Announcements No lab this week! Please refer to schedule on website (instruct.uwo.ca/earth-sci/023-> Revised lab order) Next week’s lab: Radioactivity.

Slides:



Advertisements
Similar presentations
Jeopardy 1 st Semester Final Review December 2005 Inside Earth and Scientific Method Mrs. Gibbars classes.
Advertisements

Earth’s Layered Structure
Chapter 7 Test Review Plate Tectonics.
Exploring Earthquakes By: Jordyn Friel and Kylie Edens.
Unit 3 – Dynamic Crust Review
Chapter 4 The Dynamic Crust
EARTH’S INTERIOR.
Exploring the Deep GEO/OC103 Lecture 4: The Structure of the EARTH.
Unit C Chapter 2 Section 2.3 Earthquakes. Causes of the Alaska Earthquake of 1964 This was the second largest earthquake that was ever recorded by a seismograph.
Ch 21: Earth’s interior Probing Earth’s interior
Dynamic Earth Class February Volcanic Imagination (Chapter 4) Exploring the Earth’s Interior.
Earthquake Damage and Earth’s Interior. Factors contributing to damage Duration Intensity Building Design – reinforced/flexible buildings best Materials.
Lab 2: The Interior of the Earth Key Q: What is the interior of the Earth like?
EARTHQUAKES. Features of Earthquakes Seismic Waves Seismic waves are waves of energy generated by the sudden breaking or motion of Earth’s crust. Seismic.
OC/GEO103 Lecture 5 Earth Structure. What’s inside the Earth? Is there really another world at the center? What is the energy for changing surface features?
Journey to the Center of the Earth
Earth’s Layered Structure
Earth Science Topic #12 Review Game
Hosted by Miss Bernal Category 1Category 2Category 3Category
Plate Tectonics, Earthquakes and Volcanoes Unit B - Chapters 3, 4 & 5.
Earthquakes Chapter 11 P. Lobosco
Dynamic Earth Topics: -Earth’s Interior -Continental Drift -Seafloor spreading -Plate Tectonics -Earthquakes & Epicenters.
EARTHQUAKES CHAPTER 8.
Bellringer List the four layers of Earth, starting with the innermost and moving outward.
By Mildred $100 Page 5Page 10Page 11Tectonics 1Tectonics 2 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400.
Lab # 6 – Pg. 121 Earthquakes and the Earth’s Interior
Plate Tectonics. Crust The crust is formed from continental and oceanic crust The crust covers the whole Earth.
Ch. 7 Plate Tectonics This is a satellite image of the San Francisco Bay area. The row of lakes below marks the line of the San Andreas fault, a crack.
Mercalli Scale Crust Mantle Plate Tectonics P-wave S-wave focus epicenter seismograph Richter Scale Tsunami fault.
Earth’s Oceans Some facts… Over 70% of the Earth’s surface is Ocean. That’s about 360 million square km. Ocean water is different than fresh water;
The Layers of the Earth!. Earth Layers The Earth is divided into three major zones that are defined by their compositions. *Core (Inner and Outer) *Mantle.
What’s Inside?. The Earth’s Core – Almost as hot as the surface of the sun (due to radioactive decay) Escape of this inner heat drives geological activity.
Earthquakes happen where Earth's plates meet. Most earthquakes happen under the sea. Where the plates stick, pressure builds up and then the earth shakes.
Earth’s Interior. The Earth’s Core Much of the information scientists have about the Earth’s interior has come not only from complex instruments but also.
Draw a cross section of the earth and label it with the correct names and characteristics crust - relatively thin and rocky (Oceanic 30-50km and continental.
The Earth’s Interior & Plate Tectonics Physical Science Chapter 17 Section 1.
The Earth’s Structure A Journey to the Center of the Earth.
The Layers of the Earth © Copyright 2006.  M. J. Krech. All rights reserved.
Earthquakes Chapter 8. What is an earthquake? Vibration of Earth produced by a sudden release of energy Movements along the fault line.
Created byMildred (who else?) $100 Page 10 More pg.10 Page 11 More pg.11 My Fault $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500.
EARTH’S INTERIOR. Earth’s Interior Geologists have used two main types of evidence to learn about Earth’s interior: –Direct evidence from rock samples.
The Dynamic Crust Topic 12. Principle of Original Horizontality: The assumption that sedimentary rocks form in horizontal layers. Drawing: Then how.
Earthquake Jeopardy Ride the Wave Plate Tectonic.
Earth’s Layers. The Layers: Lower mantle Transition region.
CHAPTER 12 EARTHQUAKES MOVEMENTS OF THE EARTH THAT ARE CAUSED BY A SUDDEN RELEASE OF ENERGY WHEN ROCKS MOVE ALONG A FAULT.
Earth Interdependence. What internal energy source is responsible for the convection currents in the earth’s asthenosphere?
Key Terms: Seismology - the study of earthquakes Seismology - the study of earthquakes Seismologist - a scientist who studies earthquakes and seismic.
LAYERS OF THE EARTH.
Earth’s Interior “Seeing into the Earth”
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Chapter 7-Section 1 Earth’s Moving Plates
Living in an Active Zone
Earthquakes Section 2.3.
CH 8 Earthquakes.
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Ocean Floor.
What’s inside the Earth. Is there really another world at the center
Earth’s Interior Notes.
Today’s Warm-Up Friday, January 10
DO NOW Pick up notes sheet..
Earthquakes, volcanoes, and mountains
Earth’s Interior Notes.
Teaching a Lesson ES Lesson Using Regents Diagrams
Physical Geology Composition of materials, tectonic cycle, Formation and identification of rock types.
Earth’s Interior.
Earth Science Ch. 8 Earthquakes.
There is a quiz (not a test) planned for Wedneday.
Earthquakes! Created by Mildred (who else?).
A Journey to the Center of the Earth
Nature, magnitude and frequency of seismic activity (earthquakes)
Presentation transcript:

Announcements No lab this week! Please refer to schedule on website (instruct.uwo.ca/earth-sci/023-> Revised lab order) Next week’s lab: Radioactivity experiment (detection of 137 Cs samples in a sandbox) Thursday: Midterm Exam

Midterm Exam: Thursday Multiple choice, 30 questions In class – please place backpacks etc. at front of class before sitting, but keep your student card Bring HB pencil, eraser & calculator Section: mark 023 or 123, as appropriate

What should I study? There are 5 questions that require a calculator. The remaining 24 questions are general knowledge taken from the lecture material (1 from the lab material) You will be given a Periodic Table if needed Some questions will relate to movies shown in class One bonus question from the Scugog lecture (but maximum mark is 30/30!)

Is there any scientific basis for ?

Your task Identify 3 correct and 3 incorrect statements about Earth ’ s interior Assume that the technology is possible

Why here? Is this the best launch location for a ship to go to the centre of Earth??

The Marianas Trench marks where the fast-moving Pacific Plate converges against the slower moving Philippine Plate. The Challenger Deep, at the southern end of the Marianas Trench, plunges deeper into the Earth's interior (nearly 11,000 m) than Mount Everest rises above sea level (about 8,854 m).

Marianas Trench: crustal thickness ~10 km Seismically active region

…but Earth’s radius is smaller (by 21.3 km) at the poles...

Choice of launch location: ? My core score: 6/10

Is this normal whale behaviour? How fast and how deep can whales swim?

Blue whales: - travel in small pods - can swim up to 48 km/h - can dive to depths of 105 m - use low-frequency sounds to communicate and locate krill

Whale behaviour: ? My core score: 5/10

Earthquake? What’s up with those falling boulders?

T phase : Tertiary wave, a late-arriving short-period wave often recorded at stations of island or coastal regions. Can be caused by earthquake or submarine volcanic eruption.

Submarine debris flow: maybe Falling boulders: no way! Puerto Rico Trench

Earthquake and falling boulders ? My core score: 5/10

Is this schedule accurate? Time to Moho: 15 minutes Time through mantle: 24 hours Time through core: 15 hours Average speed: 94 km/h Time to Moho (10 km): 6.4 minutes Time through mantle: 30.5 hours Time through outer core: 24 hours

Is this schedule accurate? Not too bad, for Hollywood!

Schedule/basic Earth structure: ? My core score: 7/10

Giant crystal cavern in the mid-mantle. Yeah right!

Geode: a hollow rock (usually spherical) with crystals lining the inside wall.

Giant crystal cavern in the mid-mantle. Yeah right! Pressure too high (~ 0.5 Mbar) Such large cavities would be seismically detectable.

Bathyscaphe Trieste 23 January, 1960 Challenger Deep (Marianas Trench) Pressure: Mbar

Geode in mid mantle ? My core score: 1/10

Diamond the size of Cape Cod Virgil being damaged Do diamonds exist in the lower mantle?

Diamonds are a high- pressure form of graphite (carbon) Diamonds form at depths > 100 km They are usually brought to the surface by rare volcanic eruptions (kimberlites) Diamonds from the deep mantle have recently been recognized!

Diamond the size of Cape Cod … but are they the size of Cape Cod?

Giant diamonds in lower mantle ? My core score: 7/10

Are stated temperatures and pressures correct? Temperature in outer core: 9000 o F ~ 5000 o C

Are stated temperatures and pressures correct? Pressure at Moho: 8x10 5 PSI ~ 55 kbar Actual lithostatic pressure at Moho: 4-12 kbar Note: The core is more dense than the mantle!!!

Temperatures and pressures ? My core score: 5/10

Is Earth’s magnetic field generated in the core?

Yes! But the so-called geodynamo is much more complex than depicted in the Core.

Earth’s Magnetic Field ? My core score: 7/10

Could the geodynamo be stopped by a giant electromagnet hidden somewhere in Alaska? Beams high-powered electromagnetic energy waves down fault lines to trigger earthquakes Project DESTINI

Could the geodynamo be stopped by a giant electromagnet hidden somewhere in Alaska? Project DESTINI “We need to suck up every drop of juice east of the Rockies to fire up DESTINI”

Project DESTINI Earth’s magnetic dipole moment: 6.2x10 21 Am 2 If n = , area = 100 m 2, then I = 6.2x10 20 A Assuming this is a 220V appliance, this would take 2.8TW of power (U.S. power consumption = 3.23 TW) This might just work!!!

Project DESTINI ? My core score: 1/10

Would a 200 MT nuclear explosion in the outer core have any effect? At 4x10 6 K, using ideal gas law (PV = nRT) with 1 mole H with a reaction volume of 0.01m 3, I calculate an explosive pressure of 32.5 kBar Since this is less than the pressure in the outer core, the nuclear bomb would actually do pretty much nothing.

Restarting the geodynamo using nuclear weapons ? My core score: 0/10

Would sudden loss of Earth’s magnetic field allow cosmic death rays to zap the Golden Gate Bridge?

The Earth will fry without a magnetic field ? My core score: 1/10