Page:Quarterly Journal of the Geological Society of London, vol. 33.djvu/50

28 found in Triassic strata near Runcorn, and several Calamites in the water-stones of Lymm, near Warrington. Gradually, therefore, I doubt not, the land-surfaces of the period of the dark red sandstone, as well as of the overlying Triassic beds, will be discovered, and the connexion be traced between the plants of the great Carboniferous era and those of succeeding ages.