Continental Drift.

Slides:



Advertisements
Similar presentations
Continents change position over time
Advertisements

Plate Tectonics.
Continents change Position over Time
1.1 Earth has several Layers.  Denser material sinks  Less dense material rises to the top.
Continents Change Position Over Time
Chapter 1: Plate Tectonics Earth’s Layers Continents Changing Position Over Time Plates Moving Apart Plates Coming Together
Unit 4 Lesson 2 Plate Tectonics
If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle…..the shapes of the coastlines.
Chapter 10 Plate Tectonics. Alfred Wegener Proposed they hypothesis of continental drift Proposed they hypothesis of continental drift CONTINENTAL DRIFT-
Chapter 10 Review By Chelsey Roberts. Continental drift: Wegener’s hypothesis A german scientist, Alfred Wegener (1912), came up with the hypothesis of.
Unit 4 Lesson 2 Plate Tectonics Copyright © Houghton Mifflin Harcourt Publishing Company.
Formation of the Earth. Previous Theories  Continental Drift Theory  Developed by Alfred Wegner (1900’s)  Believed continents were once all combined.
Plate Tectonics.
Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.
What makes the plates of the crust move?  Continental Drift  Pangea  Mid-Ocean Ridge  Convection  Theory of plate tectonics.
Plate Tectonics Test Study Guide Mary George King Core 1 ScienceMrs.Bannister.
Continents change position over time
List the layers of the earth from the least dense to the most dense.
. 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.
Earth has several layers ► Ch. 3, section 1-unit B ► learn:  Different properties of earth’s layers  About plates that make up the outer most layer of.
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:
What is it? Continental Drift - Earth’s continents were once joined in a single landmass, and gradually moved, or drifted apart. People thought this for.
8. 2 Continents change position over time. Learning Goals Students will: -explain how the continental drift hypothesis was developed. -explain evidence.
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.
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.
Plate Tectonics. What do the locations of Volcanoes and Earthquakes tell us?
Plate Tectonics.
Unit 4 Lesson 6 Plate Tectonics
Unit 4 Lesson 2 Plate Tectonics
PLATE TECTONICS.
Chapter 5 plate tectonics review
Unit 3 vocabulary Practice Quiz.
C H. 3 LESSON 3.2 CONTINENTS CHANGE POSITION OVER TIME
Ch 9 Plate tectonics.
Unit 4 Lesson 2 Plate Tectonics
Continental Drift & Plate Movement
Misc 1 Continental Drift Evidence of Plate Tectonics Plate Movement
Plate Tectonics EQ: How do lithospheric plates move and how do they affect the Earth’s surface?
Unit 4 Lesson 2 Plate Tectonics
Plate Tectonics.
Plate Tectonics Cornell Notes.
Plate Tectonics.
Continental Drift & Plate Movement
Chapter 7 Plate Tectonics
Continental Drift & Plate Tectonics Notes
Chapter 3: Plate Tectonics
Land Unit: Plate Tectonics
Plate Tectonics Theory that the outer rigid layer of the earth (the lithosphere) is divided into a couple of dozen "plates" that move around across the.
Land Unit: Plate Tectonics
Land Unit: Plate Tectonics
Chapter 1 Earth’s Layers.
Earth’s Structure and Pangaea
Continental Drift Pangaea
Unit 1 Lesson 3 Earth’s Plates
Unit 4 Lesson 2 Plate Tectonics
Continental Drift.
CHAPTER 10-1 CONTINENTAL DRIFT
#7 Soap Float Lab #8 Continental Drift & Plate Tectonics Notes
Earth’s Structure and Pangaea
Plate Tectonics.
QUICK REVIEW… Layers of the Earth
Continents change position over time
Unit 4 Lesson 2 Plate Tectonics
Earth’s Structure and Pangaea
Earth’s Structure and Pangaea
Earth’s Structure and Pangaea
Earth’s Structure and Pangaea
Convection Currents What causes the tectonic plates to move?
Earth’s Structure and Pangaea
Presentation transcript:

Continental Drift

What is it? Continental Drift - Earth’s continents were once joined in a single landmass, and gradually moved, or drifted apart. People thought this for centuries - they began thinking this when the first maps were introduced to the world. Alfred Wegener came up with the hypothesis of continental drift.

Fossil Evidence The same fossils have been discovered in South America as well as in western Africa. Mesosaurus - a reptile that lived in ancient time Lived 270 million years ago Fossils are only found in these two places

Climate Evidence Today, Greenland lies near the north pole. There are fossils being dug up in Greenland that have ancient tropical plants. How did tropical plants get to an area that is so cold and covered in ice? South Africa is warm today? South Africa has evidence that it was once covered by ice.

Geologic Evidence The kinds of rocks on each continent can be matched to another continent. The rock layers in Brazil match the rock layers in western Africa. Rocks in the Appalachian Mountains match rocks found in Scotland.

Pangaea With so much evidence that the continents were once connected, Wegener drew a conclusion. The continents all were connected in a supercontinent that was named Pangaea. Pangaea split apart 200 million years ago.

How do the continents move? 1950s - Scientists begin mapping the sea floor. How would you think the sea floor would look? They thought it would look smooth. Scientists found mid-ocean ridges, or underwater mountains.

Mid-Ocean Ridges Form along cracks in the crust Molten rocks rise though the cracks, cool, and the mountains are formed. Newer rock comes out, and pushes the older rock away. Scientists tested rocks and found that the youngest rocks were by cracks in Earth. The oldest ocean rock is only 160-180 billion years old. The continents that we live on is about 4 billion years old.

If we keep getting new rock, why is Earth the same size? Deep sea trenches The older crust comes to a trench, and it sinks into the trench. Old crust is destroyed at the same rate new crust is being formed; this is why we are not getting any bigger. This proves that Earth is moving!

Why do plates move? Tectonic plates rest on the asthenosphere. Rocks move by convection. Convection - energy transfer by the movement of material Hot softer rock rises, cools, and sinks, process starts again and again This is called a convection current. These convection currents are present in the mantle.

Plate Tectonic Theory Theory of plate tectonics - The lithosphere is made up of huge plates that move over the surface of the earth Plates move over a long period of time in three main ways Past each other Move apart Push together Earthquakes, volcanoes, and mountain ranges occur when the plates run into each other.