A quick look at the super-continent!

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A quick look at the super-continent!
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Presentation transcript:

A quick look at the super-continent! What is Pangaea? A quick look at the super-continent!

What do YOU know?? (Students, tell me now!) 

Set Up Your Note Sheet: What is Pangaea? Who? What? Where? Why?

Pangaea Alfred Wegener (1880-1930) first proposed the theory of Continental Drift, which states that the Earth's continents float on a more dense layer of rock He hypothesized that there was an original, gigantic super-continent 300 million years ago, which he named Pangaea (greek for “all earth/land”).

What are the names of the land pieces? Eur-Asia North America South America Africa India Australia Antarctica

How do we KNOW Pangaea existed? (Anyone?)

Scientific Evidence! Fossil Evidence - There are similar fossil remains found on more than one continent. Climate evidence – organisms that couldn’t live in certain present-day areas have had their fossils found there! Land evidence – coal mines, mountain ranges, etc.

More Scientific Evidence Land Features Mountain Ranges line up on different continents. European coal fields match up with North American coal fields. Climate Scratches in rocks show that glaciers covered Africa….so it must have been closer to the poles. Cold Arctic Islands have fossils from warm climate animals…so it must have been near the equator.

Is Continental Drift REAL? Pangaea IS, but Continental Drift is NOT! Scientists do not accept Wegener’s Theory (continents do NOT float on more dense rock!). BUT, the theory of PLATE TECTONICS is real and accepted by scientists!

So, what is the difference between Continental Drift & Plate Tectonics? Lets read the article while taking Cornell Notes! Then we can look at the interactive website! Let’s finish by completing the Venn Diagram of Continental Drift vs. Plate Tectonics!

Theory of Continental Drift vs Theory of Plate Tectonics

What happened to Pangaea? Over time the plates began to drift apart. This was caused by convection currents in the asthenosphere.