Malhamdale
Drystone walling
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Towards Bempton cliffs
Filey Brigg
Sunny Autumnal Day
Dry Stone walling
Sun and shade
2019, a beautiful finish to the year
Sunshine on Yorkshire
Viaduct over the River Nidd
A view from Knaresborough Castle
The pulpit
Organ from the front
Magnificent Organ
Ripon Cathederal
Canalside scene
Overflow
HFF at Fewston reservoir
It's downhill from here!
High above Grassington
Isolated farmhouse
A beautiful January day in Knaresborough
View from the Castle
Castle remains
Knaresborough viaduct
Viaduct and train
River Nidd and Castle
Knaresborough viaduct
River Nidd reflections
Boulder clay
Dumped old rope
Beach debris
Splish splash
Uprooted tree trunk sunbathing!
Gannets pairing up and preening
A Gannet shadow
Perched on the edge
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Malham Cove
The 70 metre (230ft) high, gently curving cliff of white limestone has amazed visitors for centuries. Formed along the line of the Middle Craven Fault, it has been eroded backwards from the line of the fault by the action of water and ice over millions of years.
Over the last one and a half million years, Malham was probably covered at least three times with huge sheets of ice. As these glaciers ground their way over the landscape they plucked rock from the face of the Cove and carried it away. Each time the glaciers melted, huge floods of water further eroded the face of the Cove.
The water flows underground now, but then, the ground was permanently frozen and so the glacial meltwater had to run over the top. The result was that a massive waterfall once thundered over the Cove.
The cave systems usually carry away any water before they reach the fall; however, Malham Cove temporarily became a waterfall for what is believed to be the first time in centuries on 6 December 2015, after heavy rainfall from Storm Desmond.
Today, the sheer rock face of Malham Cove challenges climbers and also protects a pair of nesting peregrine falcons which can be viewed during the summer months diving and wheeling alongside the house martins and jackdaws that also call the Cove home.
Best in black
Over the last one and a half million years, Malham was probably covered at least three times with huge sheets of ice. As these glaciers ground their way over the landscape they plucked rock from the face of the Cove and carried it away. Each time the glaciers melted, huge floods of water further eroded the face of the Cove.
The water flows underground now, but then, the ground was permanently frozen and so the glacial meltwater had to run over the top. The result was that a massive waterfall once thundered over the Cove.
The cave systems usually carry away any water before they reach the fall; however, Malham Cove temporarily became a waterfall for what is believed to be the first time in centuries on 6 December 2015, after heavy rainfall from Storm Desmond.
Today, the sheer rock face of Malham Cove challenges climbers and also protects a pair of nesting peregrine falcons which can be viewed during the summer months diving and wheeling alongside the house martins and jackdaws that also call the Cove home.
Best in black
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