NU2231 : Golf course strata
taken 10 years ago, near to Seahouses, Northumberland, Great Britain
This is 1 of 2 images, with title starting with Golf course in this square

Golf course strata
Below the turf the topsoil and subsoil are made up of glacial till (boulder clay) probably scraped off southern Scotland by glaciers of the last ice age. Below that are modest layers of shelly limestone, eroded away. The whiter, smoother basal layers are of carboniferous limestone (~300m years old) together with some erratics weathered out of the glacial material. For the whole context see Link
(Archive Link
) . The location is on the best walking route between Seahouses and Beadnell.


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- Grid Square
- NU2231, 180 images (more nearby
)
- Photographer
- Mike at Seahouses (find more nearby)
- Date Taken
- Tuesday, 28 August, 2012 (more nearby)
- Submitted
- Tuesday, 28 August, 2012
- Geographical Context
- Subject Location
-
OSGB36:
NU 2263 3146 [10m precision]
WGS84: 55:34.5767N 1:38.5583W - Camera Location
-
OSGB36:
NU 2253 3142
- View Direction
- East-northeast (about 67 degrees)
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Image classification(about):
Geograph
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