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Although the Millstone Grit forms the last layer of sedimentary rocks in the Peak District, it does not cover all of the Peak. The answer lies with a period of upfolding to form the Derbyshire Dome during the Variscan orogeny.
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Castleton, looking north-east. Carboniferous Millstone Grit. View from Mam Tor, across Mam Tor landslip (in foreground) and northern side of Hope Valley. ... Description: Photograph of Millstone Grit country, Castleton, Derbyshire, England.
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Hydrogeochemistry of Millstone Grit and Coal Measures groundwaters, south Yorkshire and north Derbyshire, UK. David Banks. Geological Survey of Norway, ...
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A pilot study has been performed to ascertain the baseline hydrochemistry of both shallow (springs) and deep (borehole) groundwaters of the Millstone Grit and Coal Measures. In terms of major ion composition the majority of the shallow groundwaters in the two formations are rather ... Derbyshire England ; aquifers ;
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Derbyshire Carboniferous limestone ... They eroded rapidly at the centre of the dome to reveal the more resistant Millstone grit. The grit was thinner in the southern areas of the region and so has been completely removed to reveal the oldest rocks of the Peak - the limestone.
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Building stone, Westmoreland Grit, quarried in [Derbyshire / Yorkshire / Cumbria], England, purchased 1883. A fine-grained conglomerate of the Millstone Grit series, very dense and hard and extensively used for engineering work.
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It is a landslipped crag of massive, coarse grained sandstone or grit. In the past, these coarse sandstones were used to make millstones. Today, the millstone is the emblem of the Peak District National Park and gives its name to the distinctive 'Millstone Grit' rocks of the Pennines.
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Introduction: Around the junction of the countries of Staffordshire, Derbyshire, ... The main object will be trace the thinning away, step by step, of the Millstone-grit from Lancashire to the borders of the North Staffordshire Coal-Fields; but a few other points bearing on the geology of the district will be shortly noticed.
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The following paper is an attempt to define the geographical extent, stratigraphical sequence, and palæontological horizon of the beds which lie between the top of the Mountain Limestone and the series of grits known as the Millstone Grits.
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In Derbyshire and Lancashire the Millstone-grit series is more varied and extensive; often exhi- biting in one section beds of very different lithological ...
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