Walking the Shropshire Way

Walking the Shropshire Way
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This is the official guide to the Shropshire Way, which consists of a northern and southern loop that both start in Shrewsbury. Each loop can be completed in a week or combined to form a two week 182 mile (290km) circuit that visits Stiperstones, Ludlow, Wenlock Edge, Ironbridge and the Wrekin. Split into 15 stages, this walk requires moderate fitness to cover the daily distance of 10 to 15 miles. The guide also includes the Stretton Skyline Walk, a 20 mile (32km) walk over Shropshire's peaks and ridges, which can be split over two days with an overnight stay in Church Stretton.
For both the main route and the higher-level Stretton Skyline Walk, this guide provides in-depth route description and 1:50,000 OS mapping to aid navigation, along with information about accommodation, public transport and local services. The guide also offers plenty of insight into Shropshire's vibrant history and fascinating geology.
The Shropshire Way visits some of England's most serene and beautiful scenery, as well as key historical sites including Ironbridge, the birthplace of the Industrial Revolution. Through tranquil countryside and medieval market towns, this route explores all the best that the Shropshire Hills Area of Outstanding National Beauty (AONB) has to offer.

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John Gillham. Walking the Shropshire Way

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About the Author

John Gillham was born in Bournemouth, Dorset but now lives with his wife Nicola in Hoddlesden, a small village in the West Pennine Moors.

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Down to the west from Wenlock, there’s just space to squeeze in the Ordovician Period, around Cardington at the base of Caer Caradoc. And then we arrive into the Church Stretton crumple zone. Here rocks of the earliest geological periods, Ordovician and Cambrian, are embedded within crumpled and mashed ancient crust stretching back into the Precambrian.

Ordovician rocks pop back up as the tottering towers of Stiperstones. The ancient earth movements have tilted it almost upright; after 500 million years of hard times, the stones have just been broken up a bit more by freeze-thaw of the Ice Age.

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