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The North American craton (also known as '''Laurentia'''), like all Craton land, was created as Continent s move about the surface of the Earth , bumping into other continents and drifting away.

Many times in its past, Laurentia has been a separate Continent as it is now in the form of North America. During other times in its past, Laurentia has been part of a Supercontinent . It is named after the Laurentian Shield .

This process takes millions of years to happen, but the results can be seen today in the rocks of the continents.

The middle of most continents have not been crunched or squished up the way the edges have been. That is because the middle of the continents are made of very strong old rock. This part of the continent is called the stable craton. Indiana is located near the middle of the North America n craton.


INTERIOR PLATFORM

While much of the stable craton is exposed at the surface north of Indiana as the Canadian Shield , the middle of the craton, located in the United States , is covered with sedimentary rocks of the Interior Platform . The sequence of rocks varies from approximately 3,500 in excess of 20,000 feet in thickness. The Cratonic Rock s are Metamorphic and Igneous while the overlying Sedimentary Rock s are composed mostly of Limestone s, Sandstone s, and Shale s. These sedimentary rocks were deposited from 650 to 290 million years ago.


TECTONIC SETTING

The metamorphic and igneous rocks of the " Basement Complex " were created 1.5 to 1.0 billion years ago in a tectonically active setting. It was a setting of great pressure and temperature. The younger sedimentary rocks that were deposited on top of this basement complex were formed in a setting of quiet marine and river waters. Much of this time the craton was covered by a large shallow sea, a so-called " Epicratonic Sea " (meaning literally "on" the craton). Sometimes land masses or Mountain chains rose up on the distant edges of the craton and then eroded down, shedding their sand across the landscape.


GEOLOGICAL HISTORY OF LAURENTIAN CRATON IN CHRONOLOGICAL ORDER


  • ~2.5 billion years ago, Arctica formed as an independent continent.

  • ~2.45 billion years ago, Arctica was part of the major supercontinent Kenorland .

  • ~2.1 billion years ago, when Kenorland shattered, the Arctican craton was part of the minor supercontinent Nena along with Baltica and Eastern Antarctica .

  • ~1.8 billion years ago, Laurentia was part of the major supercontinent Columbia .

  • ~1.5 billion years ago, Laurentia was an independent continent.

  • ~1.1 billion years ago, Laurentia was part of the major supercontinent Rodinia .

  • ~750 million years ago, Laurentia was part of the minor supercontinent Protolaurasia . Laurentia nearly rifted apart.

  • ~600 million years ago, Laurentia was part of the major supercontinent Pannotia .

  • ~ Cambrian , Laurentia was an independent continent.

  • ~ Ordovician , Laurentia was shrinking and Baltica got bigger.

  • ~ Devonian , Laurentia collided against Baltica, forming the minor supercontinent Euramerica .

  • ~ Permian , all major continents collide against each other for forming the major supercontinent Pangaea .

  • ~ and Gondwana . Laurentia was part of the minor supercontinent Laurasia.

  • ~ Cretaceous , Laurentia was an independent continent called North America.

  • ~ Neogene , Laurentia, in the form of North America, crashed into South America , forming the minor supercontinent America.

  • ~250 million years from now, all continents may crash together for forming the major supercontinent Pangaea Ultima . Laurentia will be part of Pangaea Ultima.



OTHER USE

"Laurentia" was also A Proposed Name for the country that united as Canada .


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