Οι καλύτερες διαδρομές τρεξίματος Rushock

Lovely bench hear to take 5 and maybe a quick drink before you carry on along the trail!

After a section under the bridge (M5), views of this gently babbling brook are shown to your eyes. It follows the lane for about 250m

Restored viaduct for the Severn Valley Railway

Guaranteed Kingfisher siteing

Spot the model Kinfisher

Hartlebury Common is an area of lowland heath in north Worcestershire, England, situated just outside the town of Stourport-on-Severn. Hartlebury Common and Hillditch Coppice are a biological and geological Site of Special Scientific Interest which covers an area of 90.2 hectares (229 acres). The common supports many varieties of wild plants and insects, especially butterflies and moths. Hartlebury Common and Hillditch Pool are a Local Nature Reserve. The name Hartlebury is derived from the Anglo-Saxon Heoertlabyrig meaning "Hill of the Deer". Hartlebury Common lies on Quaternary wind-blown sand which covers two river terraces of the River Severn overlying Bunter and Keuper Sandstone. It is situated within the Abberley and Malvern Hills Geopark which was launched in 2004. Falling within the counties of Herefordshire, Gloucestershire, Shropshire and Worcestershire the Geopark covers 3,240 km2 (1,250 square miles). The geological and geomorphological significance of the area has been recognised for many years with 13 Sites of Special Scientific Interest (SSSI) and 179 Local Geological Sites (LGS) present. The Abberley and Malvern Hills Geopark is one of only seven geoparks in the UK. Source: Wikipedia

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

Beware of mud