20의 링턴가지 명소 & 주요 장소

The concrete outlet tower serves as the central control point for the reservoir's water supply. Connected by a bridge to the main dam, the tower houses sluice gates and valves that regulate the flow and distribution of water to the River Chew and the local water supply.

Chew Valley Lake is the 5th largest artificial lake in the UK. It was constructed in the 1950s to supply drinking water for Bristol and the nearby area. There are brilliant views of the lake and surrounding countryside as you pass along the dam.

Chew Valley Lake formed by the construction of this dam on the River Chew in the 1950's. Built to provide drinking water for Bristol.

Nice traffic free route with lots of places to stop for refreshments along the way. Recommend the bakery at Winscombe. Sadly, the numerous bike gates along the route are a pain if you're on a mountain/hybrid bike as they are too narrow.

Black Down Hill or Beacons Batch is the highest hill in the Mendip Hills at 325m, Somerset, in south-western England. Black Down lies just a few miles eastward of the Bristol Channel at Weston-super-Mare, and provides a view over the Chew Valley. It has a trig pointed summit and is a UK designated Marilyn with a prominence of over 150m.

The Strawberry Line is a traffic-free trail between Yatton and Cheddar. The gravel path follows the route of a former railway line that once carried delicious cargos of strawberries from Cheddar. The line was well usd for nearly a century until its closure in 1965. Level and easygoing, the trail is suitable for all ages and abilities. It winds through some very pretty Somerset countryside, too.

Fabulous gravel track. As long as you're not too precious about getting grit and dirt on your bike, it's possible on any bike... smoother than most roads!

This special site is designated as a Site of Special Scientific interest for its valuable wildlife habitats and is a nationally important site for its archaeology from the late Stone Age and Bronze Age through to the Second World War. Black Down provides the largest area of open access on the Mendip Hills at over 400 ha. Black Down, like most heathlands, is formed through a combination of factors– soil type, rainfall and human activity. The underlying Old Red Sandstone rock together with high rainfall created a waterlogged and acidic soil. The removal of tree cover by our Bronze Age ancestors 2,000 years ago helped to make sure that the soil stayed damp and acid. Only certain plants can survive in this type of ground. The key species include heather or ling, bell heather, bilberry, purple moor grass and European gorse, along with mosses and lichens. Now the bracken is managed by harvesting and grazing by cattle and wild ponies to allow the heathers and grasses to flourish again. Black Down supports a wide variety of birds, mammals, reptiles and invertebrates.