Вирджиния штатындағы Радфорд қаласы

Independent city in Virginia, United States

Radford (formerly Lovely Mount, Central City, English Ferry and Ingle's Ferry) is an independent city in the U. S. state of Virginia. As of 2020, the population was 16,070 by the United States Census Bureau. For statistical purposes, the Bureau of Economic Analysis combines the city of Radford with neighboring Montgomery County. Radford is included in the Blacksburg–Christiansburg metropolitan area. Radford is the home of Radford University. Despite its name, the Radford Arsenal, historically a major employer of city residents, is in neighboring Pulaski and Montgomery counties. Radford City has four schools: McHarg Elementary, Belle Heth Elementary, Dalton Intermediate, and Radford High School.

Radford was named for Dr. John B. Radford. Dr. Radford's home Arnheim was listed on the National Register of Historic Places in 2002. Radford was originally a small village of people that gathered near the New River, which was a major draw to travelers for fresh water and food while traveling west. The town's population grew rapidly after 1854 when the Virginia and Tennessee Railroad was built nearby. A large depot was placed at Lovely Mount because of its strategic positioning between the eastern and western parts of the state. The actual station was not on Lovely Mountain, located on the southwestern side of town, but Lovely Mount was a known mountain and naming the station this would help people to remember the location of the depot. The Railroad Depot caused the population of Radford to boom. It also caused a major increase in the amount of trade and business in the area. Radford became a railroad town. The original name for Radford was Lovely Mount because of the location of the depot; the name was changed in 1891 to Radford. Radford, or at least the train station area, was called Central Depot because of its central location halfway between Lynchburg and Bristol, Virginia, on the original railroad, the Virginia and Tennessee Railroad (later the Norfolk and Western Railway). The names "Ingle's Ferry" or "English Ferry" were derived from Ingles Ferry over the New River, just east of the town. From 1900 to 1930, many companies came to Radford, including an ice company, a creamery, milling companies, piping, and preserving plants. In 1913, Radford was selected to become home to Radford State Normal School, a women's college. The school would later, in 1924, become Radford College and then in 1979 would be renamed Radford University. The presence of a college brought even more attention to Radford, causing even more population growth. In 1940–1941 the US Military decided to build a manufacturing plant for gunpowder and other ammunition needed by the military. Thus the Radford Army Ammunition Plant, or the "Arsenal" as it would come to be called, joined the railroad and Lynchburg Foundry as major employers creating a huge influx in population. Many families moved to the area. Housing for the Arsenal was built in specific areas of town and these neighborhoods still exist today; Monroe Terrace, Radford Village, and Sunset Village. Today these are Radford's main residential neighborhoods. The railroad ceased passenger service through Radford 1971 as personal transportation moved to the fairly new interstate highway system and the airways. However, the railroad route through Radford is still a major component of Norfolk Southern Railway's Roanoke to Bristol route. But, Radford no longer needed the railroad passenger service to survive. The James Charlton Farm, Ingles Bottom Archeological Sites, and Ingles Ferry are listed on the National Register of Historic Places.

Bisset Park is the largest of the four parks, located on the New River, it stretches Bisset Park was named for David Bisset, a major contributor and overseer of parks and recreation in Radford. Bisset Park is located in the center of town across from Wildwood Park. It features three picnic shelters, a gazebo, tennis courts, and open fields mainly used for little league soccer. The Riverway Trail is a 3.5 mile paved biking and walking path that can be accessed from Bissett Park. From there the trail extends to the east along the New River and to the south into Wildwood Park. A Civil War Trails marker can be found at the westernmost end of the park, where the foundation of a bridge burned down during the Battle of New River Bridge can be seen.

Wildwood Park is a 50 acre wooded ravine in the center of town, with a paved bikeway along a stream at the bottom of two forested hillsides crisscrossed by hiking trails. and was narrowly rescued from a highway bypass plan in 1998 with the formation of a "Pathways for Radford" group seeking city support, leading to a development plan. The park falls along the original boundary between the former towns of East Radford, home of Radford University, and the traditionally more industrial West Radford. The towns were joined with the bridging of Connelly's Run by the city's East and West Main Street. The well documented variety of flowers is especially attractive to visitors. Wildlife include many native birds as well as deer, raccoons, opossums, skunks, and groundhogs. The western slope includes Adams Cave, a limestone cave used for saltpeter during the Civil War; the cave entrance is now gated and locked. A shallow stream, Connelly's Run, flows through the park and provides great crayfish hunting for children during the summer months. A culvert carries its waters under Main Street to the New River in Bisset Park. Connelly's Run fed a city swimming pool for 45 years, but the pool was closed and filled in when faced with the prospect of racial integration in 1965.

Radford is located at (37.127585, −80.569523). According to the United States Census Bureau, the city has a total area of 10.2 square miles (26 km2), of which 9.9 square miles (26 km2) is land and 0.3 square miles (1 km2) (3.3%) is water. The New River runs along the southwestern, western and northern edge of the city.

The worst river flooding in Radford's recorded history occurred on August 14, 1940, with a slow moving tropical depression. The 1940 hurricane season produced eight storms, four of which were hurricanes. Around August 5 of that year, a tropical storm was detected along the northern Leeward Islands in the West Indies. The storm brought wind gusts of 44 mph to San Juan, Puerto Rico, as it moved northwestward. By August 6 it began a turn to the north while producing rough seas in the southeastern Bahamas. Four days later on August 10 the S. S. Maine off the southeast coast measured hurricane force winds and the storm began movement again toward the northwest. The storm made landfall as a category 1 hurricane on August 11 at approximately 4 PM near Beaufort, South Carolina (along the SC/GA border). Winds reached 73 mph in nearby Savannah, Georgia. As the Georgia – South Carolina hurricane of 1940 moved inland, record rainfall amounts were observed from South Carolina north through the Smoky Mountains and into southwest and central Virginia. The storm meandered along the Cumberland Plateau region as rain began falling in Virginia on August 13. The mountainous terrain coupled with extremely slow movement from the now tropical depression produced tremendous amounts of rain. Copper Hill in Floyd County, Virginia, received the highest rainfall in the state: 17.03 inches. The United States Geological Survey (USGS) stream gauge across the New River (Kanawha River) from Bisset Park measured an all time record height of 35 feet 11.5 inches which is nearly 22 feet above what is considered flood stage. Residents in low lying areas were forced to evacuate their homes and both the former Burlington Mills and the Lynchburg Foundry manufacturing plants were shut down because of high water. The road leading from Radford into Pulaski County towards Claytor Lake Dam was inundated and impassable. Thankfully, no deaths were reported across southwest Virginia, but several million dollars worth of damage occurred (1940 USD). On October 18, 2011, a sign recognizing the historic flooding was dedicated in Bisset Park near downtown Radford. The sign was donated by local resident Anthony Phillips, a hydrometeorologist from Snowville, Virginia, and installation was sponsored by the National Weather Service and the United States Geological Survey through the High Water Mark (HWM) Project. The project helps raise awareness of flood risk by installing high water mark signs in prominent locations within communities that have experienced severe flooding.

As of the census of 2000, there were 15,859 people, 5,809 households, and 2,643 families residing in the city. The population density was There were 6,137 housing units at an average density of The racial makeup of the city was 88.21% White, 8.10% African American, 0.25% Native American, 1.43% Asian, 0.03% Pacific Islander, 0.49% from other races, and 1.51% from two or more races. Hispanic or Latino of any race were 1.16% of the population. There were 5,809 households, out of which 18.8% had children under the age of 18 living with them, 33.9% were married couples living together, 8.9% had a female householder with no husband present, and 54.5% were non families. 32.0% of all households were made up of individuals, and 8.7% had someone living alone who was 65 years of age or older. The average household size was 2.25 and the average family size was 2.78. The age distribution, which is strongly influenced by Radford University, is: 12.9% under the age of 18, 44.0% from 18 to 24, 19.6% from 25 to 44, 14.3% from 45 to 64, and 9.2% who were 65 years of age or older. The median age was 23 years. For every 100 females, there were 83.5 males. For every 100 females age 18 and over, there were 81.6 males. The median income for a household in the city was $24,654, and the median income for a family was $46,332. Males had a median income of $33,045 versus $22,298 for females. The per capita income for the city was $14,289. About 6.9% of families and 31.4% of the population were below the poverty line, including 10.8% of those under age 18 and 9.4% of those age 65 or over.

The climate in this area has mild differences between highs and lows, and there is adequate rainfall year round. According to the Köppen Climate Classification system, Radford has a marine west coast climate, abbreviated "Cfb" on climate maps.