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Earth’s History Presented by Valerie Harrish MGMS 7401

Geologic timeline harrish

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Page 1: Geologic timeline harrish

Earth’s HistoryPresented by Valerie Harrish

MGMS 7401

Page 2: Geologic timeline harrish

Precambrian Era:also known as the Ice Age

• The time period that defined Earth as an “Ice House”.

• The oldest known supercontinent existed on Earth at this time, called Rodinia.

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Paleozoic Era:the Cambrian Period

During this period, the land mass that covered much of the Earth’s surface was known as Gondwana.

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Paleozoic Era:the Ordovician Period

The major ocean of this period was the Panthalassic Ocean.

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Paleozoic Era:the Silurian Period

There is a lack of “white” or obvious ice caps on the map during this time period, perhaps suggesting that this was a warmer time than we even know now.

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Paleozoic Era:the Devonian Period

With the collision of continents, the Appalachian Mountain began to appear during this period.

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Paleozoic: Early Carboniferous & Late Carboniferous

Coal beds begin to forming during the early period. By the late period, we see ice caps beginning to take shape.

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Paleozoic Era: the Permian Period

As the era came to a close, the continents collided once again to form the supercontinent Pangea.

Earth is nearly unrecognizable compared to current day.

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Mesozoic Era:the Triassic Period

In this period, we really see a lot of migration and movement of animals across the supercontinent, Pangea.

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Mesozoic Era:the Jurassic Period

The Atlantic ocean is beginning to form and the continents are beginning to take shapes we know

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Mesozoic Era:the Cretaceous Period

The movement of tectonic plates caused the Rocky Mountains to form. For A subduction occurred with the pacific plate and North America.

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Cenozoic Era:the Eocene Period

About 50 million years ago the Himalayans to formed when the Indian plate collided with the Eurasia plate.

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Cenozoic Era:the Miocene Period

In this period, the Earth and its continents begin to take the shape and formations that we know and recognize now.

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Future World

The continually moving plates will eventually cause continents to collide again to form a Pangea Ultima in one large Pacific Ocean.

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REFERENCES:

Scotese, C. (2010). Paleomar project: Earth

history. Retrieved September 15, 2014 from

http://www.scotese.com/earth.htm