The best MTB trails around Dodderhill

The National Transport Trust Red Wheel at Tardebigge Top Lock (Worcestershire) commemorates the site of Britain's longest lock flight. Located on the Worcester & Birmingham Canal, the top lock is an engineering landmark that replaced an 1815 experimental vertical boat lift, making it unusually deep. History & Significance The Vertical Boat Lift: Before the traditional lock was built, inventor John Woodhouse installed an experimental vertical boat lift at his own expense. A 64-ton wooden chamber lifted boats an impressive 11 feet using a windlass. The Shift to Locks: While the lift successfully raised 110 boats in 12 hours, it proved too fragile for permanent use. In 1815, it was replaced by the deep conventional lock we see today. The Red Wheel Plaque: Awarded by the National Transport Trust, the Red Wheel acts as the transport equivalent of a blue plaque, recognizing sites of profound historical and engineering importance. The Tardebigge Flight The Longest in the UK: The Tardebigge Flight consists of 30 narrow locks spread across 2.25 miles, raising or lowering boats by 67 metres (220 feet). Navigation: Transiting the whole flight typically takes narrowboat enthusiasts about 4 to 5.5 hours.

Very quiet place, which is popular among runners and walkers. However, Worcestershire&Birmingham channel is relatively well-surfaced at this section (compacted gravel with some cobblestones). So, it can be carefully(!) completed on road bikes with decent tires. If not, then ~1km of pushing in total from the nearest road.

Good path for walking and cycling. Saw a Muntjac deer further down

thick mud at the moment

mud fest

Tardebigge top lock, 1st of 30

Great place to grab breakfast

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