Slate is a metamorphic rock, formed under great pressure from what was originally mudstone. Its origins in Wales date back to the Paleozoic age between 350 and 500 million years ago. There are three types of slate found in Wales - Silurian, Ordovician and Cambrian.
Silurian is the most recent and is found in the Llangollen, Glyn Ceiriog and Corwen areas. It is not particularly durable but the industry in those parts developed because of its closeness to major markets. Its lack of durability is noticeable in the waste heaps which have turned back to shale in some cases.
Ordovician slate is found around Blaenau Ffestiniog and Corris, it is generally mined underground. It is almost uniformly blue-grey and is easily split using machines.
Cambrian
is the oldest type and found in the north around Bethesda, Llanberis and
in the Nantlle Valley. The colour is variable with a tendency towards
purple, slates of this type are still mainly split and dressed by hand
although there has been some success with mechanisation. (continued)
A
flooded pit working - Dyffryn Nantlle.
Pit
quarries suffered from the disadvantage of requiring constant pumping,
when work ceased the majority rapidly flooded leaving scenes like this
at Dorothea Quarry, Nantlle.
A
photo taken at Maenofferen quarry when it was still in production - this
shows the tunnel or adit leading to an underground working. Also
visible is a weighbridge, rubbish wagon, slab wagon and an upturned wagon
turntable.
Gallery working
in an open quarry.
Galleries could be up to 75 feet high.
One thing that all slate quarries had in common was waste rock. On average 90% of the rock excavated ended up on the tips - in extreme cases it could be over 95%. These monumental tips are at Dinorwic Quarry.