Water mills Leats generally start some distance (a few hundred metres/yards, or perhaps several miles/kilometres) above the mill or other destination, where an
offtake or
sluice gate diverts a proportion of the water from a
river or
stream. A
weir in the source stream often serves to provide a reservoir of water adequate for diversion. The leat then runs along the edge or side of the valley, at a shallower slope than the main stream. The gradient, together with the quality of the wetted surface of the leat, determines the
flow rate. The flow rate may be calculated using the
Manning formula. By the time it arrives at the
water mill the difference in levels between the leat and the main stream is great enough to provide a useful
head of water – several metres (perhaps 5 to 15 feet) for a watermill, or a metre or less (perhaps one to four feet) for the controlled irrigation of a
water-meadow.
Water supply Leats are used to increase the yield of a reservoir by trapping streams in nearby catchments by means of a contour leat. This captures part or all of the stream flow and transports it along the contour to the reservoir. Such leats are common around reservoirs in the uplands of Wales.
Mining Leats were built to work
lead,
tin and
silver ores in mining areas of Wales,
Cornwall,
Devon, the
Pennines and the
Leadhills/
Wanlockhead area of Southern Scotland from the 17th century onwards. They were used to supply water for
hushing mineral deposits, washing ore and powering mills. ==Use in Roman times==