Sarn y Bwch, (Welsh for 'buck's causeway'), is one of three parallel reefs extending beneath the sea into Cardigan Bay from the west coast of Wales.
The causeway, probably a medial moraine, is made of glacial deposits left by receding ice sheets at the end of the last ice age.
Sarn y Bwch is the central one of the three, extending south-westwards from near Tywyn.
To the north is the causeway of Sarn Badrig, whilst to the south is Sarn Gynfelyn, which extends from near Aberystwyth.
This Gwynedd location article is a stub.