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Mayen Wood

Wood, Forest in Banffshire

Scotland

Mayen Wood

Track near Moss-Side of Mayen With forested Catstone Hill beyond.
Track near Moss-Side of Mayen Credit: Alan Hodgson

Mayen Wood is a picturesque forest located in the county of Banffshire, Scotland. Covering an area of approximately 500 acres, this enchanting woodland is known for its natural beauty and diverse ecosystem. It is situated near the village of Mayen, offering visitors a peaceful escape into nature.

The wood is predominantly comprised of native trees, including Scots pine, birch, oak, and rowan. These trees provide a dense canopy that creates a cool and shaded environment, even on warm summer days. The forest floor is carpeted with a variety of wildflowers, ferns, and mosses, adding to the vibrant and colorful atmosphere.

Mayen Wood is home to a wide range of wildlife, making it a haven for nature enthusiasts. Visitors may spot red squirrels, roe deer, and a variety of bird species, such as woodpeckers and owls. The tranquil setting also attracts photographers and artists, who are drawn to the serene ambiance and the opportunity to capture the beauty of the woodland.

There are several walking trails and footpaths that wind through Mayen Wood, allowing visitors to explore its enchanting landscapes at their own pace. These paths offer stunning views of the surrounding countryside and provide an opportunity to immerse oneself in the sights and sounds of nature.

Mayen Wood is a popular destination for both locals and tourists alike, offering a peaceful and serene escape from the hustle and bustle of everyday life. Its natural beauty, diverse wildlife, and well-maintained trails make it a must-visit location for those seeking a tranquil and immersive woodland experience in Banffshire.

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Mayen Wood Images

Images are sourced within 2km of 57.526567/-2.7110742 or Grid Reference NJ5748. Thanks to Geograph Open Source API. All images are credited.

Track near Moss-Side of Mayen With forested Catstone Hill beyond.
Track near Moss-Side of Mayen
With forested Catstone Hill beyond.
Cairn of Mayen
Cairn of Mayen
Hill of Retenach Viewed from Hill of Cairns.
Hill of Retenach
Viewed from Hill of Cairns.
Mayen and the River Deveron In the middle distance is Mayen, which is almost surrounded by a meander of the River Deveron, which turns from flowing south-eastwards to flowing northwards in just a couple of miles. The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
Mayen and the River Deveron
In the middle distance is Mayen, which is almost surrounded by a meander of the River Deveron, which turns from flowing south-eastwards to flowing northwards in just a couple of miles. The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
River Deveron The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
River Deveron
The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
Mayen and the River Deveron The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. Mayen is the low hill on the opposite bank of the river from here.
Mayen and the River Deveron
The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. Mayen is the low hill on the opposite bank of the river from here.
River Deveron The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. Mayen is the cluster of buildings on the slope above the opposite bank.
River Deveron
The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. Mayen is the cluster of buildings on the slope above the opposite bank.
River Deveron The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. We were slightly hesitant because we were following a published walk description directing us straight across a field, and we were concerned about disturbing cattle, but the old maps confirm that there was a proper road here for a long time. We saw no cattle or other livestock, otherwise we would have gone round the edge of the field instead of straight across. Under the 'Right to Roam' (Land Reform (Scotland) Act 2003) we are of course entitled to walk across a field, even if it contains livestock, but I don't relish the idea of trying to explain the law to a belligerent bull or angry cow.
River Deveron
The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago. We were slightly hesitant because we were following a published walk description directing us straight across a field, and we were concerned about disturbing cattle, but the old maps confirm that there was a proper road here for a long time. We saw no cattle or other livestock, otherwise we would have gone round the edge of the field instead of straight across. Under the 'Right to Roam' (Land Reform (Scotland) Act 2003) we are of course entitled to walk across a field, even if it contains livestock, but I don't relish the idea of trying to explain the law to a belligerent bull or angry cow.
River Deveron The River Deveron, looking upstream in the direction of Milltown of Rothiemay, with Tower Hill to the right above the incised meander. The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
River Deveron
The River Deveron, looking upstream in the direction of Milltown of Rothiemay, with Tower Hill to the right above the incised meander. The glen of the Deveron between Rothiemay and Turriff is an excellent example of incised meanders, where the twisting course of an ancient river has been preserved as the river has cut down into the underlying bedrock. The bedrock here is mainly pelite and psammite, formed by metamorphosis of mudstones and sandstones deposited in a deep sea environment between 500 and 1000 million years ago.
Woodfold Farm One of a series of farms on the slope above the right bank of the River Deveron.
Woodfold Farm
One of a series of farms on the slope above the right bank of the River Deveron.
Mains of Mayen Viewed from above the opposite bank of the River Deveron.
Mains of Mayen
Viewed from above the opposite bank of the River Deveron.
Snow Shower So much for getting some sunlit shots from the road on the right bank of the River Deveron. The weather had been getting steadily worse, and we found ourselves walking into the teeth of an icy shower. This is the view back, with the camera facing away from the windblown snow.
Snow Shower
So much for getting some sunlit shots from the road on the right bank of the River Deveron. The weather had been getting steadily worse, and we found ourselves walking into the teeth of an icy shower. This is the view back, with the camera facing away from the windblown snow.
View North West from the Hill of Retenach There was no sign of the Cairns of Keith mentioned on the map.
View North West from the Hill of Retenach
There was no sign of the Cairns of Keith mentioned on the map.
Hill of Retanach The hill has been cleared of useful trees but no sign of the Cairns of Keith mentioned on the OS map.
Hill of Retanach
The hill has been cleared of useful trees but no sign of the Cairns of Keith mentioned on the OS map.
Cairns of Mayen Farm Buildings With the tree covered Catstone Hill beyond.
Cairns of Mayen Farm Buildings
With the tree covered Catstone Hill beyond.
Looking towards Knock Hill from Inchcorsie
Looking towards Knock Hill from Inchcorsie
Pool by the fishing hut on the Rothiemay beat, River Deveron. A very successful salmon and sea trout river, the River Deveron fishing season lasts from 11th February till the 31st of October.
Pool by the fishing hut on the Rothiemay beat, River Deveron.
A very successful salmon and sea trout river, the River Deveron fishing season lasts from 11th February till the 31st of October.
Rothiemay beat fishing hut. The hut is situated on the banks of the River Deveron.
Rothiemay beat fishing hut.
The hut is situated on the banks of the River Deveron.
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Mayen Wood is located at Grid Ref: NJ5748 (Lat: 57.526567, Lng: -2.7110742)

Unitary Authority: Moray

Police Authority: North East

What 3 Words

///rave.drip.unity. Near Aberchirder, Aberdeenshire

Nearby Locations

Mayen Wood Hill of Mayen

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Nearby Amenities

Located within 500m of 57.526567,-2.7110742
Caple Hill
Ele: 247
Natural: peak
Lat/Long: 57.5245707/-2.7159678
OpenStreetMap
Google Maps
Hill of Mayen
Ele: 186
Natural: peak
Lat/Long: 57.5256306/-2.7065693
OpenStreetMap
Google Maps
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.
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