Polymict conglomerate of predominantly limestone pebbles, with abundant green silicate grains in matrix. Green silicate grains are subhedral-euhedral crystals Well-rounded clasts have heavily altered rims. Matrix is white micrite/microcrystalline calcite. Note brown is filler.
Comments:
This locality has not been confirmed.
References:
Further information:
Corsi's classification:
Class 10. Pudding-stones; ii. Italian pudding-stones