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Tectonic Plates.

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Presentation on theme: "Tectonic Plates."— Presentation transcript:

1 Tectonic Plates

2 Layers of Earth Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’ so it is easier to bend and move Radioactivity is the sourc of heat in the mantle

3 2 Kinds of Crust Continental – less dense, thicker
Oceanic – more dense, thinner

4 2 Kinds of Mantle Upper – solid, floats on…
Lower – plastic (somewhat fluid) Why? Earth’s crust and upper mantle “float” on the plastic portion of the mantle. (asthenosphere)

5 Convection Currents Movement of hot liquid or gas Heated – rises
Cools – drops Earth’s Crust Cracks… Convection currents in mantle cause cracking in crust Thermal Convection cause seafloor to spread and continents to drift

6 Convergent Boundary Divergent Boundary

7 Divergent – Ocean to Ocean
New crust formed and pushed up - Mid Oceanic Ridges Ex. Mid-Atlantic Ridge Ocean Ridges

8 Divergent- Continent to Continent
Continent spreads, ocean basin may form Paleontologist noticed that fossils were on different continents Arthur Holmes – First proposed that thermal convection in the mantle causes continental drift Ex. Red Sea

9 Convergent – Ocean to Ocean
Older slips below newer Subducted plate melts Volcanic islands formed Ex. Aleutian islands, Japan

10 Convergent – Ocean to Continent
Ocean plate goes below continent Subduction Subducted plate partially melts Trenches – the deepest parts of the ocean. Volcanic mountains Ex. Western South America

11 Aleutian Islands Islands of Japan

12 Convergent – Continent to Continent
Same densities, no subduction Compression, folding, uplifting Ex. Himalayas, Alps

13 Another type of plate movement…
Transform faulting: Plates move past each other San Andreas Fault

14 How do you think scientists identified the plate boundaries?
What is the “Ring of Fire?”

15 Crustal Plates “Connect the dots” – volcanoes and earthquakes
8 major plates

16 Pangea Theory 1912 – Alfred Wegener
Idea that continents were once part of one large land mass – theory of continental drift How did he know? Continents’ shapes fit together like a puzzle Rocks and fossils found on different continents matched

17 Early 1960s Scientific evidence proves continental drift, plate tectonics, and Pangea theory

18 Ocean Features Picture 2


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