The sand looks black from a distance as you descend to the shore at Trá Chathail near An Trá Bheag (Short Strand) – otherwise known as Trabeg. The path cuts down deep through the stratified red rocks to get to the beach which is strewn with pebbles, mostly shades of red, maroon, green, grey, and white.
Trabeg is on the south coast of the Dingle Peninsula in Ireland, and is the “type section” of the Trabeg Conglomerate Formation which is exposed in the cliffs on the beach. This is place where that particular rock type was first described. The rock layers constitute part of the Dingle Group and were formed in the Devonian period between 345 and 395 million years ago. The conglomerates are composed of fairly well rounded pebbles of red sandstones and mudstones, with white vein quartz and chert. A few pebbles of volcanic rock and of grey limestone are also present.
The way in which the conglomerate rock has formed from the mass movement and subsequent accumulation of debris from terrestrial locations during, for example, river flood events, means that the pebbles are derived from a wide area covering many different geological types. The pebble beds or conglomerates are inter-bedded with layers of red sandstones and mudstones, the finer sediments of which were deposited normally by rivers during non-storm/flood times. The alternating layers are now tilted from the original horizontal orientation in which they were first deposited, and are clear to see dipping south at about 70 degrees.
As the cliffs at Trá Chathail are worn away by the action of waves and weathering, the pebbles contained in the conglomerate matrix are freed up and remain the shore below – an instant pebble beach. Added to these are pieces of other rock or matrix that became rounded into pebbles after they arrived on the beach. Some pebbles and rocks may have been transported by wave action from further along the coast were the geology is quite different: from the Eask Formation, West Cork Sandstone, Bulls Head Formation, and the earlier Silurian rocks of the Dunquin Group.
Horne, Ralph R. (1976) Geological Guide to the Dingle Peninsula, Geological Survey of Ireland Guide Series No. 1, reprinted 1999.
Ancient Acadian Forest cloaks the slopes right down to the shore along the trail from Louisbourg Lighthouse to Big Lorraine on Cape Breton Island. This unique forest is one of six identified for protection by the World Wildlife Fund because, here, the northern boreal forest blends with the southern hardwood forest to create a diverse habitat supporting a wide range of plant and animal life. The forest is mostly home to balsam fir with some black spruce and tamarack. Many of the trees are stunted and twisted from exposure to severe weather conditions, salt spray and poor soil in this coastal stretch. The bare sun-bleached branches on stands of dead trees are frequently covered with thick layers of pale branching lichens.
Amongst the trees are wetland areas of bog with shallow pools of open water which transition to fen with thick mats of sphagnum mosses, ground juniper, cotton grass, crowberry, and carnivorous pitcher plants. Despite the beautiful blue skies it was a particularly late and cold spring at the time of my visit (2 June 2016) and flowers were scarce but rare alpine species are known to occur in this location.
The forest, bogs, and fens sit on top of very old rocks responsible for the spectacular scenery along the coast beside the trail. All are derived from extensive volcanic activity in Precambrian (Neoproterozoic) times and belong to the Main-à-Dieu sequence. They include layered volcanic ash in the form of tuff, and varying kinds of conglomerates and breccias from pyroclastic flows down the sides of an arcing series of volcanoes where two land masses collided.
We stayed at the most excellent Louisbourg Harbour Inn while we explored this part of Cape Breton Island.
Freezing fog has lately covered all the vegetation in my village with a transparent icy coat bearing fringes of needle-like crystals. As the sun comes out to burn off the mist, the rising temperature begins to melt this hoar frost. As I walked along beside tall beech trees on one such frosty morning, an unexpected heavy rain of icy water began to fall from the thawing ice in the highest boughs, cascading down through the understorey of saplings where drops accumulated on the twigs and leaves, shining like diamonds in the low-slanting winter sun. Difficult to capture with the camera the brilliance of the eye-dazzling effect of reflections from the melt water rain and droplets.
These photographs of the hazy horizons of successive hilltops in the Tuscan countryside are views looking southwards from the top of Brunelleschi’s dome on the cathedral of Santa Maria del Fiori, the Florence Duomo. Spectacular vistas of the city and its surrounding countryside are the reward for climbing 463 steep steps in claustrophobic narrow passageways of herringbone brickwork through the interior of the dome.