Information AboutMillers Dale |
| CATEGORIES ABOUT MILLERS DALE | |
| cycleways in england | |
| geography of derbyshire | |
| rivers and valleys of the peak district | |
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It is a popular beauty spot in the Peak District of England , much of the area being preserved as a Site Of Special Scientific Interest . Nearby is Ravenstor and Cheedale, both popular with Rock-climbers . The local landmark is the viaduct, first built by the Midland Railway in 1866 . Increasing traffic meant that a second viaduct parallel to the first was built in 1905 , increasing the number of tracks to four. The railway station, was at the junction where passengers for Buxton joined or left the trains between London and Manchester . It was originally to be called "Blackwell Mill", but, in the end, was named "Millers Dale for Tideswell ". For such a rural location it was unusually large. Built on a shelf carved out of the hillside, it originally had two platforms, but a bay platform was added in 1905 to accommodate Buxton trains, plus the down platform became an island platform to serve the extra tracks. For a while, 'through' carriages for Buxton were attached to and detached from expresses. Part of the original Parliamentary Act, approving the line, considered the needs of invalids taking the waters at Buxton. This therefore alleviated the problem of changing trains. In addition, the two main plaftforms were connected by a subway. Since the railway was closed in 1967 the station has become a car park, although the main buildings remain. The older of the two viaducts forms part of the Monsal Trail. The area is of great interest to geologists, particularly where the strata have been exposed by quarries and railway cuttings. In Station Quarry, which is owned by the Naturalists Trust, two layers of limestone can be seen, separated by a bed of shale. At one point there is a dip in the lower layer, possibly from a watercourse, millions of years ago. This is filled with the shale and a large limestone boulder can be seen within it. Elsewhere in the area there are signs of lava flows from long-ago volcanic activity. Northwards from Millers Dale the line entered the two Chee Tor tunnels (401 and 94 Yard s), separated by a fifty Foot high bridge over the River Wye, then along a ledge cut into the rock face, before entering Rusher Cutting Tunnel (121 Yards ), crossing the Wye yet again by another viaduct. The line here was immensely difficult and expensive to construct, skirting, as it did, the base of the 300 Foot high ciff of Chee Tor . Chee number 1 has been sealed for safety reasons, but it is still possible to walk through the two others. Further on was the triangular junction for Buxton via Blackwell Mill , before continuing to Peak Forest . EXTERNAL LINKS |
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