Picture Gallery 3: Wharfedale views |
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The
pages below are under development and will
be updated on a regular basis. |
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![]() Cowside: one of Wharfedale's oldest farmsteads. February 24, 2008. |
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![]() Landslip at Raisgill: great masses of unstable glacial drift higher up the fellside slip down over the limestone terraces as an inhomogenous slurry when they become destabilised after prolonged rainfall. |
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![]() "Rolling Stones" Weathering of the exposed terraces high above the road breaks up the limestone into these unstable boulders. |
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![]() In flood conditions, the water-logged fellside is drained by numerous bedding-plane resurgences along the level of the Porcellanous Band near Starbotton. |
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![]() Foss Gill Cave is a resurgence for Foss Gill Pot and other sinks on the fell above. The strong band of limestone across the centre of the picture is a one metre thick bed of porcellanous limestone underlain by an uncertain thickness of less competent black shaly limestone. Circled is a fallen block of porcellanous limestone. |
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![]() Looking down Upper Wharfedale from Slades Pasture, Cray. A classical U-shaped valley resulting from the movement of a glacier down the valley towards the end of the last ice-age. Buckden to the left is built on an outwash fan from Buckden Gill. Redmire Farm to the right is built on a mound of glacial moraine stretching out into the flat valley floor, the remant of a glacial lake. In the left foreground Cray Gill winds away through heaps of glacial drift whilst in the right foreground a small stream has emerged from under the limestone beds to meander across the low-lying hay meadows. |
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![]() A view from above Kettlewell looks over the village and a glacial lake flat towards the limestones slopes of Knipe Scar quite typical of the Dales landscapes. |
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![]() Wharfedale from Earl Seat. The hamlet of Drebley to the left, Appletreewick to the right. |
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![]() Ancient field patterns around Thorpe. |
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Any
shortcomings in the text are entirely my
own. Steve Warren |
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Website
created by WarrenAssociates 2012 |
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