earthquakes and Mountain Building

Math Trivia

• The Himalayan Mountains formed when the Indian Plate crashed into the Eurasian Plate. Today the two plates are still colliding and the Himalayas continue to rise. If the first person climbed Everest in 1953 and the mountains grow about .5 inches per year. How many more inches would you have to climb if you climbed Everest in 2009?

Answer: 28 inches