Yorkshire Dales Photography: Photos of Horton in Ribblesdale, Pen-y-ghent and Selside in the Yorkshire Dales National Park.
RELATED PAGES: Horton Walk - Selside Walk - Ribblehead Photos - Malham Photos.
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HORTON IN RIBBLESDALE 01A - St Oswald's Church
St. Oswald's Church, Horton in Ribblesdale, North Yorkshire.
St. Oswald's has an early 12th century nave. The rest of the church dates back to the 15th century with 19th and 20th century alterations. Norman church.
Grade 1 listed.
St. Oswald's has an early 12th century nave. The rest of the church dates back to the 15th century with 19th and 20th century alterations. Norman church.
Grade 1 listed.
HORTON IN RIBBLESDALE 03A - Pen-y-ghent Cafe
Pen-y-Ghent Cafe, Horton in Ribblesdale, North Yorkshire.
Walkers 'clock in' at the cafe before attempting the Three Peaks Challenge - a gruelling 39km (24.5 mile) trek with a climb of around 1,600m (5,000 ft), taking in the three highest peaks of the Dales: Whernside, Ingleborough and Penyghent. If walkers clock back at the café within twelve hours they get a certificate and are entitled to wear the badge and tie of the Three Peaks of Yorkshire Club.
Walkers 'clock in' at the cafe before attempting the Three Peaks Challenge - a gruelling 39km (24.5 mile) trek with a climb of around 1,600m (5,000 ft), taking in the three highest peaks of the Dales: Whernside, Ingleborough and Penyghent. If walkers clock back at the café within twelve hours they get a certificate and are entitled to wear the badge and tie of the Three Peaks of Yorkshire Club.
HORTON IN RIBBLESDALE 04B - Railway Station
Horton in Ribblesdale Railway Station, North Yorkshire.
Pen-y-ghent can be seen in the distance.
Pen-y-ghent can be seen in the distance.
HORTON IN RIBBLESDALE 09A - New Inn Bridge
New Inn Bridge, Horton in Ribblesdale, North Yorkshire.
A late 18th century bridge spanning the River Ribble. Grade 11 listed.
A late 18th century bridge spanning the River Ribble. Grade 11 listed.
PEN-Y-GHENT 02A - Pen-y-ghent
A cloud-topped Pen-y-ghent near Horton in Ribblesdale, in the Yorkshire Dales.
PEN-Y-GHENT 25A - Hull Pot
A man walks beside Hull Pot on the slopes of Pen-y-ghent, Horton in Ribblesdale, North Yorkshire.
At a length of 91m and depth at waterfall of 18m, Hull Pot is the largest natural hole in the UK. Usually Hull Pot Beck has disappeared underground before it reaches the hole, but after heavy rain there may be a spectacular waterfall.
At a length of 91m and depth at waterfall of 18m, Hull Pot is the largest natural hole in the UK. Usually Hull Pot Beck has disappeared underground before it reaches the hole, but after heavy rain there may be a spectacular waterfall.
PEN-Y-GHENT 25B - Hull Pot
Hull Pot on the slopes of Pen-y-ghent, Horton in Ribblesdale, North Yorkshire.
PEN-Y-GHENT 27A - Hunt Pot
Hunt Pot on the slopes of Pen-y-ghent, Horton in Ribblesdale, North Yorkshire.
The well used description, ‘a sinister slit in the earth’s crust’ really sums up Hunt Pot. This 64m deep hole was caused by faulting and water action. It was first descended in 1898 by the Yorkshire Ramblers’ Club.
The well used description, ‘a sinister slit in the earth’s crust’ really sums up Hunt Pot. This 64m deep hole was caused by faulting and water action. It was first descended in 1898 by the Yorkshire Ramblers’ Club.
PEN-Y-GHENT 25B - Hunt Pot
Hunt Pot on the slopes of Pen-y-ghent, Horton in Ribblesdale, North Yorkshire.
PEN-Y-GHENT 29A - Churn Milk Hole
Churn Milk Hole, Penyghent, Horton oin Ribblesdale, North Yorkshire.
Churn Milk Hole on the lower slopes of Penyghent is a large shake hole (circular depression, formed when underlying limestone collapses into a cavity in the rock or even into an underground chamber). Water running into a shake hole will eventually further erode the rock to create an opening or pothole. Churn Milk Hole lies where the Great Scar Limestone meets the Yoredale Strata. Fountains Fell can be seen in the distance.
Churn Milk Hole on the lower slopes of Penyghent is a large shake hole (circular depression, formed when underlying limestone collapses into a cavity in the rock or even into an underground chamber). Water running into a shake hole will eventually further erode the rock to create an opening or pothole. Churn Milk Hole lies where the Great Scar Limestone meets the Yoredale Strata. Fountains Fell can be seen in the distance.
HORTON IN RIBBLESDALE 30A - A view of Ingleborough from Pen-y-ghent
A view of Horton Quarry and Ingleborough from the slopes of Penyghent, Horton in Ribblesdale, North Yorkshire.
HORTON IN RIBBLESDALE 34A - Horton Scar Waterfall
Waterfall at Horton Scar, Horton-in-Ribblesdale, North Yorkshire.
HORTON IN RIBBLESDALE 35A - Horton Scar Lane
Horton Scar Lane, Horton in Ribblesdale, North Yorkshire.
THIEVES MOSS 01A - Thieves Moss and Moughton Scars
The limestone amphitheatre of Thieves Moss and Moughton Scars at the head of Crummackdale in the Yorkshire Dales,
A snow-covered Pen-y-ghent can be seen in the distance.
A snow-covered Pen-y-ghent can be seen in the distance.
SULBER NICK 01A - Simon Fell and Inglegrough
Simon Fell and Ingleborough from Sulber Nick near Horton in Ribblesdale, North Yorkshire.
HORTON IN RIBBLESDALE 56A - Pen-y-ghent from Sulber Nick
Pen-y-ghent from Sulber Nick, Horton in Ribblesdale, North Yorkshire.
PEN-Y-GHENT 01A - Pen-y-ghent
Penyghent near Horton in Ribblesdale in the Yorkshire Dales.
Largely composed of Great Scar Limestone, Penyghent was formed about 330 million years ago when the area lay beneath a warm shallow sea. The limestone was deposited in layers as tiny sea creatures died and became compacted on the sea bed. Over millions of years other deposits created the later Yoredale Strata of alternating layers of limestone, sandstones and shales above the Great Scar Limestone. The summit rock of Penyghent is Millstone Grit (interbedded coarse sandstone and shale). There is black shale in the path near the summit..
Largely composed of Great Scar Limestone, Penyghent was formed about 330 million years ago when the area lay beneath a warm shallow sea. The limestone was deposited in layers as tiny sea creatures died and became compacted on the sea bed. Over millions of years other deposits created the later Yoredale Strata of alternating layers of limestone, sandstones and shales above the Great Scar Limestone. The summit rock of Penyghent is Millstone Grit (interbedded coarse sandstone and shale). There is black shale in the path near the summit..
PEN-Y-GHENT 01A - Pen-y-ghent summit
Pen-y-ghent summit, Horton in Ribblesdale, North Yorkshire.
The trig point is 694 metres or 2,277 feet above sea level.
The trig point is 694 metres or 2,277 feet above sea level.
PEN-Y-GHENT 05A - Ascent of Pen-y-ghent
A walker on the ascent of Penyghent, Horton in Ribblesdale in the Yorkshire Dales.
PEN-Y-GHENT 10A - Pen-y-ghent Pinnacle
The Pen-y-ghent Pinnacle on Pen-y-ghent Side, Horton in Ribblesdale, North Yorkshire.
PEN-Y-GHENT 11A - Pen-y-ghent Side
Pen-y-ghent Side on the western flanks of Pen-y-ghent near Horton in Ribblesdale in the Yorkshire Dales.
PEN-Y-GHENT 12A - Walker on Pen-y-ghent Side
Female walker with dogs on the slopes of Pen-y-ghent in the Yorkshire Dales.
PEN-Y-GHENT 12B - Walker on Pen-y-ghent Side
Female walker with dogs on the slopes of Pen-y-ghent in the Yorkshire Dales.
PEN-Y-GHENT 20A - Millstone Grit on Pen-y-ghent
Millstone Grit (interbedded coarse sandstone and shale) lies above the Great Scar Limestone towards the summit of Pen-y-ghent in the Yorkshire Dales National Park, North Yorkshire.
SELSIDE 10A - Pen-y-ghent from Alum Pot
A view of Pen-y-ghent from Alum Pot above the hamlet of Selside, near Horton in Ribblesdale, North Yorkshire.
SELSIDE 12A - Diccan Pot
Diccan Pot, Selside near Horton in Ribblesdale, North Yorkshire.
Diccan Pot connects with Alum Pot and Long Churn Caves to form a significant and intricate cave system.
Diccan Pot connects with Alum Pot and Long Churn Caves to form a significant and intricate cave system.
SELSIDE 13A - Entrance to Long Churn Caves
The entrance to Long Churn Caves which link with Diccan Pot and the mighty Alum Pot (hidden in the clump of trees) near Selside in the Yorkshire Dales, North Yorkshire.
Pen-y-ghent can be seen in the distance.
Pen-y-ghent can be seen in the distance.
SELSIDE 14A - Lower Long Churn Cave
A caver emerges from Wilson’s Hole in Lower Long Churn Cave, Selside near Horton in Ribblesdale, North Yorkshire.
SELSIDE 20A - Limestone pavement and Pen-y-ghent
A snow-covered Pen-y-ghent from the limestone pavement above Alum Pot on the eastern flanks of Simon Fell, Selside, Horton in Ribblesdale, North Yorkshire.
SELSIDE 23A - Limestone pavement
Limestone pavement above the hamlet of Selside near Horton in Ribblesdale, North Yorkshire.
Simon Fell can be seen in the distance.
Simon Fell can be seen in the distance.
SELSIDE 24A - Rillen karren in the limestone pavement
Park Fell from the limestone pavement above Selside, near Horton in Ribblesdale, North Yorkshire.
The clints (blocks of limestone) on the pavement above Alum Pot are good examples of 'rillen karren' (shallow channels eroded by the flow of running water)..
The clints (blocks of limestone) on the pavement above Alum Pot are good examples of 'rillen karren' (shallow channels eroded by the flow of running water)..
SWALEDALE 11A - Swaledale sheep, Selside
Swaledale sheep at Selside near Horton in Ribblesdale, North Yorkshire.
Park Fell can be seen in the distance.
Park Fell can be seen in the distance.
