Coed Llewelyn

Wood, Forest in Anglesey

Wales

Coed Llewelyn

A4080, west of Malltreath The A4080 road runs for 24½ miles along the southwestern side of Anglesey. It starts on the A5 at Llanfair Pwllgwyngyll and passes through several villages before terminating on the A5 between Bryngwran and Gwalchmai. — A4080, west of Malltreath Credit: David Dixon

Coed Llewelyn is a picturesque woodland located on the Isle of Anglesey in North Wales, United Kingdom. Covering an area of approximately 200 acres, it is one of the largest and most diverse woodlands on the island. The name "Coed Llewelyn" translates to "Llewelyn's Wood" in English, paying homage to Prince Llewelyn the Great, who is believed to have once owned the land.

The woodland is characterized by its rich and varied flora and fauna. It is predominantly composed of native broadleaf trees such as oak, birch, and beech, creating a lush and verdant environment. These trees provide a habitat for a wide range of wildlife, including birds, small mammals, and insects. The woodland floor is carpeted with an array of wildflowers, adding bursts of color and attracting butterflies and bees.

Coed Llewelyn offers a peaceful and tranquil escape for walkers, nature enthusiasts, and photographers alike. A network of well-maintained footpaths and trails winds through the woodland, allowing visitors to explore its hidden corners and discover its natural beauty. There are also picnic areas and benches scattered throughout the woodland, providing the perfect spots to rest and take in the surroundings.

In addition to its natural beauty, Coed Llewelyn is also of historical importance. It is believed to have been used as a hunting ground in medieval times, and remnants of ancient boundary walls and ditches can still be seen within the woodland today.

Overall, Coed Llewelyn is a haven of tranquility and natural beauty, offering visitors the opportunity to immerse themselves in the wonders of the Welsh countryside.

Show me another place!

If you have any feedback on the listing, please let us know in the comments section below.

Coed Llewelyn Images

Images are sourced within 2km of 53.183637/-4.4167801 or Grid Reference SH3867. Thanks to Geograph Open Source API. All images are credited.

A4080, west of Malltreath

The A4080 road runs for 24½ miles along the southwestern side of Anglesey. It starts on the A5 at Llanfair Pwllgwyngyll and passes through several villages before terminating on the A5 between Bryngwran and Gwalchmai.

David Dixon

Hermon

Hermon is a village on the island of Anglesey. It is located on the A4080 road, roughly halfway between Newborough and Aberffraw, some 6 miles to the southwest of Llangefni.

David Dixon

A4080, Hermon

Hermon is a village on the island of Anglesey. It is located on the A4080 road, roughly halfway between Newborough and Aberffraw, some 6 miles to the southwest of Llangefni.

David Dixon

Llangadwaladr, The Old School

Opened on 17th February 1873; one of a number of similar schools built during the nineteenth century prominently sited to form one of the focal points of the village landscape. The school was closed by 1904 and subsequently converted for domestic use. It is a Grade II listed building (Cadw reference 20407 Link

David Dixon

A4080 towards Aberffraw

Travelling westwards here, the A4080 continues as a dead-straight road across the dunes and the Afon Ffraw to reach Aberffraw.

David Dixon

Ysgol Bodorgan

Anthony Parkes

Former Military Buildings Associated With RAF Bodorgan

Chris Andrews

A view of Ty Gwyn, Llangadwaladr, Isle of Anglesey

The Old farmhouse known as Ty Gwyn near Llangadwaladr, built before 1734.

Stephen Elwyn RODDICK

A4080 approaching junction with B4422

Near Ty Mawr

John Firth

A4080 through Hermon westwards

Phone box can be seen on the left beyond the turning

John Firth

Sediments ancient and modern

Looking over an outcrop of the Gwna Melange, a metamorphosed sedimentary rock of Cambrian age to the contemporary sediments of the Malltraeth Sands. The Afon Cefni channel can be seen in the middle distance, at approximately low tide. The sea-washed rock outcrop has a thick growth of lichens.

Jonathan Wilkins

Tideline walkers

A party of geologists walking along the Malltraeth shore on an organised excursion.

Jonathan Wilkins

Concretions in sandstone

Variable cementing of the sandstone, Carboniferous in age, by carbonates has resulted in irregular weathering and the appearance of large, dark-coloured nodules on the eroded surfaces. The presence of bedding planes passing straight through some nodules is indicative of the structure being secondary in nature. The dark colour is largely due to the slow ablation of the surface compared to less heavily-cemented areas, and the surface is stable enough to be colonised by lichens (yellow Caloplaca is prominent).

Jonathan Wilkins

Conglomerate beds

Beds of a pebble conglomerate dip steadily to the right in this image. It is widely regarded as being a basal formation to the local Carboniferous outcrop, but here its position in the stratigraphy is rather obscure. Similar beds can be found at the side of Lligwy Bay SH5087 where limestone is also in evidence.

Jonathan Wilkins

Outcrop of unconformity

At the left of this image rocks belonging to the Gwna Melange can be seen. These are of Pre-Cambrian age and significantly metamorphosed. Falling down and spreading over the ancient topography, a rough cliff-like feature, are much younger rocks comprising a scree of angular debris obviously derived from the Gwna Melange. Higher up the succession, to the top right of the image the sediments are more obviously bedded and fine-grained in nature. The younger sediments are widely regarded to be of Devonian age, but may be Carboniferous as there is a lack of diagnostic fossils. A walking stick is stuck into a small thrust fault in the Gwna Melange for scale.

Jonathan Wilkins