Tectonic Events along East Coast of what is now North America

Event When Details
Grenvillian Orogeny 1.1 billion years ago Magmatic arc
Collision of Laurentia with Amazonia
Supercontinent of Rodinia created
High plateau like Tibet created
Area affected extends to Mexico
As bedrock eroded, plateau rose gradually due to isostasy
In Adirondacks and Hudson Highlands, Grenville rocks at surface
Grenville rocks below surface in much of eastern North America
Formation of Iapetus Ocean 560 million years ago Rifting
Taconian Orogeny  450 million years ago Subduction zone forms in Iapetus Ocean
Hartland volcanic island arc forms behind subduction zone
The oceanic crust between the island arc and Laurentia subducts until the island arc collides with Laurentia
Acadian Orogeny  380 million years ago Avalonia splits from Gondwana and becomes attached to Baltica
Baltica included the land areas now bordering the Baltic Sea
The collision of Baltica with Laurentia in the Silurian is the Caledonian Orogeny
Caledonian Orogeny progresses south and becomes the Acadian Orogeny 
Alleghanian Orogeny  300 million years ago Rheic Ocean crust between Avalonia and Gondwana  is subducted
The collision of Gondwana and Laurentia is along a transform margin
Gondwana rotates clockwise causing more intense uplift in southern Appalachians
Formation of Atlantic Ocean 200 million years ago Rifting initiates as a series of triple junctions
In each case, one extension of the three halts, while the others continue
Failed rifts: Newark Basin, Hartford Basin
Atlantic Ocean continues to widen