SAVE LONGSTONE EDGE

SAVE LONGSTONE EDGE

The Materials

Fluorspar

Fluorspar is a crystalline form of calcium fluorite CaF2 which is commonly found deposited in limestone, as at Longstone Edge. Pure fluorspar is colourless but impurities impart a wide variety of colours, the most well-known form being Blue John found nearby at Castleton in Derbyshire.

Commercially, fluorspar is used to produce aluminium fluoride and hydrofluoric acid. Aluminium fluoride is used in the glass and ceramics industries. Hydrofluoric acid (HF) has a wide variety of industrial applications including electroplating, non-stick surfaces, plastics and uranium manufacture.

Longstone Edge also houses the only UK processor of fluorspar ore - Glebe Mines at Cavendish Mill. We understand that the fluorspar refining process requires a feed stock average concentration of 28% fluorspar, with a minimum fluorspar content of 20%.

By far the largest consumption of HF goes into producing chloroflurocarbons (CFCs) which are used in refrigerants, propellants and synthetic foam and well-known as ozone-depleting chemicals. CFCs were originally being phased-out in favour of hydrofluorocarbons (HFCs) which do not deplete ozone, but HFCs are now known to contribute to the 'greenhouse effect'. This means that demand for fluorspar could decline in the future as these chemicals are phased out.

Limestone

Limestone is a sedimentary rock composed largely of calcium carbonate, CaCO3. Pure limestone is white or almost white and, like fluorspar, may be coloured by impurities. It may be crystalline, clastic, granular, or massive, depending on the method of formation.

As well as its use in architecture, it has an enormous number of industrial uses:

Longstone Edge consists of limestone deposits from the carboniferous period, which is a very low grade, friable material and, as such, its primary use is to be crushed as aggregate.