켄스윅‬에서 가장 멋진 ‪8‬개의 천연기념물

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.

This little man-made waterfall is the overflow from the big lake but is still quite realistic. Best visited in the winter for flow and less foliage to get in the way of the camera shot!|

A real picturesque old mill, and the Geopark Way affords a really good view of the weir and house from a number of angles.

This spout, formerly known as the Cowleigh Spout, is on the left as you leave Malvern on the Cowleigh Road, almost opposite the Worcestershire Way car park. The springs are in an adjacent field and their daily output is 10,000 gallons, with much running to waste. Unlike many of the other natural water sources of the Malverns, Cowleigh Spout maintained a healthy flow even during times of severe drought, such as that in 1921, and on many occasions was the sole supply over an extensive area. During the construction of the North Malvern Tank in the 1870s, when the supply from the Morris tank was cut off, the inhabitants walked the half mile from North Malvern to this spout for their household's water. This rural idyll was witness to the 'dirty' hordes of Birmingham hop-pickers who flocked to the countryside for their annual working holiday. "Cowleigh Spring was the resort of many hoppers on Sunday, the "crystal streams" being freely used for their ablutions. They borrowed a piece of soap and had a "wash and brush up, the pocket handkerchief doing service as a towel". The Madresfield Connection The original spout was replaced with this one by the 7th Earl Beauchamp. He was later immortalised as Lord Marchmain in Evelyn Waugh's Brideshead Revisited. The wording on the tiled surround reads: "This fountain was presented to the people of Cowleigh by William Earl Beauchamp 1905." The Earls Beauchamp lived at Madresfield Court, three miles away on the opposite side of the hills, and the cisterns behind the fountain originally supplied the Court, four farms and a dozen houses on the Madresfield estate. The spout fed a tank on Cowleigh Park Farm. In the 1870s, a three-inch iron main was laid to Madresfield via Dyson Perrins School, Tanhouse Lane and Newland and a 30,000-gallon reservoir/header tank at Lower Woodsfield Farm enabled the supply thereafter to be gravity fed. The laying of the supply is recorded in the local paper of 7 Dec.1872, titled `New water supply to Madresfield Court': "For some time past, the route between Madresfield Court...and the famous flow of water at the entrance to `Cowleigh Park', known as `Cowleigh Spout' has exhibited a line of excavation, in which mains have been deposited for the conveyance of the overflow of water at the spout for use at Madresfield Court. The work is now all but completed." The village was put on to the main public supply shortly after 1955 following concern about possible contamination. A sample analysed during the 1980s suggested a similar composition to the Schweppes Pewtriss Well. The tanks behind still overflow copiously and are maintained because they supply several local households with water. In 1995 water was reinstated at the public spout as a result of the efforts of local enthusiasts. Since then the area around the spout has been the subject of various initiatives to make the area more user friendly in recent years. There are now steps from the car park at the rear, which once housed the bottling works tank. Also the area in front of the spout has been restored and drainage improved. The Madresfield Estates Trust still owns about 50 acres of land behind the spout together with the nearby Cowleigh Wood, but at some time in the past the ownership of the spout changed. In 2007 the Area of Outstanding Natural Beauty managers when implementing the Heritage Lottery Fund enhancements unsuccessfully tried to trace the owners of this fountain. What they did discover was that the properties across the road from the fountain had a right to the water and in the case of The Byre it was a gift in perpetuity from the Beauchamp estate for bravery in the Great War. Source: malvernwaters.com

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

Prior's Mill is a former seventeenth century timber-framed water mill, with twentieth century alterations, and now used as a private residence. Next to it is a very high weir on the Dick Brook. There used to be several mills on this stream long ago.

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.

Walsgrove Hill boasts fantastic views from its 869-foot (265 m) summit towards Abberley Hill and its clock tower. It is at the northern end of a ridge that also contains Cockshot, Rodge, Pudford, Penny, Berrow and Ankerdine Hills. Formed during the Silurian period, the ridge is part of the Abberley and Malvern Hills Geopark, an area of considerable geological significance, spanning 700 million years of natural history.