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Dist:0.3km<br/>
©Row17
Dist:0.3km<br/>View across ripening barley towards the Wrekin. Both Lyth Hill and the Wrekin are related geologically, being made of Uriconian rock, an ancient igneous family of rocks which outcrop in Shropshire and the Malverns.
©Richard Webb
Dist:0.5km<br/>A bench amongst some young conifers above the scarp at Lyth Hill.
©Richard Webb
Dist:0.6km<br/>Seen on the Shropshire Way whilst on a week's walking in the Shropshire hills.
©Alan Rolfe
Dist:0.6km<br/>A bench at the top of the Lyth Hill scarp, just above a small quarry.
©Richard Webb
Dist:0.7km<br/>Just outside Bayston Hill, there is a large house amongst trees on the right.
©Richard Webb
Dist:0.8km<br/>A narrow path along the steep scarp slope of Lyth Hill.
©Richard Webb
Dist:0.8km<br/>Low angled conglomerate exposures on the slopes of Lyth Hill. The rocks here are old, part of the Uriconian series of rocks found throughout the West Midlands in places like Haughmond Hill, Caer Caradoc, The Wrekin and the Malvern Hills.
©Richard Webb
Dist:0.8km<br/>
©Richard Law
Dist:0.8km<br/>A small stream (little more than a drainage ditch at this point, to be fair) with a former line of alders that have recently been cut back hard.
©Richard Law
Dist:0.8km<br/>
©Roy Haworth
Dist:0.8km<br/>
©Roy Haworth
Dist:0.8km<br/>
©Roy Haworth
Dist:0.9km<br/>The front area of this small, privately-owned bed & breakfast establishment.
©Peter Whatley
Dist:0.9km<br/>
©Roy Haworth

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