where does the river weaver start and end
River Weaver The River Weaver is more than 50 miles (80Â km) long. From its source in the hills of west Cheshire just south of Peckforton Castle, and within a few hundred metres of the source of the River Gowy[1] it initially flows in a south-easterly direction towards the border with Shropshire, fed by tributaries some of which rise in north Shropshire. The first of three canal crossings occurs just before the village of Wrenbury, when the Llangollen Canal crosses its course. After flowing through the village, it passes to the west of the Cheshire village of Audlem, where it starts to flow approximately northwards across the Cheshire Plain. Shortly afterwards, the Shropshire Union Canal is carried over it on Moss Hall aqueduct. The first significant town on the river is the market town of Nantwich, where a watermill was a feature from the 13th century; 100m further north, an early 19th-century stone bridge, with a single span, crosses the river.[2] Continuing northwards, it passes under the Middlewich Branch of the Shropshire Union Canal[3] before the village of Church Minshull. The aqueduct carrying the canal was designed by Thomas Telford and was built of brick with stone bands between 1827 and 1833. The river flows through a central arch, and there are flood relief arches on each side of the channel.[4] The two waterways run roughly parallel for several miles. They diverge near Winsford, the current head of navigation,[5] and at Northwich the river turns to flow north-west across north Cheshire.
Farmington River Headwaters for both main branches of the Farmington River, referred to as the East Branch and West Branch, are found in southwestern Massachusetts, though only the West Branch officially begins north of the Connecticut border. The West Branch rises at the outlet of Hayden Pond in Otis, Massachusetts. In 1994, a 14-mile (23Â km) stretch of the branch was designated a National Wild and Scenic River.[5] The East Branch begins in Hartland, Connecticut at the confluence of Pond, Hubbard and Valley Brooks.[1] However, this branch has been impounded along the first 11 miles of its course to form the Barkhamsted Reservoir and Lake McDonough; it does not assume a particularly river-like appearance until it exits Lake McDonough in New Hartford, Connecticut. The East Branch and West Branch join in New Hartford, Connecticut just about one mile south of Lake McDonough. Upper reaches of the river flow mostly southward, but the river turns northward in Farmington, Connecticut and then runs mostly north and east until it flows into the Connecticut River near the Loomis Chaffee School in Windsor, Connecticut.