The gorge's hydroelectric plant is one of the oldest in the United Kingdom, dating back to 1890.
The river descends over 500 feet in height within the short span of the gorge.
The site is privately owned by the same family that has managed the grounds for over 100 years.
The massive 1952 Lynmouth flood, which devastated the local village, originated from a cloudburst that surged through the West Lyn River and the gorge.
The gorge displays complex geological folding in its exposed rock faces, reflecting millions of years of tectonic activity.
Glen Lyn Gorge is a private nature attraction located in Lynmouth where the West Lyn River descends through a narrow, tree-lined valley towards the Bristol Channel. The site features a series of high-energy waterfalls and rapids created by the river's rapid descent over exposed metamorphic rock. A hydroelectric power station, established in the late 19th century, remains on-site and currently generates electricity for the premises using the river's flow. The landscape is characterized by deep ravines, ancient woodland, and moss-covered boulders typical of the Exmoor National Park region. Visitors navigate the gorge via a network of steep, winding paths that follow the river’s path from the top of the valley down to the coastal village of Lynmouth.
The viewing platform overlooking the main series of waterfalls in the lower section of the gorge.
Wear sturdy, non-slip footwear as paths are often wet, steep, and uneven.
Allow extra time for the ascent if you choose to start at the bottom and walk up, as the gradient is significant.
Check the official website for seasonal status before departing, as severe weather can necessitate temporary closures.
Do not attempt the trail in flip-flops or open-toed sandals due to slippery terrain and steep inclines.
Closed during the winter months and occasionally during periods of high rainfall or storm damage.
Stay strictly on marked paths to prevent erosion and protect the fragile woodland ecosystem.
