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- Q4636066 subject Q7810036.
- Q4636066 subject Q8343740.
- Q4636066 subject Q8581831.
- Q4636066 abstract "The 38th parallel structures, also known as the 38th parallel lineament, are a series of circular depressions or deformations stretching 700 km (435 mi) across southern Illinois and Missouri into eastern Kansas at a latitude of roughly 38 degrees north.Rampino and Volk (1996) postulated that these structures could be the remains of a serial meteorite strike in the late Mississippian or early Pennsylvanian periods. Difficulty in determining the age of many of the structures and doubts about the exogenic origins of several of them leave some geologists skeptical of this hypothesis. As of May 2009, only two of the structures, Decaturville and Crooked Creek, are listed as confirmed in the Earth Impact Database.There is evidence that at least some of them, such as Hicks Dome, are volcanic in origin. They are associated with faults and fractured rock, and are accompanied by igneous rocks and mineral deposits. Hicks Dome is a structural dome which has its central Devonian core displaced upward some 4,000 feet in relation to the surrounding strata. The dome has small associated igneous dikes around its flanks.Interest in the possibility of serial impacts on Earth was piqued by observations of comet Shoemaker–Levy 9 impacting on Jupiter in 1994. It is estimated, however, that the likelihood of such an event on Earth is vanishingly small because the Earth's weaker gravitational field is much less able than Jupiter's to pull a speeding object close enough to be torn apart by tidal forces. However, evidence of serial impacts on the Moon can be seen in several chains of craters.".
- Q4636066 thumbnail 38th_parallel_structures_loc.svg?width=300.
- Q4636066 wikiPageExternalLink RI-75(2003AMGguidebook).pdf.
- Q4636066 wikiPageExternalLink RampinoVolk.html.
- Q4636066 wikiPageWikiLink Q1031161.
- Q4636066 wikiPageWikiLink Q1069.
- Q4636066 wikiPageWikiLink Q1140978.
- Q4636066 wikiPageWikiLink Q1204.
- Q4636066 wikiPageWikiLink Q12758989.
- Q4636066 wikiPageWikiLink Q1558.
- Q4636066 wikiPageWikiLink Q1581.
- Q4636066 wikiPageWikiLink Q2.
- Q4636066 wikiPageWikiLink Q232086.
- Q4636066 wikiPageWikiLink Q3076.
- Q4636066 wikiPageWikiLink Q319.
- Q4636066 wikiPageWikiLink Q3236743.
- Q4636066 wikiPageWikiLink Q34027.
- Q4636066 wikiPageWikiLink Q373772.
- Q4636066 wikiPageWikiLink Q405.
- Q4636066 wikiPageWikiLink Q42045.
- Q4636066 wikiPageWikiLink Q463796.
- Q4636066 wikiPageWikiLink Q483102.
- Q4636066 wikiPageWikiLink Q486495.
- Q4636066 wikiPageWikiLink Q5248821.
- Q4636066 wikiPageWikiLink Q5327084.
- Q4636066 wikiPageWikiLink Q65955.
- Q4636066 wikiPageWikiLink Q662806.
- Q4636066 wikiPageWikiLink Q744718.
- Q4636066 wikiPageWikiLink Q7810036.
- Q4636066 wikiPageWikiLink Q7978333.
- Q4636066 wikiPageWikiLink Q8343740.
- Q4636066 wikiPageWikiLink Q8581831.
- Q4636066 point "37.5 -88.3".
- Q4636066 type SpatialThing.
- Q4636066 comment "The 38th parallel structures, also known as the 38th parallel lineament, are a series of circular depressions or deformations stretching 700 km (435 mi) across southern Illinois and Missouri into eastern Kansas at a latitude of roughly 38 degrees north.Rampino and Volk (1996) postulated that these structures could be the remains of a serial meteorite strike in the late Mississippian or early Pennsylvanian periods.".
- Q4636066 label "38th parallel structures".
- Q4636066 lat "37.5".
- Q4636066 long "-88.3".
- Q4636066 depiction 38th_parallel_structures_loc.svg.