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View of Howgill Fells looking west from Sedgwick Trail car park |
Examining junction between Tom Croft Limestone to the left and Ashell Sandstone to the right, both dippng upstream to the right. |
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Anticline in the Danny Bridge Limestone. |
Siphonodendron sp. (colonial rugose corals) in Tom Croft Limestone. |
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Chert nodules.Chert is a type of cryptocrystaline quartz |
The Dent Fault, or one of its subsidiaries. Steeply dipping Carboniferous limestone to the left and Silurian Brathay Flags to the right. |
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Above the Brathay Flags is a conglomerate containing Silurian clasts. Devonian or Basal Carboniferous? |
Another exposure of the conglomerate. Leader, Dr. John Knight in centre |
