The Wenlock Edge is a limestone escarpment that runs about 31km (19 miles) through the countryside of Shropshire. At its northern point is the village of Much Wenlock and at the south Craven Arms.
Location & Access: Being such a long feature it isn’t that hard to miss on a map of Shropshire, basically look south of Telford and you should find it easily enough. The road B4371 runs along the top of most of the Edge. There are several car parks along the Edge as well as many paths to walk, so there are lots o places to visit depending upon your ability ad how long you want to be up there. For me I like to pull in at a car park just north-east of the village of Presthope. There is a nice walk along the top of a quarry.
Geology: The Wenlock Edge is made up of limestone and lime-muds from the Silurian Period (about 423-426ma). The area used to be a reef and fossils are abundant along this walk.
The fossils you can find there are mostly corals, crinoids and shell fragments.
Above are some pictures of some of the fossils that can be found; mostly corals and fragments of shell. It’s one of the best places in the county to go fossil hunting. Pretty much every rock you pick up will contain something of interest. Fossil collecting is allowed at the Edge, just try not to do too much damage as you do so and remember to leave something for those who will follow.
Along with fossils you can find places where you can see the results of sedimentation, bedding plains and folds (albeit in miniature).
Other Stuff: Along with geology the Edge is a good place to enjoy the English countryside. The area is a composite of mixed woodland and farmers fields full of livestock.
It’s also a place of a lot of woodland wildlife. Some of the birds that you’ll see include Blue, Great and Marsh Tits, all sorts of finches, Greater Spotter Woodpeckers, Nuthatches, Common Buzzards and I’ve even seen Red Kites on rare occasions.
Reference: The Geology of Britain; An Introduction by Peter Toghill (2006), Sedimentary Petrology (3rd Edition) by Maurice E. Tucker (2001), iGeology map from the BGS (2014) and the notice board from the site.