Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

39
Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Transcript of Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Page 1: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Plate TectonicsLearning Goal:

Comprehend plate tectonics and apply in lab.

Page 2: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Convection currents

Page 3: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Continental drift – idea that continents have moved slowly to their current positions due to convection currents in the mantle.

Pangea – the idea that the all land masses on earth were once a single large land mass.

Page 4: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Ocean floor spreading – theory that hot less dense material below Earth’s crust rises toward the surface at the mid-ocean ridges. Then, it flows sideways, carrying the seafloor away from the ridge in both directions. http://geology.com/nsta/divergent-boundary-oceanic.gif

Convection current – unequal distribution of heat in the mantel causes a net movement in a circular motion.

Page 5: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 6: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

The Earth’s CRUST is the outer most part of the Earth’s surface.

• Average 32 km thick (19.84 miles)

• Thickest point 70 km (in mountains)

• Thinnest point 8 km (under ocean)

Page 7: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Plate tectonic – theory that Earth’s crust and part of the upper mantle are broken into sections called plates.

Lithosphere – all of the earth’s crust and part of the upper mantle.

http://www.allaboutspace.com/subjects/astronomy/planets/earth/Inside.shtml

Asthenosphere – plastic like layer below the lithosphere. The ridged plates of the lithosphere “float” on the more plastic layer called the asthenosphere.

Page 8: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

l

Page 9: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 10: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Deformation – The breaking, tilting, and folding of crustal rock due to crustal movement. (three types of forces)

1. Compression – squeezing of earth’s crust that compacts the rock. Convergent boundary

2. Tension – is the pulling apart of the earth’s crust. Divergent boundary.

3. Shearing – pushes rocks side by side in opposite directions. Transform boundary.

Page 11: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Convergent boundary

Divergent boundary

Transformation boundary

Page 12: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 13: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

subduction

Rift valley

Page 14: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

FAULTS

Normal Fault (Divergent Boundary) – fault caused by tension stress that moves the hanging wall down relative to the foot wall.

Page 15: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Fault block mountain is a mountain created by blocks of rock uplifted by normal faults.

Page 16: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Divergent boundary in Iceland

Page 17: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Reverse Fault (Convergent Boundary) – fault caused by compression forces where the hanging wall will move up relative to the foot wall.

Page 18: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 19: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

In Lateral (strike-slip) faulting (Transform Boundary), the two blocks move either to the left or to the right relative to one another. Strike-slip faults are associated with crustal shear.

Page 20: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

San Andreas Fault, CA

Page 21: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Facts about folds/faults.

1. increased temp. =‘s fold

2. decreased temp =‘s fault

3. increased pressure =‘s fold

4. decreased pressure =‘s fault

5. rock type – brittle =‘s fault

6. rock type – ductile =‘s fold

7. time – greater the time =‘s fold

8. time – less time =‘s fault

Page 22: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 23: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 24: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 25: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 26: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

EarthquakesEarthquake – is the shaking and trembling that results from the sudden movement of part of the Earth’s crust.

Tsunamis – A giant sea wave produced by an earthquake.

Page 27: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 28: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Seismic WavesFocus – The point beneath the Earth’s surface where the rocks break and move, the underground origin of the earthquake.

Epicenter – The point directly above the focus, on the earth’s surface where the origin of an earthquake is above ground.

Page 29: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Faults- Once the elastic limit of rocks is passed, they break and move along

surfaces.• 3 types of faults are:

• Normal Fault- These form at divergent boundaries.

• Reverse Fault- These form at convergent boundaries.

• Strike-Slip Fault- These form at transform boundaries.

Page 30: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 31: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Seismic waves – earthquake waves. *Three types.

1. Primary waves (P-waves) - arrive at a given point before any other type of seismic wave. Will pass through solid, liquid and gas.(fastest of the three)

2. Secondary Waves (S-waves) – arrive at a given point after the P wave. (second fastest) Will only travel thru solids. Will NOT pass through liquids and gases thus creating a shadow zone.

Page 32: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 33: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

3. Surface waves (L-waves) – slowest moving seismic

waves. Arrives last.

Page 34: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 35: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

VolcanoesVolcano –A mountain that forms when layers of lava and volcanic ash erupt and build up.

Magma – rock that exists as a hot liquid deep within the earth.

Lava – is magma that reaches the Earth’s surface.

Page 36: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.
Page 37: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Composite Volcanoes –Violent eruptions due to high amount of silica (D.A.N, quartz, mica, feldspar) which is light in color and is explosive because of large amounts of gas, ash and lava.

Page 38: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Domes – is the uprising area caused by magma

Page 39: Plate Tectonics Learning Goal: Comprehend plate tectonics and apply in lab.

Shield volcano – Volcanoes composed of quiet lava flows. The lava has a low amount of silicia (D.A.N, quartz, mica feldspar) and is dark in color. These volcanoes are nice with gently sloping sides with very wide base.