Mingulay Bay, Outer Hebrides - from Aneir - postcard by Charles Tait c.1990s

• Postcard

   

• Picture / Image:  Mingulay Bay [Outer Hebrides] from Aneir
• Publisher: Charles Tait (No. W048)
• Postally used: no - has long message but not posted
• Stamp:  n/a
• Postmark(s): n/a
• Sent to:  n/a
• Notes / condition: 

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Image may be low res for illustrative purposes - if you need a higher definition image then please contact me and I may be able to send one. No cards have been trimmed (unless stated).

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NOTE: All postcards are sent in brand new stiffened envelopes which I have bought for the task. These are specially made to protect postcards and you may be able to re-use them. In addition there are other costs to sending so the above charge is not just for the stamp!

I will give a full refund if you are not fully satisfied with the postcard.

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Text from the free encyclopedia WIKIPEDIA may appear below to give a little background information (internal links may not  work) :

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Mingulay (Scottish Gaelic: Miughalaigh)[5] is the second largest of the Bishop's Isles in the Outer Hebrides of Scotland. Located 12 miles (19 km) south of Barra, it is known for its important seabird populations, including puffins, black-legged kittiwakes, and razorbills, which nest in the sea-cliffs,[6] amongst the highest in the British Isles.[7]

There are Iron Age remains, and the culture of the island was influenced by early Christianity and the Vikings. Between the 15th and 19th centuries Mingulay was part of the lands of Clan MacNeil of Barra, but subsequently suffered at the hands of absentee landlords.

After two thousand years or more of continuous habitation, the island was abandoned by its Gaelic-speaking residents in 1912 and has remained uninhabited since. It is no longer used for grazing sheep. The island is also associated with the "Mingulay Boat Song", although that was composed in 1938. The National Trust for Scotland has owned Mingulay since 2000.[4]

In the Pleistocene era Mingulay was covered by the ice sheets which spread from Scotland out into the Atlantic Ocean beyond the Outer Hebrides.[8] After the last retreat of the ice around 20,000 years ago, sea levels were lower than at present and circa 14,000 BP it was joined to a single large island comprising most of what is now the Outer Hebrides.[9] Steadily rising sea levels since that time then isolated the island, which is made up of Hebridean gneiss interspersed with some granite.[1] The ice deposited both erratic blocks of rock and boulder clay on the eastern side of the island around Mingulay Bay. The rest of the island is covered in peat, thin acidic soils, or bare rock.[4]