The best city hikes and walks around Stourport-On-Severn

Super nice and very scenic canal section with nice views. The Staffs and Worcs Canal makes for a good detour to avoid the busy road traffic of Kidderminster. There are stunning rural and urban views to be had from the canalised.

Great place for coffee and cake . Or breakfast or lunch

Restored viaduct for the Severn Valley Railway

The ‘Old Railway Line’ cuts through the red sandstone bedrock. These sandstones are Triassic in age, belonging to the ‘Sherwood Sandstone Group’ of rocks. The Sherwood Sandstone Group, the older Permian-aged Bridgnorth Sandstone and the younger Triassic-aged Mercia Mudstone Group have one thing in common; they were deposited in a vast rift basin, called the Worcester Basin. The Worcester Basin was north-south orientated and formed during the Permian period. Its western edge, in the Geopark area, followed the line of a major fault-line, the East Malvern Fault. In the present day this fault line is most clearly marked by the Malvern, Suckley and Abberley Hills. The eastern edge of the Basin followed the line of another major fault-line, the Inkberrow Fault. Into this basin a great variety of different sedimentary rocks were deposited and formed. Some were windblown deposits, others were despotised by streams and rivers, evaporate deposits also formed in lakes and the other significant deposit was alluvial fans that formed along the edge of the basin. Each of the rocks represents the changing environments experienced in the basin through the passage of time. The rocks seen along the ‘Old Railway Line’ belong to the Wildmoor Sandstone Formation, part of the Sherwood Sandstone Group of rocks. They are around 220 million years ago and comprises soft, weakly cemented, pale red-brown, micaceous, sandstones. The well-rounded, evenly sized grains suggest reworking of windblown sands that were deposited the Worcester Basin during the Permian period. Source: geopark.org

Geological overview Just south of Stourport a magnificent river cliff of fine grained red sandstone is seen. Although mainly homogenous in terms of geology, there are white streaks and thin bands of coarse material running throughout the section. The soft sandstone of Redstone Rock is easily carved and there is evidence of human-made habitation in the cliff face since Stone Age times. The caves that can be seen today were mostly made in the 12th century, when a hermitage was established there, conveniently located for the hermits to be on hand to offer blessings and prayers for passers-by in return for alms. It was said to house up to 500 men, who may have also manned the ferry crossing, which was there due to the presence of a ford until the river was dredged. The caves were later used as domestic dwellings and were inhabited almost continuously until the mid twentieth century. Source: Geopark.org

What he said ^^^^^^^

Just south of Stourport-on-Severn, Redstone Caves are made from Triassic sandstone. Carved out in the 12th century and then home to a hermitage, it seems extraordinary today that once up to 500 men lived here. The Geopark Way, a long-distance footpath specialising in geological marvels in the area, runs unsurprisingly right past these caves.

Leapgate old railway line once carried trains between Stourport and Worcester. Now a cycle and footpath, you can cross the River Stour over this viaduct and access Stourport town as well as Hartlebury Common to the east. Both National Cycle Route 45 and the Geopark Way long-distance hiking route use the old railway line.