Note 56 — PART III.
Reading edition
Blanckenhorn, thinking that the bed capping the island of Geziret el Qorn is identical with that forming the plain around and to the north of Dimê, has, in a section recently published (Neues zur Geol. u. Palænt. Ægyptens, IV. Das Pliocän, etc., Zeitschr. d. Deutsch. geol. Gesellsch., Jahrg. 1901, Taf. XIV, fig. 2), inserted a number of faults letting the beds down continually to the south. The beds however are not identical, and no faults occur.