FOULA  HERITAGE

Foula - The Edge of the World

 

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COASTAL AND INLAND EROSION IN FOULA

 

Major rock fall at Hedlicliv.  The top of the cliff is very unstable with
 cracks parallel to the cliff edge opening up

 

Less recent fall at da Geo ida Lang Hoevdi

 

Small scree fall at the foot of the Back ida Noup.
 Here the sea has now removed most of the debris.

 

More recent small scree fall above Da Lamatuns.
The rock below the fall is still covered with clay.

 

Two older scree falls between the Sneck ida Smaallie and Da Lamatuns.
Patches of grass have grown back and the sea has removed much of the spoil.

 

A recent fall from the cliff top just south of the Sneck ida Smaallie.

 

Scree fall in Da Scrodhurdins (on Right). Ian Pennie, 1948.
From the Shetland Museum archives

 

Scrodhurdins scree fall still showing in c.1970

 

Still a lot of ungrassed areas in the Scrodhurdins scree in c.2000.
Part of the dark area to the upper right of the scree is a very large cave
 which has its entrance nearly blocked by the scree.

 

Another major cave in Da Srodhurdins. A large storm beach has built up in its entrance. The cave roof is more than twenty feet above the top of the boulders,
which decrease in height further back into the cave.
 Nesting Guillemots on the ledges to the right.

 

This is the area of cliff undercut in the right of the above photograph

 

A rock fall from the face of the Kame removes a lot of soil from the Little Kame.
This was the Isle's largest nesting area for puffins so a great many lost their homes.

 

Vegetation returns to the southern part of the Little Kame

 

Looking at Simmons Head through the Kittiwakes' Haa arch.

 

Gaada Stack from the sea.

 

The western arch of Gaada Stack

 

The sea coming through Gaada Stack's eastern arch

 

Daylight showing through the arch of the Brough, Gaada Stack to the right.
Photograph from the Shetland Museum archives

 

To the left of Gaada Stack is the Brough after its arch collapsed in 1965

 

Glacial till erosion begins on the east side of Da Pier after part of the turf slumps

 

Erosion of Glacial Till on Da Pier. Fifty years ago most of Da Pier
 was covered with grass and its top was 5-6 feet wide.

 

Turf protruding over clay erosion (On left).  In shadow behind
 is the east side of Da Pier. The turf on the left has collapsed.

 

Glacial Till, at the Riggs, slumping as it is undercut by the sea

 

Two old boat noosts at the Riggs will soon disappear, 2005.

 

The slumping of the Bruggs below the old Leraback house.
Leraback means "clay slope".

 

The slumping of the Leraback Brugs.
Photographed from Hamnafeld

 

Landslide in Soberlie a year or two after it happened in 1986

 

Small landslide (Bottom right) between Tounafeld and Hamnafeld

 

The same landslide a few years later.

 

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