Page:Quarterly Journal of the Geological Society of London, vol. 35.djvu/844

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PROF. E. HULL ON THE DINGLE BEDS AND
Fig. 2.—Section across the Dingle Promontory from Brandon Head to Minard Head, showing the unconformity of the Old Red Conglomerate to the Upper Silurian and Dingle Beds, &c. (Scale 1 inch to 1 Mile.)

Quarterly Journal of the Geological Society of London, Volume 35, 0844.png

a. Old Red Sandstone and Conglomerate.

c. Wenlock and Ludlow beds: purple cleaved plates and thin grits, surmounted by green grits.

d. Green grits (Glengariff Beds).

e. Probably slates.

f. "Glengariff grits," massive green grits and conglomerates, capped by Old Red Sandstone (a).

g. Upper purple slate series.

h. Dark slates (Llandovery? or Lower Silurian).