- Wildlands 1,079 acres (437 ha) Phone +1 301-743-7613 | Area 5.305 km² | |
 | ||
Address 10540 H G Trueman Rd, Lusby, MD 20657, USA Management Maryland Department of Natural Resources Similar Calvert Marine Museum, Flag Ponds Nature Park, Cove Point Light, Calvert Cliffs Nuclear P, Greenwell State Park | ||
Hiking in calvert cliffs state park cliff beach trail red trail
Calvert Cliffs State Park is a public recreation area in Lusby, Calvert County, Maryland, that protects a portion of cliffs that extend for 24 miles along the eastern flank of the Calvert Peninsula on the west side of Chesapeake Bay from Chesapeake Beach southward to Drum Point. The state park is known for the abundance of mainly Middle Miocene sub-epoch fossils that can be found on the shoreline.
Contents
Calvert cliffs state park 2013 fossil hunting program
GeologyEdit
The park contains the type locality site of the Early to Middle Miocene Calvert Formation. These rocks are the sediment from a coastal ocean that covered the area during that time. The age of the formation is (19-)18–15(-14) million years ago (Ma), i.e. it extends essentially over the Hemingfordian stage. This formation occurs in Maryland and neighboring Virginia.
In addition, rocks of the younger Choptank and the St. Marys Formations are exposed here. This makes Calvert Cliffs State Park extremely interesting for its paleoclimatology and paleontology, because the accessible strata provide a good record of the Middle Miocene Climate Transition and document a minor mass extinction event — the "Middle Miocene disruption." Fossil collecting and "rockhounding" are permitted on the beach; the cliffs are closed due the dangers of erosion.
PaleontologyEdit
The Calvert Formation is notable for its plentiful fossil shark teeth. Especially popular among "rockhounds" are those from giants such as Carcharocles and the famous Megalodon (which is often included in Carcharocles).
The ancestral baleen whale Eobalaenoptera harrisoni and the merganser Mergus miscellus were described from the Virginian part of the formation. From the uppermost layer, deposited 15-14 Ma, they represent the oldest known member of their family and genus, respectively. Some remains of a prehistoric loon (Gavia) from the lowermost parts of the Calvert Formation, dating back nearly 18 Ma, are the oldest records of that genus from North America, and among of the oldest worldwide.
Other notable baleen whales from this area include a Cephalotropis coronatus. One was recently discovered by hobbyist paleontologist Jeffery DiMeglio in 2004 after Hurricane Isabel caused historical cliff erosion exposing the skull and scapula. Mandibles, neck vertebrae, and scapula were also found during the dig. The skull and vertebrae are now on display at the Calvert Marine Museum as part of a permanent exhibit, "Geologic Timeline". Other items found in the field jackets of the whale were fish bones, hundreds of mollusks, 1 Hexanchus gigas tooth, and 2 Carcharodon hastalis teeth.
Social historyEdit
On his 1612 map, Captain John Smith identified the area as "Rickard's Cliffes," having given them his mother's family's name. Some 350 years later, the state park was developed with the General Assembly funding land purchases in each year from 1965 to 1968, then in 1969, dedicating money to the installation of the park's initial roads, parking area, and utilities.
Industrial neighborsEdit
The Calvert Cliffs Nuclear Power Plant is located a short distance north of the park. The Dominion Cove Point liquid natural gas receiving station is visible off shore from the park beach.
Activities and amenitiesEdit
Calvert Cliffs State Park is mostly forested, with some wetland areas and a small pond for fishing. The park has 13 miles (21 km) of marked hiking trails. A quarter-mile-long sandy beach is accessible via a 1.8-mile (2.9 km) trail. Some 550 acres are open to hunting upland game, turkey, and deer. The park is rich in biodiversity and is home to numerous species of plants and animals, with at least 163 species of birds observed in the park.