Dab solver - Kentland crater

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The crater itself is a circular [[dome]], about {{convert|7.24|km|mi|abbr=on}} in diameter, deeply eroded and buried in [[glacier|glacial]] debris. Its age is estimated to be less than 97 million years ([[Cretaceous]] or younger). The Shakopee dolomite at the center of the structure is about 450 million years old ([[Ordovician]] period) and is uplifted about 2,000 feet higher than the level of the same rock in the surrounding area. The entire disturbed area is about {{convert|13|km|mi|abbr=on}} in diameter.

The estimated age is in dispute.  
* ‘’’97 MYA‘’’ Late [[Cretaceous]] Period of the [[Mesozoic]] Era ^ref
* ‘’’300 MYA‘’’= Bzhelian or Late [[Pennsylvanian]] Epoch([[Carboniferous]] Period) of the [[Paleozoic]] Era^ref

The crater's structure was studied in 1978. John Weber and his associates presented [[fission track dating]] of [[apatite]] from the crater.^ref [[Coesite]] and [[shatter cone]]s are found in the uplift near its center. The crater is exposed to the surface, resulting in erosion. It is currently being worked as a quarry.

==  Description  ==

The impact site is located {{convert|4|km|mi}} east of , [[Indiana]] in [[Newton County, Indiana|]].  The disturbance is {{convert|12.5|km|mi}} in diameter.  The bedrock has a thin layer of glacial till, with a maximum depth of {{convert|40|m|ft}} in the depression ring.  The bedrock around the impact structure is generally flat with a slight dip towards the southwest and the [[Illinois Basin]].  The upper layers are Lower [[Mississippian]] from the [[Carboniferous]] period and Upper [[Devonian]] are relatively flat throughout this area of Indiana with the exception of impact site.^ref

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{{More footnotes|date=March 2008}}
[[Image:Kentland IN rock deformation.jpg|thumb|px|right|Deformation involving bending and overturning is evident in the layered limestones exposed by quarrying at the Kentland crater.]]

The '''Kentland crater''', also known as the '''Kentland structure''' or the '''Kentland disturbed area''',  is an [[impact crater]] located near the town of [[Kentland, Indiana|Kentland]] in [[Newton County, Indiana]], United States.<ref>{{cite Earth Impact DB | name = Kentland| accessdate = 2009-08-17}}</ref>

It was discovered about 1880 when two farmers began to [[quarry]] crushed rock there. The presence of [[shatter cone]]s and deformed [[bedrock]] led geologists to conclude by the late 1960s that the Kentland structure is an [[impact crater]], rather than [[volcano|volcanic]] in origin. Deformation at the site is so great that vertical contacts between normally horizontal rock formations of different ages are common.

The crater itself is a circular [[dome]], about {{convert|7.24|km|mi|abbr=on}} in diameter, deeply eroded and buried in [[glacier|glacial]] debris. Its age is estimated to be less than 97 million years ([[Cretaceous]] or younger). The Shakopee dolomite at the center of the structure is about 450 million years old ([[Ordovician]] period) and is uplifted about 2,000 feet higher than the level of the same rock in the surrounding area. The entire disturbed area is about {{convert|13|km|mi|abbr=on}} in diameter.

The estimated age is in dispute.  
* ‘’’97 MYA‘’’ Late [[Cretaceous]] Period of the [[Mesozoic]] Era <ref>"Kentland". Earth Impact Database. University of New Brunswick. Retrieved 2009-08-17.</ref>
* ‘’’300 MYA‘’’= Bzhelian or Late [[Pennsylvanian]] Epoch([[Carboniferous]] Period) of the [[Paleozoic]] Era<ref name=Cochise>Cochise College web-page, December 18, 2012</ref>

The crater's structure was studied in 1978. John Weber and his associates presented [[fission track dating]] of [[apatite]] from the crater.<ref>[[Society for Sedimentary Geology]] (SEPM) Research Conference, "The Sedimentary Record of Meteor Impacts" (21–23 May 2003, [[Springfield, Missouri]])</ref> [[Coesite]] and [[shatter cone]]s are found in the uplift near its center. The crater is exposed to the surface, resulting in erosion. It is currently being worked as a quarry.

== Description ==
The impact site is located {{convert|4|km|mi}} east of <<link:0>>, [[Indiana]] in [[Newton County, Indiana|Newton County]].  The disturbance is {{convert|12.5|km|mi}} in diameter.  The bedrock has a thin layer of glacial till, with a maximum depth of {{convert|40|m|ft}} in the depression ring.  The bedrock around the impact structure is generally flat with a slight dip towards the southwest and the [[Illinois Basin]].  The upper layers are Lower [[Mississippian]] from the [[Carboniferous]] period and Upper [[Devonian]] are relatively flat throughout this area of Indiana with the exception of impact site.<ref name=LandySchmus>Landy, R.T. and W.R. Van Schmus; A structural study of the Kentland, Indiana Impact site; Dept of Geology, University of Kansas; Lawrence, Kansas’ 1978</ref>
The core of the site is [[Ordovician]] rocks in the Prairie Du Chien through Maquoketa Groups. Surrounding the core is [[Silurian]] rocks of Sexton Cr [[Dolomite]] and Kokomo [[Limestone]].  This uplifted core pierces the New Albany [[Shale]] of the [[Devonian]] age and the [[Mississippian]] age New Providence Shale and Rockford Limestone.<ref name= Bjørnerud>Bjørnerud, MG.; Superimposed deformation in seconds: breccias form the impact structure at Kentland, Indiana (USA); Geology Dept., Lawrence University, Appleton, WI; 2997</ref>  Prior to quarry operations, research estimates that there has been {{convert|300|m|ft}} of errosion since the initial event, followed by a shallow deposit of glacial till during the [[Wisconsian Glacial Period]]. The quarry operations have extracted the upper Ordovician carbonates of the Platteville and Galena (Prairie due Chien) groups along the northern edge of the since 1906.<ref name=LandySchmus/>

==Structure==
The Structure is a highly eroded [[complex crater]].  Since the original impact, the structure has eroded over {{convert|300|m|ft}}, eliminating the crater and other surface elements.<ref name=Cochise/> 
; Ring anticline
The ring surrounds the impact site, separating it from the surrounding  flat-lying regional bedrock.  The ring is about {{convert|6.2|km|mi}} in radius around the central disconformity.<ref name=LandySchmus/>
; Ring depression
The ring depression is the result of the displacement of materials at lower levels to fill the void created as the central uplift rose. Studies at other sites similar to the Kentland structure have found the depression to be the equivalent of the material that would have moved under the uplift as it occurred.<ref name=LandySchmus/>
; Central Uplift
A cross section of the uplift, beginning on the outer edge, moving towards the middle include:<ref name=LandySchmus/>

==See also==
{{Portal|Indiana}}
*[[List of impact craters on Earth]]

==References==
{{Reflist}}

==Additional sources==
*Cohen, A.J., Bunch, T.E., and Reid, 1961, Coesite discoveries establish cryptovolcanics as fossil meteorite craters: Science, v.134, p.&nbsp;1624-1625.
* Collet, J., 1883, Geological survey of Newton County: Ind. Dept Geol. and Nat. Hist., 12th Ann. Report, p.&nbsp;58-59.
*Dietz, R.S., 1947, Meteorite impact suggested by orientation of shatter cones at the Kentland, Indiana, disturbance: Science, v.105, n.2714, p.&nbsp;42-43.
*Dietz, R.S., 1960, Meteorite impact suggested by shatter cones in rock: Science, v.131, n.3416, p.&nbsp;1781-1784.
*Dietz, R.S., 1963, Cryptoexplosion structures-a discussion: Am. Jour. Sci., v.261, p.&nbsp;650-664. 
*Dietz, Robert S.; Shatter Cones in Cryptoexplosion Structures (Meteorite Impact?); The Journal of Geology; Vol. 67, No. 5 (Sep., 1959), pp.&nbsp;496–505
*Gutschick, R. C., Geology of the Kentland dome structurally complex anomaly, northwestern Indiana (Field Trip 5). Field trip in Midwestern Geology, Annual Meeting, Geological Society of America, Indianapolis, v. 1, pp.&nbsp;105–138. 1983.
*Gutschick, R. C., Geology of the Kentland structural anomaly, northwestern Indiana—update. Purdue University, Department of Geosciences, and Geological Society of America,North-central Section, Guidebook 4, 38 p.&nbsp;1982.
*Gutschick, R.C., 1976, Geology of the Kentland structural anomaly, northwestern Indiana: Guidebook for 1976, North-Central GSA Meeting, 59 p. 
*Gutschick, R. C., Geology of the Kentland impact structural anomaly. Meteoritical Society, 35th Annual Meeting, Guidebook for Field Trip. 1972.
*Gutschick, R. C., Geology of the Kentland impact structural anomaly, northwestern Indiana. Shaver, R.H. and Sunderman, J.A., eds., Field Guide for the National Association of Geology Teachers, East-central Section, 20 p.&nbsp;1971.
*Gutschick, R. C., The stratigraphy and structure of the Kentland impact anomaly, Indiana (abstract). The Geological Society of America, v. 2, pp.&nbsp;564–565. 1970.
*Gutschick, R. C., The Kentland structural anomaly, Indiana. Geology from Chicago to Cincinnati, Geological Society of America Guidebook for Field Trips, v. 2, pp.&nbsp;12–17. 1961.
* Laney, R.T., and W.R. Vanschmus, 1978. "A structural study of the Kentland, Indiana impact site" in ''Lunar and Planetary Science'' '''9''', pp 627–629.
* Mark J. Camp and Graham T. Richardson, ''Roadside Geology of Indiana'', (Mountain Press Publishing Co.: Missoula, Montana, 1999), pp.&nbsp;215–216.  ISBN 0-87842-396-6

==External links==
*[http://web.archive.org/web/20070927213258/http://www.somerikko.net/old/geo/imp/refer.htm#k Archived Bibliography for Kentland Crater]
*[http://adsabs.harvard.edu/abs/1993Metic..28..382K Abstract: Geochemical Study of Rocks from the Kentland, Indiana, Impact Structure]
*[http://adsabs.harvard.edu/abs/1978LPSC....9.2609L Abstract: Structural Study of the Kentland, Indiana, Impact Site]
*[http://www.springerlink.com/content/q432277548352468/ Abstract: John C. Weber et al., "The Kentland Impact Crater, Indiana (USA): An Apatite Fission-Track Age Determination Attempt", in Christian Koeberl and Herbert Henkel (eds.) ''Impact Tectonics'', Berlin and Heidelberg: Springer, 2005, pp. 447-466.] ISBN 978-3-540-24181-2
*[http://impactcraters.us/kentland_indiana United States Meteorite Impact Craters: Kentland Crater, Indiana]
*[http://www.wlfi.com/dpp/news/local/kentland-meteorite-impact-signicant-in-scientic-discovery Interview with Purdue University Professor Jay Melosh about Kentland Crater]
*[http://web.eps.utk.edu/~faculty/ifsg_files/2007_Kentland_trip.html Kentland Quarry photos]

{{Coord|40|45|N|87|24|W|type:landmark_region:US-IN|display=title}}

[[Category:Impact craters of the United States]]
[[Category:Cretaceous impact craters]]
[[Category:Geography of Newton County, Indiana]]
[[Category:Newton County, Indiana]]

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Dab solver - Kentland crater

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