Shelve, Shropshire

The Hoarstones, or Hoar Stone Circle, is a stone circle in the civil parish of Chirbury with Brompton in the English county of Shropshire. The Hoarstones are part of a tradition of stone circle construction that spread throughout much of Britain, Ireland, and Brittany during the Late Neolithic and Early Bronze Ages, over a period between 3300 and 900 BCE. The purpose of such monuments is unknown. The Hoarstones are one of up to five stone circles known from this area, on the borders between Shropshire and Powys. Of these, only the Hoarstones and Mitchell's Fold survive. Shaped elliptically, the Hoarstones circle measures 23.3 by 21.1m in diameter. It contains between 38 and 40 small stones, identified as dolerites probably sourced locally. There is a central stone inside the circle, although whether this was part of its original prehistoric design is unclear. Several of the stones contain small holes, which according to 19th-century accounts were caused by miners drilling holes into them; gunpowder was then placed into these holes and lit to produce explosions. The existence of the circle was noted by the antiquarian Reverend C. H. Hartshorne in the 1830s. An excavation took place in 1924, led by Lily F. Chitty.

Bentlawnt is a village in Shropshire, England.

The Bog is a former mining community in Shropshire, England. It lies 6 miles (10 km) north of Bishops Castle, east of the A488, at grid reference SO355979. It was once a busy village with over 200 buildings. Now only a few remain. The local mines produced lead and barytes until the early 20th century. The mine at The Bog and the adjacent Stiperstones outcrop were only viable because of a geological movement; over time the movement of the tectonic plates landed at this site, combined with the movement of the earth it crumpled the layers and the softest layers were then eroded away. After mining stopped, the undisturbed remnants provided a range of wildlife habitats: birds nest in the old buildings, bats roost in the old mine tunnels, and reservoirs and ponds are ideal for aquatic life.

White Grit is a small, scattered village beneath Corndon Hill in Powys, Wales, directly on the border with (and partly in) Shropshire. The nearby village of Priest Weston, despite being in England, actually lies to the west of White Grit. To the east is the A488 road. The nearest town is Bishop's Castle. White Grit lies in the community of Church Stoke (the small parts in Shropshire are in the civil parishes of Chirbury with Brompton and Worthen with Shelve). Adjoining is a hamlet called The Marsh. There is a stone-built Methodist chapel in White Grit, no longer used as a place of worship, and a corrugated-iron chapel, both of which are marked on Ordnance Survey maps.

Stapeley Hill is a sacred saddleback shaped hill in South-West Shropshire, near the village of Priestweston, not far from another landmark, Corndon Hill. The Hill is home to Mitchell's Fold [1] and along the path leading from the Fold which crosses Stapeley Common, home to the Cow Stone [2], or single standing Stone - Menhir and the Stapeley Hill Ring Cairn [3] [4]. There are two Bronze Age cairns at or near the summit, and such round cairns are a common feature of Welsh mountain summits. The hill rises to an elevation of 403 metres (1,322 ft) and lies in the civil parish of Chirbury with Brompton.

Meadowtown is a hamlet in west Shropshire, England, in the civil parish of Worthen with Shelve. Neighbouring hamlets include Marton, Ox Wood, Crest Wood, and Rorrington. Meadowtown contains a Site of Special Scientific Interest according to the U.K. government. A long-disused quarry in the hamlet is "a well known fossil collecting locality and has yielded typical and distinctive trilobites including Oxygiocarella debuchi, Marrolithus craticulatus, Lloydolithus lloydii and Oxyginus cordensis novenarius. Species of the brachiopod genus Dalmanella and occasional sponge spicules also occur."Meadowtown is also home to "Mammoth", a cow made famous on the internet involving a UK milk-price dispute in 2017.

Heath Mynd is a hill in the English county of Shropshire. At a height of 452 metres (1,483 ft) it is fairly unnotable except for its Marilyn status, a feature caused by the sharp drop on all sides. It is connected to Corndon Hill by a low col, and is only just inside England, being just one mile from the border with Wales. The nearby village is Norbury; nearest towns are Bishop's Castle and Church Stretton. Its nearest neighbour (visible in the photo) is called Cefn Gunthly.

The Stiperstones (Welsh: Carneddau Teon) is a distinctive hill in Shropshire, England. The quartzite rock of the ridge formed some 480 million years ago. During the last Ice Age Stiperstones lay on the eastern margin of the Welsh ice sheet. The hill itself was not glaciated though glaciers occupied surrounding valleys and it was subject to intense freezing and thawing which shattered the quartzite into a mass of jumbled scree surrounding several residual rocky tors. At 536 metres (1,759 ft) above sea level it is the second-highest hill in the county, surpassed only by Brown Clee Hill (540 metres (1,772 ft)). Stiperstones' 8-kilometre (5 mi) summit ridge is crowned by several jagged outcrops of rock, which may be seen silhouetted against the sky.

Wild Edric's Way is a waymarked long distance footpath running wholly within the county of Shropshire in England. The path runs for 49 miles (79 km), mostly sharing the route of the Shropshire Way.

Mitchell's Fold (sometimes called Medgel's Fold or Madges Pinfold) is a Bronze Age stone circle in southwest Shropshire, located near the small village of White Grit on dry heathland at the southwest end of Stapeley Hill in the civil parish of Chirbury with Brompton, at a height of 1083 ft (330m) o.d. The stone circle, a standing stone, and a cairn comprise a Scheduled Ancient Monument; the circle is in the guardianship of English Heritage.

Corndon Hill (Welsh: Cornatyn) is a hill in Powys, Mid Wales, whose isolated summit rises to 1,683 ft above sea level. It is surrounded on three sides by the English county of Shropshire and forms a prominent landmark in the Wales-England border. Corndon's prominent western edge appears to form a separate hill and is known locally as Lan Fawr (Welsh: 'Big Hill'). It is frequented by walkers and ramblers from car parks nearby at Mitchell's Fold for example. There are spectacular panoramic views from the summit, and it is itself an important landmark for the surrounding countryside and towns like Montgomery. It is close to villages such as Church Stoke and Hyssington. The hill is geologically part of the Shropshire Hills range of hills lying mainly to the north, east and south of the summit. The immediate area to the west is the Vale of Montgomery and the River Severn. The Cambrian Mountains are visible beyond to the far west. The Stiperstones and Shelve lie to the immediate north, with Caer Caradoc and the Long Mynd to the east.

The Whetstones are, or were, a stone circle beneath Corndon Hill in the parish of Church Stoke, Montgomeryshire, Wales, near the border with Shropshire, England. They lie immediately to the west of the village of White Grit and close to Priestweston. The site is also a short distance from the better-known Hoarstones and Mitchell's Fold circles. The circle was largely destroyed in the 19th century, and only a few fragments now remain. An 1841 account described them as even then fragmentary, but comprising three main stones, then "leaning, owing to the soft and boggy nature of the soil. They stand equidistant and assume a circular position [...] The highest of these is four feet above the surface; one foot six inches in thickness, and three feet in width." In 1860, the antiquarian Robert William Eyton still referred to the Whetstones as a "remarkable monument", but they were later stated to have been dug up, and the stones incorporated into a boundary wall, in about 1870. Aubrey Burl notes that "nearly all of its stones were blown up in the 1860s [...] when the last stone was uprooted around 1870 charcoal and bones were seen".The remnants of the circle can still be observed from an adjacent field boundary, or from the northern summit of Corndon Hill. Large stones are also visible now forming a boundary next to a footpath, which were probably also once incorporated in the circle.