Thames Head

EN Texto en inglés Aún no hay artículo en tu idioma: extracto en inglés.

Thames Head is a group of seasonal springs that arise in the Cotswolds, in the county of Gloucestershire, England. Their location is in fields near the villages of Coates and Kemble, on either side of the A433 road, about three miles south-west of the town of Cirencester. The spring water comes from the limestone aquifers of the Cotswolds. One or more of these springs are traditionally identified as the source of the River Thames. In actuality, the source of the River Thames does not have a fixed location – rather, it changes according to the level of the groundwater in the limestone. In dry periods, the groundwater level falls, causing the Thames Head springs to dry up and the river to begin lower down in its course. In wet conditions, the groundwaters rise and the river can begin at one of the Thames Head springs. The spring known as Lyd Well, located south of the A433 (grid reference ST989984), is often where the river starts. In 2011, the lowest recorded start of the Thames was just upstream of Ashton Keynes, which is over six miles (ten kilometres) downstream from Thames Head. During the 2022 United Kingdom heat wave, the source dried up completely, shifting five miles (eight kilometres) downstream to Somerford Keynes. The highest springs of Thames Head are located north of the A433 road (Fosse Way section), in a meadow called Trewsbury Mead. One of these springs is marked with an inscribed stone marker, located 360 feet (110 m) above sea level at grid reference ST980994. Below it, the springhead itself is in a hollow that has been lined with stones. The springs continue immediately south of the A433. The Ordnance Survey identifies Thames Head as the source of the Thames on its maps and the UK's Environment Agency...