Big Covert

Wood, Forest in Denbighshire

Wales

Big Covert

Windswept trees
Windswept trees Credit: John H Darch

Big Covert is a vast woodland located in Denbighshire, Wales. Covering a substantial area, this forest is known for its remarkable size and dense vegetation, making it a popular destination for nature enthusiasts and outdoor adventurers.

The woodland is characterized by its diverse range of tree species, including oak, beech, and pine, among others. These trees create a rich and vibrant canopy, providing a haven for numerous bird species and other wildlife. The forest floor is adorned with a thick carpet of ferns, mosses, and wildflowers, adding to the beauty and biodiversity of the area.

Big Covert offers a variety of recreational activities for visitors to enjoy. Hiking and walking trails crisscross the forest, allowing visitors to explore its hidden nooks and crannies. These paths offer breathtaking views of the surrounding landscape and provide an opportunity to observe the flora and fauna up close.

For those seeking a more adventurous experience, the forest also offers opportunities for mountain biking and horseback riding. The undulating terrain and well-maintained trails make it a perfect destination for outdoor enthusiasts of all skill levels.

Additionally, Big Covert is home to a number of picnic areas and camping sites, providing an ideal setting for a family outing or a weekend getaway. Visitors can immerse themselves in the tranquility of the forest, enjoying the fresh air and the soothing sounds of nature.

Overall, Big Covert in Denbighshire is a captivating woodland that offers a wealth of recreational opportunities and a chance to connect with nature in a truly picturesque setting.

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Big Covert Images

Images are sourced within 2km of 53.132699/-3.1997495 or Grid Reference SJ1960. Thanks to Geograph Open Source API. All images are credited.

Windswept trees
Windswept trees
Limestone pavement on Bryn Alyn
Limestone pavement on Bryn Alyn
Collapse structure The removal of material from this mineral vein running east-west on the hilltop plateau has resulted in collapse and soil has washed down into the void, leaving this linear feature on the ground. Spoil heaps <a href="https://www.geograph.org.uk/photo/2641740">SJ1959 : Spoil tip</a> and dressing areas can be identified in the valley to the west of this point, and still yield small amounts of calcite spar and galena (lead ore).
Collapse structure
The removal of material from this mineral vein running east-west on the hilltop plateau has resulted in collapse and soil has washed down into the void, leaving this linear feature on the ground. Spoil heaps SJ1959 : Spoil tip and dressing areas can be identified in the valley to the west of this point, and still yield small amounts of calcite spar and galena (lead ore).
Limestone outcrop A rugged and eroded outcrop of limestone at the top of the hill with a view over Pant-du towards Tir-y-coed.
Limestone outcrop
A rugged and eroded outcrop of limestone at the top of the hill with a view over Pant-du towards Tir-y-coed.
Holly tree A holly tree which has sprung up in the shelter of the field wall has suffered the ravages of the weather.
Holly tree
A holly tree which has sprung up in the shelter of the field wall has suffered the ravages of the weather.
Track to Bryn Alyn The farm track only carries a public footpath, but in the past it was much more important as it was the access to the busy mining field whose irregular tips can be seen in the mid-distance.
Track to Bryn Alyn
The farm track only carries a public footpath, but in the past it was much more important as it was the access to the busy mining field whose irregular tips can be seen in the mid-distance.
Disturbed ground The hummocky, disturbed ground in the near part of this image is the legacy of much mining activity, which tapped the lead veins of the Carboniferous Limestone in this area. The depression in the foreground is probably the remains of a shaft which has collapsed and slowly filled with spoil from the surface.
Disturbed ground
The hummocky, disturbed ground in the near part of this image is the legacy of much mining activity, which tapped the lead veins of the Carboniferous Limestone in this area. The depression in the foreground is probably the remains of a shaft which has collapsed and slowly filled with spoil from the surface.
Winding house The remains of an engine or winding house adjacent to one of the many shafts sunk for access to the lead veins crossing the area. The remains of thick iron bars which secured machinery to heavy timbers, now rotted away, can still be found on the level platform to the right of the walls imaged here. Spoil raised from the shaft was tipped nearby, and can still be seen although the heaps are mostly grass-covered.
Winding house
The remains of an engine or winding house adjacent to one of the many shafts sunk for access to the lead veins crossing the area. The remains of thick iron bars which secured machinery to heavy timbers, now rotted away, can still be found on the level platform to the right of the walls imaged here. Spoil raised from the shaft was tipped nearby, and can still be seen although the heaps are mostly grass-covered.
Bryn Alyn Limestone country easily approach from east and well worth walking to all 3 likely tops...as the least interesting one is the highest. Dry with some occasional sunshine.
Name: Bryn Alyn
Hill number: 5156
Height: 408.3m / 1340ft
Area: 30C: Llandudno to Wrexham
Class: Hu
Grid ref: SJ 20082 58752
Summit feature: no feature: grassy top
Drop: 100.9m
Bryn Alyn
Limestone country easily approach from east and well worth walking to all 3 likely tops...as the least interesting one is the highest. Dry with some occasional sunshine. Name: Bryn Alyn Hill number: 5156 Height: 408.3m / 1340ft Area: 30C: Llandudno to Wrexham Class: Hu Grid ref: SJ 20082 58752 Summit feature: no feature: grassy top Drop: 100.9m
Limestone pavement The pavement of Bryn Alyn is an SSSI, and the largest area of such pavement away from the North Wales coastal outcrop of the Carboniferous Limestone. In this image, the hillside and pavement form a natural 'dip' surface which reflects the tilt of the bedded limestone formation.
Limestone pavement
The pavement of Bryn Alyn is an SSSI, and the largest area of such pavement away from the North Wales coastal outcrop of the Carboniferous Limestone. In this image, the hillside and pavement form a natural 'dip' surface which reflects the tilt of the bedded limestone formation.
Gorse scrub Gorse and occasional heather make an impenetrable scrub in the rough pasture of Bryn Alyn amid outcrops of Carboniferous Limestone.
Gorse scrub
Gorse and occasional heather make an impenetrable scrub in the rough pasture of Bryn Alyn amid outcrops of Carboniferous Limestone.
Limestone outcrop Outcrops on the hillside are composed of the Loggerheads Limestone, of Carboniferous (Asbian) age. This rock is very pure and valuable and is exploited in a number of quarries nearby.
Limestone outcrop
Outcrops on the hillside are composed of the Loggerheads Limestone, of Carboniferous (Asbian) age. This rock is very pure and valuable and is exploited in a number of quarries nearby.
Spoil tip Despite the value of limestone for agricultural or metallurgical use, here it is mineral veins that have resulted in digging and tipping of waste rock. A mineralised fracture intersects the crags just to the right of the image and a fan of debris has been thrown down the hill.
Spoil tip
Despite the value of limestone for agricultural or metallurgical use, here it is mineral veins that have resulted in digging and tipping of waste rock. A mineralised fracture intersects the crags just to the right of the image and a fan of debris has been thrown down the hill.
A494 south of Llanferres
A494 south of Llanferres
Flowers On top of the ridge at the southern end of Big Covert
Flowers
On top of the ridge at the southern end of Big Covert
Bryn Alyn Looking towards Bryn Alyn from the top of the hill in Big Covert.
Bryn Alyn
Looking towards Bryn Alyn from the top of the hill in Big Covert.
Pot Hole Quarry, Llanferres A popular limestone escarpment for climbers.
Pot Hole Quarry, Llanferres
A popular limestone escarpment for climbers.
Road at Pant Du On a typically damp Welsh day.
Road at Pant Du
On a typically damp Welsh day.
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Big Covert is located at Grid Ref: SJ1960 (Lat: 53.132699, Lng: -3.1997495)

Unitary Authority: Denbighshire

Police Authority: North Wales

What 3 Words

///lung.coconuts.applauded. Near Mold, Flintshire

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Nearby Amenities

Located within 500m of 53.132699,-3.1997495
Burley Hill
Ele: 352
Natural: peak
Lat/Long: 53.1341772/-3.1960662
Man Made: mineshaft
Lat/Long: 53.1339912/-3.2054139
Man Made: mineshaft
Lat/Long: 53.1339412/-3.2050313
Carolyn Guillot
Historic: memorial
Lat/Long: 53.1324817/-3.200363
Information: guidepost
Tourism: information
Lat/Long: 53.1353/-3.2023477
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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