striation – linear grooves formed in the surface of some minerals as they grow

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Striation – linear grooves formed in the surface of some minerals as they grow.

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Page 1: Striation – linear grooves formed in the surface of some minerals as they grow

Striation – linear grooves formed in the surface of some minerals as they grow.

Page 2: Striation – linear grooves formed in the surface of some minerals as they grow

Plate Tectonics

Page 4: Striation – linear grooves formed in the surface of some minerals as they grow

The Prune Effect - 1800s - (failed attempt 1)

The molten Earth cools and contracts

The crust wrinkles and crumples

Mountains form

What about rift valleys?

What about shape and position of the continents?

Page 5: Striation – linear grooves formed in the surface of some minerals as they grow

Rift Valley

Page 6: Striation – linear grooves formed in the surface of some minerals as they grow

The Expanding Earth – (failed attempt 2)

20th century - radioactive decay

Land masses are ripped apart

Explains the continents

What about the mountains?

Page 7: Striation – linear grooves formed in the surface of some minerals as they grow

- An idea before its time

- Alfred Wegener 1915

- Processor to plate tectonics

Continental Drift

Pangaea - supercontinent

Fragmented and floated around

Page 8: Striation – linear grooves formed in the surface of some minerals as they grow

Pangaea 200 million years ago

Super Continent

Page 9: Striation – linear grooves formed in the surface of some minerals as they grow

Lines of Evidence

•Matching Coastlines

•Matching Geology

•Glacial Deposits

•Fossil Evidence

•Apparent Polar Wandering

Page 10: Striation – linear grooves formed in the surface of some minerals as they grow
Page 11: Striation – linear grooves formed in the surface of some minerals as they grow

Matching

Coatlines

Page 12: Striation – linear grooves formed in the surface of some minerals as they grow

Where is the coastline?

Page 13: Striation – linear grooves formed in the surface of some minerals as they grow

Matching

Geology

Page 14: Striation – linear grooves formed in the surface of some minerals as they grow

The Collision

Page 15: Striation – linear grooves formed in the surface of some minerals as they grow

The Separation

Page 16: Striation – linear grooves formed in the surface of some minerals as they grow

Glacial Deposits

Striations

Page 17: Striation – linear grooves formed in the surface of some minerals as they grow
Page 18: Striation – linear grooves formed in the surface of some minerals as they grow
Page 19: Striation – linear grooves formed in the surface of some minerals as they grow

Fossil Evidence

Glossopteris

Page 20: Striation – linear grooves formed in the surface of some minerals as they grow

Mesosaurus - links South America and Africa during the late Paleozoic and early Mesozoic eras.

Page 21: Striation – linear grooves formed in the surface of some minerals as they grow

Apparent Polar Wandering

Page 22: Striation – linear grooves formed in the surface of some minerals as they grow

A study by S. K. Runcorn in the 1950s, indicated that the magnetic north pole had apparently moved over the last 500 million years, from Hawaii to its present location.

Page 23: Striation – linear grooves formed in the surface of some minerals as they grow

All the parts are in place,

but 1.

How are the continents moving?

Page 24: Striation – linear grooves formed in the surface of some minerals as they grow

The Revolution Begins

early 1960s

Page 25: Striation – linear grooves formed in the surface of some minerals as they grow

RingOf

Fire

Page 26: Striation – linear grooves formed in the surface of some minerals as they grow

Discovery of Midoceanic Ridge

Detailed sea-floor mapping

Page 27: Striation – linear grooves formed in the surface of some minerals as they grow

Harry Hess - essay in geopoetry

* Sea-floor spreading hypothesis

Page 28: Striation – linear grooves formed in the surface of some minerals as they grow

Paleomagnetism

Youngest rock in the center

Page 29: Striation – linear grooves formed in the surface of some minerals as they grow
Page 30: Striation – linear grooves formed in the surface of some minerals as they grow

Unifying Theory - Plate Tectonics

Page 31: Striation – linear grooves formed in the surface of some minerals as they grow

Tectonic cycle- deals with the movement and interactions of the lithospheric plates.

Page 32: Striation – linear grooves formed in the surface of some minerals as they grow

Seafloor Spreading and Plate Boundaries

Page 33: Striation – linear grooves formed in the surface of some minerals as they grow

Plate Boudaries / MarginsDivergent Plate Bounderies

1. continental - rift valleys

Page 34: Striation – linear grooves formed in the surface of some minerals as they grow

Divergent Plate Boundaries

2. ocean - midoceanic ridge / spreading sea floor

Page 35: Striation – linear grooves formed in the surface of some minerals as they grow

Transform Plate Bounderies

San Andreas Fault

Page 36: Striation – linear grooves formed in the surface of some minerals as they grow

Convergent Plate Bounderies

Oceanic - Continental

Oceanic - Oceanic

Continental - Continental

Andes Mountains

Japan, Philippines

Himalaya Mountains

Page 37: Striation – linear grooves formed in the surface of some minerals as they grow

West Coast of United States

Page 38: Striation – linear grooves formed in the surface of some minerals as they grow

Earthquakes, Volcanoes, and Plate Boundaries

Page 39: Striation – linear grooves formed in the surface of some minerals as they grow
Page 40: Striation – linear grooves formed in the surface of some minerals as they grow
Page 41: Striation – linear grooves formed in the surface of some minerals as they grow
Page 42: Striation – linear grooves formed in the surface of some minerals as they grow

Benioff ZoneAssociated with Subduction

Page 43: Striation – linear grooves formed in the surface of some minerals as they grow

How old is the ocean floor?

Page 44: Striation – linear grooves formed in the surface of some minerals as they grow

Driving Mechanism - convection currents