Cell Fechan


LocationSH614164 (Area map showing location.)
ParishLlanaber
GeologyThe ore bed is about .25m thick, is interbedded with Harlech grits and imediately underlain by a 50mm bed of shaly sandstone containing numerous large cubes of iron pyrites. The whole series dips east at about 70°. The ore consists mostly of carbonate of manganese with hydrated black oxide coating it where exposed to the weather. Associated with the ore are many veins of quartz which sometimes contain copper pyrites. Large botryoidal lumps of manganese also occur. [Dewey & Bromehead 1915: 51]
Owners
1899  Edith M Abraham
1900–1902  Thomas Abraham  Down [1980: 63] shows Abraham as Operator 1900–1903
1903  Mary Edith Abraham presumed same person as Edith M Abraham above agent Thomas Abraham
1904–1905  Mrs Laura Williams
1906  Edward Jones
1907–1908  Miss Laura Williams  presumed same person as Mrs Laura Williams above
Agents
1903  Thomas Abraham
Recorded output

(tons)
Manpower
underground surface
189928  
1900277  
1901150  
190280  
1903120  
190490  
190550  
1906100  
190741  
19084011
Total867 
TransportThere is a network of tracks cut into the slope or on stone embankments which possibly served the workings.
RemainsA series of shallow depressions and grassed-over waste tips with two underground workings at SH615167. The workings continue northwards across a ravine (with stream) as Cell Fechan mine and southwards as Barmouth mine. (December 2001)
There are remains of a leat at SH617167 associated with a boggy depression SH618167 which may be the site of an old reservoir. However, it is not known if this was associated with the mine.

graphic: plan

Dewey & Bromehead [1915: 51] reporting on Cell Fechan and Hafotty about this time describe the mines as “abandoned” with the levels flooded and overgrown but with a good deal of ore remaining.

photo: entrance   Entrance

Entrance to worked out chamber at SH615167.

This entrance faces north and is the more northerly of the two underground workings referred to above. The other working has a south facing entrance and is a few metres to the south of this entrance, roughly aligned with it on the other side of a knoll.



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