The principal fuel in the islands is peat, the cutting of which, carried on for centuries, ever since the time of Torf Einar, who is said to have taught the natives the use of “turf” for burning, has denuded the surface, and left it blacker than it otherwise would be. That, and the practice of “scalping” turf for roofing purposes, have laid bare great stretches of what might have been fairly good pasture ground.

The proportion of arable land is very small compared with the whole land surface of the islands. For this reason Shetland has never figured as an agricultural county; and other causes may be mentioned, such as divided attention between the two branches of industry—fishing and crofting; indifferent soil; variable climate; antiquated methods of cultivation; and want of markets for agricultural produce.

Being far removed from the centres of commerce, and having few natural resources in themselves, the islands are almost entirely lacking in manufactures. Fishing and farming are the chief industrial pursuits, while the rearing of native sheep, ponies and cattle form a considerable part of the rural economy. Along with every croft or holding goes the right of common pasturage in the hills and moors, called “scattald.” Crofts would be of little value without this common grazing, which is a remnant of the old Norse odal system of land tenure, and is peculiar to the islands of Shetland and Orkney. The word scattald is from scat, a payment, akin to scot in “scot and lot.”

3. Size. Position. Boundaries

In size, Shetland ranks fifteenth among the Scottish counties; but in population only twenty-seventh. The total area (excluding water) is 352,319 acres or 550½ square miles. The group consists of about one hundred islands, of which twenty-nine are inhabited. The largest is Mainland, which embraces about three-fourths of the whole land-surface; and the others, in point of size, are Yell, Unst, Fetlar, Bressay and Whalsay. Yell measures 17½ miles by 6½, Unst 12 by nearly 6. The smaller islands include East and West Burra, Muckle Roe, Papa Stour, Skerries, Fair Isle and Foula; the remainder consisting of islets, holms, stacks and skerries. From Fair Isle, which lies about mid-way between Orkney and Shetland, to Sumburgh Head, is 20¼ miles; and from that point to Flugga in Unst, in a straight line, is 71 miles. From Sumburgh Head to Fethaland, the most northerly part of the Mainland, is 54 miles; and the greatest breadth, from the Mull of Eswick to Muness, is about 21 miles.

Including Fair Isle and Foula, the group lies between the parallels of 59° 30´ and 60° 52´ north latitude; and between 0° 43´ and 2° 7´ west longitude. The general trend of the islands is north-easterly, and their position in relation to the mainland of Scotland is also in that direction; Sumburgh Head being 95 miles north-east of Caithness and 164 miles north of Aberdeen.

The North Sea washes the eastern sea-board, and the Atlantic Ocean the western; sea and ocean join forces between Sumburgh Head and Fair Isle to form that turbulent tideway called the “Roost.” They also meet north of Yell and Unst, where the Atlantic sets strongly through Yell Sound and Blue Mull Sound for six hours during flood tide, and the North Sea, in its turn, in the opposite direction for the other six hours.

4. Surface and General Features

The surface of the larger islands is hilly, and the general direction of the ridges is north and south, corresponding to the length of the islands. The inland parts present an undulating surface of peat bogs and moorland, dotted here and there with fresh-water lochs, which accentuate, rather than relieve, the monotony of the landscape. The hills are round or conical in shape and of moderate height, ranging from 500 to 900 feet. Unlike the rounded hills of the Lowlands of Scotland, which are often grassy to the top, most of the Shetland hills are brown and barren, being covered with heather and moss or short coarse grass. Neither have they the rugged grandeur of the Highlands, for the sides are generally smooth and rounded, the result of intense glaciation.