Stainforth Force, Catrigg Force, Attermire Scar & Warrendale Knotts

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Route: Langcliffe, Stainforth, Pennine Bridleway, Catrigg Force, Winskill Stones, Cowside, Jubilee Cave, Victoria Cave, Brent Scar, Attermire Scar, Warrendale Knotts

Date: 09/09/2018
From: Langcliffe

Parking: Langcliffe
Start Point: Langcliffe
Region: Yorkshire Dales

Route length:  miles (12.2 km)
Time taken: 03:20
Average speed: 2.3 mph
Ascent: 448m
Descent: 446m

Summits: None

Other points of interest: Stainforth Force, Catrigg Force, Winskill Stones, Jubilee Cave, Victoria Cave, Attermire Scar, Warrendale Knotts

The Craven Fault is a series of geological fault lines which run along the southern and western edges of the Yorkshire Dales and includes the North Craven Fault, the Mid Craven Fault and the South Craven Fault. It is a wonderful place to walk and includes many of the Yorkshire Dales' finest features; Malham Cove and Cross Field Knotts to name a couple. Our highlights would be the scars at Attermire and the interesting Warrendale Knotts. Throw in a few waterfalls and caves and you have a classic Dales day out.

We started from Langcliffe, a small village that sits on the border of the National Park. We joined the Ribble Way, another long-distance route along the length of the River Ribble, making our way along the river banks towards Stainforth. I must admit that this leg of the walk is fairly uninteresting though it takes you close to the immense Stainforth Scar. There was also Stainforth Force to look forward to.

Langcliffe Mill

The River Ribble

Weir on the River Ribble

The Ribble Way

Stainforth Force is a fine waterfall, very close to the village of Stainforth (which should not come as a surprise). It is where the River Ribble tumbles over a series of cascades much like Aysgarth Falls near Hawes. Today it was absolutely roaring and make for quite a sight. Just upstream of the falls is an old packhorse bridge, a single span bridge dating from 1672. On 23rd September 1931, the bridge was transferred into the care of the National Trust.

Stainforth Force

Stainforth Force and the packhorse bridge

The packhorse bridge

Above Stainforth Force

From Stainforth, we took the Pennine Bridleway as it initially climbs steeply out of the village before wending its way across open fields towards Catrigg Force. The Pennine Bridleway is a recent long-distance route designed to complement the famous Pennine Way by allowing horse riders and cyclists to make the 200-mile journey through the Pennine hills.

Stainforth

Stainforth

The Pennine Bridleway

The Pennine Bridleway

You'd be forgiven for walking past Catrigg Force were it not signposted. It's craftily hidden in a deep ravine which makes it all the more spectacular. You can stand right on the precipice of the 6m drop before making your way down into the depths to see the waterfalls full height. After hanging around for lunch, we returned back to the bridleway to continue across Winskill Stones.

The path down to Catrigg Force

Catrigg Force

Catrigg Force

Catrigg Force

Winskill Stones is an area of limestone grassland and limestone pavement, one of Britain’s most threatened habitats. It is a National Nature Reserve overseen by an advisory group that includes representatives from the Yorkshire Dales National Park Authority, the farming community and local residents.

Pen y Ghent makes an appearance

The path at Winskill Stones

Winskill Stones

The weather begins to clear

The path reaches the Langcliffe - Malham road, a superb drive if you're in the area, which we used to make our way to Jubilee Cave on the fringes of Langcliffe Scar. Jubilee Cave is very modest in size though gave us a much-needed respite from the cold wind that was blowing in from the northwest. It is, however, overshadowed by the monstrous Victoria Cave which is hidden up the hillside at Brent Scar.

Brent Scar and Warrendale Knotts

Brent Scar

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If waterfalls and caves weren't enough already, the next part of the walk was equally as impressive; a wander through Brent Scar and Attermire Scar, a ravine that runs out through the exposed limestone and provides an excellent route back towards Settle. Attermire Scar is a high limestone cliff that forms part of the Craven Fault in the hills beyond Settle.

Attermire Scar

Attermire Scar

Attermire Scar

 The path heads into Attermire Scar, a large geological fault that isolates Warrendale Knotts on the opposite side from the rest of the fault. Attermire Scar formed part of a gigantic subterranean cliff face which arose from the sea approximately 200 million years ago.

Warrendale Knotts

Warrendale Knotts

Warrendale Knotts

After rounding the bottom of the scar, a short uphill section leads beneath Warrendale Knotts towards Settle before a swift descent towards the town. Prior to actually reaching Settle, however, another bridleway serves as an easy route back to Langcliffe.

Settle

The Ribble valley

Stainforth Scar

Settle's Waterfalls

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Route: Settle, Pennine Bridleway, Blua Crags, Cow Close, Winskill Stones, Upper Winskill, Catrigg Force, Winskill Stones, Jubilee Cave, Victoria Cave, Brent Scar, Attermire Scar, Attermire Cave, Sugar Loaf Hill, High Hill Lane, Scaleber Force, Upper Settle, Settle

Date: 09/09/2012
From: Settle

Parking: Parking in Settle
Start Point: Settle
Region: Yorkshire Dales

Route length: 8.4 miles (20.1 km)
Time taken: 04:05
Average speed: 2.1 mph
Ascent: 405m
Descent: 407m

Points of interest: Catrigg Force, Jubilee Cave, Victoria Cave, Attermire Scar, Scaleber Force

We chose a truly fabulous day to get out into Yorkshire Dales to investigate some of the waterfalls that can be found near Settle. A glorious late-summers day greeted us as we arrived and parked the car, a real Indian summer sort of day. Settle is nestled just outside the National park, much like Buxton in the Peak District. It stands within the valley of the River Ribble, underneath some impressive limestone formations, namely a great exposed ridge, the Craven Fault, that runs east to Malham Cove. The walk, though a little disjointed, would pass a number of geological features including waterfalls, ravines and caves, a perfect day out for the geographer and walker alike and a great way to see out the summer.

The small town of Settle

The most challenging part of this walk hits you right at the start, a fairly steep climb up Constitution Hill, along the Pennine Bridleway and passing the Castlebergh Plantation. Immediately it became obvious that we had dressed inappropriately from the very start and required a quick de-layering to prevent overheating. The Pennine Bridleway is a relatively new long-distance trail, starting at Middleton-in-Wirksworth in Derbyshire and ending close to Kirkby Stephen. In addition to the 73-mile trail, a couple of additional loops take the total distance to 130 miles. The Pennine Bridleway would take us all the way to our first port of call; Catrigg Force.

The Pennine Bridleway looking towards a distant Ingleborough

Ribblesdale

After the steep climb out of Settle, the Pennine Bridleway is a much more gentle affair, passing beneath Blua Crags (the western extent of the Craven Fault) before a steady climb up to the road that links Langcliffe and Malham. A drive along the road is highly recommended, especially as it gives a fine view of Malham Cove as you descend into the valley.

Rounding Clay Pits Plantation

Unfortunately, reaching the road means that you begin one of two short sections of walk that are actually along the road, so be on the lookout for traffic. The location does, however, provide a fine view northwards into Three Peaks territory; Pen-Y-Ghent is just 7 short kilometres in the distance along the Ribble Valley.

A distant Pen-Y-Ghent

After leaving the road, the track crosses an area called Winskill Stones, a 74-acre area of limestone pavement and discarded erratics (an erratic being a piece of rock that differs from the size and type of rock native to the area in which it rests. They are carried by glacial ice, often over distances of hundreds of kilometres). The largest of the erratics we passed is called Samson's Toe.

Samson’s Toe is approx 2.5m high and it stands upon a series of small limestone stilts that have not eroded away thanks to the protection of their boulder. It is said to be possible to rock the stone on its limestone pivots.

Samson's Toe

Its name is derived from the legend of Samson the giant. According to the story, he lost his footing when jumping across from Langcliffe Scar, breaking off his toe whilst attempting this. In reality, the boulder was deposited in this location during the last Ice-Age by the retreating glaciers moving back to the north. It is suggested that the boulder may have come from as far away as the Lake District, where the Greywacke type of rock the boulder is made from is abundant.

Traffic up ahead

After crossing Winskill Stones and passing the farm at Upper Winskill, we made our way through a cow field (luckily we didn't have a dog with us) before dropping down, off the Pennine Bridleway, into the depths of Catrigg Force. The waterfall is reached by a steep, stepped path the leads down to the plunge pool. Catrigg Force is completely hidden from view to those who do not deliberately seek it out and is one of the few spectacular Dales waterfalls that does not fall directly underground. In addition to being a stunning waterfall, the location was the inspiration for some of Sir Edward Elgar's most famous works including Land of Hope and Glory. Our inspiration at the time was the prospect of a well-earned bite to eat.

Descending the path to Catrigg Force

Catrigg Force lies in a secluded gorge

It is possible to get closer by scrambling over the rocks

The tumbling water of Catrigg Force

Retracing our steps back to the Pennine Bridleway, we rounded the eastern side of Winskill Stones this time, returning to the Langcliffe - Malham road. After travelling south towards Settle a short distance, we took the path that spears off towards Brent and Attermire Scar. Prior to that, though would be Jubilee Cave.

The eastern edge of Winskill Stones

A view back to Ribblesdale

Jubilee Cave

Jubilee Cave is a small limestone cave (unsurprisingly enough) visible and easily accessible from the track that leads towards Attermire Scar. There are actually three entrances to the cave, though the one we had a poke around in is easily the largest and roomiest. Excavations in the cave have revealed Iron Age human remains along with Neolithic, Romano-British and Celtic material.

The view looking out!

If waterfalls and caves weren't enough already, the next part of the walk was equally as impressive; a wander through Brent Scar and Attermire Scar, a ravine that runs out through the exposed limestone and provides an excellent route back towards Settle. Attermire Scar is a high limestone cliff that forms part of the Craven Fault in the hills beyond Settle. The path leads down into Brent Scar before heading into Attermire Scar, a large gash that isolates Warrendale Knotts on the opposite side from the rest of the fault. Attermire Scar formed part of a gigantic subterranean cliff face which arose from the sea approximately 200 million years ago.

Brent Scar

Attermire Scar

Warrendale Knotts

The full spectacle of the Craven Fault; Warrendale Knotts, Attermire Scar and Settle Scar

Leaving Attermire Scar behind, we passed between Sugar Loaf Hill and High Hill on our way down to High Hill Lane, one of the routes leading into Upper Settle. Despite being relatively close to the end of the walk, there was still one treat left in store; Scaleber Force, reached by a short walk along the lane before following a signposted path through a wall stile.

Scaleber Force

Scaleber Force is split into two, the upper and lower falls. The upper falls are perhaps the most exciting, especially when viewed from the path higher up, however, it is well worth a scramble down to the lower falls also to get an up-close look at the rocky terraces. After finally working out how to put my camera in a manual shutter speed setting, it was time to try and take the classic 'water cascading with a slow shutter speed' shots. Here they are:

Scaleber Force

Scaleber Force

Photographic urges appeased, it was time to make our way back to Settle and the waiting car. We'd exhausted the natural features in this area (aside from a few additional caves and an exploration of Warrendale Knotts) so it was time to finally head back down the hill into Upper Settle and eventually Settle proper.

High Hill

One of the many old-fashioned road signs around Settle

A view of Malham Cove on the drive home

Settle lies right in the very heart of some of the most exciting and often overlooked scenery in the Yorkshire Dales (despite the town actually being located just outside the boundary). Where Horton-in-Ribblesdale may take the prize for being the starting point of the Yorkshire Three Peaks and Ingleton cowers in the shadow of the shapely Ingleborough, Settle is spoilt for choice in the sheer number of things that surround it, many in addition to the ones you have just read about. Other routes take in some classic Yorkshire Dales limestone scenery such as Giggleswick Scar and Stainforth Force. This walk alone has waterfalls, caves and ravines to which you can add or remove at your leisure. In short, it's great fun and a great day out.