Stafford Springs

History

The land that would become Stafford Springs was originally Mohegan territory. Indigenous peoples had long frequented the area's iron and sulfur mineral springs, reportedly drinking the waters for their invigorating properties. The region was acquired by Major James Fitch of Canterbury in a transaction that the Connecticut General Assembly did not fully accept; in 1718, the Assembly ordered that a town be laid out "of seven mile square ... eastward of Enfield," marking the beginning of legal settlement. Stafford was formally incorporated as a town in 1719. At the time of incorporation, the area was sparsely settled by farming families, with early industries closely tied to the agricultural economy: grist, saw, and fulling mills were built along fast-moving streams such as Furnace Brook. Bog iron was discovered early in the settlement's history, and furnaces were built to smelt the ore for iron castings and tools. This early iron industry laid the groundwork for the village's later industrial growth. The village developed into a popular resort destination drawing wealthy and prominent visitors throughout the late 18th and early 19th centuries. In 1771, a young John Adams—then a lawyer, years before his presidency—stayed in Stafford Springs for several days while recovering from overwork and anxiety, drawn by the reputation of the mineral waters. The first woolen mill in Stafford Springs, the Mineral Springs Manufacturing Company, was established in 1839 by Solva Converse on Spring Street. Following a serious fire and subsequent rebuilding in 1848, Solva and his brother Parley Converse became partners; by 1854, Solva became the sole owner and transitioned production from satinets to woolen goods over the following decade. The mill complex was eventually sold to the…

Geography

According to the United States Census Bureau, the CDP has a total area of 6.41 mi2 (16.6 km2), of which 6.37 mi2 (16.5 km2) is land and 0.036 mi2 (0.093 km2) (0.56%) is water. The village sits at an elevation of approximately 607 feet (185 m) above sea level. It is located near the source of the Willimantic River, the flow of which historically powered the mill operations that shaped the community.

Race & ethnicity