Chapter 8 Worksheets Section 1-4.

Slides:



Advertisements
Similar presentations
Plate Tectonics Chapter - 8
Advertisements

Plate Tectonics.
Plate Tectonics Review
Tectonic Plates Made of the Lithosphere Oceanic Crust -Dense -(tightly packed) -Made of Iron, and Magnesium Continental Crust -Less dense -Made mainly.
Major Geological Events Caused by Plate Tectonics
Continental Drift Who is Alfred Wegener?
Plate Tectonics Review Misc. Plate Tectonics Plate Evidence Earth's Interior Geologic Events Plate Boundaries.
8 Plate Tectonics 8.1 What Is Plate Tectonics?
Chapter 8 Notes Place these notes into your Geology Notebooks.
Chapter 10 Plate Tectonics. Alfred Wegener Proposed they hypothesis of continental drift Proposed they hypothesis of continental drift CONTINENTAL DRIFT-
Chapter 17 Plate Tectonics. Structure of the Earth Earth.
Chapter 7 Section 1: Continental Drift Section 2 : Sea Floor Spreading
The Sea Floor. Continental vs. oceanic crust What is Continental Drift? The idea that the plates are floating and moving around on a liquid mantle.
Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)
Continental Drift Chapter 10. Wegener’s Hypothesis  Once a single supercontinent  Started breaking up about 200 mya  Continents drifted to current.
Plate Tectonics. Plate Tectonics is a theory that describes the formation, movements, and interactions of Earth’s plates.
Wegener Pangaea Continental Drift. Evidence for Continental Drift Mesosaurus dino fossils Glossopteris plant fossils Formation and age of particular mountains.
The Theory of Plate Tectonics The Earth’s crust is broken up into plates which move around on top of the mantle **Driven by convection currents**
Chapter 14 Plate Tectonics. Continental Drift Theory 1. Fit like a jigsaw 2. Matching fossils 3. Tropical plant fossils in Polar regions. Drift explained.
 Alfred Wegener – developed the Continental Drift hypothesis  The continents were once joined as one single “supercontinent”  Pangea was the name given.
Plate Tectonics Continental Drift Crust is broken into plates that are in constant, very slow motion, driven by convection currents in the mantle. Puzzle-like.
 In 1912, German scientist Alfred Wegener proposed the idea of continental drift.  Based on evidence he saw, he believed that the continents must have.
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 Theory that describes the formation, movements, and interactions of Earth’s lithospheres' plates. *Copy the notes that are in RED.*
Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)
 How does the distribution of fossils provide evidence for continental drift?  How does the location of mountain chains provide evidence of continental.
Plate Tectonics Earth Science Chapter 9. Continental Drift  scientific theory proposing the slow, steady movement of Earth’s continents  Alfred Wegener:
8 Plate Tectonics 8.1 What Is Plate Tectonics?
Plate Tectonics Chapter 9. Section 9.2 Plate Tectonics.
Unit 4 Lesson 6 Plate Tectonics
Plate Tectonics Section 1: Drifting Continents
Chapter 5 plate tectonics review
What was Wegener’s hypothesis called?
LAYERS OF THE EARTH PLATE BOUNDARIES PLATE TECTONICS CONTINENTAL DRIFT
PLATE TECTONICS A Moving Experience!!!.
Plate Tectonics.
Plate Tectonics Cornell Notes.
Inside Earth Chapter 1.5 Pages 42-47
Sci 10 – Class Starter Please hand in your Plate Movement Assignment at the front of the room Collect a “What we have learned so far…” Quiz from the front.
Plate Tectonics.
Chapter 3: Plate Tectonics
Geology Notes Part 6.
Plate Tectonics Chapter 10.
Theory of Plate Tectonics
Plate Tectonics.
Land Unit: Plate Tectonics
The Earth’s Crust in Motion…
Land Unit: Plate Tectonics
Warm-Up: March 18, 2016 Write down everything you know about plate tectonics.
Chapter 7 Section 2 Pages Continental Drift.
PART 1: The Theory of Continental Drift is a hypothesis that states the continents once formed a large, single landmass called Pangaea.
Chapter 10 Plate Tectonics.
Land Unit: Plate Tectonics
2 oceanic plates colliding 3 Types of Plate Boundary Movements
Chapter 7 Section 2 Pages Continental Drift.
Chapter 7 Section 2 Pages Continental Drift.
Continental Drift Pangaea
Unit 1 Lesson 3 Earth’s Plates
Continental Drift 1912 – German Scientist Alfred Wegener
Plate Tectonics.
Place these notes into your Geology Notebooks.
Plate Tectonics.
Plate Tectonics.
Jeopardy Final Jeopardy Tectonic Plates Divergent Transform Convergent
Plate Tectonics.
Chapter 7 Section 2 Pages Continental Drift.
Chapter 4 Plate Tectonics
Plate Tectonics Notes.
Chapter 8: Plate Tectonics
Warm-up Week 13 Day 1 Describe Alfred Weneger’s “Continental Drift” hypothesis in your own words. Give 4 pieces of evidence that support the “Continental.
Presentation transcript:

Chapter 8 Worksheets Section 1-4

8-1 After You Read: Complete the table by describing evidence that has been used to support the continental drift hypothesis and the theory of plate tectonics. Hypothesis or Theory Supporting Evidence Continental drift hypothesis Theory of plate tectonics Similarities in shapes of the continents; same fossils and distinctive rock formations found in South America and Africa; climate change evidence. Location of earthquakes and volcanoes; magnetism of ocean floor; age of ocean floor.

8-2 Complete the graphic organizers to explain the processes that take place at a subduction boundary and a divergent boundary. Molten rock rifts or cracks Oceanic continental Molten rock Deep-sea trench Deep-sea trench Volcanic islands Mountain chain Moves away

Cause of plate movement 8-3 After You Read Complete the table by listing three hypothetical causes for plate movements. Identify the type of boundary associated with each. Put a plus or minus sign next to the factors most or least influential on plate movement. Cause of plate movement Type of boundary 1. Mantle convection Divergent boundary 2. Slab pull 3. Ridge push Subduction boundary

8-4 After You Read Mountain ranges far from plate boundaries today. Data about ages of rocks. Fossils Evidence of glaciers in lands that are now tropical.

8-4 After You Read Deep-sea sediments Igneous rock River sediment Terranes