THE FOUR BELTS
These four great belts may be traced, not only in the relief of the county, but also in its superficial geology; the sea plain is throughout of a deep, strong, brown loamy soil, among the most fertile in England, and fetching by far the highest rents paid anywhere in the county. In the best of its stretch, between Chichester and Worthing, it is from four to six miles broad, closely inhabited and, though recently marred by the growth of a whole string of watering-places, still preserving a very characteristic life of its own. Except Chichester no town of any antiquity stands upon it, but it nourishes a great number of prosperous agricultural villages, the size and the architecture of whose churches are sufficient to prove their economic condition in the past.
Among the most characteristic of these is Yapton, which is supposed to be the “tun” or hamlet of Eappa—a comrade of St. Wilfred’s, the missionary and the first bishop of the county. Lyminster is another excellent example of what these places were in the past, and its great church is the more striking from the decay of the parish around it.
The forest ridge (to take the farther boundary first) has, though somewhat confused, a geological characteristic of its own, for it consists of sand rising from and mixed with the clay of the Weald. This clay, in its turn, lying between the forest ridge and the Downs, though diversified by occasional outcrops of sand, is fairly uniform. From the beginning it has been covered, not very thickly, but very generally, with those short, strong oaks which have furnished the timber for all the old buildings of the county. We will turn later to the question of whether this stiff and somewhat ungrateful soil of the Weald was ever wholly uninhabited: in this initial survey it must suffice to remark that even to-day the development of that soil is difficult. Places specially favoured with good water have been occupied for centuries, and form at the present time the market towns of the Weald. The spaces between them are remarkable
LYMINSTER
WATER ON THE WEALD
for the isolation of their farmhouses, and to-day for the way in which the Londoner is discovering to his cost the stubborn nature of the county. Modern invention, and especially the invention of the motor car, has made this situation tempting enough to townsmen, but the new buildings which they attempt to found upon places whose desertion is incomprehensible to them are met with continual difficulties. The water is often bad, the soil much damper in winter than the summer promised—for these experiments are nearly always the result of a first view taken in the height of summer. The long, and often futile, digging for good water, the cost of pumping it when, if ever, it is found, combine to make the new attempts at building on the clay of the Weald grow slacker as time proceeds. There are, however, more grateful opportunities scattered here and there in those outcrops of sand and gravel of which I have spoken. Haywards Heath has grown up in this way, and there are a multitude of villages half-way between the forest ridge and the Downs which owe the greater part of their beauty to the sharp contours of the sandstone.
These outcrops have formed centres of population from the very earliest times, as, for example, at Burton, Egdean, Thakeham, Ashington, and in many other places.