The eastern Lowlands of England consist of a succession of gently
undulating ridges, separated from each other by winding vales or
plains. These features have a general trend across the country from
south-west or west to north-east or east--a direction determined by the
successive outcrops of the different formations. But the denudation
of the surface has been so great and so unequal that, despite the
continuity and parallelism of the formations, their outcrops have
been worn into endless diversities of topographical detail, producing
abundant variety among the gentle profiles of the landscapes.
As examples of the ridges, we may take the North and South Downs, and
the chain of heights that stretches from Wiltshire into Norfolk. The
intervening plains may be illustrated by the Weald of Sussex, and by
the lower basin of the Thames.
The differences between the successive geological formations of the
English lowlands never pass a restricted limit in regard to composition
and structure. Essentially soft and easily decomposable, the rocks
include no thick bands of much harder material than the rest, such as
might project in prominent features. The prevailing characteristic
of the topography is therefore unbroken placidity. Nowhere does any
ruggedness obtrude itself. No part of the ground towers abruptly above
or sinks suddenly beneath the general level. The successive ranges of
low hills have rounded summits and smooth slopes, which, even when
steep, seldom allow naked rock to appear, but conceal it everywhere
under a carpet of herbage. So gentle is the inclination of the ground,
from the watersheds to the coast, that the drainage winds in sluggish
streams that often hardly seem to flow. 'Purling brooks' are scarcely
ever to be found. Since the running waters of the country have played
no inconsiderable part in the inspiration of our poets, it is well
worthy of remark that in the east and south-east of England the streams
are, for the most part, silent. We shall see how strongly they are thus
contrasted with the brooks that traverse the lowlands of the north.
Public-domain text, read in full here on John Shaqi.
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