Western Gully

Valley in Caernarfonshire

Wales

Western Gully

Emerging onto flat ground A few minutes after <a href="https://www.geograph.org.uk/photo/1671327">SH6562 : Down the headwall of Cwm Ffynnon Lloer, winter conditions</a>, and just about at the top of the steep frozen snowslope that covered the scree on the hillside. The steep craggy buttresses of Craig Lloer are visible behind the climber, with a tiny patch of open water in Llyn Lloer in the depths of the cwm below.
Emerging onto flat ground Credit: Richard Law

Western Gully is a picturesque valley located in the county of Caernarfonshire, Wales. Nestled amidst the stunning Snowdonia National Park, this valley offers breathtaking views and a serene atmosphere that attracts nature enthusiasts and hikers from around the world.

The valley is encompassed by towering mountains, with the majestic peaks of Snowdon and Glyderau dominating the skyline. As a result, Western Gully benefits from a unique microclimate, with an abundance of rainfall that nourishes the lush vegetation and cascading waterfalls that adorn the landscape.

The valley boasts a diverse range of flora and fauna, making it a haven for wildlife lovers. Rare species such as the red kite, peregrine falcon, and otter can be spotted in their natural habitats, adding to the allure of this natural wonder.

For adventure seekers, Western Gully provides an array of outdoor activities. Hiking and climbing opportunities are aplenty, with challenging trails that lead to panoramic viewpoints offering unparalleled vistas of the surrounding mountains and valleys. The valley is also intersected by the Afon Colwyn River, providing opportunities for fishing and canoeing.

Western Gully is not only a natural paradise but also steeped in history and culture. The remnants of ancient settlements and hill forts can be found scattered throughout the valley, offering a glimpse into the area's rich past.

With its awe-inspiring scenery, abundant wildlife, and a plethora of outdoor activities, Western Gully is a must-visit destination for those seeking solace in the embrace of nature.

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Western Gully Images

Images are sourced within 2km of 53.148196/-3.9891618 or Grid Reference SH6763. Thanks to Geograph Open Source API. All images are credited.

Emerging onto flat ground A few minutes after <a href="https://www.geograph.org.uk/photo/1671327">SH6562 : Down the headwall of Cwm Ffynnon Lloer, winter conditions</a>, and just about at the top of the steep frozen snowslope that covered the scree on the hillside. The steep craggy buttresses of Craig Lloer are visible behind the climber, with a tiny patch of open water in Llyn Lloer in the depths of the cwm below.
Emerging onto flat ground
A few minutes after SH6562 : Down the headwall of Cwm Ffynnon Lloer, winter conditions, and just about at the top of the steep frozen snowslope that covered the scree on the hillside. The steep craggy buttresses of Craig Lloer are visible behind the climber, with a tiny patch of open water in Llyn Lloer in the depths of the cwm below.
On the hillside above Glan Dena On the first part of the climb up from the A5 at the eastern end of Llyn Ogwen, heading for a fine winter day out around the hills of the southern Carneddau. The route on this occasion took the Wrekin Mountaineering Club members directly up the steep headwall of Cwm Ffynnon Lloer, a line of ascent that wouldn't normally be at all wise due to masses of loose scree high up, but with a covering of frozen snow on the ground it was perfectly viable <a href="https://www.geograph.org.uk/photo/1671327">SH6562 : Down the headwall of Cwm Ffynnon Lloer, winter conditions</a>
On the hillside above Glan Dena
On the first part of the climb up from the A5 at the eastern end of Llyn Ogwen, heading for a fine winter day out around the hills of the southern Carneddau. The route on this occasion took the Wrekin Mountaineering Club members directly up the steep headwall of Cwm Ffynnon Lloer, a line of ascent that wouldn't normally be at all wise due to masses of loose scree high up, but with a covering of frozen snow on the ground it was perfectly viable SH6562 : Down the headwall of Cwm Ffynnon Lloer, winter conditions
Fallen blocks Large blocks of sandstone have fallen from the steep hillside. They preserve features such as bedding, cross-stratification and ripple-marking. In these sandstones are recorded the erosion of volcanic highlands to the north, and the deposition of the debris by braided rivers crossing wide plain to the contemporary ocean. All belong to the Llewelyn Volcanic Group (ordovician, Caradoc age).
Fallen blocks
Large blocks of sandstone have fallen from the steep hillside. They preserve features such as bedding, cross-stratification and ripple-marking. In these sandstones are recorded the erosion of volcanic highlands to the north, and the deposition of the debris by braided rivers crossing wide plain to the contemporary ocean. All belong to the Llewelyn Volcanic Group (ordovician, Caradoc age).
Competent crags Rock outcrop here is showing fewer signs of periglacial erosion and more evidence for flowing, solid ice which has carried away blocks quarried from the flanks of the valley. The cliffs of Y Braich form the backdrop to ground which is covered with moraine deposits.
Competent crags
Rock outcrop here is showing fewer signs of periglacial erosion and more evidence for flowing, solid ice which has carried away blocks quarried from the flanks of the valley. The cliffs of Y Braich form the backdrop to ground which is covered with moraine deposits.
Change of rock-type Rockfalls from the southern margin of Craig y Llyn are mostly of a dark grey sandstone (Llewelyn Volcanic Group) but there are also pale blocks of rhyolite. Looking up the slope shows a contact between grey sandstone and pale grey rhyolite, actually welded ash-flows of the Capel Curig Volcanic Formation. The silica-rich volcanic rock weathers to a very pale grey colour and is distinctive in outcrops. Both rock types are of Ordovician, Caradoc age.
Change of rock-type
Rockfalls from the southern margin of Craig y Llyn are mostly of a dark grey sandstone (Llewelyn Volcanic Group) but there are also pale blocks of rhyolite. Looking up the slope shows a contact between grey sandstone and pale grey rhyolite, actually welded ash-flows of the Capel Curig Volcanic Formation. The silica-rich volcanic rock weathers to a very pale grey colour and is distinctive in outcrops. Both rock types are of Ordovician, Caradoc age.
Craig y Llyn A cliff face developed in hard, volcanic rocks belonging to the Capel Curig Volcanic Formation (Ordovician, Caradoc). A rowan tree is growing on a rather inhospitable cliff face, but probably only survived because sheep could not reach it. The Capel Curig Volcanic Formation represents the accumulation of rhyolitic tuffs which were erupted from volcanoes spread between Tryfan and the northern coast beyond Conwy. It is chilling to consider the violence of eruptions which would hurl red-hot clouds of ash as far as 25km before they coalesced and hardened, often under water.
Craig y Llyn
A cliff face developed in hard, volcanic rocks belonging to the Capel Curig Volcanic Formation (Ordovician, Caradoc). A rowan tree is growing on a rather inhospitable cliff face, but probably only survived because sheep could not reach it. The Capel Curig Volcanic Formation represents the accumulation of rhyolitic tuffs which were erupted from volcanoes spread between Tryfan and the northern coast beyond Conwy. It is chilling to consider the violence of eruptions which would hurl red-hot clouds of ash as far as 25km before they coalesced and hardened, often under water.
Eastern flank of Pen yr Ole Wen Pen yr Ole Wen is the seventh highest mountain in Snowdonia and is the same height as England's highest, Scafell Pike. It is the most southerly of the Carneddau range. Seen from across Llyn Ogwen.
Eastern flank of Pen yr Ole Wen
Pen yr Ole Wen is the seventh highest mountain in Snowdonia and is the same height as England's highest, Scafell Pike. It is the most southerly of the Carneddau range. Seen from across Llyn Ogwen.
Looking down on Cwmglas Mawr
Looking down on Cwmglas Mawr
Rocks and the steep NE face of Mynydd Du The steep slope beyond drops down into Cwm Pen-llafar on the right, about 600ft below
Rocks and the steep NE face of Mynydd Du
The steep slope beyond drops down into Cwm Pen-llafar on the right, about 600ft below
Rocky outcrop on the ridge of Mynydd Du This is a slightly different view of the same set of rocks shown in <a href="https://www.geograph.org.uk/photo/5159020">SH6564 : Rocky outcrops on the Mynydd Du ridge</a>
Rocky outcrop on the ridge of Mynydd Du
This is a slightly different view of the same set of rocks shown in SH6564 : Rocky outcrops on the Mynydd Du ridge
Steeply down into Cwm Pen-llafar A drop of about 600ft very steeply down into the cwm below. I'd not recommend it as a descent or ascent, unless you were training for something.
Steeply down into Cwm Pen-llafar
A drop of about 600ft very steeply down into the cwm below. I'd not recommend it as a descent or ascent, unless you were training for something.
The head of Cwm Pen-llafar, seen from the Mynydd Du ridge The steep Black Ladders (Ysgolion Duon) cliffs lie just out of sight on the right, sporting a series of fine winter climbs.
The head of Cwm Pen-llafar, seen from the Mynydd Du ridge
The steep Black Ladders (Ysgolion Duon) cliffs lie just out of sight on the right, sporting a series of fine winter climbs.
Down the ridge of Mynydd Du A view downhill towards Bethesda town, just visible over the hillslope.
Down the ridge of Mynydd Du
A view downhill towards Bethesda town, just visible over the hillslope.
Incipient path forming on the slopes of Foelcraig A walkers' path, narrow and unobtrusive at present. There were clear bootmarks in a patch of scree a little further up from here, but it'll probably never be a popular ascent route for the Carneddau, as it's much longer than the obvious route(s) from Ogwen.
Incipient path forming on the slopes of Foelcraig
A walkers' path, narrow and unobtrusive at present. There were clear bootmarks in a patch of scree a little further up from here, but it'll probably never be a popular ascent route for the Carneddau, as it's much longer than the obvious route(s) from Ogwen.
Boulder scree and outcrops on the slopes of Foel Meirch
Boulder scree and outcrops on the slopes of Foel Meirch
Across the hillside of Foel Meirch Looking across the hills towards Y Garn on the far side of Ogwen
Across the hillside of Foel Meirch
Looking across the hills towards Y Garn on the far side of Ogwen
Boulder scree high on Foel Meirch
Boulder scree high on Foel Meirch
Boulder scree on the hillside below the summit of Carnedd Dafydd Surprisingly easy ground to traverse, certainly on a hot & dry day at any rate.
Boulder scree on the hillside below the summit of Carnedd Dafydd
Surprisingly easy ground to traverse, certainly on a hot & dry day at any rate.
Show me another place!

Western Gully is located at Grid Ref: SH6763 (Lat: 53.148196, Lng: -3.9891618)

Unitary Authority: Conwy

Police Authority: North Wales

What 3 Words

///lousy.faces.dared. Near Bethesda, Gwynedd

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Nearby Amenities

Located within 500m of 53.148196,-3.9891618
Ysgolion Duon
Ele: 960
Natural: peak
Lat/Long: 53.1495064/-3.9834
The data included in this document is from www.openstreetmap.org. The data is made available under ODbL.

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