Albemarle

History

This place-name is derived from the English surname Albemarle. According to a 1905 publication by the United States Geologic Survey, based on research by University of North Carolina - Chapel Hill history professor Kemp P. Battle, it was named specifically for General George Monck, the first Duke of Albemarle and one of the original proprietors of the colony of Carolina, which included the town. The site of modern-day Albemarle was originally peopled by small tribes of hunter-gatherers and mound builders whose artifacts and settlements have been dated back nearly 10,000 years. Large-scale European settlement of the region came in the mid-18th century via two primary waves: immigrants of Dutch, Scots-Irish and German descent moved from Pennsylvania and New Jersey seeking enhanced religious and political tolerance, while immigrants of English backgrounds came to the region from Virginia and the Cape Fear River Basin in Eastern North Carolina. In early English colonial times, the Albemarle area was politically part of the New Hanover Precinct, out of which the Bladen Precinct was created in 1734. The renamed Bladen County was subdivided to create Anson County in 1750, which in turn spawned Montgomery County in 1779. The Albemarle region's first post office was established in 1826; it was then known as Smith's Store. The nearby crossroads of the Old Turnpike Road from Fayetteville to Salisbury and the Old Stage Road connecting Charlotte and Raleigh emerged as an important hub for regional commerce and trade. The region remained part of Montgomery County until 1841, when after years of attempted separation, prominent residents of the increasingly populous areas west of the Yadkin/Pee Dee River system successfully petitioned the North Carolina General Assembly for the…

Geography

According to the United States Census Bureau, Albemarle has a total area of , of which is land and (0.44%) is water. The city is centered on the junction of U.S. Route 52 and the duplexed NC-24/27 in the Piedmont Region of North Carolina. Its topography is characterized by rolling, eroded hills, deciduous forests, and fast-running, narrow, shallow streams that feed the Yadkin/Pee Dee River Basin. Little Long Creek and Town Creek are the major non-seasonal streams through Albemarle; both flow generally southward into the Long and Big Bear Creek Sub-basin. Albemarle is located in the Floyd Church Formation of the Carolina Slate Belt. Thickly bedded, axially cleaved meta-mudstone and meta-argillite are common in this formation, interbedded with meta-sandstone, meta-conglomerate and meta-volcanic rock. Biotite is the most prevalent Paleozoic metamorphic rock in the region. Albemarle has a humid subtropical climate (Köppen climate classification Cfa), with cool to mild winters and hot, humid summers.

Race & ethnicity