Acairseid na h-Uamhaidh Mòire

Island in Argyllshire

Scotland

Acairseid na h-Uamhaidh Mòire

Descending Creag Bhàn The descent of Creag Bhàn offers a fine view over the south and west of the Isle of Gigha, and a distant Islay.  In this view, Ardailly can be noted, with the covered Gigha service reservoir below.  Mill Loch and High Loch can be noted to the left in the near and far distance, respectively.

This photograph was taken during the Coronavirus (COVID-19) pandemic of 2020/21.
Descending Creag Bhàn Credit: James T M Towill

Acairseid na h-Uamhaidh Mòire is a small island located in Argyllshire, Scotland. Situated off the western coast of the mainland, it is part of the Inner Hebrides archipelago. With a total area of approximately 100 hectares, the island is characterized by its rugged landscape, with rocky cliffs and rolling hills dominating the scenery.

The name Acairseid na h-Uamhaidh Mòire translates to "archipelago of the big caves" in Scottish Gaelic. This name reflects the geological significance of the island, as it is home to several large sea caves that have been formed through years of erosion by the powerful waves of the Atlantic Ocean.

The island is uninhabited, with no permanent residents. However, it attracts a small number of visitors each year who come to explore its natural beauty and diverse wildlife. Acairseid na h-Uamhaidh Mòire is known for its rich bird population, with species such as puffins, guillemots, and razorbills nesting along the towering cliffs. Seal colonies can also be spotted lounging on the rocky shores.

Access to the island is predominantly by boat, with a few tour operators offering trips for visitors. The surrounding waters are popular among kayakers and divers, who are drawn to the abundance of marine life and the opportunity to explore the sea caves.

Overall, Acairseid na h-Uamhaidh Mòire is a remote and picturesque island, offering a unique and untouched natural environment for those seeking a tranquil and adventurous experience in the Scottish wilderness.

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Acairseid na h-Uamhaidh Mòire Images

Images are sourced within 2km of 55.683398/-5.7663939 or Grid Reference NR6349. Thanks to Geograph Open Source API. All images are credited.

Descending Creag Bhàn The descent of Creag Bhàn offers a fine view over the south and west of the Isle of Gigha, and a distant Islay.  In this view, Ardailly can be noted, with the covered Gigha service reservoir below.  Mill Loch and High Loch can be noted to the left in the near and far distance, respectively.

This photograph was taken during the Coronavirus (COVID-19) pandemic of 2020/21.
Descending Creag Bhàn
The descent of Creag Bhàn offers a fine view over the south and west of the Isle of Gigha, and a distant Islay. In this view, Ardailly can be noted, with the covered Gigha service reservoir below. Mill Loch and High Loch can be noted to the left in the near and far distance, respectively. This photograph was taken during the Coronavirus (COVID-19) pandemic of 2020/21.
Ardailly Mill and miller's cottage At the far end of a long and winding track on the Isle of Gigha stands Ardailly  Mill. It's in an idyllic spot on Gigha's remote west shore, looking out to the neighbouring islands of Islay and Jura. In this photograph it is seen with building works under way, transforming the old millers cottage into someone's dream house.....
Ardailly Mill and miller's cottage
At the far end of a long and winding track on the Isle of Gigha stands Ardailly Mill. It's in an idyllic spot on Gigha's remote west shore, looking out to the neighbouring islands of Islay and Jura. In this photograph it is seen with building works under way, transforming the old millers cottage into someone's dream house.....
Grassland near Ardailly Looking towards the west coast of Gigha and beyond to the Paps of Jura. Just visible (towards the left) are the gables of the ruined old water mill at Port An Duin, which dates from the 18th century.
Grassland near Ardailly
Looking towards the west coast of Gigha and beyond to the Paps of Jura. Just visible (towards the left) are the gables of the ruined old water mill at Port An Duin, which dates from the 18th century.
Looking towards the Paps of Jura From near Ardailly on the west coast of Gigha.
Looking towards the Paps of Jura
From near Ardailly on the west coast of Gigha.
Approaching Rain at Creag Bhan, Gigha
Approaching Rain at Creag Bhan, Gigha
Gigha trig point at Creag Bhan
Gigha trig point at Creag Bhan
North east view from Gigha trig point
North east view from Gigha trig point
East view from Gigha trig point
East view from Gigha trig point
North view from Gigha trig point
North view from Gigha trig point
West view from Gigha trig point
West view from Gigha trig point
Summit of Creag Bhan The toposcope or topograph on the summit of Creag Bhan the highest point on Gigha
Summit of Creag Bhan
The toposcope or topograph on the summit of Creag Bhan the highest point on Gigha
Meadowsweet view A view across boggy ground towards the coast which includes a luxuriant growth of wet-loving plants such as Meadowsweet, Loosestrife and Iris. I had difficulty in identifying the dun which is labelled on the map, but the profile of Islay on the skyline made up for it.
Meadowsweet view
A view across boggy ground towards the coast which includes a luxuriant growth of wet-loving plants such as Meadowsweet, Loosestrife and Iris. I had difficulty in identifying the dun which is labelled on the map, but the profile of Islay on the skyline made up for it.
Coastal rock outcrops The shore of the small inlet of Garbh Phort comprises sheared metasedimentary rocks belonging to the Dalradian intruded by a thick dyke of Palaeogene basalt. The dykes are associated with the extensive volcanism which is characteristic of Mull, and the Hebrides.
Coastal rock outcrops
The shore of the small inlet of Garbh Phort comprises sheared metasedimentary rocks belonging to the Dalradian intruded by a thick dyke of Palaeogene basalt. The dykes are associated with the extensive volcanism which is characteristic of Mull, and the Hebrides.
Ardailly view A view from Creag Bhan of the farm at Ardailly with the Mill Loch appearing at the left of the image.
Ardailly view
A view from Creag Bhan of the farm at Ardailly with the Mill Loch appearing at the left of the image.
Creag Bhan rocks and trig The summit of Creag Bhan is a magnificently ice-moulded landscape surmounted by a cairn and triangulation pillar. That the hill survives this obvious abrasion is a surprise, since the surrounding rocks are obviously much lower. The reason is that the hill comprises a massive body of amphibolite, a relic of basaltic magmatism that affected the sedimentary succession long before the Caledoniam metamorphism which produced the classic Dalradian metasediments. Most of the prominent ridges and hills on the island have the same origin, including Eilean Garbh <a href="https://www.geograph.org.uk/gridref/NR6554">NR6554</a> which can be seen in the near distance.
Creag Bhan rocks and trig
The summit of Creag Bhan is a magnificently ice-moulded landscape surmounted by a cairn and triangulation pillar. That the hill survives this obvious abrasion is a surprise, since the surrounding rocks are obviously much lower. The reason is that the hill comprises a massive body of amphibolite, a relic of basaltic magmatism that affected the sedimentary succession long before the Caledoniam metamorphism which produced the classic Dalradian metasediments. Most of the prominent ridges and hills on the island have the same origin, including Eilean Garbh NR6554 which can be seen in the near distance.
Sheared outcrop Rock strata on the coast comprise metasedimentary rocks belonging to the Dalradian. These have not only suffered metamorphism due to heat and pressure compacting the rocks and generating schist, but intense shearing movement which has created an almost slatey texture. This is not a hospitable environment for exploration!
Sheared outcrop
Rock strata on the coast comprise metasedimentary rocks belonging to the Dalradian. These have not only suffered metamorphism due to heat and pressure compacting the rocks and generating schist, but intense shearing movement which has created an almost slatey texture. This is not a hospitable environment for exploration!
Rock sculpture garden The slatey outcrops of the Dalradian metasediments have eroded very deeply to create exceptionally delicate projections. These cannot have originated during the abrasive action of glaciers passing through, so must instead be periglacial (eroded by frost action in the absence of glacier cover) or more modern in origin. Sometimes there are even neat holes right through the projecting plates. This is a remarkable and delicate landscape.
Rock sculpture garden
The slatey outcrops of the Dalradian metasediments have eroded very deeply to create exceptionally delicate projections. These cannot have originated during the abrasive action of glaciers passing through, so must instead be periglacial (eroded by frost action in the absence of glacier cover) or more modern in origin. Sometimes there are even neat holes right through the projecting plates. This is a remarkable and delicate landscape.
Creag Bhan on Isle of Gigha Creag Bhan on Isle of Gigha, looking north with Paps of Jura in distance
Creag Bhan on Isle of Gigha
Creag Bhan on Isle of Gigha, looking north with Paps of Jura in distance
Show me another place!

Acairseid na h-Uamhaidh Mòire is located at Grid Ref: NR6349 (Lat: 55.683398, Lng: -5.7663939)

Unitary Authority: Argyll and Bute

Police Authority: Argyll and West Dunbartonshire

What 3 Words

///instance.caressed.polite. Near Craighouse, Argyll & Bute

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Located within 500m of 55.683398,-5.7663939
Created By: dmgroom_coastlines
Lat/Long: 55.679587/-5.770206
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Lat/Long: 55.681071/-5.766911
Created By: dmgroom_coastlines
Lat/Long: 55.683669/-5.765281
Created By: dmgroom_coastlines
Lat/Long: 55.684181/-5.765317
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Lat/Long: 55.684692/-5.765353
Created By: dmgroom_coastlines
Lat/Long: 55.685981/-5.764991
Created By: dmgroom_coastlines
Lat/Long: 55.686237/-5.765009
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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