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Speedwell Mine (Oakden Level), Castleton, High Peak, Derbyshire, England, UKi
Regional Level Types
Speedwell Mine (Oakden Level)Mine
CastletonCivil Parish
High PeakBorough
DerbyshireCounty
EnglandConstituent Country
UKCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
53° 20' 28'' North , 1° 47' 31'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SK139827
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Hope900 (2018)3.0km
Hope Valley1,001 (2012)3.2km
High Peak92,600 (2012)4.6km
Bamford859 (2018)6.9km
Tideswell1,647 (2018)7.1km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Peak Lapidary and Mineral SocietyBakewell, Derbyshire17km
Mindat Locality ID:
5210
Long-form identifier:
mindat:1:2:5210:1
GUID (UUID V4):
bdf37d7d-02a3-400c-b579-ebb3c9639171


While it was earlier believed that this level was driven to open up the veins on Long Cliff hill at depth (Carruthers & Strahan, 1923), there is now evidence that it was actually designed to intersect previously known stream caverns so as to develop a boat-haulage mining operation (Rieuwerts & Ford, 1985).

In 1771, a shaft was sunk to a depth of 72 feet at the foot of Long Cliff and in 1772, the level was started southwards from the shaft bottom at an average rate of 4 feet 6 inches per week. Around 1778-1779, it intersected Faucet Rake at 750 yards from its entrance, which was found completely hollowed out, leaving a deep but narrow cavern which extends more than 150 feet above the level and 50 feet below it and is now known as the Bottomless Pit. When the level was continued, the excavated rubbish was dumped in the chasm without any visible effect. At 270 feet south of the cavern, the level turns southwest and continues another 700 feet where it holed into the stream caverns along New Rake in 1781. A length of 350 feet of the natural passageways was then modified by the miners until 1782.

While the veins of New Rake are exposed in the caverns, they do not carry much ore and do not appear to have been worked. Most of the production of the mine obviously came from pipes that branch from the caverns at various places and some of them have been mined out. Operations ceased in 1794, presumably because the returns were disappointing, but the mine was reworked several times until the middle of the 19th century.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Galena2.CD.10PbS
Group 3 - Halides
Fluorite3.AB.25CaF2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4
Wulfenite7.GA.05Pb(MoO4)

List of minerals for each chemical element

CCarbon
C CalciteCaCO3
OOxygen
O BaryteBaSO4
O CalciteCaCO3
O WulfenitePb(MoO4)
FFluorine
F FluoriteCaF2
SSulfur
S BaryteBaSO4
S GalenaPbS
CaCalcium
Ca CalciteCaCO3
Ca FluoriteCaF2
MoMolybdenum
Mo WulfenitePb(MoO4)
BaBarium
Ba BaryteBaSO4
PbLead
Pb GalenaPbS
Pb WulfenitePb(MoO4)

Other Regions, Features and Areas containing this locality

British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
EuropeContinent
UK

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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