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references from: www.nationalgeographic.net  and links off Mrs. Sedmak's reference website. 

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references from: www.nationalgeographic.net  and links off Mrs. Sedmak's reference website. 

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Madeline Ramsey, Lily Tatara and Sarah Jones.   period 7 

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Madeline Ramsey, Lily Tatara and Sarah Jones.   period 7 

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Similar rock composition has been found between all of these mountains. Though the rocks in these mountains are not exactly the same today because over time rocks change under extreme heat and pressure.  This heat and pressure can also cause Igneous rock inside the mountain to melt into a liquid to thick and sticky to erupt, but gives off enough bouyancy to make the mountain taller.
Britanica.com

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When the continents collided during the time Pangaea was formed, a convergent boundary occurred.  This is when two crustal plates with the same density of 2.7 g/cc(so Subduction does not occur), collided together to create a mountain.
thisoldearth.net

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Continental Drift is the gradual moving of continents. Convection currents cause Continental Drift.

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4. Why is this good evidence of Continental drift?

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4. Why is this good evidence of Continental drift?

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It exemplifies that these land masses must have been connected at one point, based on how all mountain ranges match  up, and how the rock found in these mountains are the same.

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A group of mountains were once one long vertical mountain range in western of Pangaea. Today these mountains are separated across the world in North America (Appellations mountains), South America(Brazilian Highlands and Gujana Highlands), Africa(Atlas mountains), and Western Antarctica (Transantarctic mountains).
http://www.ucmp.berkeley.edu/geology/techist.html

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1.Which Mountain Range might have been connected at one point?

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1.Which Mountain Range might have been connected at one point?

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3. How would the land masses look if they were put back together?

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3. How would the land masses look if they were put back together?

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The Appalachian mountains would stretch from the east coast of America, to the east coast of South America, becoming the Andes The South west of Africa, through Antarctica and Australia.