Hill End to Spaniard Rocks & Back: Step-by-Step Part 7

Walking back from Spaniard Rocks now, I took a route closer to the dunes where the character of the shore is quite different from the wet sand and strandlines between high and low tide levels. Here there are pebbles. Rhossili’s pebbles intrigue me. I love scrambling over the banks of stones at the very top of the beach. The colours are lovely pastel shades with pinks and blues and overall reminding me of sugared almonds. A total delight. Many rock types are represented. Some have interesting patterns.

I like the way that the numbers of beach stones seem to increase or decrease depending on how they are pushed around the shore between one visit and the next, and how the sand changes its level and distribution throughout the year and the transition from season to season. This time the wooden ribs and keel of the shipwrecked ketch Anne were only just visible above the sand and pebbles. I like the way that pebbles are arranged partly buried in the damp sand that quickly dries to a different hue and texture. The pebbles underlie the tall sand dunes of the Llangennith Burrows. The dunes have been scooped out by stormy seas and footsteps in many places to demonstrate that even wind-blown sand is stratified; and marram grass roots exposed to air show how deep they penetrate the soft fine sediments to bind them together and stabilise the dunes.

Erosion of the tombolo at Dogs Bay

View of Dogs Bay, Connemara, Ireland

Looking northeast from the offshore island towards the white calcareous sandy beach and dune system, known as a tombolo, that connects the island to the mainland at Dogs Bay in Connemara on the west coast of Ireland.

Dogs Bay is a famously beautiful sandy beach in Connemara on the west coast of Ireland. The beach is actually part of a geomorphological feature known as the Dogs Bay/Gorteen Bay tombolo. A tombolo is a spit or bar of sand or gravel connecting an island to the mainland or another island. In general terms, persistent winds from the southwest have meant that waves meeting the island and wrapping around it, slow down as they converge on the northeast and landward side of the island, where force and speed of the waves decreases and they deposit their load of sediment. Over time the sediments gradually accumulate to such an extent that they rise as a bar above the water. The sediment bank eventually stretches all the way from the island to the mainland, and the connecting bar is termed a tombolo.

The sand has become stabilised by the growth of vegetation; and at the present time is a very special and rare type of habitat known as machair. Machair only forms on calcareous soils. At Dogs Bay the sand is  composed mainly of minute fragments of the carbonate skeletons of marine animals such as sea urchins and their spines, sponge spicules, bryozoa, seashells, snails, and most remarkable of all, the intricate microscopic skeletons of one-celled creatures called Foraminifera. Dogs Bay is one of only a few beaches in the world with predominantly Foraminiferan sand.

Machair, and the surface of the Dogs Bay tombolo, is unlike many of the coastal dune systems that I have visited in England, where the dunes are full of peaks and troughs, and where marram grass dominates. Marram is often a major initial factor in the stabilisation of the loose grains. Here, however, a grassland vegetation of low species diversity is encouraged to grow in a moist, cool, windy, oceanic climate on the fairly level and compacted alkaline soil of a mature sand dune system, and grazing by animals is vital to the maintenance of the habitat. Useful information about the features in this area is available from an on-line field guide produced by the Irish Quaternary Association. Click here for details of tombolo formation and machair habitat (pages 13-17).

Arriving at Dogs Bay, it was clear to see the impact of the earlier winter waves. Storms in the first few months of the year had ripped up and washed away the road and the car park at the entrance to the beach. A sign post now lying on the shore showed where it had been. On scrambling down to the beach, a close inspection of the wonderful curve of the dunes at the top of the shore revealed that the leading edges had been sliced away leaving hanging sheets of machair turf and huge clumps of vegetated dune material on the shore. Wooden posts, perhaps fencing from the top of the dunes delineating boundaries and preventing grazing animals from falling over the edge, were lying loose on the beach below, sometimes apparently supporting  the dune-top hanging mats of vegetation.

The tombolo is a vulnerable feature of the landscape. It seems that there is a history of natural damage to it in this location. In pictures 4 and 5 of the gallery below, the cross-section through the eroding dune shows a narrow horizontal dark brown band about half way down the vertical surface. This is a richly organic ancient soil level (palaeosol) that is associated with archaeological remains such as shell middens and the remains of a settlement, showing that people in the past used the site and exploited its marine resources to augment their diet. The palaeosol  is present at each end of the line of dunes but is absent in the central part. Its absence in this part could indicate that either the dunes at that time in that place were not stabilised by vegetation, or that the centre of the tombolo has been severely eroded in the past and recovered from the damage.

Apparently, about ten years ago, local people feared that the tombolo would be totally breached. Maybe it was at that time that steps were taken to prevent destruction of the spit. It is clear from the presence of rock-filled metal gabion cages on the beach that conservation measures were in place prior to last winter’s storms that battered much of the coastline around Ireland and Britain. However, at the time of my visit on a cold, wet, mostly dull day at the end of March 2014, it was evident that more of these measures might be required in future to prevent further damage.

Sand patterns at Studland Bay

Sand photograph: Sand ripple patterns in the dunes on the National Trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast World Heritage Site (P1060957aBlog1) 

Sculpted by the wind as well as the waves, thousands of intricate and endlessly fascinating patterns of ripples in the sand weave their way across the seashore at Studland Bay in Dorset.

Here are a few of them for you to enjoy. The one above in the fine dry sand amongst the marram grass in the dunes; the others below in the wet intertidal zone – both sorts defined by the angle of the sun and the degree of shadow.  

Sand pattern picture: Intertidal sand patterns on the National trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast (P1110262aBlog2) 

Fish tails?

Sand pattern picture: Intertidal sand patterns on the National Trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast (P1110266aBlog3) 

Fish scales or over-lapping tiles?

Seashore sand photograph: Intertidal sand patterns on the National Trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast (P1110401aBlog4)  

Deep corrugations and crumples.

Sand ripple picture: Intertidal sand patterns on the National Trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast (P1110406aBlog5)  

Sinuously weaving and bifurcating ripples.

Sand pattern picture - Sand ripples on the National Trust owned beach at Studland Bay, Dorset, UK on the Jurassic Coast (P1110407aBlog6) 

Revision of a post previously published 31 May 2009


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Beached balls

There’s something sad about finding toys on the beach. There’s no telling whether they have been simply lost or forgotten; or if they were abandoned because they were broken. Some of them have been travelling around the coast for some time, riding in and out with the tides, becoming the worse for wear during their journeys – and these can be termed as flotsam. The toys pictured here were all found in remote stretches of shore without a person, let alone a child in sight, far from the busy parts where families play. It’s fair to assume they have washed ashore after floating out to sea.



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