Tithe Barn, Manor Farm, Doulting

St Aldhelm's Well in Doulting, Somerset, England, is an ancient spring which is the source of the River Sheppey. The site is a Grade II listed building, although it is a medieval site, most of what remains has been rebuilt.The well was named after St Aldhelm after he died in Doulting village in 709, some accounts say on the day of his death he sat by the well singing psalms before being carried up to the church in the village where he died. The Church of St Aldhelm in Doulting was dedicated to Aldhelm in the 8th century.Folklore has attributed healing powers to the spring water in which pilgrims were known to have bathed, the well is still visited by people who use the water and leave flowers and other offerings of reverence. The spring has never been known to fail, even in times of drought.Water flows through two low pointed arches in a stone wall in the hillside, along a bathing pool with stone sides and collapsed stone walls on each side. The carved masonry which can be seen around the site indicates the bathing pool would have once had a roof over it. The water passes through a wall to fill a stone drinking trough in the lane below, pouring over the trough's edge into a grate in the floor. The water passes under the lane into a confluence with a group of springs to the west of Doulting to become the River Sheppey, which ultimately joins the River Brue.Next to the well is a chamber containing the remains of a waterwheel which once pumped water up the hill to supply drinking water for Doulting village, a well head built in the late 19th century still stands in the village featuring a wrought-iron pump handle. The well head is also a Grade II listed building.

Doulting is a village and civil parish 1.5 miles (2 km) east of Shepton Mallet, on the A361, in the Mendip district of Somerset, England.

Doulting Railway Cutting (grid reference ST648424) is a 2.8 hectare geological Site of Special Scientific Interest in Somerset, notified in 1971. The cutting was made in the 1850s for the East Somerset Railway which still runs steam trains through the cutting today. It shows rocks of the Middle Jurassic period including both the Inferior Oolite/Great Oolite Junction and the Bajocian-Bathonian stage boundary.

Doulting Stone Quarry (grid reference ST648436) is a limestone quarry at Doulting, on the Mendip Hills, Somerset, England. At present there are only three quarries quarrying Doulting stone. The largest, The Doulting Stone Quarry, was producing building stone in Roman times. In the 20th century it was operated by the Keevil family. Until 1994 it was operated by Amalgamated Roadstone Corporation (now part of Hanson plc) but was then bought out as a stand-alone business. Ham & Doulting Stone Co Ltd own the east quarry which was originally in use for centuries after which followed a period of inactivity. It was reopened 12 years ago. The quarry also offers primary and secondary cutting and profiling.The stone quarried at Doulting is a 2 m (6.6 ft) thick layer of oolite of middle Jurassic age, deposited as sediments in fairly shallow coastal seas. The stone is unusual as it shows unconformity at the division between the oolite and Carboniferous limestone beneath, representing two types of rocks laid down millions of years apart, the intervening sediments having been eroded away before the Jurassic strata were laid down. It has a high level of water absorption and porosity.The stone is used for building purposes, including Glastonbury Abbey and the west façade of Wells Cathedral, and other structures in the cathedral close, such as the fortified gate called The Bishop's Eye.

Merryfield Lane Halt is a railway station at the summit of the East Somerset Railway. It was built in 1981 and originally served as the terminus of the railway.

Mendip Vale is the western terminus of the East Somerset Railway.

Maes Down (grid reference ST647406) is a 0.2 hectare geological Site of Special Scientific Interest between Shepton Mallet and Stoney Stratton in Somerset, notified in 1985. It is a Geological Conservation Review site. The rocks seen at Maes Down were laid down about 190 million years ago, during the Upper Pliensbachian and Lower Toarcian Stages of the Jurassic Period of geological times, when this part of Britain lay beneath the sea.

Cranmore West is a railway station on the East Somerset Railway.

The Anglican Church of St Mary in Chesterblade, Somerset, England was built in the 12th century. It is a Grade II* listed building. It is located 3 miles northeast of Evercreech (to which parish it belongs), and three miles south east of Shepton Mallet.

Shepton Mallet (Charlton Road) was a station on the Somerset and Dorset Joint Railway in the county of Somerset in England. Opened as Shepton Mallet on 20 July 1874, it was renamed to avoid confusion with the nearby GWR station in 1883. The station consisted of two platforms with the station building on the up side. There was also a goods yard and cattle dock controlled from a signal box. The station closed to goods in 1963: passenger services were withdrawn when the SDJR closed in 1966.

Cranmore is a village and civil parish east of Shepton Mallet, in the Mendip district of Somerset, England. The parish includes the hamlets of Waterlip, East Cranmore and Dean.

Cranmore is the main railway station (and also the headquarters) of the preserved East Somerset Railway, in Somerset, England.