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Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Plate Movements, Continents and Connecticut: A Guide to Big Ideas

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Page 1: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Page 2: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 3: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Why is Connecticut so Amazing?

• Connecticut shows evidence of various earth processes, such as continental collisions, rifting, and folding that have shaped its structure.

Page 4: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Once Upon A Time

• Some time over 1 billion years ago, there was an ancient land mass called “Proto- North America”

• Proto North America eventually became the North American continent.

• About 1 billion years ago, another continent collided with proto-North America.

Page 5: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

A Big CRUNCH• Sediments (rock pieces) were caught in

between and pushed up onto North America.

Page 6: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• The collision crumpled the crust, creating a tall mountain range that stretched from Canada to Mexico: the Grenville Mountains.

• These mountains are the earliest evidence of mountain building in our region, and

Page 7: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Where Did They Go?

•Over time, the Grenville Mountains eroded.

Page 8: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• Rocks remaining from that ancient mountain chain are the oldest rocks that we see exposed at the surface in the Northeast today.

Page 9: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Oh No…Not Again!

• Sometime about 470 million years ago, the ancient Iapetus Ocean began to close as the plate carrying Baltica (proto-Europe) approached the North American plate

Page 10: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• Baltica did not collide with North America until several million years later, but the convergence of the two plates created a whole new look for eastern North America.

Page 11: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• As the continents approached one another, the oceanic crust in the middle was forced under the Baltica plate.

• The friction and melting of the crust from the intense pressure of the colliding plates created a string of volcanic islands along the area where the plates converged (known as the subduction zone).

Page 12: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• Over millions of years, more and more land was added on during collisions. Mountains were built up on the east coast of North America.

Page 13: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 14: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

• More land continued to add on to North America over time

Page 15: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Chatfield Hollow: Gneiss Rocks Form

Page 16: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

It metamorphoses then uplifts

Page 17: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 18: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Pangaea Forms

• Africa collides with North America between 360 - 245 million years ago

• Pangaea forms a supercontinent!!!

Page 19: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

These collisions resulted in the formation of the supercontinent of Pangaea. Mountain chains form.

Page 20: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Pangaea begins to rift apart

Page 21: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Pangaea Rifts Apart

By around 200 million years ago, rifted apart and set the stage for the development of Africa, North America, and the Atlantic Ocean as we know them

Page 22: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 23: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Breaking Up is Hard to do…

• Pangaea breaks up!• Africa pulls away from North America• Rifts form and fill with sediment and lava

Page 24: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Hills and Valleys• After the

crunching and pulling of continents, Connecticut had north-south ridges and valleys.

Page 25: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

What happened to New England?

Page 26: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Volcanoes forced out great flows of lava through long cracks in the floor

of the Connecticut Valley.

Page 27: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

Tying it all together

Page 28: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 29: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 30: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 31: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 32: Plate Movements, Continents and Connecticut: A Guide to Big Ideas
Page 33: Plate Movements, Continents and Connecticut: A Guide to Big Ideas

The Big Question: What Changed the Surface of the Earth After This?