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Bàgh Achadh dà Mhaoilein

Bay in Argyllshire

Scotland

Bàgh Achadh dà Mhaoilein

Estate track at Ormsary
Estate track at Ormsary Credit: John Ferguson

Bàgh Achadh dà Mhaoilein, also known as Bay of Achadh dà Mhaoilein, is a picturesque bay located in Argyllshire, on the west coast of Scotland. This bay is situated approximately 10 miles south of Oban, a popular tourist destination.

The bay is surrounded by stunning natural beauty, with its crystal-clear waters and sandy beaches attracting visitors from near and far. It offers breathtaking views of the surrounding hills, which are covered in lush greenery. The bay is also home to a variety of wildlife, including seals, otters, and a wide range of bird species.

Bàgh Achadh dà Mhaoilein is not only a haven for nature enthusiasts but also offers recreational activities for visitors. The bay is ideal for swimming, kayaking, and sailing, with its calm waters providing a safe environment for water-based activities. The sandy beaches are perfect for sunbathing and picnicking, making it a popular spot for families during the summer months.

In addition to its natural beauty, Bàgh Achadh dà Mhaoilein has historical significance. There are remnants of ancient settlements and burial sites in the vicinity, giving a glimpse into the area's rich past.

Overall, Bàgh Achadh dà Mhaoilein is a hidden gem on the Scottish coast, offering visitors a tranquil and scenic escape from the hustle and bustle of everyday life. Whether it's exploring the natural wonders, engaging in water sports, or simply enjoying a leisurely day on the beach, this bay has something to offer for everyone.

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Bàgh Achadh dà Mhaoilein Images

Images are sourced within 2km of 55.89378/-5.6214606 or Grid Reference NR7372. Thanks to Geograph Open Source API. All images are credited.

Estate track at Ormsary
Estate track at Ormsary
Ormsary sawmill
Ormsary sawmill
Loch Caolisport Just South of Ormsary.
Loch Caolisport
Just South of Ormsary.
Loch Caolisport Eileann Traighe in the foreground and Jura in the far distance.
Loch Caolisport
Eileann Traighe in the foreground and Jura in the far distance.
Ormsary Water looking upstream from the bridge
Ormsary Water looking upstream from the bridge
Remains of shielings at Sean-ghart
Remains of shielings at Sean-ghart
Country near Baile Boidheach Looking out to Loch Caolisport. The Paps of Jura are in the far distance, left of centre.
Country near Baile Boidheach
Looking out to Loch Caolisport. The Paps of Jura are in the far distance, left of centre.
Loch Caolisport shoreline
Loch Caolisport shoreline
Baigh Sean-Ghairt, Ormsary
Baigh Sean-Ghairt, Ormsary
Burial ground at Ormsary
Burial ground at Ormsary
Rushy field at An Dùn, Ormsary
Rushy field at An Dùn, Ormsary
Field overlooking Loch Caolisport
Field overlooking Loch Caolisport
Erratic boulders on the shore The sandy shore of the bay at Ormsary sports some fine glacial erratic boulders.
Erratic boulders on the shore
The sandy shore of the bay at Ormsary sports some fine glacial erratic boulders.
Schist outcrops Eroded outcrops of Dalradian schists show a very slatey character; some are reduced to blade-like protrusiuons from this small, stony beach. The form of these outcrops differs significantly from outcrops of amphibolite to the north (<a href="https://www.geograph.org.uk/photo/5091530">NR7373 : Amphibolite outcrops</a>).
Schist outcrops
Eroded outcrops of Dalradian schists show a very slatey character; some are reduced to blade-like protrusiuons from this small, stony beach. The form of these outcrops differs significantly from outcrops of amphibolite to the north (NR7373 : Amphibolite outcrops).
Amphibolite outcrops In complete contrast to the schist outcrops further south (<a href="https://www.geograph.org.uk/photo/5091512">NR7372 : Schist outcrops</a>) on the shore, here we have massive amphibolites which only show a strong jointing pattern in place of the strong foliation of the schist. The amphibolites are basalt intrusions into the sediments of the Dalradian succession before the pervasive metamorphism of the Caledonian continental collision and mountain building.
Amphibolite outcrops
In complete contrast to the schist outcrops further south (NR7372 : Schist outcrops) on the shore, here we have massive amphibolites which only show a strong jointing pattern in place of the strong foliation of the schist. The amphibolites are basalt intrusions into the sediments of the Dalradian succession before the pervasive metamorphism of the Caledonian continental collision and mountain building.
Rocks with grey lichen Lichens are highly specific in their preference for substrates and location. It was particularly interesting that only one type appeared to be present here, and almost exclusively on the crests of these jointed blocks of rock. The rock is amphibolite belonging to the Dalradian Supergroup, where it represents metamorphosed basaltic intrusions - a rock most notably low in silica, but rich in iron and magnesium.
Rocks with grey lichen
Lichens are highly specific in their preference for substrates and location. It was particularly interesting that only one type appeared to be present here, and almost exclusively on the crests of these jointed blocks of rock. The rock is amphibolite belonging to the Dalradian Supergroup, where it represents metamorphosed basaltic intrusions - a rock most notably low in silica, but rich in iron and magnesium.
Rock with green lichen Intriguing and colourful lichen on a boulder above the tide mark. A small tuft of Sea Ivory at the bottom right of the image is a second (or third) species present on this boulder. I think that the green lichen is Rhizocarpon geographicum. The nodular surface of the rock is due to differential weathering and erosion of the gabbroic rock, which contains large, prominent crystals of pyroxene.
Rock with green lichen
Intriguing and colourful lichen on a boulder above the tide mark. A small tuft of Sea Ivory at the bottom right of the image is a second (or third) species present on this boulder. I think that the green lichen is Rhizocarpon geographicum. The nodular surface of the rock is due to differential weathering and erosion of the gabbroic rock, which contains large, prominent crystals of pyroxene.
Intermittent cleavage In this sea-washed and eroded outcrop of Dalradian metamorphosed sedimentary rock the layers of finely-bedded sandstone are well displayed. Layers which were more muddy, and of finer-grain have developed a cleavage at a steep angle to the bedding during dynamic metamorphism. The coarser sandstones have a less-reactive composition and have not developed a foliation due to orientated mineral growth to the same degree, and are also more resistant to erosion, resulting in the cleaved layers being more rapidly cut back.
Intermittent cleavage
In this sea-washed and eroded outcrop of Dalradian metamorphosed sedimentary rock the layers of finely-bedded sandstone are well displayed. Layers which were more muddy, and of finer-grain have developed a cleavage at a steep angle to the bedding during dynamic metamorphism. The coarser sandstones have a less-reactive composition and have not developed a foliation due to orientated mineral growth to the same degree, and are also more resistant to erosion, resulting in the cleaved layers being more rapidly cut back.
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Bàgh Achadh dà Mhaoilein is located at Grid Ref: NR7372 (Lat: 55.89378, Lng: -5.6214606)

Unitary Authority: Argyll and Bute

Police Authority: Argyll and West Dunbartonshire

What 3 Words

///future.backswing.initiates. Near Tarbert, Argyll & Bute

Nearby Locations

Sgeir Dhubh Bàgh Achadh dà Mhaoilein Eilean Tràighe

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Nearby Amenities

Located within 500m of 55.89378,-5.6214606
Power: pole
Lat/Long: 55.892202/-5.6182797
OpenStreetMap
Google Maps
Ormsary
Name Gd: Ormsaraidh
Place: hamlet
Wikidata: Q11027651
Wikipedia: en:Ormsary
Lat/Long: 55.8921251/-5.6143768
OpenStreetMap
Google Maps
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.
Camas Dubh Ross-shire
Camas na Gaibhre Ross-shire

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