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TUCKING MILL is a small hamlet within the parish of Monkton Combe , Somerset
Somerset
, England. It lies on Midford Brook
Midford Brook
and was a key point on the now disused Somerset
Somerset
Coal Canal .

It is at the southern end of the Two Tunnels Greenway which follows the disused railway trackbed of the Somerset
Somerset
and Dorset Joint Railway from East Twerton
Twerton
through the Bath suburb of Oldfield Park to the Devonshire Tunnel , emerging into Lyncombe Vale before entering the Combe Down Tunnel , and then coming out to cross Tucking Mill
Tucking Mill
Viaduct into Midford .

There is also a small reservoir, which is now a fishery for the disabled.

CONTENTS

* 1 William Smith\'s home * 2 Fuller\'s earth factory * 3 Gallery * 4 References

WILLIAM SMITH\'S HOME

From 1798 until 1810 Tucking Mill
Tucking Mill
was the home of William Smith , an English geologist , credited with creating the first nationwide geological map . He is known as the "Father of English Geology
Geology
" for collating the geological history of England
England
and Wales into a single record. He worked on the Somerset
Somerset
coalfield and the Somerset
Somerset
Coal Canal . There is a plaque on Tucking Mill
Tucking Mill
Cottage saying that it was Smith's home, which was erected in 1888, on the mill which was demolished in 1927, and the tablet was mislaid. When the plaque was rediscovered in the 1930s the Geological Society of London
Geological Society of London
and the Bath Royal Literary and Scientific Institution placed it on the 18th century cottage,. However, it is now believed that he actually lived in the nearby Tucking Mill
Tucking Mill
House. During his occupation he built a small railway to transport stone from a quarry at Kingham Field, Combe Down to the canal.

FULLER\'S EARTH FACTORY

From 1883 until the end of World War II
World War II
it was the site of a fuller\'s earth factory. George Dames and his brother Charles Richard Dames set up a mine in Horsecombe Vale. At the bottom of the valley was the pan grinding works where water from Horsecombe Brook was used to make a slurry from which sand settled at the bottom of troughs. The slurry then passed through an earthenware pipe to Tucking Mill, where a second stage of sedimentation took place in large troughs where it settled for up to 30 days. Once the water had been drained by sluices the damp caked earth was carried in wooden trams to kilns where it was dried for three to four days. The product was used in the oil refining and pharmaceutical industries. The original uses in woollen production no longer used fuller's earth. A railway siding at Midford railway station was built specifically to load fuller's earth.

GALLERY

*

The cottage at Tucking Mill
Tucking Mill
which has a plaque saying that William Smith lived there *

The house William Smith actually lived in

REFERENCES

* ^ "Two Tunnels Greenway, Bath". Explore. Ordnance Survey. Retrieved 2008-07-09. * ^ "Tucking Mill". wessex Water. Retrieved 19 November 2010. * ^ "Tucking Mill, Pilgrimage to Smith of the Rocks". Bath Daily Photo. Retrieved 19 July 2010. * ^ " Tucking Mill
Tucking Mill
Cottage". Images of England
England
. English Heritage
English Heritage
. Retrieved 19 July 2010. * ^ "William Smith". Bath Royal Literary & Scientific Institution. Archived from the original on 13 October 2007. Retrieved 19 July 2010.

* ^ " Tucking Mill
Tucking Mill
House". Images of England
England
. English Heritage