ヒルハンプトンのおすすめウォーキング＆ハイキングルート

These stepping stones are fine in the summer, but will typically be well under water for much of the winter and the water can be fast flowing. Fortunately there is a bridge about half a mile to the east.

Alas for most of 2024, the stepping stones are missing, presumably washed away. As mentioned about - footbridge available near where the brook meets the Severn (SO 811 666)

This beautiful open meadow is situated on the banks of the River Severn, where it meets the Dick Brook. It offers plenty of space for activities and is perfect for running around with your dog.

This view contains many layers of history, dating back thousands of years. The scattered farms of the manor of Abberley were established from at least Anglo Saxon times with the original road system winding around large round fields and the medieval common land. This area is part of the medieval deerpark given to Ralph de Toni by William the Conqueror which stretched up onto Abberley Hill. The manor passed to the Earls of Warwick fairly soon afterwards. Medieval legal documents record frequent fines to local people for breaking in and hunting.

Shelsley Walsh is the oldest motorsport venue in the world still to run events on the original course and is older than Indianapolis, Le Mans or Monza. Brooklands has been and gone, but Shelsley Walsh is still here, as old as the sport but as modern as today.

The mill has a stone with the date 1652 on it. The Dick Brook was canalised in the 1650s by Andrew Yarranton and the mill built as a tilt hammer mill to service a nearby blast furnace. The mill later became a fulling and paper mill until it was taken over by the Worcester Porcelain Company for the grinding of ‘grog’ from about 1760 till about 1808. It reverted back again to an iron works when a puddling furnace was installed (which has been excavated in the recent past). The site then evolved into domestic residences and was ultimately cleared. Source: geography.org.uk

Dick Brook is thought to be the first canalised brook in England, engineered by Andrew Yarranton, a local pioneer of the industrial revolution. He did this in the mid-17th century, 100 years before James Brindley embarked on the canal-building revolution. The brook was dredged and locks built to enable boats to carry iron ore from the River Severn up Dick Brook to a blast furnace. 500m along the path, marked by a way-marker post, you reach the site of a former iron forge. There are some building remains and the area is being studied by local historians. As you continue westwards, to the right of the path there are the earthworks of the leat which fed water to turn the wheels at the forge. The furnace site was 100m up the valley to the south of the path as you go towards Glasshampton. Source: Geopark guide

Shavers End Quarry is one of many quarries in the area located on the Abberley Hills, where the limestone is a sought after material for lime kilns, construction and the aggregates industry. Quarrying activity at Shavers End Quarry has sliced through the North West corner of Abberley Hill, providing a geological cross section for people to study the structure of the area in detail. The scale of the site, partnered with the bare rock faces allows visitors to fully appreciate the complex tectonic history of the area. Within the quarry there are two distinct rock formations exposed; the Lower Ludlow Shales Group and the Aymestry Limestone Formation. The Lower Ludlow Shales Group is the lower of the two units and consists of a series of siltstones and bluish grey mudstones. These rocks can be best seen at the southern end of the quarry, as well as on the eastern banks of the quarry lakes. The Aymestry Limestone is a blue-grey, nodular argillaceous limestone and forms the main rock face that extends along the western side of the quarry. The limestone is shaly and impure and notably contains a thick band of bentonite. Shavers End Quarry sits variably in the hinge zone and on the overturned limb of a large fold. The Lower Ludlow Shales and Aymestry Limestone at this locality are upside-down, suggested by the wrong-way-up orientation of fossils and other sedimentary structures. The age of folding has been the subject of much debate, with many different interpretations; it may have formed during the Variscan Orogeny (~300 million years ago); others suggested that folding occurred during the earlier Caledonian Orogeny (390 million years ago). However it is generally agreed that folding was instigated by thrust faulting on the East Malvern Fault system. This site is part of the Community Earth Heritage Champions Project.