Àird Ghlas

Coastal Feature, Headland, Point in Argyllshire

Scotland

Àird Ghlas

Forking dyke at Carraig MhÃ²r This dyke doesn&#039;t seem to have been thought big enough to map on the 1:50000 1992 Geological sheet 44 but seems to be parallel to a fault which marks the boundary between lava flows to the east downfault past the Lower Jurassic Strata exposed either side of the dyke. On the aerial view it appears very curved, but seen here close up, the main dyke indeed curves west, but a subsidiary dyke, on the left in this view, and much more jointed, suggesting more rapid cooling, splits off from the main one and continues straight down towards the tide line. For anyone wanting to get across the slippery weed-covered tidal rocks to reach the tiny bit of land in the square to the south, the dyke forms a convenient walkway, for the most part remaining high enough not to have been colonised by the seaweed. — Forking dyke at Carraig MhÃ²r Credit: Andy Waddington

Àird Ghlas is a prominent coastal feature located in Argyllshire, Scotland. It is a headland that extends into the sea, forming a distinct point along the rugged coastline. The name "Àird Ghlas" translates to "green headland" in English, which aptly describes its picturesque surroundings.

Situated in an area of outstanding natural beauty, Àird Ghlas offers breathtaking views of the surrounding landscape and the vast expanse of the Atlantic Ocean. The headland is characterized by its steep cliffs, which provide nesting sites for various seabird species, including puffins, guillemots, and razorbills. These cliffs also serve as a natural barrier, protecting the coast from erosion caused by the relentless waves.

The headland itself is covered in lush green vegetation, giving it a vibrant appearance and adding to its beauty. The rugged terrain and rocky outcrops provide a habitat for a diverse range of flora and fauna, making Àird Ghlas a popular spot for nature enthusiasts and hikers.

Access to Àird Ghlas is relatively easy, with well-maintained paths and trails leading to the headland. Visitors can explore the area on foot, taking in the stunning views and enjoying the fresh sea breeze. The headland is also a popular spot for fishing, with anglers often casting their lines into the waters below in search of a catch.

Overall, Àird Ghlas is a captivating coastal feature that showcases the natural beauty of Argyllshire. Its striking cliffs, abundant wildlife, and panoramic views make it a must-visit destination for those seeking a connection with nature and the Scottish coastline.

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Àird Ghlas Images

Images are sourced within 2km of 56.31887/-5.9895355 or Grid Reference NM5321. Thanks to Geograph Open Source API. All images are credited.

Forking dyke at Carraig MhÃ²r

This dyke doesn't seem to have been thought big enough to map on the 1:50000 1992 Geological sheet 44 but seems to be parallel to a fault which marks the boundary between lava flows to the east downfault past the Lower Jurassic Strata exposed either side of the dyke. On the aerial view it appears very curved, but seen here close up, the main dyke indeed curves west, but a subsidiary dyke, on the left in this view, and much more jointed, suggesting more rapid cooling, splits off from the main one and continues straight down towards the tide line. For anyone wanting to get across the slippery weed-covered tidal rocks to reach the tiny bit of land in the square to the south, the dyke forms a convenient walkway, for the most part remaining high enough not to have been colonised by the seaweed.

Andy Waddington

Footpath to Carsaig

The part of the Carsaig to Loch Buie coast path nearest the road system at the west end is an easy walking route through bracken-infested grassland with none of the obstacles that those heading east from here will encounter along the way. A change in the geology a short way to the east is caused by a fault, dropping the rough basalt plateau lavas to sea level, whilst here we are above softer Lower Jurassic sedimentary rocks which make for gentler terrain. The sediments form the shore for some way round Carsaig Bay before dipping below the shore just shy of Carsaig Arches and Malcolm's Point seen in the distance.

Andy Waddington

Emerging square

They say that time and tide waits for no man. Well, here, no man was waiting for time and tide - although it was falling it was going to be getting late if we waited until the land emerged much more. As it was, the GPS said I was in the square (but just by a metre or so with my feet overhanging the sea) and that was going to have to be good enough.

Andy Waddington

Road down Glen Leidle with Firth of Lorn in the distance

Jo and Steve Turner

Glimps of Carsaig House from the Glen Leidle road

Category B Listed house of about 1800 formerly the seat of Macleans of Pennycross and called Pennycross House that was superseded by Innimore Lodge in 1877. George Well Cheape of Wellfield acquired the house in the late 19th century. The house is currently (2015) available for holiday rental.

Jo and Steve Turner

Carsaig Bay

Alan Reid

Aird Ghlas basalt dyke in Carsaig Bay

Alan Reid

Shore at Rubh' a' Chromain

Alan Reid

Cadha an Aon Dorais

Very steep coastal slope.

Alan Reid

Sgeir Bhuidhe, the yellow rock

Alan Reid

Intertidal rocks and boulders

The Paps of Jura on the horizon.

Alan Reid

Hollow boulder cast in sandstone

Alan Reid

Waterfall near the Nuns' Pass

Following in the footsteps of David Balfour, the hero of Robert Louis Stevenson's Kidnapped, as he makes his way back to Edinburgh to confront his wicked uncle. Stage 1, June 2016 from Erraid to Fishnish on the Isle of Mull. See Link