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Calvert Cliffs

United States, Maryland

Calvert Cliffs

LocationUnited States, Maryland
RegionMaryland
TypeState Park
Coordinates38.4000°, -76.4167°
Established1968
Area5.91
Nearest CityLusby (3 mi)
Major CityWashington DC (55 mi)
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About Calvert Cliffs

Calvert Cliffs State Park is a 1,460-acre day-use park located along the western shore of the Chesapeake Bay in Calvert County, Maryland. The park is named for the massive fossil-bearing cliffs that dominate approximately 24 miles of the Chesapeake Bay shoreline. Established to protect and provide access to one of the most significant paleontological sites on the East Coast, the park offers visitors a unique opportunity to search for Miocene-era fossils while enjoying coastal recreation. The park features 13 miles of hiking trails through diverse habitats, a sandy beach for swimming and fossil hunting, freshwater and tidal marshlands, and an accessible recycled-tire playground. Due to active erosion and landslide dangers, climbing on or walking beneath the cliffs is permanently prohibited, though visitors can collect fossils that have naturally eroded onto the beach.

Wildlife Ecosystems

Calvert Cliffs State Park supports diverse wildlife communities across its coastal and forested habitats. The park is notable for hosting two federally threatened tiger beetle species: the Puritan tiger beetle and the northeastern beach tiger beetle, both state-listed as endangered. These large, colorful predatory beetles hunt invertebrates on the open sandy beaches and represent a significant conservation priority. The bay waters offshore support substantial waterfowl populations during winter, with 25 species documented. Double-crested cormorants and brown pelicans are abundant from April through late November. The park's marshlands provide habitat for great blue herons, egrets, and various wading birds. White-tailed deer, eastern box turtles, and numerous songbird species inhabit the forested uplands. The intertidal zones along the beach support crabs, horseshoe crabs during spawning season, and various marine invertebrates.

Flora Ecosystems

The park encompasses multiple distinct ecological communities shaped by its coastal location. The upland forests consist primarily of mixed hardwoods including oaks, hickories, tulip poplars, and American beech, providing a shaded canopy over the trail system. These forests transition into freshwater marshland ecosystems featuring cattails, phragmites, and various sedge species. The tidal marsh areas support salt-tolerant vegetation including cordgrass and marsh elder. The forest understory includes mountain laurel, holly, and various fern species. Seasonal wildflowers bloom throughout spring and summer along the trails. The park's diverse plant communities support the wildlife populations and help stabilize the terrain while providing natural erosion control in areas away from the cliffs. The maritime influence from the Chesapeake Bay creates microclimates that support both northern and southern plant species at the edge of their ranges.

Geology

The Calvert Cliffs represent one of the most significant Miocene-era fossil deposits in North America. Formed 10 to 20 million years ago when southern Maryland was covered by a warm, shallow sea, the cliffs expose three distinct geological formations. The oldest Calvert Formation is overlain by the Choptank Formation, with the youngest St. Marys Formation at the top. When the ancient sea receded, these sedimentary layers were exposed and began eroding, continuously releasing fossils onto the beach below. Over 600 species of Miocene fossils have been identified, including shark teeth from multiple species, whale bones, ray teeth, ancient crocodilian remains, and seabird fossils. The iconic Ecphora gastropod and Chesapeake tenas shells are common finds. The cliffs continue to actively erode, making fossil hunting productive but also creating dangerous landslide conditions that necessitate permanent closure of the cliff base.

Climate And Weather

Calvert Cliffs State Park experiences a humid subtropical climate moderated by the Chesapeake Bay. Summers are warm and humid with temperatures typically reaching the mid-80s°F, making the beach a popular destination for swimming. Winters are generally mild with occasional cold snaps and light snowfall. The bay moderates temperature extremes, keeping the area slightly cooler in summer and warmer in winter compared to inland locations. Spring and fall offer the most pleasant hiking conditions with moderate temperatures and vibrant foliage in autumn. Summer visitors should be aware of jellyfish in bay waters and biting flies along the beach. The park is open sunrise to sunset year-round, though beach conditions and water temperatures are most favorable from late May through September. Hunting seasons occur during certain periods, affecting trail access in designated areas.

Human History

The Calvert Cliffs region has attracted human attention for millennia due to its abundant natural resources. Native American peoples inhabited the area for thousands of years, utilizing the bay's rich fisheries and the forests for hunting. European colonization brought tobacco farming to Calvert County in the 17th century, and the region developed as an agricultural community. The remarkable fossil deposits in the cliffs drew scientific attention as early as the 1600s when naturalists began documenting the unusual shells and shark teeth eroding from the bluffs. Throughout the 19th and 20th centuries, the cliffs became increasingly recognized for their paleontological significance, attracting researchers and collectors from institutions across the country. The site has contributed substantially to scientific understanding of Miocene marine ecosystems and has yielded type specimens for numerous species new to science.

Park History

Calvert Cliffs State Park was established to protect the significant natural and paleontological resources along this stretch of Chesapeake Bay shoreline. The Maryland Department of Natural Resources acquired the land to ensure public access to the fossil-bearing cliffs while implementing conservation measures. The park has developed infrastructure to balance visitor access with resource protection, including constructing trail systems that provide a 1.8-mile route to the beach along the Red Trail. Recognition of the site's geological importance led to its designation as a significant paleontological locality. The park works with scientific institutions to monitor the cliffs and document significant fossil discoveries. Safety measures have been implemented including permanent closure of the cliff base due to ongoing erosion and landslide hazards, while still allowing visitors to collect fossils that have naturally washed onto the beach.

Major Trails And Attractions

The park features 13 miles of trails through varied terrain. The most popular is the Red Trail, a 1.8-mile route that provides the shortest access to the beach and fossil-hunting areas. This well-maintained trail passes through shaded forest and crosses boardwalks over marshland before reaching the sandy beach. Other trails loop through the forested uplands, offering longer hiking options and wildlife observation opportunities. The primary attraction is the beach itself, where visitors can search for Miocene fossils including shark teeth, whale bones, and ancient shells that have eroded from the cliffs. An accessible playground constructed from recycled tires provides recreation for families. Freshwater and tidal marsh areas offer birdwatching opportunities. Fishing is permitted along the shoreline. The cliffs themselves, while off-limits for climbing, provide a dramatic scenic backdrop visible from the beach.

Visitor Facilities And Travel

Calvert Cliffs State Park is a day-use facility open sunrise to sunset throughout the year. The park is located in Lusby, Maryland, accessible via Calvert Cliffs Parkway off Route 765. Facilities include a parking area, restrooms, and picnic areas near the trailhead. The recycled-tire playground offers accessible recreation for children. There is no camping within the park. Visitors should bring water and appropriate footwear for the trail to the beach. Swimming is permitted in the bay but is not lifeguarded; visitors should exercise caution regarding currents, jellyfish, and water conditions. Fossil collecting is allowed on the beach using hand tools only. A Maryland fishing license is required for shoreline fishing. The park can become crowded on summer weekends, so early arrival is recommended. Dogs are permitted on leashes but are not allowed on the beach from April 1 through October 31.

Conservation And Sustainability

Conservation at Calvert Cliffs State Park focuses on protecting both the paleontological resources and the sensitive coastal ecosystems. The permanent closure of the cliff base protects visitors from landslide hazards while reducing human impact on the actively eroding geological features. Management efforts address invasive species that threaten native plant communities in the forests and marshlands. The park's tiger beetle populations receive special attention due to their federal threatened status, with monitoring and habitat protection measures in place. Coordination with scientific institutions ensures that significant fossil discoveries are documented and preserved for research. The park balances public access for recreation and education with resource protection, limiting activities that could accelerate erosion or disturb sensitive habitats. Water quality in the adjacent bay is monitored as part of broader Chesapeake Bay restoration efforts.

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International Parks
January 22, 2026

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Frequently Asked Questions

Where is Calvert Cliffs located?

Calvert Cliffs is located in Maryland, United States at coordinates 38.4, -76.4167.

How do I get to Calvert Cliffs?

To get to Calvert Cliffs, the nearest city is Lusby (3 mi), and the nearest major city is Washington DC (55 mi).

How large is Calvert Cliffs?

Calvert Cliffs covers approximately 5.91 square kilometers (2 square miles).

When was Calvert Cliffs established?

Calvert Cliffs was established in 1968.

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