Wallaceton (Chesapeake, Virginia)

Cornland School is a one-room schoolhouse located in Chesapeake, Virginia. "It is believed to be the oldest pre-Rosenwald School still standing in Tidewater Virginia." It was listed on the National Register of Historic Places in 2015.

The Dismal Swamp Canal is a canal located along the eastern edge of the Great Dismal Swamp in Virginia and North Carolina in the United States. Opened in 1805, it is the oldest continually operating man-made canal in the United States. It is part of the Intracoastal Waterway.

Cavalier Wildlife Management Area is a 4,550-acre (18.4 km2) Wildlife Management Area in Chesapeake, Virginia. It preserves habitat for a number of species, including black bear, canebrake rattlesnakes, white-tailed deer, eastern wild turkeys, and many varieties of songbirds.The preserve comprises two separate tracts of land. The 3,800-acre (15 km2) main tract is located about 2.5 miles (4.0 km) east of the Great Dismal Swamp National Wildlife Refuge and adjacent to the Virginia–North Carolina border; it was once a part of the Great Dismal Swamp but was drained more than 200 years ago. The main tract today is typified by recently logged forestlands planted with young pine. A smaller, 758-acre (3.07 km2) tract lies about six miles (9.7 km) north of the main area of land, immediately adjacent to the Great Dismal Swamp National Wildlife Refuge.The area is open to the public for seasonal hunting, trapping, fishing, hiking, and primitive camping. Firearms are prohibited in the Dismal Swamp tract, where only bow-hunting is permitted; firearms may be used for hunting within the main tract. Neither area permits horseback riding.Cavalier Wildlife Management Area is owned and maintained by the Virginia Department of Game and Inland Fisheries. Access for persons 17 years of age or older requires a valid hunting or fishing permit, or a WMA access permit.

The Great Dismal Swamp National Wildlife Refuge was created in 1974 to help protect and preserve a portion of the Great Dismal Swamp, a marshy region on the Coastal Plain of southeastern Virginia and northeastern North Carolina between Norfolk, Virginia, and Elizabeth City, North Carolina in the United States. It is located in parts of the independent cities of Chesapeake and Suffolk in Virginia, and the counties of Camden, Gates, and Pasquotank in North Carolina.

The Great Dismal Swamp is a large swamp in the Coastal Plain Region of southeastern Virginia and northeastern North Carolina, between Norfolk, Virginia, and Elizabeth City, North Carolina. It is located in parts of the southern Virginia independent cities of Chesapeake and Suffolk and northern North Carolina counties of Gates, Pasquotank, and Camden. Some estimates place the original size of the swamp at over one million acres (4,000 km2). As of 2022 the size of the Great Dismal Swamp is around 750 square miles (480,000 acres) (1,940 square km). Lake Drummond, a 3,100-acre (13 km2) natural lake, is located in the heart of the swamp. Lake Drummond is a circular body of water, and is one of only two naturally occurring freshwater lakes in Virginia. Along the Great Dismal Swamp's eastern edge runs the Dismal Swamp Canal. The canal is 22 miles long, and was completed in 1805 to provide a pathway for trade between Chesapeake Bay, Virginia and the Albemarle Sound in North Carolina. The largest water supply for the Dismal Swamp Canal is through Lake Drummond.The Great Dismal Swamp National Wildlife Refuge was created in 1973 when the Union Camp Corporation of Franklin, Virginia, donated 49,100 acres (19,900 ha) of land after centuries of logging and other human activities devastated the swamp's ecosystems. The refuge was officially established through the Dismal Swamp Act of 1974, and consists of over 167 square miles (433 square km) of forested wetlands. Outside the boundaries of the refuge, the state of North Carolina has preserved and protected additional portions of the swamp through the establishment of the Dismal Swamp State Park. That park protects 22 square miles (57 km2) of forested wetland.The swamp was a refuge location for the Great Dismal Swamp maroons, including enslaved people in the Southern states before the American Civil War, and Native Americans who were escaping colonial expansion. Prior to the maroons inhabiting the swamp, it was inhabited by Algonquian-speaking Native American coastal tribes. A 45,611-acre (184.58 km2) remnant of the original swamp was declared a National Natural Landmark in 1973, in recognition of its unique combination of geological and ecological features.

Lake Drummond is a freshwater lake at the center of the Great Dismal Swamp, a marshy region on the Coastal Plain of southeastern Virginia and northeastern North Carolina between Norfolk, Virginia, and Elizabeth City, North Carolina, in the United States. Its surface area is approximately 3,142 acres (13 km2) and its maximum depth is 6 ft (2 m). It is managed by the United States Fish and Wildlife Service. Geologists believe the Great Dismal Swamp was formed when the continental shelf experienced sudden settling. The entire swamp is underlain by a layer of peat. Several theories exist about the lake's origin. Some postulate that it was created by a large underground peat fire 3,500–6,000 years ago. Native American legends speak of "the fire bird" creating Lake Drummond. Other theories include a meteorite impact and a tectonic shift. Lake Drummond is one of only two natural freshwater lakes in Virginia. The other, Mountain Lake in Giles County, is also of unknown origin. Curiously, both are lakes essentially on top of hills. Drummond is the highest point in the Dismal Swamp, with nine small ditches flowing out of it. The precise time of the Great Dismal Swamp's discovery and settlement is not known, but archaeological evidence indicates human occupation began nearly 13,000 years ago. By 1650, few Native Americans remained in the area, and European settlers showed little interest in the swamp. In 1665, William Drummond, a future governor of North Carolina, found the lake which now bears his name. Several centuries of exploitation and logging reduced the swamp to about 50% of its original size. It was common practice for merchant ships of the time to fill up water casks with the dark-stained water from Lake Drummond. With its high tannin content, the water stayed fresher longer on trans-Atlantic voyages than water from other sources. Lake Drummond and much of the Great Dismal Swamp are within the bounds of the Great Dismal Swamp National Wildlife Refuge, officially established through the Dismal Swamp Act of 1974. The refuge includes almost 107,000 acres (43,000 ha) of forest wetlands. North Carolina established a state park to protect another portion of the swamp. Dismal Swamp State Park protects 22 square miles (57 km2) of forested wetland.Due to relatively low pH levels caused by the leaching of acidic materials from surrounding peat soils, the lake has a relatively low level of nutrients. A few species of fish are present, including crappie, bowfin, and longnose gar.

Dismal Swamp State Park is a North Carolina state park in Camden County, North Carolina, in the United States. The park was created as a state natural area in 1974 with the help of The Nature Conservancy, and on July 28, 2007, the North Carolina General Assembly re-designated it as a state park. It opened to the public in 2008. This marked the first time that public access to Great Dismal Swamp was made possible in North Carolina. The park covers 14,432 acres (58.40 km2) of protected land on the North Carolina/Virginia border. Park offices are 3 miles (4.8 km) south of the border on U.S. Route 17 near South Mills. Features of the park include the canal which is used regularly by boaters using the Intracoastal Waterway and several miles of hiking and biking trails.

Grassfield High School is a public high school located in Chesapeake, Virginia, USA, and is administered by Chesapeake City Public Schools. It was built to ease overcrowding at Deep Creek High School, Great Bridge High School, and Hickory High School. Grassfield, along with Western Branch High School and Oscar Smith High School, features the latest technology available in the school district. Grassfield is also the City of Chesapeake's location for the STEM (Science, Technology, Engineering, and Mathematics) school as various high school students around the city can apply for admission into the program.

Deep Creek is a former unincorporated town of the former Norfolk County (extinct) which since 1963 has been located in the independent city of Chesapeake in the South Hampton Roads region of southeastern Virginia. Deep Creek is located on the original route of U.S. Highway 17 (also known as the Ocean Highway), on a section now designated as U.S. Route 17 Business, and has been largely bypassed by modern highway improvements.

Deep Creek High School is a public secondary school in Chesapeake, Virginia. It is part of Chesapeake City Public Schools and is located on 2900 Margaret Booker Drive.

The Veterans Bridge is a fixed span concrete bridge that spans the Southern Branch of the Elizabeth River in the Deep Creek neighborhood of Chesapeake in southeastern Virginia, USA. The bridge, which partially opened in 2014, currently carries two lanes of U.S. Route 17 (US 17; Dominion Blvd) on each direction across its northbound and southbound spans. The corridor frequently acts as a bypass route for congested I-64 High Rise Bridge traffic. It replaces the much shorter and smaller Dominion Boulevard Steel Bridge, which because of its 11-foot underwater clearance opened on average of 16 times per day.Tolling began on the route on February 9, 2017. Most cars, SUVs and passenger trucks that use the bridge and utilize an E-ZPass transponder will only pay $1 to cross. Larger vehicles, such as transit busses and semi-trailer trucks, will face an E-ZPass toll ranging from $1.50 to $2.50, depending on its classification. However, those same vehicles crossing without a transponder will still pay their respective base toll, but will also incur a $2 processing fee in addition to the original toll.The toll is expected to increase by approximately 5 percent each year through 2035.

Dominion Boulevard Steel Bridge (known locally as simply the Steel Bridge) was a double-leaf bascule, two-lane drawbridge which spanned the Southern Branch Elizabeth River in the City of Chesapeake in South Hampton Roads in southeastern Virginia. Built in 1962 and operated by the City of Chesapeake, it carried U.S. Route 17 (US 17) which is Dominion Boulevard (formerly numbered as State Route 104). The corridor frequently acts as a bypass route for congested I-64 High Rise Bridge traffic. Because of the low water clearance, bridge openings were commonplace for the bridge, with an average of 16 lifts per day. Combined with an average daily traffic count of 33,000, it frequently became a choke point for commuters who lived in the Deep Creek part of the city, with a failing level of service on the entire stretch according to a during a 2006 traffic plan by the HRPTO.In January 2013, Chesapeake Public Works began construction on a $345 million fixed-bridge replacement project called the Veterans Bridge, which was completed in late 2017. It expanded Dominion Blvd. from two to four lanes from the intersection of Cedar Road & Moses Grady Trail to the interchange of Great Bridge Blvd. The Veterans Bridge is tolled, which started at the rate of $1 in 2017. This project is also a part of the planning for the future Interstate 87 that will connect the Raleigh-Durham Metro area to the Hampton Roads region.After the first span of the Veterans Bridge opened in December 2014, the Steel Bridge was shut down and demolished.