USGS Live

USGS Live

@USGSLive

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Reston, VA · http://usgs.gov

Tweets

  1. Join us March 6th for our lecture on Geomagnetism with Dr. Jeffrey Love. See you then!

  2. DP: So even though it happened 35 million years ago, the Impact Crater is still important to us today

  3. DP: In addition, the continued activity of the crater is part of why there's seismic activity in the area

  4. DP: The subsiding of the crater also helps explain why there's more sea level rise in the than other places

  5. DP: Only after it clears the crater does the water then turn and flow out to the Atlantic Ocean

  6. DP: If you look at the direction of the flow of water in the , it flows directly to the crater

  7. DP: Because the crater is subsiding, it lowers the local area, drawing river flows to it

  8. DP: As the crater continues to subside, it affects us in that it helped form the as it is today

  9. DP: Now, the crater has not been still throughout time. It has slowly been subsiding, or sinking

  10. DP: Tektites are fuzed minerals created when silicon is shocked, such as from an impact

  11. DP: Another long-standing mystery we solved was why tektites were found all over the eastern U.S. from Houston to NYC to Miami

  12. DP: People kept finding saltwater in wells where there shouldn't be any. They thought they must have been over-pumping

  13. DP: The crater also helped us explain a long-standing puzzle--the inland saltwater intrusion of Central Virginia

  14. DP: The smoking gun was the shocked minerals we found in the cores. There's no other way for those minerals to form except impacts

  15. DP: We worked with oil companies to use some of their overburden seismic data, which helped prove what the cores showed us

  16. DP: After obtaining more cores and exhausting other ideas, we hypothesized that it might be a crater

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