Updated 14 Jul 2007
WIRKSWORTH Parish Records 1600-1900
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Unposted. Notice: Huge lump of tufa as lintel, two more as
gateposts. Tufa outhouse on right and perhaps toilet on left.
Fire from right room, 30 panes of glass in large windows.
Margaret Howard of Bonsall writes:
The following is the OS reference for the above taken from my very battered copy of the O.S. 1.25000 First Series, Wirksworth, Sheet SK25:- SK 269.567.
As one is travelling from Cromford westwards along the Via Gellia (after the Bonsall road turns off up the Clatterway) towards the Grange Mill crossroads on which the "Holly Bush" Inn is found, the cottage is sited at road level on the northern side of the Via Gellia, just before the very bad bend below Good Luck mine (on the southern side of the Via Gellia in Middleton parish). Northwards uphill from the cottage is located Dunsley spring, which presumably was used as a water supply to the cottage. This spring runs off the volcanic rock found on Bonsall Leys and was a source of water for Bonsall farmers living on Bonsall Leys.
I understood this cottage to be a game keeper's cottage belonging to the Keys Estate from Cromford, which was sold off from the estate in the late 1980's early 1990's. I had a friend who lives at Elton whose grandfather was the last gamekeeper to occupy with his wife the cottage, they retired to Elton when Tuffa cottage was sold but I don't know their name. Incidently the Via Gellia was the Cromford/Newhaven Turnpike opened in 1804...Margaret
Inhabitants of Tufa Cottage, as listed in the Census, seem to be: 1901:Edward BROOKS | 1891:Edward BROOKS | 1881:William CHARLTON | 1871:William CHARLTON | 1861:William CHARLTON | 1851:William CHARLTON
Some learned words about Via Gellia and Tufa Cottage.
Tufa is a rough, thick, rock-like calcium carbonate deposit that forms by precipitation from bodies of water with a high dissolved calcium content.
(Note that tufa is entirely different from tuff, which is a type of rock consisting of consolidated volcanic ash ejected from vents during a volcanic eruption.)
The road from Grangemill to Cromford was constructed through the Griffe Grange
Valley in the eighteenth century by Philip GELL and given the name Via Gellia,
as a consequence of the "GELLs" alleged Roman descent. The purpose was to
improve access between the family lead mines at Carsington and the Cromford
smelter. Now the valley, as well as the road, is more commonly known as Via
Gellia. Whatever name is used, it is one of the most beautiful valleys in the
county and Lord BYRON could have had it in his mind when he wrote "I assure
you there are things in Derbyshire as noble as in Greece or Switzerland"
Early in the nineteenth century there were seven mills set at different levels up a two mile stretch of the Via Gellia from Cromford. The trade name Vyella originated from the fabric that was once produced at one of the textile mills in the valley. On the steep hillside, where the Bonsall road meets the Via Gellia, a skull, thought to be that of a mammoth, was discovered at the entrance to a cave. Further up the valley the Tufa Cottage is most unusual, being constructed of tufa rock formed from dissolved limestone which has been re-deposited in water.
The continuity of the distinctive limestone plateau scenery of the
White Peak is broken by a few deeply incised dales and by a wider
network of shallower dry valleys. Although the valleys are water-cut
features, most are now dry, providing evidence of a change in climate.
During cold phases of the Ice Age, meltwaters from snowfields cut into the limestone surface forming valley features. When the climate changed, the volume of drainage water reduced and lacked the capacity for valley excavation. What little drainage remained now flows underground through cave and fissure systems, leaving a network of dry valleys.
The Via Gellia is a steep-sided, narrow, wooded valley running eastwards from Grangemill to Cromford. Most of the Via Gellia is a dry valley, although it does carry an ephemeral stream in wet weather. Its curious name 'Via Gellia', is thought to derive from the name of a local landowner, John Gell of Hopton, who first drove a road along the valley floor.
British Geological Survey.
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