Plynlimon Mine, Ponterwyd, Cwmrheidol, Ceredigion, Wales, UKi
Regional Level Types | |
---|---|
Plynlimon Mine | Mine (Abandoned) |
Ponterwyd | - not defined - |
Cwmrheidol | - not defined - |
Ceredigion | County |
Wales | Country |
UK | Country |
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Latitude & Longitude (WGS84):
52° 27' 19'' North , 3° 46' 30'' West
Latitude & Longitude (decimal):
UK National Grid Reference:
SN794857
Type:
Mine (Abandoned) - last checked 2020
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Capel Bangor | 256 (2017) | 14.5km |
Machynlleth | 2,235 (2017) | 15.9km |
Llanidloes | 2,929 (2017) | 15.9km |
Bow Street | 1,572 (2017) | 17.2km |
Borth | 1,269 (2017) | 19.0km |
Mindat Locality ID:
4250
Long-form identifier:
mindat:1:2:4250:8
GUID (UUID V4):
1872d17e-bb1f-48eb-994b-7eb9274b9b67
Other/historical names associated with this locality:
Dyfed; Cardiganshire
Probably the highest mine developed in the mid-Wales area at 540 mts. Although the mine is one of the most remote in in mid-Wales. It was quite succesfull at times. A shoot of ore was developed between the 36 and 48 fathom levels for a lenth of about 58 fathoms. The first recorded working was in about 1854, and then on a number of occassions utill 1896.
The total recorded output is 3271 tons of lead ore.
Jan 2019. The mine was developed on a lode that obliquely crosses the stream from the south-west to north-east. An adit is located above the track on the west bank whilst between the track and stream are several spoil heaps and a well preserved wheelpit.
Tips dominate the eastern bank with 2 shafts and a flooded open gunnis towards the north where the track crosses the stream. The tips have been excavated for aggregate for the track which is consequently a source of galena.
There is a prominent dam that once retained a reservoir north of the bridge. Where the dam has been breached the stone facing on the pond side has been revealed. The course of the aqueduct from the western side of the dam is apparent and beneath the tips beside the stream the remnants of a wooden boxed launder can be seen.
A further shaft is located at the crest of the hill on the north east side of the site, though development does not appear to have been extensive.
The main tips are abundant with solid pieces of galena many bigger than a golf ball with bright cubic crystal habit (possibly the best samples of galena from any of the mines so far visited within the Ceredigion Mountains locality). Sphalerite and marcasite are also relatively common, whilst pyromorphite is uncommon though abundant within individual samples. The tip at the north-eastern shaft on the hilltop produces abundant calcite associated with pyrite, rarely as 1-2mm cubes, and is also abundant with sphalerite whilst galena is noteably absent which represents a distinct change from the main tips which were presumably excavated from the shafts beside the stream.
Also notable is the tip associated with the adit which is barren for minerals but is comprised of highly fractured sandstone, whereas the main tip is comprised of blocks of foliated mudstone and the tip at the crest of the hill is of a paler mudstone. These are all classed within the Bryn-glas formation but clearly represent different phases of deposition as noted by the British Geological Survey: "Bryn-glas Formation - Slumped Mudstone, Slumped Siltstone And Slumped Sandstone. Sedimentary Bedrock formed approximately 444 to 445 million years ago in the Ordovician Period. Local environment previously dominated by deep seas. These sedimentary rocks are marine in origin. They are detrital and comprise coarse- to fine-grained slurries of debris from the continental shelf flowing into a deep-sea environment, forming distinctively graded beds."
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
7 valid minerals.
Detailed Mineral List:
β Calcite Formula: CaCO3 Description: This is quite abundant in the small tip associated with the shaft at the highest point of the mine but elsewhere is only infrequently found. It was found associated with sphalerite and pyrite but not galena. References: |
β Cerussite Formula: PbCO3 |
β Galena Formula: PbS |
β Marcasite Formula: FeS2 |
β Pyrite Formula: FeS2 |
β Pyromorphite Formula: Pb5(PO4)3Cl |
β Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Galena | 2.CD.10 | PbS |
β | Pyrite | 2.EB.05a | FeS2 |
β | Marcasite | 2.EB.10a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
β | Quartz | 4.DA.05 | SiO2 |
Group 5 - Nitrates and Carbonates | |||
β | Calcite | 5.AB.05 | CaCO3 |
β | Cerussite | 5.AB.15 | PbCO3 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
β | Pyromorphite | 8.BN.05 | Pb5(PO4)3Cl |
List of minerals for each chemical element
C | Carbon | |
---|---|---|
C | β Calcite | CaCO3 |
C | β Cerussite | PbCO3 |
O | Oxygen | |
O | β Calcite | CaCO3 |
O | β Cerussite | PbCO3 |
O | β Pyromorphite | Pb5(PO4)3Cl |
O | β Quartz | SiO2 |
Si | Silicon | |
Si | β Quartz | SiO2 |
P | Phosphorus | |
P | β Pyromorphite | Pb5(PO4)3Cl |
S | Sulfur | |
S | β Galena | PbS |
S | β Marcasite | FeS2 |
S | β Pyrite | FeS2 |
Cl | Chlorine | |
Cl | β Pyromorphite | Pb5(PO4)3Cl |
Ca | Calcium | |
Ca | β Calcite | CaCO3 |
Fe | Iron | |
Fe | β Marcasite | FeS2 |
Fe | β Pyrite | FeS2 |
Pb | Lead | |
Pb | β Cerussite | PbCO3 |
Pb | β Galena | PbS |
Pb | β Pyromorphite | Pb5(PO4)3Cl |
Other Regions, Features and Areas containing this locality
British and Irish IslesGroup of Islands
Eurasian PlateTectonic Plate
EuropeContinent
UK
- Wales
- Cambrian MountainsMountain Range
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