An English Shire

For the reasons which have determined the existence of Sussex as a county of England, and which have given it the exact boundaries that it now possesses, we must go back to the remote geological history of the secondary ages. Its limits and its very existence as a separate shire were predetermined for it by the shape and consistence of the mud or sand which gathered at the bottom of the great Wealden lake, or filled up the hollows of the old inland cretaceous sea. Paradoxical as it sounds to say so, the Celtic kingdom of the Regni, the South Saxon principality of Ælle the Bretwalda, the modern English county of Sussex, have all had their destinies moulded by the geological conformation of the rock upon which they repose. Where human annals see only the handicraft and interaction of human beings--Euskarian and Aryan, Celt and Roman, Englishman and Norman--a closer scrutiny of history may perhaps see the working of still deeper elements--chalk and clay, volcanic upheaval and glacial denudation, barren upland and forest-clad plain. The value and importance of these underlying facts in the comprehension of history has, I believe, been very generally overlooked; and I propose accordingly here to take the single county of Sussex in detail, in order to show that when the geological and geographical factors of the problem are given, all the rest follows as a matter of course. By such detailed treatment alone can one hope to establish the truth of the general principle that human history is at bottom a result of geographical conditions, acting upon the fundamentally identical constitution of man.

In a certain sense, it is quite clear that human life depends mainly upon soil and conformation, to an extent that nobody denies. You cannot have a dense population in Sahara; and you can hardly fail to have one in the fruitful valley of the Nile. The growth of towns in one district rather than another must be governed largely by the existence of rivers or harbours, of coal or metals, of agricultural lowlands or defensible heights. Glasgow could not spring up in inland Leicestershire, nor Manchester in coalless Norfolk. Insular England must naturally be the greatest shipping country in Europe; while no large foreign trade is possible in any Bohemia except Shakespeare's. So much everybody admits. But it seems to me that these underlying causes have coloured the entire local history of every district to an extent which few people adequately recognise, and that until such recognition becomes more general, our views of history must necessarily be very narrow. We must see not only that something depends upon geographical configuration, not even merely that a great deal depends upon it, but that everything depends upon it. We must unlearn our purely human history, and learn a history of interaction between nature and man instead.

From the great central boss of the chalk system in Salisbury Plain, two long cretaceous horns or projections run