Fracture flow and preferential groundwater flow paths in hard rocks : illustrations from Precambrian and lower Palaeozoic strata in Wales

Groundwater in the Lower Palaeozoic and Precambrian hard rocks is mainly constrained to
limited storage and circulation in an upper weathered and fractured zone. Some deeper
circulation via favourable fractures is possible and there may be hydraulic connection with
storage in Quaternary gravels and with surface waters. Examples from Wales illustrate some of
the features typical of the small aquifer units that occur in these hard rocks and provide some of
the methodologies that have been attempted in understanding groundwater recharge, storage and
transport on a catchment scale.