Pegswood Flash, Coney Garth, Northumberland
Sheffield's traditional solution to over-crowded b…
A thoughtful, relaxing snap time
Old Red Sandstone cliffs, Whiting Ness, Arbroath,…
Old copper mine on Carmel Head, Anglesey, North Wa…
"The Great Opencast", Parys Mountain copper mine,…
Windsurfing off Mersea Island, Essex
Stone trough at Carl Wark hill fort, Derbyshire
Cliff erosion 1
Cliff erosion 3
Geese 1
Geese 2
Pink and black
Pleistocene river gravels of the proto-Thames
Reeds
Stiff easterly in the Colne
Tree root 1
Tree root 2
Tree root 3
Windsurfing 1
Windsurfing 3
Windsurfing - close to a capsize!
Windsurfing 5
O'er Bill's Mother's (moody skies over Blea Rigg)
Lang How Tarn and the Langdale Pikes
At Three Tarns
The Golden Bog (Lang How Tarn)
Sheffield Peace Gardens Fountain
Hood Brook
Hathersage wall
Ford at Green's Mill
North Lees cloudscape
Clouds over Stanage Edge
Sky, church and clouds
Ruined chapel near North Lees Hall, Hathersage
Bubble Dragon Dance
Stainless? Steel Balls
Dragon's Head
Dragon Dance 9
Dragon Dance 8
Dragon Dance 7
Dragon Dance 6
Dragon Dance 3
Dragon Dance 2
Happy Children with Lord Mayor Jackie Drayton
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
-
428 visits
The Keptie Hills esker, Arbroath, Scotland


Originally posted for the Guesswhere UK group.
The Keptie Hills in Arbroath is a good example of an esker.
Eskers are formed from rock debris deposited by meltwater in a sub-glacial meltwater tunnel. The confines of the glacier ice means that the deposits are closely constrained and tend to build upwards rather than spreading out. When the glacier finally melts away, the esker is left as a sinuous ridge of gravel and sand. They often superficially resemble railway embankents and can be many miles long.
Scanned from Kodachrome 64 transparency film, taken with a Zenit 'E'.
See where this picture was taken. [?]
--------------------
Here's a photo of a sub-glacial tunnel on Mt Ranier in Washington, USA, taken by Flickr member Tom.
www.flickr.com/photos/lazybeagle/409343860/
You can see the debris in the tunnel floor which may eventually become an esker.
The Keptie Hills in Arbroath is a good example of an esker.
Eskers are formed from rock debris deposited by meltwater in a sub-glacial meltwater tunnel. The confines of the glacier ice means that the deposits are closely constrained and tend to build upwards rather than spreading out. When the glacier finally melts away, the esker is left as a sinuous ridge of gravel and sand. They often superficially resemble railway embankents and can be many miles long.
Scanned from Kodachrome 64 transparency film, taken with a Zenit 'E'.
See where this picture was taken. [?]
--------------------
Here's a photo of a sub-glacial tunnel on Mt Ranier in Washington, USA, taken by Flickr member Tom.
www.flickr.com/photos/lazybeagle/409343860/
You can see the debris in the tunnel floor which may eventually become an esker.
- 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.