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The coarse sand bed also pinches out in between the stretch marked by VES-13 and VES-14, revealing that the older course of Sone river is controlled by the tectonic activity of the region (Sahu et al. 2010) and further south from VES-13 older alluvium of Pleistocene age is exposed.
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The old course of the Don gradually silted up.
This is the old course of the river, which rejoins the canal below Cobblers lock.
At Outwell the Well Creek is also joined by the old course of the River Nene.
At the confluence of the Mersey and Irwell near Irlam, the canal follows the old course of the River Irwell into Manchester.
It provided a link from Bramwith lock to the River Trent, broadly following the old course of the River Don prior to Vermuyden's improvements.
From here the route is along the old course of the River Nene, passing through the twin villages of Outwell and Upwell, where the abandoned Wisbech Canal once formed a route back to the new course of the River Nene.
In addition to these new channels, the Middle Level also contained 26 mile of the old course of the Nene, and the ancient artificial waterways of King's Dyke and Whittlesey Dyke, which connect Stanground to Floods Ferry.
Glastonbury Lake Village was an Iron Age village, close to the old course of the River Brue and Sharpham Park approximately 2 mile west of Glastonbury, that dates back to the Bronze Age.
In January 1764 one barge experimentally carried one load of coal from the Thames at Oxford up the River Cherwell to Islip and thence up the old course of the River Ray to Arncott.
Glastonbury Lake Village was an Iron Age village, close to the old course of the River Brue, on the Somerset Levels near Godney, some 3 mile north west of Glastonbury.
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