Chesapeake and Ohio Canal National Historical Park
The layers of red sandstone, siltstone, shale and limestone beneath the limekilns on the other side of the canal are like pages in a book to geologists. These folded, even rock layers indicate that millions of years ago this area was covered by a shallow sea. As the waters swelled and retreated, due to climatic change and tectonic plate movement, the colorful layers of sedimentary rock were exposed.HM Number | HM1T90 |
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Tags | |
Placed By | National Park Service, U.S. Department of the Interior |
Marker Condition | No reports yet |
Date Added | Monday, July 25th, 2016 at 9:03pm PDT -07:00 |
UTM (WGS84 Datum) | 17S E 737863 N 4395602 |
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Decimal Degrees | 39.67715000, -78.22661667 |
Degrees and Decimal Minutes | N 39° 40.629', W 78° 13.597' |
Degrees, Minutes and Seconds | 39° 40' 37.74" N, 78° 13' 35.82" W |
Driving Directions | Google Maps |
Area Code(s) | 301, 240 |
Closest Postal Address | At or near Western Maryland Rail Trail, Hancock MD 21750, US |
Alternative Maps | Google Maps, MapQuest, Bing Maps, Yahoo Maps, MSR Maps, OpenCycleMap, MyTopo Maps, OpenStreetMap |
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