Thrang Quarry 26 Jun 2010
Thrang Quarry old level 1
Thrang Quarry old level 2
Thrang Quarry old level 3
Great Langdale golden light
Golden evening in Chapel Stile
Sunset over the Langdale Pikes
Langdale Pikes sunset
Great Langdale afternoon light
Side Pike 1
Side Pike 2
Coming through...
Side Pike slab squeeze
Side Pike summit cairn 1187 ft
Wha House, Eskdale
Brotherikeld, Upper Eskdale
Wallhead Crag, Harter Fell
On the way up Harter Fell
Scafells from Harter Fell
West from Harter Fell main summit, 2140 ft
Loughrigg Fell summit, 1101 ft
Grasmere
Old Dungeon Ghyll Hotel in the spotlight
Concretionary tuff on Pavey Ark
Pavey Ark - very strange rocks
Chavery Coal and roof strata, Duckmanton Railway C…
Chavery Coal and roof measures, Duckmanton Railway…
Duckmanton Railway Cutting SSSI (2)
Duckmanton Railway Cutting SSSI
Snowy beeches - extraordinary light
Snowy blue and gold
In among the snowy beeches
Looking up at the snowy beeches
Descent into the snowy beeches
Snow field at the edge
Snowy cold and gold
Snowy gateway to heaven
Snowy Limb Brook 2
Snowy branches
Snowy Limb Brook 1
Snowy handfasting ground
Solstice 2009
Wide open
Northcott Mouth anticline - detail
Northcott Mouth anticline 1
1/200 • f/5.6 • 20.0 mm • ISO 100 •
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Violent Vulcanism in England - the Pavey Ark Breccia


Near the summit of Pavey Ark, Lake District National Park, England.
The rocks in this photo belong to the Pavey Ark Member (formerly the 'Pavey Ark Breccia') in the Borrowdale Volcanic Group (Ordovician). This is a very coarse tuff with many angular rock fragments, volcanic bombs and andesite lava spatter, possibly resulting from a pyroclastic flow settling into water; the whole lot subsequently disrupted by slumping and mass movement (Millward et al, 2000). This is indicative of the very violent volcanic activity which took place here way back in the Ordovician.
Reference:
Millward, D. et al. 2000. Geology of the Ambleside district, British Geological Survey Memoir for 1:50000 Geological Sheet 38, London HMSO.
The rocks in this photo belong to the Pavey Ark Member (formerly the 'Pavey Ark Breccia') in the Borrowdale Volcanic Group (Ordovician). This is a very coarse tuff with many angular rock fragments, volcanic bombs and andesite lava spatter, possibly resulting from a pyroclastic flow settling into water; the whole lot subsequently disrupted by slumping and mass movement (Millward et al, 2000). This is indicative of the very violent volcanic activity which took place here way back in the Ordovician.
Reference:
Millward, D. et al. 2000. Geology of the Ambleside district, British Geological Survey Memoir for 1:50000 Geological Sheet 38, London HMSO.
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