ニュートンポップルフォード&ハープフォードには必見のスポットがたくさんあります。ハイキング愛好家やサイクリング愛好家の方は、ぜひニュートンポップルフォード&ハープフォードを探索してこのエリアにある20
の隠れたスポットを訪れてみてください。このエリアの必見スポットを確認し、次の冒険に出かける計画を立てましょう。
最終更新日: 9月 12, 2026
ハイライト • トレイル
役立つ情報 は
ハイライト (セグメント) • 自然記念物
役立つ情報 は
今すぐサインアップして、こんな場所を発見しよう
最高のシングルトラック、ピーク、その他のエキサイティングなアウトドアスポットのおすすめを受け取ろう。
ハイライト • サイクリングロード
役立つ情報 は
ハイライト • 展望台
役立つ情報 は
ハイライト • 展望台
役立つ情報 は
無料でサインアップして、さらに多くの観光スポットを発見しましょう ニュートンポップルフォード&ハープフォードでの。
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Look out for an entrance onto a footpath on your right, which follows beside the railway tracks on your left, and the exe estuary on your right. The path is too narrow for cycling but great for walking and running.
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Beautiful walk and perfect opportunity to see wildlife
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great flat path lots of birds to see, sheep cows and fish
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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
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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😀
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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.
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