Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Slides:



Advertisements
Similar presentations
Mr. Russo Beaumont High School
Advertisements

Continental Drift & Plate Tectonics
Plate Tectonics.
1.1 Earth has several Layers.  Denser material sinks  Less dense material rises to the top.
Plate Tectonics Review
Chapter 7 Earth’s Moving Crust
Chapter 17: Plate tectonics
Chapter 8 BHS Earth Science
Chapter 1: Plate Tectonics Earth’s Layers Continents Changing Position Over Time Plates Moving Apart Plates Coming Together
Unit 4 Lesson 2 Plate Tectonics
Notes Courtesy of your kind & intelligent teacher, Mr. Whallen.
Plate Tectonics And Continental Drift. Early Evidence for Continental Drift.
What type of boundary is represented here?
Unit 4 Lesson 2 Plate Tectonics Copyright © Houghton Mifflin Harcourt Publishing Company.
The Changing Earth Chapter 9: Plate Tectonics. Review Earth Has Several Layers.
1 Plate Tectonics Notes Geology – the study of the Earth and its processes.
Plate Tectonics Overview I. The Theory of Plate Tectonics  The Earth’s surface is divided into plates that move and interact with one another.
.. Plate Tectonics Theory that the Earth’s crust is made of rigid plates that float on the molten layer of the mantle. Comes from the Greek word meaning.
 Pangea  A land mass created by Alfred Wegner  Alfred Wegner  was a German scientist who claimed the continents were once joined.  Fossils  Fossils.
Our Amazing Planet. Planet Earth Earth’s Layers Crust Earth’s thin outermost layer. – Continental Crust (land) - thick low density rock (granite). –
Continental Drift Theory
Our Amazing Planet.
Plate Tectonics Earth Science. Continental Drift Alfred Wegener proposed the idea of continental drift in Looking at the continents, it is possible.
. PLATE TECTONICS. Plate Tectonics -Scientists think the earth formed about 4.6 billion years ago. It was originally a large ball of molten rock. As the.
Plate Tectonics 8th Science.
Plate Tectonics. Plate Tectonics is a theory that describes the formation, movements, and interactions of Earth’s plates.
Warm-up #43 Mar. 26  Brainstorming: Will California eventually slide into the ocean? Have continents really drifted apart over the centuries?
Chapter 8: Plate TectonicsChapter 8: Plate Tectonics 8.1: Earth has several layers 8.2: Continents change position over time 8.3: Plates move apart 8.4:
Africa The Red Sea between Africa and the Arabian peninsula in Asia marks a region where two pieces of the lithosphere are slowly moving apart. Over the.
CHAPTER TEN PLATE TECTONICS. Background Information  The Earth is made up of several layers that have different properties and compositions.  There.
Plate Tectonics. Plate Tectonics Pop Quiz 1) What was the name of the scientist that developed the idea that the continents had been once joined together.
 In 1915 Alfred Wegener proposed the Theory of Continental Drift  = continents are not fixed and in the past all continents had been joined.
 Alfred Wegener – developed the Continental Drift hypothesis  The continents were once joined as one single “supercontinent”  Pangea was the name given.
Continental Drift Theory Proposed by Alfred Wegener in million years ago, all of the continents were combined into one super-continent called.
+ Unit 4: Lesson 2: Theory of Plate Tectonics. + REVIEW What layer of the Earth is broken into tectonic plates? What layer of the Earth has convection.
Plate Tectonics Chapter 6. Earth is made up of materials with different densities. Scientists theorize that Earth began as a spinning mass of rocks and.
8. 2 Continents change position over time. Learning Goals Students will: -explain how the continental drift hypothesis was developed. -explain evidence.
Plate Tectonics.
Plate Tectonics Chapter 8. What Is Plate Tectonics? The Earth’s crust and upper mantle are broken into sections called plates Plates move around on top.
Plate Tectonics Study Guide. Alfred Wegener = Continental Drift Continents were once part of a single land mass called Pangaea (all lands). During the.
PLATE TECTONICS. Continental Drift Theory the continents were once joined into a supercontinent, Pangaea, proposed by Alfred Wegener Hypothezised about.
Continental Drift Hypothesis proposed by Alfred Wegener in 1915 The idea that Earth’s continents were once joined in a single landmass and gradually drifted.
Plate Tectonics Earth Science Chapter 9. Continental Drift  scientific theory proposing the slow, steady movement of Earth’s continents  Alfred Wegener:
Warm – Up 12/10/14  Please get out your layers of the Earth foldable that you made yesterday! On the yellow sheet of paper write your first and last name.
Good Afternoon! Please get your science notebook and get out your plate boundaries map and worksheet from Friday.
Chapter 7. What are the 3 Major Zones of the Earth?
Plate Tectonics Video Clip of Continental Drift. Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer core.
Unit 4 Lesson 6 Plate Tectonics
Unit 4 Lesson 2 Plate Tectonics
Chapter 5 plate tectonics review
Continental Drift.
LAYERS OF THE EARTH PLATE BOUNDARIES PLATE TECTONICS CONTINENTAL DRIFT
Unit 4 Lesson 2 Plate Tectonics
PLATE TECTONICS A Moving Experience!!!.
Unit 4 Lesson 2 Plate Tectonics
Plate Tectonics Cornell Notes.
Plate Tectonics.
Plate Tectonics Chapter 10.
Plate Tectonics.
Land Unit: Plate Tectonics
Land Unit: Plate Tectonics
Land Unit: Plate Tectonics
Plate Tectonics.
Continental Drift Pangaea
Unit 1 Lesson 3 Earth’s Plates
Unit 4 Lesson 2 Plate Tectonics
Scientific Theory of Plate Tectonics
The Changing Earth Plate Tectonics.
Plate Tectonics.
Unit 4 Lesson 2 Plate Tectonics
Presentation transcript:

Plate Tectonics

Earth’s Layers

The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They move like pavement resting on hot tar Convetion Currents in the Earth's Crust

The lithosphere looks like a jigsaw puzzle…on the surface of the earth Tectonic plates- large slabs of rock parts of ocean crust and continents rest on.

Geologists Geologists study earth processes such as landslides, earthquakes, floods and volcanic eruptions. Geologists work to understand the history of our planet. The better they can understand Earth’s history the better they can foresee how events and processes of the past might influence the future.

Alfred Wegener A geologist who first proposed continental drift theory in 1912 His hypothesis was that all of earth’s continents were once one giant land mass Gradually they drifted apart His scientist peers and friends did not agree until the middle of the 1900’s

Evidence for Continental Drift 1. Fossil Record: the fossil of the same ancient reptile was found in both South America and southern Africa, but no other place in the world. Both continents must have been joined together at some time in the past.

Evidence for Continental Drift Evidence of Climate change- Fossils of ancient ferns from jungles exist on Greenland, which is now covered in ice. Greenland must have once been near the equator. Evidence of glaciers existed in South Africa, where the climate is now a jungle and desert in parts.

Evidence for Continental Drift Geology- rock typing found on different continents matches up. Rocks from Brazil matches up with Africa. Carbonado diamondites supernova rocks that impacted on Earth in the Brazil and Central African Republic area (these were originally next to each other, before the ancient Gondwana continent rifted apart).

Rock Evidence

SuperContinents Pangaea was formed 270 mya during the Permian and Triassic time periods of Earth’s history. Most of the dry land was joined together into one huge land mass. The Permian mass extinction, which wiped out an estimated 96% species about 248 million years ago, was a major event during this time. Pangaea began to split apart 200 mya

New Technology, New Discoveries Scientists began mapping the sea floor Using drilling, SONAR, lasers bounced off of satellites, and undersea explorers, they started making detailed maps of the sea bed. These discoveries gave evidence of continental drift and how the tectonic plates moved.

Sea Floor Spreading Molten rock rises through cracks It cools and forms new crust Old crust is pulled away Oldest crust is pulled down into trenches into asthenosphere and destroyed. Called Subduction So…Sea floor is only 180 million years old Earth continents are 4 billion years old

Sea floor spreads because of…Convection Currents

Sea floor spreading and convection ctonics/p_paleomag.html Floor Spreading with Bill Nye/Sea Floor Spreading with Bill Nye

Divergent Boundary Where plates move apart Can form Rift Valley on land

Divergent Boundary Example: divergent plate boundary is the Red Sea. Once, the Arabian peninsula and Africa formed a single continent. They are now being ripped apart. The white arrows show the directions the two plates are moving. You can see that a new ocean, the Red Sea is being formed as they separate.

Convergent Boundary

The dense, leading edge of the oceanic plate actually pulls the rest of the plate into the flowing asthenosphere and a subduction zone is born! Where the two plates intersect, a deep trench forms. Volcanoes and mountain ranges usually occur along these boundaries. Think Ring of Fire, Swiss Alps, Appalachian Mountains!

Transform Boundary Two plates scrape past each other Usually form along plate lines

Transform Boundary Example of Transform Boundary would be the San Andreas Fault in California Earthquakes usually happen along transform boundaries.

Boundaries ce/terc/content/visualizations/es0804/es0804 page01.cfm?chapter_no=visualization urse/descr/EAS220/2008%20Lectures/Lecture %207%20web/PlateMotionppt.htmlwww.geo.cornell.edu/eas/education/co urse/descr/EAS220/2008%20Lectures/Lecture %207%20web/PlateMotionppt.html

Magnetic Reversals shows/greatest-discoveries/videos/100- greatest-discoveries-magnetic-field- reversal.htmscience.discovery.com/tv- shows/greatest-discoveries/videos/100- greatest-discoveries-magnetic-field- reversal.htm explanation of sea floor spreading and magnetic reversalsVideo explanation of sea floor spreading and magnetic reversals