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Topic VI: The Dynamic Earth. Earth’s Four Zones: 1. Crust: the outside or surface—made up of mostly igneous rock with a thin shell of sedimentary rock.

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Presentation on theme: "Topic VI: The Dynamic Earth. Earth’s Four Zones: 1. Crust: the outside or surface—made up of mostly igneous rock with a thin shell of sedimentary rock."— Presentation transcript:

1 Topic VI: The Dynamic Earth

2 Earth’s Four Zones: 1. Crust: the outside or surface—made up of mostly igneous rock with a thin shell of sedimentary rock on the outside

3 a. Oceanic Crust: only about 5 miles thin— made up of basalt (dense) b. Continental Crust: about 30 miles thick— made up of granite (less dense) Crust types….

4 2. Mantle: the middle layer that the crust “floats” on—divided into 3 parts: a. a. Rigid Mantle b. b. Asthenosphere c. c. Stiffer Mantle **the Lithosphere is the crust AND rigid mantle **the MOHO—boundary between the crust and mantle

5 3. Outer Core: liquid nickel & iron

6 4. Inner Core: solid because of high pressure / made of nickel and iron

7 Why Nickel & Iron?..... Meteorites!—more dense, sank to “center” of young molten Earth Meteorites!—more dense, sank to “center” of young molten Earth

8 What happens the deeper you go in the Earth? Density, temperature, pressure all increase Density, temperature, pressure all increase

9 Page 10

10 How do we know what Earth’s interior looks like? Study Earthquake waves (like an ultrasound) Study Earthquake waves (like an ultrasound)

11 What does the heat from the core cause? Continental Drift: the lithosphere (crust) is made up of solid plates that move (plate tectonics) Continental Drift: the lithosphere (crust) is made up of solid plates that move (plate tectonics)

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13 Plates move because of heat that rises in the Asthenosphere due to density differences—called convection currents or cells Plates move because of heat that rises in the Asthenosphere due to density differences—called convection currents or cells

14 More Convection Currents….

15 Even More Convection Currents:

16 Plate Boundaries: areas on Earth where two plates are interacting with each other Plate Boundaries: areas on Earth where two plates are interacting with each other **this is Where most Volcanoes / EQ’s / and Mountains Occur

17 Three Types of Plate Boundaries: 1. Convergent: plates collide (subduction zone—plate moves under another)

18 2. 2. Divergent: plates move apart

19 Page 10

20 3. 3. Transform: plates move side to side USA

21 Hotspots: places in Earth’s crust with an unusually high heat flow (Hawaii) Hotspots: places in Earth’s crust with an unusually high heat flow (Hawaii)

22 **plates move only a few centimeters per year—about as fast as your fingernails grow

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24 Evidence of Plate Motion: 1. Deformed (messed up) Rock Strata (layers) **because of gravity, all sedimentary rocks formed in horizontal layers (law of original horizontality)

25 If not horizontal, the layers can be… a. Tilted: force pushes rock layers from 1 side Force

26 b. Folded: forces push on rock layers from 2 sides (rocks are not broken) Force

27 c. Faulted: a break in the earth’s crust where movement occurs Force

28 Williamsport, PA

29 2. Displaced Fossils: marine fossils found in rock layers several hundred feet above sea level (uplift)

30 3. Subsidence: sinking of rock layers (fossils being found deep underground)

31 4. Continents Fit together like a puzzle

32 5. Rock layers and fossils may be correlated (matched-up) across oceans

33 6. Continuation of mountain chains from continent to continent

34 7. Evidence (fossils / rock) indicates that the climate was much different (coal found in Antarctica) Coal forms in a tropical swamp

35 New York: Salt and Marine Fossils Evaporated Ocean

36 8. Sea Floor Spreading (Divergent Plate Boundary)

37 Evidence of Sea-Floor Spreading: a. Radioactive Dating found that as rocks get closer to the continents they get older **more on this later

38 b. Reversal of Magnetic Polarity: the Earth’s magnetic poles switch from time to time—this can be seen because of iron in basaltic ocean rocks

39 **Iron (magnetic) in the liquid basalt line up like compass needles (stays when it hardens)

40 Hot Cold Young Old Mid-Ocean Ridge

41 Earthquakes Earthquakes: a sudden shaking or trembling of rock layers along a fault line or plate boundary (the rock layers slip) Earthquakes: a sudden shaking or trembling of rock layers along a fault line or plate boundary (the rock layers slip)

42 **energy is released and is transmitted by 2 types of waves 1. Primary or “P” waves (Compressional  ) 2. Secondary or “S” waves (Shear waves  )

43 Seismic Stations: located around the world— used to study earthquake waves. Seismic Stations: located around the world— used to study earthquake waves.  Seismographs: device that records the vibrations of earthquake waves waves

44 P-waves: travel “phastest” so it arrives at the seismic stations “phirst” P-waves: travel “phastest” so it arrives at the seismic stations “phirst”  Can travel through solid rock & magma (can travel through ALL Layers)

45 S-waves: travels slower so it arrives at seismic stations second S-waves: travels slower so it arrives at seismic stations second  Only travel through SOLIDS—all layers EXCEPT LIQUID outer core and Solid Inner Core

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47 Origin Time (what time EQ began at the epicenter) Epicenter Felt

48 Epicenter: point on the surface (city) directly above the focus (in the interior where the earthquake occurs) Epicenter: point on the surface (city) directly above the focus (in the interior where the earthquake occurs) **P & S waves travel out in all directions

49 1. Get P and S wave arrival times from 3 different seismic stations How is an earthquake’s epicenter located on a map?

50 2. Using the ESRT’s, find the distances from the epicenter for each station **The larger difference between P and S wave arrival times means that the seismic station is farther away from the epicenter

51 3. Using the distances and a compass, draw 3 circles **Where the three circles intersect the epicenter is located

52 **as these P & S waves travel, they change speed and bend (refract) as they enter different substances and / or different densities **remember the ultrasound? **this is how we know what Earth’s interior Looks like

53 Shadow Zone: a region on the Earth where no P and S waves are recorded (because of refraction & lack of s-waves) Shadow Zone: a region on the Earth where no P and S waves are recorded (because of refraction & lack of s-waves)

54 Earthquakes in NY (rare) **Remember Lat / long

55 Earthquake Strength Richter Magnitude Scale: measures the amount of energy an earthquake releases (uses seismographs) Richter Magnitude Scale: measures the amount of energy an earthquake releases (uses seismographs) Strong Weak **1 (little energy)  10 (tremendous energy)

56 Mercalli Intensity Scale: based on what damage people observe and shaking felt— can be used for historical earthquakes (newspaper articles) Mercalli Intensity Scale: based on what damage people observe and shaking felt— can be used for historical earthquakes (newspaper articles) Roman Numerals: I (little)  XII (lots)

57 in the cases of both scales, the closer you are to the epicenter, the more you will feel the shaking—meaning the numbers will be higher the closer you are to the quake in the cases of both scales, the closer you are to the epicenter, the more you will feel the shaking—meaning the numbers will be higher the closer you are to the quake

58 Does this make sense….. The closer you are to the epicenter, both P & S waves will be found at nearby seismic stations The closer you are to the epicenter, both P & S waves will be found at nearby seismic stations Stations on the other side of the world may or may not pick up P & S waves Stations on the other side of the world may or may not pick up P & S waves

59 Earthquakes can cause: a. Tsunamis: seismic sea waves (oceans)—can cause severe coastal damage

60 b. Landslides / avalanches c. Fires d. Train / Car wrecks

61 Earthquake Emergency Planning a. Get away from windows, chimneys b. Get under something strong (doorway) c. Don’t try to get outside (last < 30 sec)

62 Volcanoes: mountain composed of extrusive igneous rocks that can erupt gases, lava, ash, and rocks onto Earth’s surface Volcanoes: mountain composed of extrusive igneous rocks that can erupt gases, lava, ash, and rocks onto Earth’s surface

63 Volcanic Hazards a. Ash (buries everything)

64 b. Lava (usually moves slow—people avoid) c. Shooting, hot rocks (bombs)

65 d. Mudslides (ash mixes with snow and dirt from mountain tops)


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