Everton Carr and the valley of the River Idle, Not…
Pines 1
Pines 2
Lone pine
Backlit trunks
Sunlit trunks
Walberswick wind pump, Suffolk
Dunwich River
Harvest in progress
Walberswick Westwood Marsh
Reeds in seed
Minimalist
Walberswick beach huts....
Cloudscape with River
Hooken convergence
Slowly falling trees at Pinhay Bay, Devon
The Undercliff overlooking Pinhay Bay, east Devon
Clue photo
Charton Bay, Devon
The Spittles: toe of May 2008 landslide
The Spittles landslide area
The Cobb
Cliffs of composed of Otter Sandstone, Budleigh Sa…
Odin Sough outfall, Castleton, Derbyshire
Blue Bay
Blue Harbour
Ladies Cave Anticline
You have been warned....
Tenby
Pendine Sands from Gilman Point
Pendine land, sea and sky
Pendine Sands from Dolwen Point
Coastal erosion near Skipsea, East Yorkshire.
Sewerby cliff interpretation
Danger - Coastal Erosion
Narrowing the field - very recent coastal erosion…
The 'buried' palaeo-cliff at Sewerby, near Bridlin…
West from Dolwen Point, near Pendine, Carmarthensh…
Hinge Zone
Along the crest
Disharmonic recumbent fold
A peaceful sunset at Marloes Sands
Looking up the Chimneys
Three Chimneys at Marloes
Illuminated bedding planes at Marloes
1/125 • f/4.0 • 17.0 mm • ISO 400 •
Location
Lat, Lng:
You can copy the above to your favourite mapping app.
Address: unknown
You can copy the above to your favourite mapping app.
Address: unknown
See also...
Keywords
Authorizations, license
-
Visible by: Everyone -
All rights reserved
-
533 visits
Odin Sough tail


This rather insignificant looking structure is the tail of Odin Sough (also known as Trickett Bridge Sough) in Castleton, Derbyshire.
The sough drains water from the old Odin lead mine about 1.6 km away to the west. The mine worked lead ore from veins in the Carboniferous Limestone close to the junction with the overlying dark, pyritic Edale Shales, and the sough itself is driven in the latter for most of its length. It is the oxidation and solution of pyrite (iron sulphide) in the shales and its reprecipitation as ferric hydroxide which causes the orange colouring on the stream bed.
The sough drains water from the old Odin lead mine about 1.6 km away to the west. The mine worked lead ore from veins in the Carboniferous Limestone close to the junction with the overlying dark, pyritic Edale Shales, and the sough itself is driven in the latter for most of its length. It is the oxidation and solution of pyrite (iron sulphide) in the shales and its reprecipitation as ferric hydroxide which causes the orange colouring on the stream bed.
- Keyboard shortcuts:
Jump to top
RSS feed- Latest comments - Subscribe to the comment feeds of this photo
- ipernity © 2007-2025
- Help & Contact
|
Club news
|
About ipernity
|
History |
ipernity Club & Prices |
Guide of good conduct
Donate | Group guidelines | Privacy policy | Terms of use | Statutes | In memoria -
Facebook
Twitter
Sign-in to write a comment.