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SIBERIAN NATIVES.

The exploration of this seaboard had thus to be prosecuted in Siberia itself by means of vessels built for the river navigation. In 1648, the Cossack Dejnev sailed with a flotilla of small craft from the Kolîma round the north-east extremity of Asia, passing long before the birth of Bering through the strait which now bears the name of that navigator. Stadukhin also explored these eastern seas in search of the islands full of fossil ivory, of which he had heard from the natives. In 1735, Pronchishchev and Lasinius embarked at Yakutsk and sailed down the Lena, exploring its delta and neighbouring coasts. Pronchishchev reached a point east of the Taimir peninsula, but failed to double the headlands between the Lena and the Yenisei estuaries. The expedition begun by Laptiev in 1739, after suffering shipwreck, was continued overland, resulting in the exploration of the Taimir peninsula and the discovery of the North Cape of the Old World, Pliny's Tabin, and the Cheluskin of modern maps, so named from the pilot who accompanied Pronchishchev and Laptiev. The western seaboard between the Yenisei and Ob estuaries had already been surveyed by Ovtzin and Minin in 1737–9.

But the problem was already being attacked from the side of the Pacific Ocean. In 1728, the Danish navigator, Bering, in the service of Russia, crossed Siberia overland to the Pacific, whence he sailed through the strait now named from him, and by him first revealed to the West, though known to the Siberian Cossacks eighty years previously. Even Bering himself, hugging the Asiatic coast, had not descried the opposite shores of America, and was uncertain as to the exact position of the strait. This point was not cleared up till Cook's voyage of 1778, and even after that the Sakhalin, Yezo and Kurile waters still remained to be explored. The shores of the mainland and islands were first traced by La Pérouse, who determined the insular character of Sakhalin, and ascertained the existence of a strait connecting the Japanese Sea with that of Okhotsk. This completed the general survey of the whole Siberian seaboard.

The scientific exploration of the interior began in the Eighteenth Century with Messerschmidt, followed by Gmelin, Müller, and Delisle de la Croyère, who determined many important physical points between the years 1733 and 1742. The region stretching beyond Lake Baikal was explored by Pallas and his associates in 1770–3. The expeditions, interrupted by the great wars following on the French Revolution, were resumed in 1828 by the Norwegian Hansteen, whose memorable expedition in company with Erman had such important results for the study of terrestrial magnetism. While Hansteen and Erman were still prosecuting their labours in every branch of natural science, Alexander von Humboldt, Ehrenberg, and Gustav Rose made a short visit to Siberia, which, however, remained one of the most important in the history of science. Middendorff's journeys to North and East Siberia had also some very valuable results, and were soon followed, in 1854, by the "expedition to Siberia" undertaken by Schwartz, Schmidt, Glehn, Usoltzev, and associates, extending over the whole region of the Trans-baikal to the Lena and northern tributaries of the Amur. Thus began the uninterrupted series of modern journeys, which are now being systematically continued in every part of Siberia, and which promise soon to leave no blanks on the chart of that region.

The work of geographical discovery, properly so called, may be said to have been brought to a close by Nordenskjöld's recent determination of the north-east passage, vainly attempted by Willoughby, Barents, and so many other illustrious navigators.

Such a vast region as Siberia, affected in the west by Atlantic, in the east by Pacific influences, and stretching north and south across 29° of latitude, must obviously present great diversities of climate. Even this bleak land has its temperate zones, which the Slav colonists are fond of calling their "Italies." Nevertheless as compared with Europe, Siberia may, on the whole, be regarded as a country of extreme temperatures—relatively great heats, and, above all, intense colds. The very term "Siberian" has justly become synonymous with a land of winds, frosts, and snows. The mean annual temperature in this region comprised between the rivers Anabara and Indigirka is 20° Fahr. below freezing point. The pole of cold, oscillating diversely with the force of the lateral pressure from Yakutsk to the Lena estuary, is the meteorological centre round which the atmosphere revolves. Here are to a large extent prepared the elements of the climate of West Europe.

Travellers speak of the Siberian winters with mingled feelings of terror and rapture. An infinite silence broods over the land—all is buried in deep sleep. The animals hibernate in their dens, the streams have ceased to flow, disappearing beneath the ice and snow; the earth, of a dazzling whiteness in the centre of the landscape, but grey in the distance, nowhere offers a single object to arrest the gaze. The monotony of endless space is broken by no abrupt lines or vivid tints. The only contrast with the dull expanse of land is the everlasting azure sky, along which the sun creeps at a few degrees only above the horizon. In these intensely cold latitudes it rises and sets with hard outlines, unsoftened by the ruddy haze elsewhere encircling it on the edge of the horizon. Yet such is the strength of its rays that the snow melts on the housetop exposed to its glare, while in the shade the temperature is 40° to 50° below freezing point. At night, when the firmament is not aglow with the many-tinted lights and silent coruscations of the aurora borealis, the zodiacal light and the stars still shine with intense brightness.

To this severe winter, which fissures the surface and rends the rocks of the rivers into regular basalt-like columns, there succeeds a sudden and delightful spring. So instantaneous is the change that nature seems as if taken by surprise and rudely awakened. The delicate green of the opening leaf, the fragrance of the budding flowers, the intoxicating balm of the atmosphere, the radiant brightness of the heavens, all combine to impart to mere existence a voluptuous gladness. To Siberians visiting the temperate climes of Western Europe, spring seems to be unknown beyond their lands. But these first days of new life are followed by a chill, gusty and changeful interval, arising from the atmospheric disturbances caused by the thawing of the vast snowy wastes. A relapse is then experienced analogous to that too often produced in England by late east winds. The apple blossom is now nipped by the night frosts falling in the latter part of May. Hence no apples can be had in East Siberia, although the summer heats are otherwise amply sufficient for the ripening of fruit. After the fleeting summer, winter weather again sets in. It will often freeze at night in the middle of July; and after the 10th of August the sear leaf begins to fall, and in a few days all are gone, except perhaps the foliage of the larch. The snow will even sometimes settle early in August on the still leafy branches, bending and breaking them with its weight. Below the surface of the ground, winter reigns uninterrupted even by the hottest summers.

With its vast extent and varied climate, Siberia naturally embraces several vegetable zones, differing more from each other even than those of Europe. The southern Steppes have a characteristic and well-marked flora, forming a continuation of that of the Aral, Caspian and Volga plains. The treeless northern tundras also constitute a vegetable domain as sharply defined as the desert itself, while between these two zones of Steppe and tundra the forest region of Europe stretches, with many subdivisions, west and east right across the continent. Of these subdivisions the chief are those of the Ob, Yenisei, Lena, and Amur basins.

Beyond the northern tundras and southern Steppes by far the greatest space is occupied by the forest zone. From the Urals to Kamchatka the dense taiga, or woodlands are interrupted only by the streams, a few natural glades and some tracts under cultivation. The term taiga is used in a general way for all lands under timber, but east of the Altai it is applied more especially to the moist and spongy region overgrown with tangled roots and thickets, where the mari, or peat bogs, and marshes alternate with the padi, or narrow ravines. The miners call by this name the wooded mountains where they go in search of auriferous sands. But everywhere the taiga is the same dreary forest, without grass, birds, or insects, gloomy and lifeless, and noiseless but for the soughing of the wind and crackling of the branches.

The most common tree in the taiga is the larch, which best resists the winter frost and summer chills. But the Siberian woodlands also include most of the trees common to temperate Europe—the linden, alder, juniper, service, willow, aspen, poplar, birch, cherry, apricot—whose areas are regulated according to the nature of the soil, the elevation or aspect of the land. Towards the south-east, on the Chinese frontier, the birch is encroaching on the indigenous species, and the natives regard this as a sure prognostic of the approaching rule of the "White Tsar."

Conflagrations are very frequent in the Siberian forests, caused either by lightning, the woodmen, or hunters, and sometimes spreading over vast spaces till arrested by rivers, lakes or morasses. One of the pleasures of Siberian travelling is the faint odour of the woods burning in the distance.

The native flora is extremely rich in berries of every kind, supplying food for men and animals.

The extreme eastern regions of the Amur basin and Russian Manchuria, being warmer, more humid and fertile, also abound more in animal life than the other parts of Asiatic Russia. On the other hand, the Siberian bear, deer, roebuck, hare, squirrel, marmot and mole are about one-third larger, and often half as heavy again as their European congeners. This is doubtless due partly to the greater abundance of nourishment along the rivers and shores of Siberia, and partly to the fact that for ages the western species have been more preyed upon by man, living in a constant state of fear, and mostly perishing before attaining their full development.

The Arctic Seas abound probably as much as the Pacific Ocean with marine animals. Nordenskjöld found the Siberian waters very rich in molluscs and other lower organisms, implying a corresponding abundance of larger animals. Hence fishing, perhaps more than navigation, will be the future industry of the Siberian coast populations. Cetacea, fishes, molluscs, and other marine organisms are cast up in such quantities along both sides of Bering Strait that the bears and other omnivorous creatures have here become very choice as to their food. But on some parts of the coast in the Chukchi country whales are never stranded, and since the arrival of the Russians certain species threaten to disappear altogether. The Rhytina stelleri, a species of walrus formerly frequenting Bering Strait in millions, was completely exterminated between the years 1741–68. Many of the fur-bearing animals, which attracted the Cossacks from the Urals to the Sea of Okhotsk, and which were the true cause of the conquest of Siberia, have become extremely rare. Their skins are distinguished, above all others, for their great softness, warmth, lightness, and bright colours. The more Alpine or continental the climate, the more beautiful and highly prized become the furs, which diminish in gloss towards the coast and in West Siberia, where the south-west winds prevail. The sables of the North Urals are of small value, while those of the Upper Lena, fifteen degrees farther south, are worth a king's ransom. Many species assume a white coat in winter, whereby they are difficult to be distinguished from the surrounding snows. Amongst these are the polar hare and fox, the ermine, the campagnol, often even the wolf and reindeer, besides the owl, yellow-hammer, and some other birds. Those which retain their brown or black colour are mostly such as do not show themselves in winter. The fur of the squirrels also varies with the surrounding foliage, those of the pine forests being ruddy, those of the cedar, taiga, and firs inclining to brown, and all varying in intensity of colour with that of the vegetation.

Other species besides the peltry-bearing animals have diminished in numbers since the arrival of the Russian hunters. The reindeer, which frequented the South Siberian highlands, and whose domain encroached on that of the camel, is now found only in the domestic state amongst the Soyotes of the Upper Yenisei and is met with in the wild state only in the dwarf forests and tundras of the far north. The argali has withdrawn to Mongolia from the Siberian mountains and plains, where he was still very common at the end of the last century. On the other hand, cold and want of food yearly drive great numbers of antelopes and wild horses from the Gobi Steppes towards the Siberian lowlands, tigers, wolves and other beasts of prey following in their track, and returning with them in the early spring. Several new species of animals have been introduced by man and modified by crossings in the domestic state. In the north, the Samoyeds, Chukchis, and Kamchadales have the reindeer and dog, while the horse and ox are everywhere the companions of man in the peopled regions of Siberia. The yak has been tamed by the Soyotes of the Upper Yenisei, and the camel, typical of a distinctly Eastern civilization, follows the nomads of the Kirghiz and Mongolian Steppes. All these domesticated animals seem to have acquired special qualities and habits from the various indigenous or Russian peoples of Siberia.