The Chesapeake Bay impact crater is a buried impact crater, located beneath the mouth of Chesapeake Bay, United States. It was formed by a bolide that struck the eastern shore of North America about 35.5 ± 0.3 million years ago, in the late Eocene epoch. It is one of the best-preserved "wet-target" impact craters in the world.[3]
| Chesapeake Bay impact crater | |
|---|---|
 Location of impact site in relation to North America | |
| Impact crater/structure | |
| Confidence | Confirmed |
| Diameter | 53 miles (85 km) |
| Depth | 0.81 miles (1.3 km) |
| Impactor diameter | 1.9 miles (3 km) |
| Age | 35.5 ± 0.3 million |
| Exposed | No |
| Drilled | Yes |
| Bolide type | L chondrite[1] |
| Location | |
| Location | Chesapeake Bay |
| Coordinates | 37°17′N 76°1′W / 37.283°N 76.017°W[2] |
| Country | United States |
| State | Virginia |
| Municipality | Cape Charles |
  Impact location Location of impact site in Virginia | |
| Access | U.S. Route 13 to S.R. 184 |
Continued slumping of sediments over the rubble of the crater has helped shape the Chesapeake Bay.
Formation and aftermath
editDuring the warm late Eocene, sea levels were high, and the tidewater region of Virginia lay in the coastal shallows. The shore of eastern North America, about where Richmond, Virginia is today, was covered with thick tropical rainforest, and the waters of the gently sloping continental shelf were rich with marine life that was depositing dense layers of lime from their microscopic shells.[citation needed]
The bolide made impact at a speed of approximately 17.8 kilometers per second (11.1 miles per second),[4] punching a deep hole through the sediments and into the granite continental basement rock. The bolide itself was completely vaporized, with the basement rock being fractured to depths of 8 km (5 mi), and a peak ring being raised around it. The deep crater, 38 km (24 mi) across, is surrounded by a flat-floored terrace-like ring trough with an outer edge of collapsed blocks forming ring faults.[citation needed]
The entire circular crater is about 85 km (53 mi) in diameter and 1.3 km (1,300 m; 0.81 mi; 4,300 ft) deep, an area twice the size of Rhode Island, and nearly as deep as the Grand Canyon. However, numerical modeling techniques by Collins et al. indicate that the post-impact diameter was likely to have been around 40 km (25 mi), rather than the observed 85 km (53 mi).[4]
The surrounding region suffered massive devastation. USGS scientist David Powars, one of the impact crater's discoverers, described the immediate aftermath: "Within minutes, millions of tons of water, sediment, and shattered rock were cast high into the atmosphere for hundreds of miles along the East Coast." An enormous megatsunami engulfed the land and possibly even reached the Blue Ridge Mountains.[5] The sedimentary walls of the crater progressively slumped in, widened the crater, and formed a layer of huge blocks on the floor of the ring-like trough. The slump blocks were then covered with the rubble or breccia. The entire bolide event, from initial impact to the termination of breccia deposition, lasted only a few hours or days. In the perspective of geological time, the 1.2 km (0.75 mi) breccia was an instantaneous deposit. The crater was then buried by additional sedimentary beds that have accumulated during the 35 million years following the impact.[citation needed]
The impact has been identified as the source of the North American tektite field, namely the Georgiaite and Bediasite fields.[6]
Discovery
edit
Until 1983 there was no evidence of a large impact crater buried beneath the lower part of the Chesapeake Bay and its surrounding peninsulas. The first hint was an 8-inch-thick (20 cm) layer of ejecta found in a drilling core taken off Atlantic City, New Jersey, about 170 miles (274 km) to the north. The layer contained the fused glass beads called tektites and shocked quartz grains that are unmistakable signs of a bolide impact.
In 1993, data from oil exploration revealed the extent of the crater.[7]
Effects on local rivers
editThe continual slumping of the rubble within the crater has affected the flow of the rivers and shaped the Chesapeake Bay. The impact crater created a long-lasting topographic depression which helped predetermine the course of local rivers and the eventual location of the Chesapeake Bay. Most important for present-day inhabitants of the area, the impact disrupted aquifers. The present freshwater aquifers lie above a deep salty brine, remnants of 100- to 145-million-year-old Early Cretaceous North Atlantic seawater, making the entire lower Chesapeake Bay area susceptible to groundwater contamination.[8]
See also
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- Toms Canyon structure probable impact crater 322 km (200 mi) to the northeast.
- Popigai impact structure of similar age
- Grande Coupure
- Carolina bays
References
edit- ^ Schmitz, Birger; Boschi, Samuele; Cronholm, Anders; Heck, Philipp R.; Monechi, Simonetta; Montanari, Alessandro; Terfelt, Fredrik (2015). "Fragments of Late Eocene Earth-impacting asteroids linked to disturbance of asteroid belt" (PDF). Earth and Planetary Science Letters. 425: 77–83. Bibcode:2015E&PSL.425...77S. doi:10.1016/j.epsl.2015.05.041. ISSN 0012-821X.
- ^ "Chesapeake Bay". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 15 September 2019.
- ^ "Chesapeake Bay impact structure: Morphology, crater fill, and relevance for impact structures on Mars". USGS. United States Geological Survey. 2006. Retrieved 5 March 2019.
- ^ a b Collins, Gareth S.; Wünnemann, Kai (2005). "How big was the Chesapeake Bay impact? Insight from numerical modeling". Geology. 33 (12): 925–928. Bibcode:2005Geo....33..925C. doi:10.1130/G21854.1.
- ^ Dell'Amore, Christine (2013-11-21). ""Mind-Blowing" Discovery: Oldest Body of Seawater Found in Giant Crater". National Geographic. National Geographic Society. Archived from the original on 2013-11-21. Retrieved 2015-07-01.
- ^ Koeberl, C.; Poag, C. W.; Reimold, W. U.; Brandt, D. (1996-03-01). "Impact Origin of the Chesapeake Bay Structure and the Source of the North American Tektites". Science. 271 (5253): 1263–1266. Bibcode:1996Sci...271.1263K. doi:10.1126/science.271.5253.1263. S2CID 128672140.
- ^ Poag, C. Wylie; Koeberl, Christian; Reimold, Wolf Uwe (1 January 2004). The Chesapeake Bay crater: geology and geophysics of a Late Eocene submarine impact structure. Impact Studies. Berlin, Germany: Springer-Verlag. pp. 69–93. doi:10.1007/978-3-642-18900-5. ISBN 978-3-642-62347-9. Archived from the original on 9 October 2016. Retrieved 7 October 2016.
- ^ Sanford, Ward E.; Doughten, Michael W.; Coplen, Tyler B.; Hunt, Andrew G.; Bullen, Thomas D. (13 November 2013). "Evidence for high salinity of Early Cretaceous sea water from the Chesapeake Bay crater". Nature. 503 (7475): 252–256. Bibcode:2013Natur.503..252S. doi:10.1038/nature12714. PMID 24226889. S2CID 1735841.
Bibliography
edit- Poag, C. Wiley. Chesapeake Invader: Discovering America's Giant Meteorite Crater. Princeton, NJ: Princeton University Press, 1999. ISBN 0-691-00919-8
- Post-impact Effects of the Eocene Chesapeake Bay Impact, Lower York-James Peninsula, Virginia, 31st Annual Meeting, Virginia Geological Field Conference, Williamsburg, Virginia, Oct. 19 and 20, 2001, G.H. Johnson et al. (fieldtrip guidebook)
External links
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- 'Isostatic Rebound and its effects on the Chesapeake Bay' Archived 2014-02-05 at the Wayback Machine
- A brief introduction to the Chesapeake Bay Impact Crater.
- USGS, 'Investigating the Chesapeake Bay Impact Crater.'
- USGS, 'The Chesapeake meteorite: message from the past.'
- 'The Chesapeake Bay bolide: modern consequences of an ancient cataclysm.'
- Earth Impact Database
- Satellite image of the region (from Google Maps)
- Chesapeake Bay Impact Structure Deep Drilling Project
