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Geology of the Yorkshire Dales
Sat. June 25th 2016 Dr Liam Herringshaw
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Today's timetable 10 – 11 Introduction & Early Palaeozoic
11 – Tea break Early Carboniferous 12.20 – Lunch break Late Carboniferous 2.00 – Tea break The Ice Ages 3.20 Discussion
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Yorkshire Dales geology
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Sedimentary Dales
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Time in the Dales (1) Geogeek 1726
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Time in the Dales (2) geolsoc. org.uk
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Why the Dales are there
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Buoyant granite The Askrigg Block
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Yorkshire's oldest rocks
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Yorkshire's oldest rocks
Thornton Force: Carboniferous rocks overlying metamorphosed Ingleton Group
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The Ingleton Group Intensely folded, deep marine, sedimentary rocks
Pecca Quarry, photograph © Ashley Dace
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Not fossiliferous Very rare microfossils found
Pecca Quarry, photograph © Ashley Dace
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Above the Ingleton, the Lakes
Windermere Supergroup (Ordovician-Silurian turbidites): Horton Formation (Silurian), Dry Rigg Quarry, nr Helwith Bridge. Photograph © Karl and Ali
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Turbidites Subaqueous sediment gravity flows
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Also fossil-poor Occasional shell debris found
Photograph © Karl and Ali
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The Devonian is missing
Combs Quarry, Ribblesdale: Unconformity between Silurian and Carboniferous rocks
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Why? Late Caledonian-Variscan orogeny
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