The falls are situated on the course of the Harmby Beck, which eventually drains into the River Ure.
The waterfall is technically a 'stepped cascade' formed by layers of Yoredale limestone, characteristic of the Wensleydale region.
The gill is a designated wildlife habitat, often hosting varied bird species and flora native to Northern England limestone dales.
The site remains largely off the main tourist circuit, preserving a sense of local tranquility compared to nearby attractions like Aysgarth Falls.
Harmby Waterfall is a multi-tiered cascade situated on a tributary of the River Ure in Wensleydale. The waterfall features a series of limestone steps that create a stepped aesthetic across the rock face. It is located within a wooded ravine known as Harmby Gill. The site is accessible via a public footpath that runs through the village of Harmby. The cascade is naturally fed by rainfall, meaning its intensity fluctuates significantly with seasonal weather. The area is maintained as a natural woodland feature rather than a manicured park. The path leading to the falls passes through local farmland and established deciduous woodland. The geological composition of the site showcases typical North Yorkshire limestone formations.
From the small footbridge spanning the beck near the base of the main waterfall tiers.
Wear waterproof footwear with good grip as the paths through the gill can become extremely muddy and slippery.
The walk to the falls involves uneven terrain and steep banks, so it is not suitable for strollers or those with limited mobility.
Check the weather forecast before visiting; the path becomes hazardous immediately following heavy rainfall.
Do not attempt to scramble down the steep banks directly into the stream, as the rock is unstable and prone to erosion.
Stay on marked public footpaths to avoid trespassing on private farmland bordering the gill; take all litter away.
