쉬운 스투르포트-온-세번 주변 하이킹 및 워킹 코스

One of the highlights of this part of the Geopark Way, rather better than walking through Stourport.

Great place for coffee and cake . Or breakfast or lunch

Charlton Lane is very often flooded, but fords aren't too deep

mud fest

The nature reserve is approximately 35 hectares (86 acres) in size. The dominant habitat is heath and acid grassland, surrounded by oak and birch scrub. The acid grassland has been surveyed by many professional bodies, and Natural England rated it as the best quality acid grassland in the county. Wildlife on the site is typical for what you would expect on a heathland site, while reptiles are scarce due to the levels of disturbance from the public; however common lizard, grass snake and slow worm have been seen. There are many notable species of solitary bee and wasp which make use of the bare sandy soil, as do unusual heathland specialists, the green tiger beetle. The open areas are also utilised by a variety of ground feeding birds such as green woodpecker and as nesting sites for rarities like woodlark. There are a few small pools on site; one in particular supports a good breeding population of smooth newt, common frog, various dragonflies, damselflies and great diving beetle. Although traditionally a heath, this has given way in the main to gorse and broom scrub. There has been an increase in the density of rare grey hair grass after scrub clearance carried out in previous years. The area has an interesting history, with the site being used as a World War II American Army training and hospital camp. All that remains from those days are concrete paths, and some foundations from the original buildings. Much of this has been highlighted along a way marked ‘History’ trail. The website 'Burlish Camp' has more on the history of the site. In addition to the history trail, there are 3 other trails around the site, including 2 easy going routes, which take advantage of the sites historical concrete tracks, and a heathland circular, which also incorporates much of the Rifle Range SSSI. Source: Wyre Forest District Council

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

Poppy’s are fantastic in this area… when they are in flower. If you want to see them they do check before you travel…