The town was established in the early 19th century by Jacob Ball, a United Empire Loyalist. The Ball or Bahl family had a long association with the English Crown, and had originally emigrated to the County of Norfolk in England from lands in what is now Germany. In 1690, the family purchased lands in New York'sMohawk Valley, paying one shilling per acre to the Crown. Subsequently, they emigrated and settled there. During the American Revolution, the Ball family maintained their allegiance to the Crown. In 1782, Jacob moved to what is now Canada with most of his sons and fought with the Loyalist Butler's Rangers and Queen's Rangers militias for the remainder of the Revolutionary War. Jacob, a Captain in the Rangers, brought much of his company with him. The family received a land grant from the Crown in 1783, and the remainder of the family emigrated to Canada in the following year, 1784. Two of Jacob's sons, John and George, received 1200 acres of land in Niagara in 1807. Twenty Mile Creek, which runs through the area, has two waterfalls. The Ball brothers built a grist mill, a saw mill at the lower falls and a woollen mill at the upper falls. During the War of 1812, the settlement was heavily utilized by the military, as part of a regiment was stationed there for a time. The town began flourishing and soon a blacksmith, tailor, weaver and butcher lived on the land. By 1852 the population of the town, then Glen Elgin, grew to 19 inhabitants. In the late 1850s, the Great Western Railway was established and many moved away from Glen Elgin and were located closer to the railway. In 1962 Manly Ball sold the land to the Niagara Peninsula Conservation Area and the town, now known as Ball's Falls, is a tourist attraction.
Geography
Located in the Niagara region of Ontario, Ball's Falls currently occupies around one sixth of the 1200 acres bought by the Ball brothers. It has a mild climate as a result of its location, which is south of Lake Ontario and north of Lake Erie. There are two waterfalls on Twenty Mile Creek. The upper falls are 35 feet high, and the lower falls are 90 feet high. ]The falls can be viewed from above and below. The gorge has also become an area of scientific interest. The lower falls pass over Irondequoit limestone, a firm layer over several weaker sandstone layers. The rock of the upper falls is formed of the same unit, the Lockport Formation, that forms the crest of Niagara Falls.
After the purchase of Ball's Falls by the Niagara Peninsula Conservation Authority in 1962, the area became a conservation area. The park features the Ball's Falls Centre for Conservation to help visitors learn of the area's cultural and natural history. The building, designed to have a limited impact of the surrounding environment, features permanent and temporary galleries, exhibits and interactive displays, including the conservation practices of the Niagara Peninsula Conservation Authority, archaeological findings, and the watershed ecosystem of Twenty Mile Creek. Still standing within the park are the original Ball family home, an operating gristmill, a lime kiln, a restored church, a blacksmith shop, and a carriage shed.