Masson Hill Quarry, Matlock, Derbyshire Dales District, Derbyshire, England, UKi
Regional Level Types | |
---|---|
Masson Hill Quarry | Quarry (Reclaimed) |
Matlock | Town |
Derbyshire Dales District | District |
Derbyshire | County |
England | Constituent Country |
UK | Country |
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Latitude & Longitude (WGS84):
53° 7' 40'' North , 1° 34' 21'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SK286591
Type:
Quarry (Reclaimed) - last checked 2020
Köppen climate type:
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Peak Lapidary and Mineral Society | Bakewell, Derbyshire | 12km |
The Russell Society | Knighton | 34km |
Mindat Locality ID:
1495
Long-form identifier:
mindat:1:2:1495:6
GUID (UUID V4):
a963c14b-f993-498a-9a99-6f515683ad9c
Other/historical names associated with this locality:
Masson Opencast
Mining has been active around Matlock, Derbyshire, from medieval times to the present, firstly for lead and more recently for fluorspar. Amongst the more important areas has been around the summit of Masson Hill, which has been intensely mined for fluorspar throughout the 20th century. Masson Hill itself is a prominent topographical feature, rising to 335 m, and situated 1.5 km west of Matlock. The mineralisation consists of a series of intermittent smaller flats and/or pipes over a distance of 1500 m. The largest single flat worked (or more strictly a pipe since the strike length was greater than its width along the dip) was that at the site of Masson Opencast Quarry, having a strike length of greater than 500 m and width of 240 m. The main ore horizon was restricted to the basal 6 m of the Matlock Lower Limestone (Lower Carboniferous, Brigantian Age), although mineralisation was found to occur above this within the overlying dolomites of the same formation. The basal limestone at the locality is thickly bedded and poorly jointed, containing noticeable fossil debris and with calcite veining.
Mineralogically, the ore consists of approximately 60% fluorite, 20% quartz, 15% calcite and less than 5% baryte, and traces of galena, sphalerite and other sulphides. It occurs as replacements of the limestone and as open space infilling, and is a direct result of the interaction of a number of geological processes. The fluorite is normally colourless to pale yellow, less often it is blue, green, or purple, the last colour being especially common at the crystal edges or surfaces near to other minerals, especially baryte and smithsonite. Cubic crystals are common. Three types of inclusions in the fluorite occur: the relict sedimentary carbonates and quartz within; fluid inclusions; and primary sulphides common to all fluorites. The most common inclusions are bravoite, pyrite, marcasite, and chalcopyrite.
In the early 30s there was, for a short time, up to ten limestone quarries in production along the Derwent Valley between Matlock Bath and Darley Dale. All were eating into the base of Masson Hill, whilst to the south and west (at Cromford, Bonsall and Ible) there were other quarries nibbling at the same hill.
In 1935, Derbyshire Stone Ltd was formed to bring together the quarrying assets of several local companies.
From 1939 to 1945, the growing demand for minerals caused hitherto deserted lead mines to be explored and reopened for the winning of gangue minerals. Old tips and hillocks were removed even though the quality was low grade. This demand for crude ore continued long after the war to enable rebuilding. The wartime production at the summit of Masson Hill was opencast, limestone being crushed in a mill at the site or taken to Derbyshire Stones primary crushers at nearby Cawdor Quarry, whilst the minerals won were taken to the mineral processing plant at Megdale, sited just above Cawdor Quarry.
After the war (and into the 1960s) fluorspar, baryte, calcite, the lead/zinc ores, sands and gravel and of course coal, all had a great future in Derbyshire.
In 1968, Tarmac acquired Derbyshire Stone Ltd and continued with quarrying operations. The large opencast quarry at Masson Hill frequently broke into 18th/19th century old mine workings.
Beneficiation of fluorspar was carried out at Cavendish Mill, near Eyam, operated by Laporte Industries Ltd. Opened in 1965, Cavendish Mill was designed to process ore from a variety of sites throughout the Derbyshire Orefield, including Masson Opencast. At one stage Cavendish Mill was one of the largest and most efficient fluorspar processing sites in Europe.
However, diminishing reserves of ore eventually resulted in quarrying operations at Masson Opencast gradually coming to an end during the 1970s. Many of the quarries in the area also ceased operating due to cheaper imports. By August 1979, the large hole at Masson Hill, originally excavated by Derbyshire Stone Ltd and subsequently run by Laporte Industries Ltd, had been back-filled to original contours and by 1980 the surface of the site had been cleaned up and landscaped, although a section of the opencast was left open so as to preserve geological features.
In the 1980s, Laporte disposed of its manufacturing operations due to loss of their business to foreign imports. Despite the cessation of fluorspar processing by Laporte, Glebe Mines was established in November 1999 to continue the processing business based at Cavendish Mill because U.K. users of acid grade fluorspar still wished to use the high quality Derbyshire material.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
ⓘ Baryte Formula: BaSO4 |
ⓘ Calcite Formula: CaCO3 References: |
ⓘ Cerussite Formula: PbCO3 |
ⓘ Fluorite Formula: CaF2 References: |
ⓘ Galena Formula: PbS |
ⓘ Hemimorphite Formula: Zn4Si2O7(OH)2 · H2O |
ⓘ Quartz Formula: SiO2 |
ⓘ Quartz var. Rock Crystal Formula: SiO2 |
ⓘ Smithsonite Formula: ZnCO3 References: |
ⓘ Sphalerite Formula: ZnS |
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Sphalerite | 2.CB.05a | ZnS |
ⓘ | Galena | 2.CD.10 | PbS |
Group 3 - Halides | |||
ⓘ | Fluorite | 3.AB.25 | CaF2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | var. Rock Crystal | 4.DA.05 | SiO2 |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Calcite | 5.AB.05 | CaCO3 |
ⓘ | Smithsonite | 5.AB.05 | ZnCO3 |
ⓘ | Cerussite | 5.AB.15 | PbCO3 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Baryte | 7.AD.35 | BaSO4 |
Group 9 - Silicates | |||
ⓘ | Hemimorphite | 9.BD.10 | Zn4Si2O7(OH)2 · H2O |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
C | Carbon | |
C | ⓘ Calcite | CaCO3 |
C | ⓘ Cerussite | PbCO3 |
C | ⓘ Smithsonite | ZnCO3 |
O | Oxygen | |
O | ⓘ Baryte | BaSO4 |
O | ⓘ Calcite | CaCO3 |
O | ⓘ Cerussite | PbCO3 |
O | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
O | ⓘ Quartz | SiO2 |
O | ⓘ Smithsonite | ZnCO3 |
O | ⓘ Quartz var. Rock Crystal | SiO2 |
F | Fluorine | |
F | ⓘ Fluorite | CaF2 |
Si | Silicon | |
Si | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Quartz var. Rock Crystal | SiO2 |
S | Sulfur | |
S | ⓘ Baryte | BaSO4 |
S | ⓘ Galena | PbS |
S | ⓘ Sphalerite | ZnS |
Ca | Calcium | |
Ca | ⓘ Calcite | CaCO3 |
Ca | ⓘ Fluorite | CaF2 |
Zn | Zinc | |
Zn | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
Zn | ⓘ Smithsonite | ZnCO3 |
Zn | ⓘ Sphalerite | ZnS |
Ba | Barium | |
Ba | ⓘ Baryte | BaSO4 |
Pb | Lead | |
Pb | ⓘ Cerussite | PbCO3 |
Pb | ⓘ Galena | PbS |
Other Regions, Features and Areas containing this locality
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