6
PHYSICAL
ASPECTS OF SUFFOLK.
In a subtropical climate palms grew on the coast with figs, sequoias and magnolias. T h e sea covered most of Suffolk and extended to northern France. After long ages, in the OLIGOCENE epoch, the sea floor rose again ; land stretched from Ireland to north Germany. Over this there wandered mammals, such as Hyopotamus and Palaotherium, in a landscape very different from any that had gone before, since, in addition to other plants of which we may name Sequoia and Osmunda, there was grass, which sheltered snails and insects and the like. It is hard to over-estimate the debt we owe to the grasses on which almost all modern animals and all mankind depend. Denudation continued its work, and much of the Oligocene land (made of Eocene material) was worn off. T h e climate grew somewhat colder as Oligocene passed into MIOCENE.—All about this time, for many millennia, the world was undergoing a seismic and volcanic revolution of such a vast and thorough-going type that mountains were crushed up all round the earth : the Alps and Himalayas are legacies of those days. Suffolk however was in a quiet area and, although on a map it would have been quite unrecognisable, there were certain similarities with the conformation today. A North Sea was formed, somewhat east of the present. There was even an Aide, a Deben, a Gipping and a Stour, which were the vague beginnings of those we know.—Finally a new subsidence occurred and the sea ran in, probably forming the ' Coprolite Bed ' at the base of the Crags with its ear bones of Whales and other remains now black and phosphatised.
ON
THE
LOCAL BY T .
NIOBE
NAUNTON
BUTTERFLY.
WALLER.
IT has been suggested to me as desirable that, in view of the forthcoming detailed Catalogue of Suffolk Lepidoptera that our Society proposes to issue, I should State the facts of my " beginner's l u c k " in having possessed the sole example of Argynnis Niobe, Linn., found in Britain throughout the whole of last Century. For this purpose it is essential to wax personal: I was born in 1863 ; and in 1876 my late father, the Revd. T . H . Waller of Waldringfield near Woodbridge, sent me to King Edward vi's Grammar School in Bury St. Edmunds, then under the headmastership of the Revd. A. H . Wratislaw, M.A. (Trans, ii, p. 64), father of our present Member A. C. Wratislaw, C.B., C.M.G., etc. Occasionally the Head, who was very keen on