Brae of Bognie

Downs, Moorland in Aberdeenshire

Scotland

Brae of Bognie

Entrance to Forgue
Entrance to Forgue Credit: Alex McGregor

Brae of Bognie is a picturesque area located in Aberdeenshire, Scotland. Situated on the eastern edge of the Grampian Mountains, it is characterized by its stunning downs and moorland landscapes.

The downs of Brae of Bognie offer wide expanses of open grasslands, gently rolling hills, and panoramic views of the surrounding countryside. The grasslands are home to a variety of plant species, including heather, gorse, and wildflowers, providing a vibrant burst of color during the summer months. These downs also support a diverse range of bird species, including curlews, lapwings, and skylarks, making it a haven for birdwatching enthusiasts.

The moorland of Brae of Bognie showcases the unique flora and fauna of the Scottish uplands. It consists of vast stretches of heather-covered hills, interspersed with peat bogs and small lochs. The moorland is home to various species, such as red grouse, golden plovers, and mountain hares, which have adapted to the harsh conditions of this environment.

Brae of Bognie is a popular destination for nature lovers and outdoor enthusiasts. It offers numerous opportunities for hiking, walking, and wildlife spotting. The area is crisscrossed by a network of trails, allowing visitors to explore its diverse landscapes and discover its hidden gems. The tranquility and untouched beauty of Brae of Bognie make it an ideal place for those seeking an escape from the hustle and bustle of city life.

Overall, Brae of Bognie is a captivating region in Aberdeenshire that showcases the natural beauty of Scotland's downs and moorland. Its unspoiled landscapes and rich biodiversity make it a must-visit location for anyone with an appreciation for the great outdoors.

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Brae of Bognie Images

Images are sourced within 2km of 57.499274/-2.687367 or Grid Reference NJ5845. Thanks to Geograph Open Source API. All images are credited.

Entrance to Forgue
Entrance to Forgue
Yonder Bognie Recumbent Stone Circle (1) Only nine of the stones here are thought to be parts of the original circle, the rest being boulders collected from the fields and dumped inside the circle. See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more details. <a href="https://www.geograph.org.uk/photo/4743276">NJ6045 : Yonder Bognie Recumbent Stone Circle (2)</a>
Yonder Bognie Recumbent Stone Circle (1)
Only nine of the stones here are thought to be parts of the original circle, the rest being boulders collected from the fields and dumped inside the circle. See LinkExternal link for more details. NJ6045 : Yonder Bognie Recumbent Stone Circle (2)
Yonder Bognie Recumbent Stone Circle (2) The recumbent and west flanker are still standing. The alignment of the recumbent is towards the Hill of Foudland in <a href="https://www.geograph.org.uk/gridref/NJ6033">NJ6033</a>. See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743288">NJ6045 : Yonder Bognie Recumbent Stone Circle (3)</a>
Yonder Bognie Recumbent Stone Circle (2)
The recumbent and west flanker are still standing. The alignment of the recumbent is towards the Hill of Foudland in NJ6033. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (3)
Yonder Bognie Recumbent Stone Circle (3) This shows the recumbent setting. The recumbent and west flanker (on the left) are still standing, but the east flanker has fallen.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743292">NJ6045 : Yonder Bognie Recumbent Stone Circle (4)</a>
Yonder Bognie Recumbent Stone Circle (3)
This shows the recumbent setting. The recumbent and west flanker (on the left) are still standing, but the east flanker has fallen. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (4)
Yonder Bognie Recumbent Stone Circle (4) Several of the stones still standing are visible in this view. At extreme left is the recumbent setting. Two of the orthostats are on the right, one close to the camera and one on the far side of the circle. The remaining stones are difficult to pick out among the dumped field boulders. <a href="https://www.geograph.org.uk/photo/4743299">NJ6045 : Yonder Bognie Recumbent Stone Circle (5)</a>
Yonder Bognie Recumbent Stone Circle (4)
Several of the stones still standing are visible in this view. At extreme left is the recumbent setting. Two of the orthostats are on the right, one close to the camera and one on the far side of the circle. The remaining stones are difficult to pick out among the dumped field boulders. NJ6045 : Yonder Bognie Recumbent Stone Circle (5)
Yonder Bognie Recumbent Stone Circle (5) This is the easternmost of the stones, and the largest of the orthostats.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743301">NJ6045 : Yonder Bognie Recumbent Stone Circle (6)</a>
Yonder Bognie Recumbent Stone Circle (5)
This is the easternmost of the stones, and the largest of the orthostats. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (6)
Yonder Bognie Recumbent Stone Circle (6) This is one of the four remaining stones in the circumference of the circle, with an accumulation of field boulders around it.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743305">NJ6045 : Yonder Bognie Recumbent Stone Circle (7)</a>
Yonder Bognie Recumbent Stone Circle (6)
This is one of the four remaining stones in the circumference of the circle, with an accumulation of field boulders around it. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (7)
Yonder Bognie Recumbent Stone Circle (7) I think the tallest stone in this collection is one of the four surviving orthostats, and the upright one in the background is another, but the rest are field boulders that have been dumped here.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743309">NJ6045 : Yonder Bognie Recumbent Stone Circle (8)</a>
Yonder Bognie Recumbent Stone Circle (7)
I think the tallest stone in this collection is one of the four surviving orthostats, and the upright one in the background is another, but the rest are field boulders that have been dumped here. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (8)
Yonder Bognie Recumbent Stone Circle (8) Closest to the camera is one of the stones of the circumference, with the recumbent setting to the right and one of the other standing stones in the background. The rest of the stones are dumped field boulders.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743316">NJ6045 : Yonder Bognie Recumbent Stone Circle (9)</a>
Yonder Bognie Recumbent Stone Circle (8)
Closest to the camera is one of the stones of the circumference, with the recumbent setting to the right and one of the other standing stones in the background. The rest of the stones are dumped field boulders. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (9)
Yonder Bognie Recumbent Stone Circle (9) The closest stone is the most northerly of the circle, now fallen and moved out of position outside the circumference. Beyond it are the two remaining stones of the east arc, another, lower, stone which appears to be on the arc but is actually inside the circle, and the end of the recumbent.  See <span class="nowrap"><a title="https://canmore.org.uk/site/18335/yonder-bognie" rel="nofollow ugc noopener" href="https://canmore.org.uk/site/18335/yonder-bognie">Link</a><img style="margin-left:2px;" alt="External link" title="External link - shift click to open in new window" src="https://s1.geograph.org.uk/img/external.png" width="10" height="10"/></span> for more information. <a href="https://www.geograph.org.uk/photo/4743267">NJ6045 : Yonder Bognie Recumbent Stone Circle (1)</a>
Yonder Bognie Recumbent Stone Circle (9)
The closest stone is the most northerly of the circle, now fallen and moved out of position outside the circumference. Beyond it are the two remaining stones of the east arc, another, lower, stone which appears to be on the arc but is actually inside the circle, and the end of the recumbent. See LinkExternal link for more information. NJ6045 : Yonder Bognie Recumbent Stone Circle (1)
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.
Misshapen Larches These two larches beside the old road from Rothiemay to Bognie appear to have suffered from growing in a spot very exposed to winter gales. The prominent hill is Knock Hill.
Misshapen Larches
These two larches beside the old road from Rothiemay to Bognie appear to have suffered from growing in a spot very exposed to winter gales. The prominent hill is Knock Hill.
End of a Yowe It looks as if this yowe (ewe to you) has climbed into the tank, been unable to climb out, and has drowned.
End of a Yowe
It looks as if this yowe (ewe to you) has climbed into the tank, been unable to climb out, and has drowned.
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.
An Obstruction The road here is obstructed by trees felled by one of the recent gales. Fortunately it was not difficult to pick our way through it.
An Obstruction
The road here is obstructed by trees felled by one of the recent gales. Fortunately it was not difficult to pick our way through it.
Fourmanhill Croft In the 19th century there were two or three crofts here, but only this cottage remains.
Fourmanhill Croft
In the 19th century there were two or three crofts here, but only this cottage remains.
Show me another place!

Brae of Bognie is located at Grid Ref: NJ5845 (Lat: 57.499274, Lng: -2.687367)

Unitary Authority: Aberdeenshire

Police Authority: North East

What 3 Words

///invent.inert.goggles. Near Aberchirder, Aberdeenshire

Nearby Locations

Brae of Bognie

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Nearby Amenities

Located within 500m of 57.499274,-2.687367
Power: pole
Lat/Long: 57.5015015/-2.6945521
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Lat/Long: 57.5019729/-2.6935968
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Lat/Long: 57.5015491/-2.6886736
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Lat/Long: 57.5012953/-2.6876187
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Lat/Long: 57.5001362/-2.6828575
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Lat/Long: 57.499807/-2.6814768
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Lat/Long: 57.4996633/-2.6803981
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Lat/Long: 57.4995253/-2.6792159
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Lat/Long: 57.4984309/-2.6842146
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Lat/Long: 57.4977158/-2.6841724
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Lat/Long: 57.4971934/-2.6841283
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Lat/Long: 57.496671/-2.6840976
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Lat/Long: 57.4960331/-2.6840497
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Lat/Long: 57.4954983/-2.6840036
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Lat/Long: 57.497314/-2.6852654
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Lat/Long: 57.4974428/-2.6864256
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Lat/Long: 57.4976231/-2.6878139
Power: pole
Lat/Long: 57.4978158/-2.689185
Power: pole
Lat/Long: 57.4980033/-2.6905657
Man Made: mast
Lat/Long: 57.5018312/-2.6825202
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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