Neugrund crater
| Neugrund crater | |
|---|---|
 Boulder of gneiss breccia on Osmussaar, Estonia, possibly thrown there by the Neugrund impact | |
| Impact crater/structure | |
| Confidence | Confirmed |
| Diameter | 8 km (5.0 mi) |
| Age | ~535 Ma Cambrian |
| Exposed | No |
| Drilled | - |
| Location | |
| Location | Baltic Sea |
| Coordinates | 59°20′N 23°40′E / 59.333°N 23.667°E |
| State | Estonia |
| District | Lääne County |
  Location of the crater in Estonia | |
Neugrund is a
Ma, with later research revealing a possible Cambrian origin (around 535 Ma). The crater is at the bottom of the sea and is not exposed at the surface. Boulders of gneissic breccia found on the coast of Osmussaar, a nearby island, are believed to have been thrown there by the explosion.[1]
It has been proposed that the Neugrund crater was created during the Ordovician meteor event when a hypothetical large asteroid transferred directly into a resonant orbit with Jupiter, which shifted its orbit to intercept Earth.[2][3][4]
This attractive theory may need to be changed as more recent study puts the age of the impact in the Cambrian.[5]
See also
References
- ^ "Neugrund". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2017-10-14.
- S2CID 4393398.
- ^ H. Haack et al. Meteorite, asteroidal, and theoretical constraints on the 500-Ma disruption of the L chondrite parent body, Icarus, Vol. 119, p. 182 (1996).
- ^ Korochantseva et al. "L-chondrite asteroid breakup tied to Ordovician meteorite shower by multiple isochron 40Ar-39Ar dating" Meteoritics & Planetary Science 42, 1, pp. 3-150, Jan. 2007.[dead link]
- ^ S. SUUROJA1, K. SUUROJA & T. FLODÉN (2013). A comparative analysis of two Early Palaeozoic marine impact structures in Estonia, Baltic Sea: Neugrund and Kärdla Bulletin of the Geological Society of Finland, Vol. 85, 2013, pp 83–101.
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| Confirmed≥20 km diameter |
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