Wirksworth

Wirksworth is a market town and civil parish in the Derbyshire Dales district of Derbyshire, England. Its population was 4,902 in the 2021 census. Wirksworth contains the source of the River Ecclesbourne. The town was granted a market charter by Edward I in 1306 and still holds a market on Tuesdays in the Memorial Gardens. The parish church of St Mary's is thought to date from 653. The town developed as a centre for lead mining and stone quarrying. Many lead mines were owned by the Gell family of nearby Hopton Hall.

The name was recorded as Werchesworde in the Domesday Book of 1086 A.D. Outlying farms (berewicks) were Cromford, Middleton, Hopton, Wellesdene [sic], Carsington, Kirk Ireton and Callow. It gave its name to the earlier Wirksworth wapentake or hundred. The Survey of English Place-Names records Wyrcesuuyrthe in 835, Werchesworde in 1086, and Wirksworth(e) in 1536.

The toponym might be "Weorc's enclosure", or "fortified enclosure".

The origins of Wirksworth are thought to have related to the presence of thermal warm water springs nearby, coupled with a sheltered site at the head of a glaciated valley, able to yield cereals such as oats and provide timber suitable for building.

The Wirksworth area in the White Peak is known for Neolithic and Bronze Age remains.

Woolly rhino bones were found by lead miners in 1822 in Dream Cave, on private land between Wirksworth and present-day Carsington Water. A nearby cave at Carsington Pasture yielded prehistoric finds in the late 20th century.

In Roman Britain, the limestone area of today's Derbyshire yielded lead, the prime site probably being Lutudarum in the hills south and west of present-day Matlock. Wirksworth is a candidate for the site of Lutudarum. Roman roads from Wirksworth lead to Buxton (The Street) and to Brough-on-Noe (The Portway). The town has the oldest charter of any in the Peak District, dating from 835, when the Abbess of Wirksworth granted nearby land to Duke Humbert of Mercia.

Many lead mines in Anglo-Saxon times were owned by Repton Abbey. Three of these are identified in Wirksworth's Domesday Book entry from 1086. Scientists studying a Swiss glacial ice core have found that levels of lead in European air pollution between 1170 and 1216 were similar to those during the Industrial Revolution, pointing to the local lead and silver smelting around Wirksworth, Castleton etc. as the main source with a remarkable correlation. There is a tiny carving in Wirksworth Church of a miner with a pick and whisket (basket); the figure is known as "T'Owd Man of Bonsall." It stood in Bonsall Church for centuries, but was moved for safekeeping during a restoration project. It was later found in a Bonsall garden and moved to Wirksworth by the vicar of the time. The ore was washed out through a sieve, whose iron wire had been drawn in Hathersage since the Middle Ages. Smelting took place in boles, hence the name Bolehill. The lead industry, the miner, the ore and the waste were also known collectively as "t'owd man".