Keld Scar

Waterfall in Yorkshire Richmondshire

England

Keld Scar

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. — Path down to Semer Water Credit: Marathon

Keld Scar is a stunning waterfall located in the Yorkshire Dales, England. Situated near the village of Keld, it is a popular tourist attraction due to its natural beauty and accessibility. The waterfall is formed by the Keld Beck, a small river flowing through the picturesque Swaledale valley.

Keld Scar waterfall is approximately 80 feet high and cascades down a series of limestone steps, creating a mesmerizing sight for visitors. The water flows gracefully over the rocks, creating a soothing sound that adds to the tranquility of the surroundings. The lush greenery and the rugged landscape of the Yorkshire Dales provide a breathtaking backdrop for the waterfall.

Visitors can reach Keld Scar by following a well-maintained footpath that leads directly to the waterfall. The path offers stunning views of the surrounding countryside, including meadows, dry-stone walls, and traditional farmhouses. Along the way, nature enthusiasts can also spot various species of birds and wildflowers, adding to the charm of the experience.

The area around Keld Scar is a haven for hikers and nature lovers, with several walking trails and footpaths that allow visitors to explore the stunning Yorkshire Dales National Park. The waterfall is also a popular spot for picnics and photography, with many visitors capturing the beauty of the cascading water against the rugged cliffs.

Overall, Keld Scar waterfall is a must-visit destination for those seeking natural beauty and tranquility. Its picturesque setting, accessibility, and the surrounding Yorkshire Dales make it a perfect spot for a day trip or a longer exploration of the area.

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Keld Scar Images

Images are sourced within 2km of 54.269818/-2.1298967 or Grid Reference SD9186. Thanks to Geograph Open Source API. All images are credited.

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.

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.

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.

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.

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.

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.

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.

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.

Marsett Lane This is just outside the hamlet of Marsett on the way to Countersett. The hill in the distance is Addlebrough.

Marsett Lane

This is just outside the hamlet of Marsett on the way to Countersett. The hill in the distance is Addlebrough.

Footbridge over Cragdale Water The footpath between Stalling Busk and Marsett is wet at the best of times. Cragdale water and then Raydale Beck are crossed by footbridges. This is the first one.

Footbridge over Cragdale Water

The footpath between Stalling Busk and Marsett is wet at the best of times. Cragdale water and then Raydale Beck are crossed by footbridges. This is the first one.

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

A barn in Raydale

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

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.

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.

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.

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.

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.

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.

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.

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.

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.

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.

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.

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.

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.

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.

Old barn seen from Marsett Lane The barns in the Yorkshire Dales are in varying stages of dilapidation. This one seems quite good and it appears to have a new roof. The hill in the distance on the left is Addlebrough.

Old barn seen from Marsett Lane

The barns in the Yorkshire Dales are in varying stages of dilapidation. This one seems quite good and it appears to have a new roof. The hill in the distance on the left is Addlebrough.

Marsett Beck This looks downstream from Marsett Bridge. Marsett Beck flows into Crooks Beck a short distance ahead which in turn flows into Semer Water.

Marsett Beck

This looks downstream from Marsett Bridge. Marsett Beck flows into Crooks Beck a short distance ahead which in turn flows into Semer Water.

Track between two streams The track has just crossed Raydale Beck and is heading to the footbridge over Cragdale Water.

Track between two streams

The track has just crossed Raydale Beck and is heading to the footbridge over Cragdale Water.

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.

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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Keld Scar is located at Grid Ref: SD9186 (Lat: 54.269818, Lng: -2.1298967)

Division: North Riding

Administrative County: North Yorkshire

District: Richmondshire

Police Authority: North Yorkshire

What 3 Words

///twin.scooters.rally. Near Leyburn, North Yorkshire

Nearby Locations

Keld Scar Raydale

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Nearby Amenities

Located within 500m of 54.269818,-2.1298967

Stalling Busk

Place: hamlet

Source: NPE

Wikidata: Q7597311

Wikipedia: en:Stalling Busk

Lat/Long: 54.2682085/-2.1298666

Natural: spring

Source: OS_OpenData_Streetview

Lat/Long: 54.2664177/-2.1264367

Natural: spring

Source: OS_OpenData_Streetview

Lat/Long: 54.2716837/-2.1329598

Natural: spring

Source: OS_OpenData_Streetview

Lat/Long: 54.2718975/-2.1282458

Old Church

Historic: ruins

Lat/Long: 54.2724851/-2.13027

Telephone

Booth: KX100

Covered: booth

Operator: BT

Payment Coins: no

Phone: +44 1969 650254

Lat/Long: 54.2685198/-2.1302026

Post Box

Collection Times: Mo-Fr 09:00; Sa 07:00

Operator: Royal Mail

Operator Wikidata: Q638098

Post Box Mounting: stone_wall

Post Box Type: wall

Ref: DL8 80

Royal Cypher: GR

Royal Cypher Wikidata: Q33102273

Lat/Long: 54.268345/-2.1302321

Bench

Lat/Long: 54.2686231/-2.1307676

Power: pole

Lat/Long: 54.2682304/-2.1311037

Power: pole

Lat/Long: 54.2678494/-2.1328527

Power: pole

Lat/Long: 54.2675431/-2.1342504

Power: pole

Lat/Long: 54.2679783/-2.1348577

Power: pole

Lat/Long: 54.2686407/-2.1358564

Power: pole

Lat/Long: 54.2690334/-2.136436

Power: pole

Lat/Long: 54.2697925/-2.1375502

The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

Crag Scar Force Yorkshire

Harthope Linn Northumberland

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