Blean High Pasture

Downs, Moorland in Yorkshire Richmondshire

England

Blean High Pasture

Higher than Addlebrough The top of Stake Road is higher than the more dramatic Addlebrough. — Higher than Addlebrough Credit: T Eyre

Blean High Pasture is a vast expanse of land situated in the beautiful county of Yorkshire, England. Nestled amidst the picturesque surroundings of the Yorkshire Downs and Moorland, it covers a substantial area of approximately 2,000 acres. This expansive pasture is known for its diverse ecological and archaeological significance.

As an area of outstanding natural beauty, Blean High Pasture boasts a rich biodiversity. The land is home to a variety of plant and animal species, including heather, bilberry, curlew, and skylark. The undulating moorland terrain, punctuated by small streams and tarns, adds to the scenic charm of the area.

Apart from its natural beauty, Blean High Pasture holds great archaeological importance. The site is dotted with numerous ancient monuments, including burial mounds, stone circles, and cairns. These remnants of the past provide valuable insights into the region's history and cultural heritage, with some dating back to the Neolithic era.

The land is also known for its extensive network of footpaths and trails, making it a popular destination for hikers, nature enthusiasts, and history buffs alike. Visitors can enjoy long walks, observing the wildlife and admiring the breathtaking vistas of the Yorkshire countryside.

Blean High Pasture is a protected site, managed by conservation organizations and local authorities. Efforts are made to preserve the natural habitat and maintain the historical integrity of the area. As a result, it offers a unique and serene experience for those seeking to immerse themselves in the beauty of Yorkshire's Downs and Moorland.

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Blean High Pasture Images

Images are sourced within 2km of 54.271852/-2.1089122 or Grid Reference SD9386. Thanks to Geograph Open Source API. All images are credited.

Higher than Addlebrough

The top of Stake Road is higher than the more dramatic Addlebrough.

T Eyre

Busk Lane

Busk Lane descending towards Carpley Green.

T Eyre

Carpley Green & Addlebrough

Looking north down Busk Lane towards Carpley Green with Addlebrough behind.

T Eyre

Addlebrough

Looking towards Addlebrough from Carpley Green Road.

T Eyre

Path down to Semer Water

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. This is the footpath back down to Semer Water in evening sunlight.

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Semer Water at sunset

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. Legend has it that there is a drowned village under the water.

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View from a footpath above Semer Water

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. Legend has it that there is a drowned village under the water. The hill in the distance is Addlebrough.

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Semer Water

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. Legend has it that there is a drowned village under the water. The River Bain, which flows out of Semer Water, at two and half miles is the shortest river in England.

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A barn in Raydale

This view is from a meeting of footpaths downhill from Stelling Busk on the way to Cragdale Water.

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The head of Semer Water at sunset

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. This is the view from the footpath looking back to the head of Semer Water at sunset.

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Erratic at Semer Water

Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley and leaving erratic boulders like this one behind. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep.

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Semer Water Bridge

The River Bain flows from Semer Water under the bridge here. As a tributary of the River Ure, it is one of the shortest, named rivers in England.

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Part of Semer water

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. This is Semer Water in Wensleydale. It was clearly fuller than normal making this look like a mangrove swamp. Legend has it that there is a drowned village under the water.

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Semer Water

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Semer Water

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Semer Water seen from Marsett Lane

There are only two lakes in the Yorkshire Dales, Malham Tarn and Semer Water. Semer Water was formed during the last Ice Age by a moraine which effectively dammed the valley. The lake today is a shadow of its former self but is still three miles in circumference and 45 feet deep. Legend has it that there is a drowned village under the water.

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Isolated barn in a field

The barns in the Yorkshire Dales are in varying stages of dilapidation. This one seems in quite good condition and it appears to have a decent roof. This view is from the footpath which leads from Busk Lane towards Semer Water.

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