Yorkshire Dales National Park

Yorkshire Dales National Park is a protected upland area in northern England covering large swathes of North Yorkshire and parts of Cumbria, designated as a national park in 1954. It is recognised for its extensive limestone scenery, peat moorlands, and traditional dry-stone field walls.

Key attractions include dramatic karst landforms, deep valleys known as dales, cave systems, and the well-known Yorkshire Three Peaks - Whernside, Ingleborough, and Pen-y-ghent - which rise to roughly 736 m, 723 m, and 694 m respectively and attract walkers and climbers. The park contains numerous villages and market towns, plus networked public rights of way for walking, cycling, and riding covering thousands of kilometres.

The area’s landscape evolved through glacial and fluvial processes acting on Carboniferous limestone and millennia of pastoral farming, producing the distinctive drystone walls and barns. Conservation and farming continue to shape the park through grazing, hay meadows, and upland management practices.

The park sits in northern England, roughly 40-80 km north and west of Leeds and Manchester depending on the sector, with main gateways at towns such as Skipton, Settle, and Hawes. Terrain ranges from low rolling hills and limestone pavements to higher moorland plateaus.

• Practical advice: Best lowland walking and cycling conditions are late spring through early autumn; weather can change quickly at higher elevations so carry warm, waterproof clothing and a map or GPS device.
• Trailheads and services: Many popular starting points for walks are in market towns such as Grassington, Hawes, and Settle, which provide parking, public transport links, and visitor services.

What to See #

• Yorkshire Three Peaks: A karst limestone landscape featuring the Yorkshire Three Peaks - Whernside, Ingleborough, and Pen-y-ghent - with heights of about 736 m, 723 m, and 694 m respectively; these three peaks form a popular 37 km walking challenge when linked as a circuit.
• Karst features and villages: Dry valleys, scar limestone edges, and features such as Malham Cove - a large limestone amphitheatre formed by glacial meltwater - along with extensive drystone walls and traditional stone-built villages across the park.