The Chesapeake Bay Crater
35 million years ago, the Earth was much warmer than today due to higher abundances of carbon dioxide in the atmosphere. There were either small or no ice caps at the poles, leading to high sea levels that flooded the edges of the continents that are exposed today. This was the situation when a large rock from space came hurtling in, hitting the submerged continental shelf off the coast of what is today the state of Virginia. The object was between 3 and 5 kilometers in diameter. The impact of this rock caused a massive explosion and formed a crater 85 kilometers in diameter. It shattered the existing rocks, creating a debris pile known as a breccia that has since been buried by sediment shed off the continent.
The Chesapeake Bay Impact Structure still controls features of the shoreline today. It’s no coincidence that it sits right at the mouth of the modern day Chesapeake Bay.
The presence of this crater has caused the land above to subside, or sink, more than the surrounding land for 35 million years. That subsidence has caused rivers to flow to this location, making it a central point for erosion and downcutting.
15,000 years ago, sea level was much lower due to the presence of huge ice caps, so rivers flowed through the Chesapeake Bay impact structure out to sea, cutting wide canyons. When sea level rose, it flooded those canyons, creating shoreline features called estuaries around the world. The Chesapeake Bay is an estuary created by the flooding of river valleys that were fixed in location by an asteroid impact 35 million years ago. The East Coast of the United States today is shaped, in part, by a rock from space that landed tens of millions of years ago.
-JBB