The Transforming Tide
I have been reading James Millar's fascinating book, A Wild and Open Sea : The Story of the Pentland Firth, which details both the history and the marine geology of this turbulent body of water. I was particularly interested in the detailing of the action of the waves upon the coastline- the process, over centuries, of the swell pounding and continually eating away at the cliff-edge. Interestingly, the terminology used locally to describe cliff erosion gives a tantalising hint of the old Norn language once used in Caithness: Gloups, Geos, Cletts, Thirl doors, Skerries. Some of the Norn bird names survive in usage to this day : gulls are still referred to as scorries (skári, N. ) cormorants, scarf (skarfr, N.) (http://nornlanguage.x10.mx)
It was the continual transformation from one rock formation to another that I found intriguing: the sea carves an opening into the side of the cliff (Thirl Door): this can continue through to the interior , creating an upwards surge which creates a blowhole (Gloup) on the interior of the cliff: this can then wear away further to form an arch: this, in turn, can collapse into a freestanding stack, or clett: this eventually disintegrates or is worn down into a small islet, a skerry.
Thirl Door, Holborn Head, Scrabster.
Gloup on the interior surface of the thirl door - the inlet at the back drops right down to the sea ( this was as near to the edge as I was prepared to get!)
|
The top surface of the same cliff : the opening to the gloup is in the centre |
Cliff edge, looking Northwest |
Another Holborn Head gloup , this time the sea is clearly visible |
Geo: a very common feature of the Caithness coastline. The sea below (1) and water flow from the surface (2) combine to carve a narrow inlet into the cliff. These vary in scale and size- some are very narrow: others, like the one at Whaligoe (https://en.wikipedia.org/wiki/Whaligoe) on the East Coast of the county, are substantial enough to have been used as small natural harbours. Geos provide a perfect, "high rise" habitat for nesting seabirds : the shags and cormorants lay a single egg on the bare rock ledges at the bottom, guillemots live up a level, fulmars and kittiwakes on the higher shelves and puffins burrow in the sandy topsoil . (http://caithnessbirds.co.uk/wp-content/uploads/2013/11/Caithness-map-21.jpg)
(1)
(2)
Man-made activity on the clifftop- slate cairn and names graffitti'd on to the surface of the rock |
More slate formations, in a geo and on the clifftop. |
Holborn Head lighthouse and the terminal for the Orkney ferry, with Thurso in the background. |
Duncansby Head, John O'Groats
Possibly one of the most well-known sights in Caithness - the stacks at Duncansby head, on the most northeasterly point of the county.
Thirl door transforming into an arch near the Stacks- at the sea edge of the picture below- note the red sandstone here, in contrast to the black slate of Holborn Head |
Firth
Corrosion
Corrasion
Geo carves into stone:
Birds' haven, fishers' landing.
Thirl Door
Thirl Door
Sonic boom
Walls echo an ominous percussion.
Hydraulic action
land.
Gloup within
punches Sea
through.
Corrosion
Corrasion
arch
clings on
by umbilical gneiss.
Corrosion corrasion
Waves a relentless quernstone.
Arch succumbs to
Clett
Clett stands defiant but
Cannot resist
Attrition
to skerry
Sker
rry
to
.
Comments
Post a Comment