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HIGHLAND BRITAIN AND LOWLAND BRITAIN

SIR HALFORD MACKINDER in his now classic book, Britain and the British Seas, published in 1902, made a simple yet fundamental distinction between two roughly equal halves of the island of Britain. If one draws a line approximately from the mouth of the Tees to the mouth of the Exe it will be found that all the main hill masses and mountains lie to the north and west, the major stretches of plain and lowland to the south and east. To the north and west lies Highland Britain, to the south and east lies Lowland Britain. There is rarely, in nature, a sharp line between two such regions but rather does the one fade gradually into the other. This is true in Britain; nevertheless it is possible to draw a line with some accuracy and this has been done in Fig. 1.

In Highland Britain the dominant character of the country is upland. There are large and continuous stretches more than a thousand feet above sea level; plains and valleys occur but they are of limited extent and tend to form interruptions in the general upland character of the country as a whole. In some places are rugged mountains and even at lower levels crags of rock may appear at the surface. Even where the rocks do not thus appear at the surface itself they are often but thinly covered by poor stony soils, whilst the many steep slopes as well as the broken character of the relief may make farming difficult. On the whole man has sought out for himself the more sheltered situations for his farms, his villages and his towns. They nestle in valleys ; they flourish and spread only where the larger tracts of flat land or more fertile soil occur or where man has been attracted to otherwise inhospitable surroundings by stores of mineral wealth. The higher, poorer, wetter or less accessible parts of Highland Britain have been left largely to nature. There are vast stretches of moorland, some of it covering land from which the original forest cover has been removed, as well as mosses and bogs, scrub woodland and forests. We may summarise the position by saying that in Highland Britain human settlement is essentially discontinuous: the cultivated areas occupy valleys and plains separated by large expanses of uncultivated hill lands. This is well shown in the aerial view of a Lakeland valley in Plate I.

Lowland Britain offers a striking contrast in many ways. Though so much less rugged, there are few parts where level land is uninterrupted by hills and such true plains as do exist are to a considerable degree the result of man’s handiwork—as the large stretch of the drained fenlands of eastern England bears witness. Lowland Britain is best described as an undulating lowland where lines of low hills are separated by broad open valleys and where “islands” of upland break the monotony of the more level areas.

FIG. 1.—Highland Britain and Lowland Britain

Even the highest of the hills scarcely ever exceed a thousand feet above sea level, though many of the ridges reach 600 or 700 feet. The environment is kinder ; the soils tend to be deeper and richer, there are few steep slopes to interrupt cultivation and plough lands are to be found right to the tops of the hills. There is little to hinder man’s use of the whole: human settlement is essentially continuous and the cultivated land of one parish merges into that of the next. Villages and towns are closely and evenly scattered ; their siting has sometimes been dictated by convenience of a water supply, sometimes by situation on a natural routeway, sometimes just to maintain an even spacing of settlements. It follows that the greater part of Lowland Britain is occupied by farmland—by “cultivated” or “improved” land, which includes both plough and grass land—and that such moorlands, heaths, “wastes” and other unimproved lands as occur, do so as islands interrupting the otherwise continuous farmland and coinciding with patches of poorer soils.

It so happens that the rain-bearing winds in Britain blow from the west, especially from the south-west, and that the hill masses of Britain are in the west of the country. As a result Highland Britain as a whole gets a heavy rainfall, for the hills stand in the path of the rain-bearing winds, whilst most of the Lowland Britain is relatively dry. Taking a very general figure, most of Highland Britain gets more than 30 inches of rain a year while most of Lowland Britain gets less. Since the trouble with our climate is that we tend to get too much rain and too little sun it is clear that differences in climate reinforce those due to other features between Highland and Lowland Britain. In the far north-west, for example, where lowland does exist it is of comparatively little value because heavy rainfall and constant cloud result in water-logged conditions and almost useless bogs occur where otherwise good farmland might be found. The contrast in rainfall is shown in the accompanying map, while the effect of the combination of high ground and high rainfall is well brought out in Fig. 3 which shows the general distribution of moorland.

Although the chief visible contrasts between Highland and Lowland Britain are thus to be found in elevation, relief of the ground and soils, these are, in fact, the results of the underlying geological structure. The rocks which underly the hills are for the most part old even in the geological sense and in the course of ages have tended to become indurated and hard or at least resistant to weathering and hence tend to form hill masses rising above the general level. The rocks which underly the lowlands on the other hand are younger in the geological sense, though often very ancient if measured in years. They are softer or less resistant to weathering—there is evidence of this in the muddy streams to be seen after heavy rain, showing that soil or mud or silt is being swept off the land and carried seawards.

It happens that Highland Britain is made up mainly of rocks which are older than the Coal Measures (which contain the bulk of workable coal seams in this country) whereas Lowland Britain is made up mainly of rocks which are younger than the Coal Measures. It is for this reason that we find most of the coalfields of Britain on the margins of the highlands and the lowlands.

FIG. 2.—The Mean Annual Rainfall of the British Isles, showing the contrast between the wetter west and the drier east

The greatest of them all, the Yorkshire, Nottinghamshire and Derbyshire Coalfield, stretches up on to the Pennines and down on to the lowlands ; so do the coalfields of Lancashire and of Northumberland and Durham. The great South Wales field lies just north of the fertile Vale of Glamorgan and amongst the moorland heights.

FIG. 3.—The Chief Moorland Areas of Great Britain, showing the close correspondence with areas of heavy rainfall (Fig. 2) and their association with Highland Britain

As a prelude to understanding the different regions of Britain and consequently the varied habitats in which our plants and animals live it is thus essential to understand. the geology and structure of the ground and to appreciate something of the long and complicated geological history of the country.