The area between the North and South Ayres is known as The Houb and it contains submerged peat deposits and in situ tree stumps, which have been dated as being c4600 years old. They were submerged as a result of rising sea levels at the end of the last ice age.
The Ayres of Swinister are a rare example of a triple gravel tombolo-barrier complex, where a tombolo, bay-head barrier and mid bay barrier are located in close proximity.
The island of Fora Ness, which is 1 mile long by just under a mile wide, is covered with grass and heather moorland. The highest point is 100 metres above sea level. I didn't explore it very thoroughly, as its was cold and windy with intermittent horizontal hail showers on the day I visited.
North Ayre from Mainland
South Ayre looking towards Fora Ness
South Ayre looking towards Fora Ness
South Ayre from Fora Ness
North Ayre from Fora Ness
South Ayre from Mainland
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