노턴‬에서 가장 멋진 ‪7‬개의 천연기념물

지금은 약간 진흙탕이지만 매우 분위기가 좋습니다

It's a steep pull up Walsgrove Hill from the north, and in the winter it will be slippery and muddy due to the activities of the sheep that live in this field. However, it offers fine views across to the clocktower and beyond.

Red sandstone rock formation - low cliffs of exposed stone that has been historically quarried for building materials. A path runs along the bottom and the top, currently (Sept 2024) overgrown in places. An information sign gives details among the nettles.

The sunken lane cuts through Triassic aged rocks of varying grain size, deposited in the Worcester Basin some 220 million years ago. The rock types seen are fine grained siltstones, course sandstones and conglomerates containing large pebbles.

View to the West The lower part of Walsgrove Hill and the hill on which Abberley clock tower stands are Silurian siltstone. The valley of the River Teme cuts into soft mudstones of the upper Silurian Old Red Sandstone with the harder sandstones of the lower Devonian Old Red Sandstone forming the Bromyard plateau. The low hummocky ground at the base of these hills is underlain by Carboniferous age Coal Measures rocks. These form the southerly tip of the Wyre Forest coalfield. Coal was mined here until the early twentieth century. To the north west, the Clee Hills are also formed of Carboniferous rocks. A molten layer of rock pushed between the layers and formed a hard black dolerite rock, the Dhustone, which slowed the erosion of these still prominent hills and is quarried for roadstone to this day. Source: Local signage

Great views. Nice place for taking a break

The trig point at the top of Hegdon Hill stands at 255m, making this peaceful summit officially a Marilyn. The views out across miles of rolling Herefordshire countryside are well worth the climb, and nearby Hegdon Hill Vineyard is well worth a visit, too.

Ankerdine Hill, at 489 feet (149 m), is part of the Abberley Hills ridge in the Abberley and Malvern Hills Geopark. The ridge was formed during the Silurian period and is of considerable geological significance. The River Teme loops around the hill, surrounding it on its western, southern and eastern side, giving it superb views of the Teme Valley. It is most commonly ascended from the village of Knightwick, where the award-winning Talbot pub is a good post-hike option.