The Taconic orogeny was the result of a collision between Laurentia and

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The Taconic orogeny was a significant mountain-building event that occurred during the Late Ordovician period, primarily as a result of the collision between the continent of Laurentia and a series of island arcs. This process involved not just a single landmass but also included interactions with parts of Baltica and Gondwanaland, along with several island arcs or exotic terranes, leading to the formation of mountains along the eastern margin of what is now North America.

The Taconic Orogeny Was the Result of a Collision Between