ブランスクーム周辺のアトラクション＆必見スポット - トップ20

Harnessing the power of moving water to drive a mill wheel is an ancient invention of human ingenuity, whose origins can be traced back to ancient times. Thanks to such a design, a watercourse – natural or artificial – made it possible to simply replace human or animal muscle power with the power of natural elements, for example, to grind grain into corn or press oil from fruit. There are essentially two drive variants for watermills: * Either the flowing water simply hits the blades of the water wheel from below to set it in motion; or * the water is guided above the wheel – usually through a so-called "mill channel" – and falls onto the blades. This design utilizes natural gravity to achieve greater efficiency.

Perfect day trip for wild life spotting

this road becomes flooded would avoid when on yellow 🟡 weather warning cause you might need a boat, but otherwise it's very pretty and worth a visit great pubs for food nearby and air BnB places

great flat path lots of birds to see, sheep cows and fish

The paths where really good not to muddy, a few puddles which you can walk around however on the road was a big stream and got a little dirty lucky my walking boots are waterproof no to many hills, and a very nice farm shop with a catering van, the bakery sells the best pasties. You won't be disappointed

From the car park on Budleigh Salterton, walk beside the river Otter and experience the wonder of the Wetlands, and marvel at the visiting and nesting birds😀

Quite the section this. Has a little bit of everything.

Ladram Bay is a secluded bay with a pebble beach. Among the most impressive sights along the Jurassic Coast are the sea stacks at Ladram Bay. The sandstones contain many vertical fractures and joints that were formed deep in the Earth's crust during past mountain building periods. The sea picked out these planes of weakness to form caves and natural arches that have since collapsed to produce sea stacks. The “Otter Sandstone” that forms the cliffs and sea stacks were deposited in a hot dry climates in the Triassic Period, about 220 million years ago. The stacks are composed of the same rock, which is relatively soft, but they have a harder band of sandstone at their base which prevents their rapid erosion by the sea. The striking red colour of the rock is caused by iron oxide, which indicate that the layers were formed in a desert. The presence of ripple marks and channels in the sandstones, together with the remains of the long-extinct plants, insects, fish, amphibians and reptiles, show that the desert was crossed by fertile river valleys.