Des Plaines crater
Encyclopedia
The Des Plaines crater or Des Plaines disturbance is recognized as an impact crater
in Illinois
, United States. It is located beneath the eastern part of the city of Des Plaines, which is a suburb of Chicago
.
It is 5.5 miles (8.9 km) in diameter and the age is estimated to be less than 280 million years (Permian
or younger). The crater is buried beneath 75 to 200 feet (23–60 m) of glacial till and can only be seen as a series of faults and deformation in well logs and seismic surveys. Faulting in the structure has produced as much as 600 feet (182.9 m) of vertical displacement. Subsurface strata
of Cambrian
through Pennsylvanian
age has been faulted and tilted by the event. The anomalous area was first noted by water well drillers in 1893 who noted an absence of water in a 1600 foot deep well. Prior to being recognized as an impact structure the feature was referred to as a cryptoexplosion structure or cryptovolcanic structure as were several others in the midwestern U. S. The upfaulted central portion and the presence of shatter cone
structures support the impact origin.
Impact crater
In the broadest sense, the term impact crater can be applied to any depression, natural or manmade, resulting from the high velocity impact of a projectile with a larger body...
in Illinois
Illinois
Illinois is the fifth-most populous state of the United States of America, and is often noted for being a microcosm of the entire country. With Chicago in the northeast, small industrial cities and great agricultural productivity in central and northern Illinois, and natural resources like coal,...
, United States. It is located beneath the eastern part of the city of Des Plaines, which is a suburb of Chicago
Chicago
Chicago is the largest city in the US state of Illinois. With nearly 2.7 million residents, it is the most populous city in the Midwestern United States and the third most populous in the US, after New York City and Los Angeles...
.
It is 5.5 miles (8.9 km) in diameter and the age is estimated to be less than 280 million years (Permian
Permian
The PermianThe term "Permian" was introduced into geology in 1841 by Sir Sir R. I. Murchison, president of the Geological Society of London, who identified typical strata in extensive Russian explorations undertaken with Edouard de Verneuil; Murchison asserted in 1841 that he named his "Permian...
or younger). The crater is buried beneath 75 to 200 feet (23–60 m) of glacial till and can only be seen as a series of faults and deformation in well logs and seismic surveys. Faulting in the structure has produced as much as 600 feet (182.9 m) of vertical displacement. Subsurface strata
Stratum
In geology and related fields, a stratum is a layer of sedimentary rock or soil with internally consistent characteristics that distinguish it from other layers...
of Cambrian
Cambrian
The Cambrian is the first geological period of the Paleozoic Era, lasting from Mya ; it is succeeded by the Ordovician. Its subdivisions, and indeed its base, are somewhat in flux. The period was established by Adam Sedgwick, who named it after Cambria, the Latin name for Wales, where Britain's...
through Pennsylvanian
Pennsylvanian
The Pennsylvanian is, in the ICS geologic timescale, the younger of two subperiods of the Carboniferous Period. It lasted from roughly . As with most other geochronologic units, the rock beds that define the Pennsylvanian are well identified, but the exact date of the start and end are uncertain...
age has been faulted and tilted by the event. The anomalous area was first noted by water well drillers in 1893 who noted an absence of water in a 1600 foot deep well. Prior to being recognized as an impact structure the feature was referred to as a cryptoexplosion structure or cryptovolcanic structure as were several others in the midwestern U. S. The upfaulted central portion and the presence of shatter cone
Shatter cone
Shatter cones are rare geological features that are only known to form in the bedrock beneath meteorite impact craters or underground nuclear explosions...
structures support the impact origin.