How Did Connecticut Form? A Geological History
By Erica Campbell
Our little state of Connecticut is rich in history. From its storied past of maritime adventure, to it importance during the American Revolution and even the Underground Railroad, all the way up to today, Connecticut has a story to tell. Of course, some stories of the history of Connecticut are more interesting than others. But, have you ever wondered about how Connecticut itself was formed? Quite possibly, this could be one of the most interesting stories of all.
Connecticut likely began to take shape about one billion years ago, with the collision of huge continental plates deep within the Earth. Between 450 and 500 million years ago, a shallow sea washed up over the land, depositing thick layers of sand, mud and seashells, eventually creating limestone. Amazingly, this would later create the so-called “marble belt.” The marble belt is an area stretching from the northwestern part of Connecticut, into Massachusetts and Vermont, rich in marble rock.
The continual upheaval of the continents would eventually form a super continent known as Pangaea. Near the center of this continent was our state of Connecticut. As time went on, around 200 million years ago, Pangaea began to break apart, as heat from deep within the earth caused the continent to stretch. Deep depressions in the crust, known as “rift basins” began to form. The Connecticut rift basin, known as the Hartford Basin, began to form. Within this basin were periods of volcanic activity, the remnants of which can still be seen today.
Eventually, the upheavals and volcanic activity, responsible for forming our river valleys, mountains and rock formations quieted down. This sense of quiet, however, would be followed by an Ice Age. The first Ice Age began about two million years ago, with the last retreat of ice being about 12,000 years or so ago. When the ice disappeared, it left behind huge moraines…creating what is now known as Long Island. A moraine is “an accumulation of boulders, stones, or other debris carried and deposited by a glacier.” (American Heritage Dictionary, pg. 541) Long Island Sound was created by water filling in the space between Connecticut and the new moraine. Originally, it was fresh water, as the Atlantic Ocean was miles away from Connecticut’s shoreline. However, as the ice continued to melt, the sea levels rose and salt water from the ocean eventually replaced the freshwater in Long Island Sound.
As time went on and the ice retreated all the way up to present day Canada, Connecticut’s landscape began look as it does today. Unique rocks can be found all over Connecticut. One can find rocks up to one billion years old, deep in Connecticut’s bedrock. One can also find metamorphic rocks, sedimentary rocks and igneous rocks from millions of years of continental upheaval and volcanic activity across our state. It was that continental upheaval which raised our mountains and created our rivers. Our beaches are leftovers to when our land was covered by ice. Specific examples of geographic places (and there are so many) around our state are: Kent Falls State Park (formed from metamorphic rock), the Hanging Hills in Meriden (remains of ancient lava flows) and the Connecticut River (a water filled rift basin). There are even places around the state where seemingly simple rock formations are actually the seam of where North America and Africa were once joined together.
Look at Connecticut and you will have witnessed the evidence of an incredible geographical story. The shapes, colors and formations of the land, rivers, mountains and rocks across our Connecticut, are evidence of the millions and millions of years it took to create the state in which we live.
Posted by John William Tuohy