The main lead ore mineral within the Northern Pennine carbonate-hosted gale
na-fluorite orefield is silver-bearing galena. Numerous reliable assay and
recovery records, from the heyday of lead mining during the eighteenth and
nineteenth centuries, indicate that silver values in the ores then being mi
ned were typically fairly modest, in the range 100-250 ppm Ag. Historical r
ecords from the area written during the eleventh and twelfth centuries, alt
hough very much less complete and more open to interpretation, indicate lev
els of silver production which could not have been sustained from such ores
. It is suggested that lead ores with much higher silver content may have b
een available in these earlier times. A few scattered occurrences of galena
with enhanced silver content may represent the vestiges of these ores.