Ries - Hypervelocity Impact Crater
Alternate Names | Nördlinger Ries |
Local Language | |
Coordinates |
48° 52' 37" N; 10° 33' 21" E Notes
|
Country | Germany |
Region | Bavaria |
Date Confirmed | 1961 Notes
|
Buried? |
No Notes
|
Drilled? |
Yes
Notes
|
Target Type |
Mixed
Notes
|
Sub-Type | Carbonate, Claystone, Gneiss, Sandstone, Shale |
Apparent Crater Diameter (km) | 24 km |
Age (Ma) | 14.808 ± 0.038 Notes :
Method :
|
Impactor Type |
Ordinary chondrite or achondrite
Notes
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Advanced Data Fields
Notes
- Largely preserved, with only partial erosion of the ejecta blanket (Hörz et al., 1983).
- The outer rim is 24 km in diameter (Engelhardt, 1997). Some earlier dimensions were 26 km (Hörz et al., 1983) and 23 km (Pohl et al., 1977).
- Consists of a multi-ring depression; a poorly developed central uplift is surrounded by an inner ring filled with suevite and lake deposits and an outer ring of deformed sediments, Bunte breccia, and ejecta megablocks (Hörz et al., 1983). The centre of the structure comprises a flat-floored central basin (depth ~ 0.6–0.7 km) due to uplifted crystalline basement bordered by an inner ring of uplifted basement and sedimentary megablocks (radius 6 km) (Pohl et al., 1977).
- Authigenic breccia contains anomalously high concentrations of Fe, Cr, Ni, and Co; may be a chondrite or a stony aubrite meteorite (Morgan et al., 1979).
- Reidite found in granite clasts in suevite (Erickson et al. 2017) Impact diamonds (Rost et al., 1978) (Hough et al., 1995). Maskelynite (Horz and Banholzer, 1980)."
- Shatter cones are very rare. Best in granite block in breccia (Dressler et al., 1969). Shatter cones clasts found in ejectas (Dietz, 1963).
- PDF in quartz grains and feldspars (Engelhardt and Stoffler, 1968) (Engelhardt and Graup, 1977) (Horz and Banholzer, 1980).
- (Shoemaker and Chao, 1961)
- (Stoffler, 1971)
- Crater-fill: - MB. Melt-poor and melt-rich breccias present (referred to as crater suevites). Table 2 in (Osinski et al., 2016). Melt content decreases downward (Stoffler, 1977). Proximal ejecta: - LB corresponds to the "Bunte Breccia" and is a glass-free polymict breccia with sedimentary clasts (Horz, 1982) (Horz et al., 1983). - LB is also as polymict breccias with mainly crystallline clasts, as irregular bodies of 10s of meters overlying the Bunte Breccia (Pohl et al., 1977) (Engelhardt, 1990). - Melt rocks have traditionally been referred to as surficial suevite (Horz, 1965) (Bringemeier, 1994), however, it was shown that the groundmass of some of these "suevites" is not clastic (Osinski et al., 2004). They overlie Bunte Breccia . Dyke suevites occur in the parautochthonous crater basement (Stoffler et al., 2013). Tektites (referred to as moldavites) up to distances of 260-400 km to the east and northeast (Barnes, 1964) (Horz, 1982) (Engelhardt et al., 1987) (Osinski et al., 2004). (Grieve and Cintala, 1992)
References
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(1995) New shocked calcite and iron grains from Nördlingen Ries impact crater, Meteoritics & Planetary Science 30(5), Derek W G Sears (ed.), p. 550-551, Meteoritical Society, Fayetteville, AR, url
(1995) Suevite breccia from the Ries crater, Germany: Origin, cooling history and devitrification of impact glasses, Meteoritics 30(3), p. 279-293, url, doi:10.1111/j.1945-5100.1995.tb01126.x
(1996) Trace elements in quartz grains from the Ries impact crater and lechatelierites from southern Bohemian moldavites, Chemie der Erde 56(4), p. 487-492, Gustav Fischer Verlag, Jena, url
(1996) Impact diamonds in glass from Otting quarry, Ries crater, Germany, Meteoritics & Planetary Science 31, Suppl., Derek W G Sears (ed.), p. 5, Meteoritical Society, Fayetteville, AR, url
(1997) Suevite breccia of the Ries impact crater, Germany: Petrography, chemistry and shock metamorphism of crystalline rock, Meteoritics & Planetary Science 32(4), p. 545-554, url, doi:10.1111/j.1945-5100.1997.tb01299.x
(1998) Impact diamonds in glass bombs from suevite of the Ries crater, Germany: new observations, Meteoritics & Planetary Science 33(4, Suppl.), p. 1, Meteoritical Society, Fayetteville, AR, url
(1998) Carbon chemistry of suevites and target rocks at the Ries crater, Germany, Meteoritics & Planetary Science 33(4, Suppl.), p. 1, Meteoritical Society, Fayetteville, AR, url
(1998) Impact diamonds from suevites of Ries Crater, Germany: new data, Mineralogicheskiy Zhurnal 20(3), p. 3-12, Akademiya Nauk Ukrainy, Kiev, url
(1998) A comparative study of impact diamonds from the Popigai, Ries, Sudbury, and Lappajarvi craters, Meteoritics & Planetary Science 33(4, Suppl.), p. A90-A91, Meteoritical Society, Fayetteville, AR, url
(1999) Distribution of impact diamonds in the Ries crater, Germany, Meteoritics & Planetary Science 34(4, Suppl.), p. 102, Meteoritical Society, Fayetteville, AR, url
(1999) Carbonate-silicate liquid immiscibility upon impact melting: Ries crater, Germany, Meteoritics and Planetary Science 34(3), p. 425-438, DEPT CHEMISTRY/BIOCHEMISTRY, UNIV ARKANSAS, FAYETTEVILLE, AR 72701 USA: METEORITICAL SOC
(1999) In situ discovery of shock-induced graphite-diamond phase transformations in polished thin sections of shocked gneisses from the Ries crater, Germany, Meteoritics & Planetary Science 34(4, Suppl.), p. 125-126, Meteoritical Society, Fayetteville, AR, url
(1999) A new natural dense silicon dioxide glass in shocked garnet gneisses from the Ries crater, Germany, Meteoritics & Planetary Science 34(4, Suppl.), p. 112, Meteoritical Society, Fayetteville, AR, url
(2000) Impact glasses from the suevte of the Nördlinger Ries, Earth and Planetary Science Letters 17(July 1972), p. 275-293
(2000) Raman microspectrometry of impact diamonds from the Ries crater, Germany, Meteoritics and Planetary Science 35(S), p. A95, DEPT CHEMISTRY/BIOCHEMISTRY, UNIV ARKANSAS, FAYETTEVILLE, AR 72701 USA: METEORITICAL SOC, url
(2001) Hydrocode modeling of the Ries impact event, Lunar and Planetary Science XXXII, p. 14-15
(2001) An ultradense polymorph of rutile with seven-coordinated titanium from the Ries crater, Science (New York, N.Y.) 293(5534), p. 1467-1470, url, doi:10.1126/science.1062342
(2001) A natural shock-induced dense polymorph of rutile with α-PbO2 structure in the suevite from the Ries crater in Germany, Earth and Planetary Science Letters 192(4), p. 485-495, url, doi:10.1016/S0012-821X(01)00480-0
(2001) Ries crater, Germany: Geology and numerical modeling of impact cratering, Meteoritics & Planetary Science 36(9, Suppl.), p. 199, Meteoritical Society, Fayetteville, AR, url
(2001) Organic matter from the Bunte breccia of the Ries crater, southern Germany: Investigating possible thermal effects of the impact, Planetary and Space Science 49(8), p. 845-851, url, doi:10.1016/S0032-0633(01)00034-4
(2001) Raman microspectrometry on experimentally shocked calcite and naturally shocked limestones from the Ries crater, Meteoritics & Planetary Science 36(9, Suppl.), p. 79-80, Meteoritical Society, Fayetteville, AR, pdf
(2001) Stable isotope study of carbonates from the Ries meteorite impact crater - evidence for impact-induced carbonate decomposition, Lunar and Planetary Science Conference 32, p. 1572 pdf, pdf
(2001) In situ finding of the fabric settings of shock-induced quartz/coesite phase transition in crystalline clasts in suevite of the Ries crater, Germany, Meteoritics & Planetary Science 36(9, Suppl.), p. 69-70, Meteoritical Society, Fayetteville, AR, pdf
(2001) New SEM-CL data on the Popigai, Ries and Lappajarvi impact diamonds, Meteoritics & Planetary Science 36(9, Suppl.), p. 115-116, Meteoritical Society, Fayetteville, AR, url
(2001) In situ discovery of shock-induced graphite-diamond phase transition in gneisses from the Ries crater, Germany, American Mineralogist 86(5-6), p. 611-621, url
(2001) Geochemical evidence for the formation of a large miocene “travertine” mound at a sublacustrine spring in a soda lake (Wallerstein castle rock, Nördlinger Ries, Germany), Facies 45(1), p. 211-230, url, doi:10.1007