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Craigmancie Woods

Wood, Forest in Banffshire

Scotland

Craigmancie Woods

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 Credit: Anne Burgess

Craigmancie Woods, located in Banffshire, is a picturesque woodland area renowned for its natural beauty and diverse flora and fauna. Spanning over a vast expanse, the woods are a popular destination for locals and tourists alike, offering a serene escape from the hustle and bustle of city life.

The woodland is characterized by its dense canopy of towering trees, primarily consisting of native Scottish species such as oak, birch, and pine. These trees provide shelter and a suitable habitat for a wide array of wildlife, including red squirrels, roe deer, and various species of birds.

Tranquil walking trails wind their way through the woods, allowing visitors to immerse themselves in the serene ambiance and explore the natural wonders at their own pace. The paths are well-maintained and offer varying levels of difficulty, catering to both casual strollers and more avid hikers.

Craigmancie Woods also boasts several clearings and picnic spots, providing opportunities for visitors to relax and enjoy a picnic amidst the natural surroundings. The peaceful atmosphere, coupled with the gentle rustling of leaves and chirping of birds, creates a truly idyllic setting.

Moreover, the woods are a haven for nature enthusiasts and photographers, as the changing seasons bring forth a kaleidoscope of colors, from the vibrant hues of autumn foliage to the delicate blossoms of spring. The diversity of the woodland landscape ensures stunning photo opportunities year-round.

In conclusion, Craigmancie Woods in Banffshire is a captivating destination for nature lovers, offering a tranquil retreat amidst the beauty of Scottish woodlands. Its rich biodiversity, well-maintained trails, and peaceful ambiance make it a must-visit location for those seeking solace in nature.

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Craigmancie Woods Images

Images are sourced within 2km of 57.519331/-2.6859914 or Grid Reference NJ5947. Thanks to Geograph Open Source API. All images are credited.

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.
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 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.
Broken Tree More evidence of damage by recent gales. This tree has broken as it fell, and it was no problem to step over it.
Broken Tree
More evidence of damage by recent gales. This tree has broken as it fell, and it was no problem to step over it.
Fallen Beech A mature beech felled by a recent gale. It must have blocked the road, and has been dealt with by a chainsaw. There's going to be no shortage of firewood in the next year or two.
Fallen Beech
A mature beech felled by a recent gale. It must have blocked the road, and has been dealt with by a chainsaw. There's going to be no shortage of firewood in the next year or two.
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.
An Old Petrol Pump Or perhaps a diesel pump. It stands just beside the road at Corniehaugh Farm, but it's obviously some years since it dispensed any fuel.
An Old Petrol Pump
Or perhaps a diesel pump. It stands just beside the road at Corniehaugh Farm, but it's obviously some years since it dispensed any fuel.
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.
Woodhead Steading Woodhead Farm by Auchingoul.
Woodhead Steading
Woodhead Farm by Auchingoul.
Cottages at Yonder Bognie The Bed and Breakfast signs belong to a house further down the road.
Cottages at Yonder Bognie
The Bed and Breakfast signs belong to a house further down the road.
Snowcrops at Yonder Bognie The farm buildings of Yonder Bognie are on the right hand side of the A97. The B and B signs are for the house on the left.
Snowcrops at Yonder Bognie
The farm buildings of Yonder Bognie are on the right hand side of the A97. The B and B signs are for the house on the left.
River Deveron from Marnoch Cemetery
River Deveron from Marnoch Cemetery
Corniehaugh fishing hut on the southern banks of the Deveron. The fishing hut opposite is that of Mains of Mayen.
Corniehaugh fishing hut on the southern banks of the Deveron.
The fishing hut opposite is that of Mains of Mayen.
Corniehaugh cattle graze on the fertile banks of the Deveron.
Corniehaugh cattle graze on the fertile banks of the Deveron.
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Craigmancie Woods is located at Grid Ref: NJ5947 (Lat: 57.519331, Lng: -2.6859914)

Unitary Authority: Moray

Police Authority: North East

What 3 Words

///handed.tastes.slimming. Near Aberchirder, Aberdeenshire

Nearby Locations

Craigmancie Woods Hill of Craigmancie

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Nearby Amenities

Located within 500m of 57.519331,-2.6859914
Power: pole
Lat/Long: 57.5187546/-2.6785317
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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