Conococheague Formation facts for kids
Quick facts for kidsConococheague Formation
Stratigraphic range: Cambrian
Etched section of rock from the Conococheague Formation from Washington County, Maryland (dolomite is lighter than the limestone)
|Sub-units||Big Spring Station Member|
|Region||Appalachian Basin of eastern North America|
|Extent||Maryland, Pennsylvania, Virginia, West Virginia|
|Named for||Conococheague Creek|
|Named by||G. W. Stose, 1908|
The Conococheague Formation is a mapped Appalachian bedrock unit of Cambrian age, consisting primarily of limestone and dolomite. It occurs in central Maryland, southern and central Pennsylvania, the Valley and Ridge of Virginia and easternmost West Virginia.
The depositional environment of the Conococheague was most likely shallow marine to tidal on a carbonate platform.
Accessible outcrops occur along various roadcuts and waterways in the area, including roadcuts near mile marker 20 of I-70 near Hagerstown, Maryland. The bedding at this site is nearly vertical, with the strike nearly perpendicular to the highway, and thus one can easily walk up and down the sections.
The Conococheague also forms dramatic, 100-foot cliffs along the Potomac River upstream of Shepherdstown, West Virginia (northwest of Harpers Ferry), where entrenched meanders expose mile-long sections of tilted Conococheague strata. These may be easily seen from the towpath trail of the Chesapeake and Ohio Canal National Historical Park along the Maryland bank of the Potomac. In Shepherdstown itself, the top of a Conococheague cliff provides the setting for the monument to steamboat-inventor James Rumsey.
Conodonts are present in the Conococheague.
Relative-age dating of the Conococheague places it in the Upper Cambrian period.
Conococheague Formation Facts for Kids. Kiddle Encyclopedia.