Read Ebook: Ukraine the land and its people by Rudnytskyi Stepan

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Only at a point where a river, a streamlet, even a balka opens into the sea, is the steep incline of the steppe-plateau broken. We then see before us an enormous pond as it were, at the upper end of which the water-course enters and the lower end of which is locked from the sea side by a land-tongue or bar as by a flat dam. This sea-water lake is called liman in Ukrainian.

Wherever a stream of great volume empties into a liman, the bar is severed at one or more places. These liman deltas are called, in Ukrainian, hirl?. Limans which have such connections with the sea are broken. Of such a kind are the limans of the Kunduk, Dniester, Boh and Dnieper. Where a little streamlet discharges which has not a sufficient volume of water to cover the loss from evaporation of the liman surface and still retain an excess for keeping open the outlet, then the bar of the liman is without an opening and the water contains a great deal of salt. Of this kind are, above all, the limans of Kuyalnik and Khadshib? near Odessa, the large, deep Tilih?l and many smaller ones. The water and the mud of such limans possess healing powers, and every summer thousands of patients travel to the hot shores of the limans to regain their health.

The limans are simply submerged eroded valleys of steppe rivers which are now being filled in by alluvial deposits. Therefore, the limans of all larger rivers are too shallow to serve as good harbors for the larger sea-going vessels. The liman of the Dniester allows entrance only to small ships drawing two meters of water; the gigantic Dnieper liman is only 6 m. deep, and only the Boh liman is accessible to larger sea-going ships. Systematic dredging, however, could, without a doubt, bring relief, and would change a number of the limans into profitable harbors.

Beginning at the liman of the Dnieper, the coast is strongly indented as far as the bay of Karkinit, but these indentations are closed off by long tongues of land and the undersea extension of the bar of Bakalsk. The west coast of Crimea is also a uniform liman coast, increasing constantly in height, however, toward the south. At the Alma delta the coast becomes steep and has two excellent harbors, Sevastopol and Balaklava, which are submerged deep valleys. The southeast coast of the Crimean peninsula is a strongly marked acclivitous shore. The steep descent of the Yaila Mountains has been transformed here, thru the abrasive action of the sea, into a beautiful coastline. Eruptive rock, capable of offering great resistance, is found here in places, forming picturesque capes, jetties and crags, between which lie pretty little bays and coves. The agreeable climate, the clear sky, the good sea-baths and the beautiful country annually lure to this Ukrainian Riviera thousands of consumptives and health-seekers. There are rows and rows of cottage-colonies and mansions.

Beginning at the crescent-shaped bay of Feodosia, the coast again becomes lower and also has a number of salty lagoons and bars. Of the same description are the coasts of the Strait of Kerch, leading into the Sea of Azof, which is 35,000 sq. km. in area. This extremely flat sea is often compared to a liman. Numerous tongues of land jut out here into the sea, showing very clearly in their direction the effect of the cyclonal motion of the air. The low coast has an enormous number of limans and lagoons, e.g., Utluk, Mius, Molochni, Yeski, Akhtirski, Tamanski, Kisiltash, etc. The most remarkable part of the Sea of Azof, however, is the Sivash. A bar 111 km. in length shuts the Sivash off from the Sea of Azof, leaving only a connecting passage of 150 m., near Henichesk. The curiously ragged banks of red-clay, the salt swamps, lagoons and islands, the bracken, ill-smelling water, which is salty in summer, and in a few spots at other times as well, have given the Sivash the name of Foul Sea .

The eastern part of the Ukraine's Black Sea coast is a mountainous cliff-coast again. The plications of the western Caucasus, which approach the sea obliquely, are here so quickly destroyed by the powerful abrasive action of the surf, that the erosive action of the rivers and mountain streams cannot keep pace. Therefore, the crest is difficult of access and only the two harbors of Novorossiysk and Gelendshik offer shelter for ships along this part of the coast. But even this shelter is doubtful, because of the bora-like winds.

As we perceive from this description of the Ukrainian coast, it is not one which would promote navigation among the inhabitants. Lack of harbors, isolation, remoteness from the main lines of the world's traffic, never could have an encouraging effect upon the development of navigation among the Ukrainians. Despite all this, however, they developed very high seafaring qualities in the time of the old Kingdom of Kiev and later on in the Cossack period, and the present age, too, has brought a revival of the nautical skill of the Ukrainian coast population.

GENERAL SURVEY OF THE PHYSICAL GEOGRAPHY OF UKRAINE

THE UKRAINIAN MOUNTAIN COUNTRY

Glancing at the map of the Ukraine, we perceive at once that in this country we should seek in vain for such a variety of surface configuration as is peculiar to Central or Western Europe. In Germany or France there appear in a comparatively small space the most varied landscape--chains of high mountains, central chains of mountains, terrace and hill country, plateaus and plains.

It is different here in our wide Ukraine. One can travel hundreds of miles in any direction without seeing a change in the character of the scenery. The uniformity which is typical for Eastern Europe is peculiar also to the Ukraine. But not to the extent that it is to Great Russia, where the endlessness of the flat country wearies the eye of the traveler. For there are in the Ukraine landscapes of high and central chains of mountains, picturesque hill districts and richly cut plateaus, marshy plains and steppes strewn with barrows. There is, then, in the Ukraine, a variety of surface configuration, but on a large scale, not as in Western or Central Europe, confined in a small space.

The morphological nucleus of the Ukraine is the closed group of plateaus, which extends from the country at the foot of the Carpathians and the Polish part of the Vistula region to the Sea of Azof. Pontian Plateau or Avratinian Ridge are the commonly used but incorrect names of this plateau group. The first designation might do, but the second transfers the name of a little destitute hamlet at the source of the Sbruch to a territory of hundreds of thousands of square miles. We shall, therefore, select for this plateau group the name Ukrainian Plateau Group.

It forms a compact whole between the Carpathians and the Dnieper and is divided into the following individual sections: The Rostoch, between the San and Buh Rivers; Volin, between the Boh and the Teterev; Podolia, between the Dniester and the Boh; the Pocutian--Bessarabian Plateau, between the Dniester and the Prut; the Dnieper Plateau, between the Boh and the Dnieper. The plateau character continues at the rapids section of this river on the left bank, where, at some distance, the last member of the Ukrainian Plateau Group lies--the Donetz Plateau.

The plateau group of the Ukraine is bordered on the north and south by two plain districts. The northern district consists of adjoining lowlands--Pidlassye, Polissye, and the Dnieper plain--and their extensions along the Donetz; the southern district is made up of the long stretch of the Pontian steppe-plain, which, in the country at the foot of the Caucasus, merges into the Caspian desert-steppe.

Beyond the northern plain district, Ukrainian territory does not extend, except in the Don region, where it embraces the southern spurs of the Central Russian Plateau.

Besides these plateau and plain regions the Ukraine takes in also parts of three mountain systems of the European continent. The Ukraine is the only country of Eastern Europe which extends over into the region of the European mountains of plication. Parts of the Carpathians, the little Yaila chain of Crimea, and the western parts of the Caucasus lie, together with their environs, in Ukrainian territory.

From this general survey of the surface configuration of the Ukraine, we can easily see that more than nine-tenths of the surface of this land is taken up by plains and plateaus. Nine-tenths of the Ukrainians have certainly never seen a mountain and do not even know what one looks like. Expressive of this circumstance is the fact that in the wide plateau and plain region of the Ukraine the most insignificant hills bear the high-sounding name of "mountain." But, despite this, the Ukraine also has its share in the three mountain systems of Europe--the Carpathians, the Yaila, and the Caucasus. All three were formed thru plication of the rock-layers.

The vast plication-formed mountain range of the Caucasus, even in the small part belonging to Ukrainian territory, attains an alpine height; the scenery of the Yaila along the Crimean Riviera is wonderful, but the Carpathians, altho not as lofty as the Caucasus and not of such scenic beauty as the Yaila, are the dearest to the heart of the Ukrainian. For the Ukrainian nation expanded in the Caucasus only a century ago and has but just reached the Yaila. And the Eastern Carpathians have for more than a thousand years been a Ukrainian mountain range.

Still, hardly one-third of the 1300 km. curve of the Carpathians belongs to Ukrainian national territory. Toward the west the Carpathians are inhabited by Poles and Slovaks; in the east and south by the Roumanians.

The boundary-posts of the Ukrainian territory extend in the west beyond the famous defile of Poprad. From the rounded peaks of the mountain country where the last Ukrainian villages lie, one sees rising at a very short distance the imposing range of the Tatra; still nearer lie the cliffs of the Pienini, famous geologically as well as for their scenery. In the eastern part of the Carpathian chain, Ukrainian territory reaches the Prislop pass, which connects the valleys of the Golden Bistritz and the Visheva . To the Ukraine, then, belongs the sandstone district of the Carpathians at that point where it is highest and most developed. It is called simply the "wooded Carpathians."

The western part of the sandstone Carpathians which lies within Ukrainian territory is called the Low Beskid. It is also known as Lemkivski Beskid because it is inhabited by the Ukrainian mountain tribe of the Lemkes. The Low Beskyd extends from the defile of Poprad to the valleys of the Strviazh River, the Oslava , and the Laboretz. It is a broad-backed but not a high mountain country. In long chains, gently undulating mountain ridges stretch from west to east and southeast. Their slopes are gentle; one can easily walk or even ride up, and numerous wagon-roads and highways lead straight over the crest or even along the edge of the crest. The peaks are rounded and of uniform height, except where an occasional gently vaulted mountain top rises above the low-hill country. Between gently sloping ranges there extend, in a longitudinal direction, valleys with watersheds and communicating passes. Broad, well-developed defiles separate the range into different sections. The Galician-Hungarian dividing-ridge has only slight gorges of genuine mountain passes.

The peaks and high passes of the Lower Beskid are insignificant. Only in the extreme west, on the Poprad and the Torissa, do the peaks reach a height of 1000 and 1100 m.; further toward the east hardly 700 to 800 m. The important Dukla Pass is hardly 500 m. above sea-level. In the middle of the Beskid mountain country we even see a great longish strip of lower country whose low hills are less than 300 m. high.

There is a connection between the insignificant height and soft landscape forms of the Low Beskid and the geological construction and evolution of the mountain range. This mountain country, like the whole sandstone-region of the Carpathians, is built up of strongly plicate and compressed Flysch--a series of sandstones, slates, conglomerates, clays, etc., of the cretacian and tertiary ages. All these species of rock occur in this region in thin layers and have little power of resistance; everywhere the basic mountain ridge is covered with a thick coat of weathering loam; rock piles are found very seldom. There is added the fact that all the sandstone Carpathians of the Ukrainian territory have been evened out by the destructive action of water and air into a more or less perfect plain. Not until the quaternary was the "obliterated" range raised anew and transformed into a mountain district by the action of the rivers which were cutting in again.

The Low Beskid was once covered with great, mixed forests. Now the once splendid virgin forests are completely thinned and all the ill effects of forest destruction have visited the poor mountain country. The fertile soil was washed away on the mountain-sides and heaped up with rubble and mud in the valley bottoms. The tribe of the Lemkos is therefore, perhaps, the poorest of all the Ukrainians and is compelled to seek an existence in distant lands.

In the southern part of the Low Beskid the boundaries of the Ukrainian nation in Hungary reach the northern part of the Hegyalia-Sovari Ridge, which, at this point, is 1100 m. high, and is composed of extinct trachyte volcanoes.

To the east of the Lupkiv Pass begins the second section of the Ukrainian Carpathians--the High Beskid. It stretches to the southeast as far as the valleys of the Stri, Opir and Latoritzia Rivers .

The High Beskid like the Low is composed of a number of parallel, weakly joined mountain ranges, which run northwest and southeast. The type of the Rost Mountains is, therefore, even more clearly marked in this part of the sandstone Carpathians than in the preceding. The mountain crests are gently sloped, the edge of the crests slightly curled, the height of the peaks constant, the passes only walled passes. Toward the southeast, tho, the ridge steadily increases in height. The highest peaks are Halich , the beautifully pyramid-shaped rocky Piku and the massive Polonina ruvna

In the Flysch of the High Beskid, two species of sandstone attain greater power of forming layers and of resisting pressure--the chiefly upper cretacian Yamna sandstone and the oligocene Magura sandstone. The former forms beautiful groups of rocks on peaks and precipices. The cliffs of Noich, with its traces of a rock castle, are the most famous.

The longitudinal valleys are much less developed in the High Beskid than in the Low. They are traversed only by smaller brooks. All larger streams like the Strviazh, Dniester and Opir, flow thru well-formed passes. Expansions of valleys alternate with contractions of valleys . Most remarkable are the deeply cut out winding valleys , which offer the best proof of the former smoothing down and the later raising of the mountains.

Beautiful beech and evergreen forests still cover large parts of the High Beskid. Above the tree-line we meet for the first time with the characteristic plant-formation of the Polonini which yield excellent pasturage for large and small cattle during the summer and create the foundation for a primitive dairy industry.

Along the southern foot of the High Beskid, and separated from it by a chain of longitudinal valleys, a long chain of mountains rises above the neighboring Hungarian plain, bearing the name of Vihorlat . The Rivers Uz , Latoritzia and Bershava, have cut the Vihorlat into four sections. The range is lower than the Beskyd, since it is less than 1100 m. high, but it is strongly cut up by deep-gorged valleys, and has steep, rocky precipices, bold rocky summits and pretty little mountain lakes. The range, which is covered with thick oak forests, owes its scenic character to its geological composition. The Vyhorlat is a line of extinct volcanoes, in the old craters of which the mountain lakes of the region lie. The firm trachyte lava forms picturesque rock walls and peaks. East of the Verezki Pass begins a new mountain section, perhaps the most characteristic one in the sandstone Carpathians. It extends toward the east as far as the passes of the Prut and the Black Tyssa and the Yablonitza Pass. This part of the sandstone Carpathians bears the name of Gorgani.

The uniform mountain walls of the Beskid give way here to shorter mountain ridges, strongly cut up by cross valleys. The main streams of the northern slope, Opir, Limnitzia--the two Bistritzas--flow thru deep, picturesque passes; still deeper are the valleys of the mountain streams which flow into the Theiss, as the Torez, Talabor, etc. It is a remarkable circumstance that the dividing border ridge is lower than the ridges facing it on the north and south, which are broken thru by magnificent passes.

The edge of the Gorgani ridge also shows traces of the old leveling-surface and has only small gorges, yet it is much more curled than in the Beskid. The ridge often becomes a sharp edge and the cone-shaped peaks further break its monotony. The height of the peaks is much greater than in the Beskyd. On the Galician side the Popadia attains a height of 1740 m.; Doboshanka, 1760 m.; Visoka, 1810 m.; Sivula, 1820 m.; in Hungarian territory the Stoh in the picturesque Bershavi group is 1680 m.; the Blisnitza, in the Svidovez Range, 1890 m., etc.

The ridges and peaks of the Gorgani are covered with seas of sandstone boulders and are, therefore, difficult of access. The light gray Yamna sandstone, of great resisting power, appears in this mountain section in very thick layers, and is the cause of the greater height and the bolder forms which, in places, are suggestive of high mountain ranges. The energetic weathering process, aided by the cover of winter snow, breaks up the mighty sandstone layers into great rocks, boulders, fragments and rubble. Deep fissures yawn between moss and lichen-covered boulders, many boulders rock under the foot of the wanderer, and many of them, thru caving-in and thru accumulation, have formed natural chambers and hollows. The rocky ridges, covered with seas of boulders, are Arshizia, the Gorgan peaks, whence comes the name of the entire mountain range. The seas of boulders and rubble-stone are called Zekit or Grekhit.

In the highest groups of the Gorgani Range are found also distinct traces of the glacial age, glacial excavations with small lakes or with swamps that have taken the place of lakes.

A splendid, only slightly thinned dress of virgin forest covers the Gorgani Chain. The lower forest section is composed of beech, ash and fir trees, the upper part of pines and stone-pines. The tree limit is very irregular and vascillates between 1100 and 1600 m. Mountain pastures are very rare, because of the seas of boulders and rubble-stone, but there are large and beautiful, tho not easily accessible, stocks of mountain pines.

The last section of the Ukrainian Carpathians is called Chornohora . It extends from the Prut and the Black Theiss to the Prislop Pass; to the valley of the Visheva and of the Golden Bistritza. In this wide and long mountain district we find greater morphological variety than in the mountain sections hitherto discussed. In the wide zone of the northern foothills, which separate with a distinct edge from the sub-Carpathian hills and continue into the Bukowina, we find low ridges and rounded peaks, as in the High Beskid. Only in places on peaks and valley sides piles of rock are seen. Then toward the interior of the range follows the wide vale of Zabie, imbedded in soft slate, and above it rises the mighty chain of the Chornohora, the only part of the sandstone region of the Carpathians which has high mountain formations. The chain is composed of the hard magura sandstone, rich in mica. A whole stretch of peaks here attains a height of 2000 m., the highest being the Hoverla . Well-formed, partly rocky ribs branch off from the main ridge on either side. The rock piles of the Shpitzi, Kisli and Kisi Ulohy, are some of the most imposing rock formations of the Carpathian sandstone region. Between the rocky ribs, finely developed glens lie on both sides of the main ridge of the Chornohora, the beds of the ancient glaciers. Waterfalls dash down the steep rock walls in silver streams--of particular interest is the cascade of the Prut under the Hoverla--and down below lie little crater lakes reflecting the patches of summer snow on the crater walls. Almost three-fourths of the year the Chornohoras are covered with snow. In summer the snow almost wholly disappears, and the beautiful carpet of flowers of the mountain pastures, only occasionally interrupted by dark green reserves of mountain-pine, spreads out over the ridges and peaks of the Chornohora. Every summer innumerable herds of cattle, small Hutzul horses and sheep are seen here. Then an intensive dairy industry enlivens the peak regions of the range for three months. The lower regions are still covered with extensive forests; in lower locations we find mixed forests here; in higher altitudes, almost pure stocks of pines.

Standing on one of the Chornohora peaks, on the Hoverla for instance, or the Petros or Pip Ivan, we see, in the near southwest, a new and strange mountain world. It is the third zone of the Chornohora Mountains, the mountain land of Marmarosh. Situated in the region of the headwaters of the Theiss and orographically related to the Chornohora, the mountains of the Marmarosh are of entirely different geological composition and have a different morphological appearance. Gneiss and other kinds of crystalline slate, permotriassic and jurassic conglomerates and limestones, as well as eruptive rock of older and of more recent date, lend great geological and morphological variety to the Marmarosh Mountains. The high mountain character here is even more marked than in the Chornohoras. Rocky peaks, ridges, mountain walls, numerous craters, with small glacial lakes, adorn the Marmarosh mountains, which rise higher than 1900 m.: Pip Ivan, Farko, Mikhalek, Petros, Troiaga. Toward the southeast the range wanders over into South Bukowina, where its last boundary-posts, the rocky peaks of Yumalen and Rareu really stand on Roumanian ground. And in the south, beyond the Visheva Valley, which divides the settlements of the Ukrainian Hutzuls from those of the Roumanians, rises the magnificent lofty rampart of the Rodna Mountains, with its two peaks of 2300 m., Pietrosu and Ineu.

On the outside of the Carpathian curve stretches a hill country of varying breath, the sub-Carpathian hill-country, in Ukrainian: Pidhirye or Pidkarpatye. The mountain-edge of the Carpathian, which is at all points very distinct, rises steeply over the low-hill country at the foot, along an extended line in the neighborhood of the cities of Peremishl, Sambir, Drohobich, Striy, Kolomia. The Carpathian rivers leave the mountains by way of funnel-shaped valleys, bordered by boulder terraces, and spread their alluvial mounds over the low hill country. Wide stretches of meadow accompany the river courses; fields and woodland lie at a distance. The sub-Carpathian hill-country is built up of miocene gray clays which, along the edge of the Carpathians, contain an enormous treasure of petroleum, ozokerite, kitchen salt and potash salts. Boulders lie on the clay, not only along the rivers, but also on the hilltops--traces of old watercourses, which transported Carpathian and northern rubble-stone toward the east in the direction of the Dniester. The yellowish cover of loam and loess lies over the whole, and its surface-layer, abounding in vegetable soil, is, in places, very fertile.

The sub-Carpathian hill country reaches to the two sub-Carpathian plains in the north--the Vistula and the Dniester Plain. Only along the European main divide a tongue of hill-country projects in the direction of Lemberg. In the glacial period, watercourses of great volume flowed directly across this hill-country divide, which, as might be expected, is now completely cleft by the bifurcation of the Vishnia, depositing considerable masses of rubble-stone and sand. Thru destruction of forests, the sands have become subject to wind action and dreary landscapes of sand-dunes have been formed.

Only the southeastern reaches of the Vistula Plain, extending along the San River to Peremishl are part of Ukrainian territory. The low loam bags, which lie between sandy and swampy valleys of the San, form the only rises of ground in this plain, which borders in the northeast on the spurs of the Rostoch.

The Dniester Plain extends in a broad ribbon along the river from the place where it leaves the mountains to the delta of the Striy. Its western part is a single great swamp region, a one-time large lake. The rivers flow on flat dams, and when the melting snows come and the rains of early summer, they overflow their banks and flood the swampy plains far and near. In some years the swamp region changes into a lake for days and weeks. In the dry season only a few swamp lakes remain, but the entire region remains a swamp and produces only a poor sour hay. Settlements lie only on the high banks of the rivers.

The eastern part of the Dniester Plain extends beyond the great alluvial mounds of the Striy River, and then reaches over into the broad valley of the Dniester, which ends in the Podolian Plateau at the point where the river enters. The eastern Dniester Plain is not very swampy, and only in places do ravines, swamps, and old river beds accompany the river course. For the most part pretty meadows, fields and woods lie on the thick sub-layer of rubble-stone and river-loam.

If the Carpathians represent a primeval section of Ukrainian ground, the mountain ranges of Crimea and the Caucasus were entirely strange to the Ukrainians not so very long ago. How many Ukrainian slaves, in the time of Tartar oppression, cursed the rocky-wall of the Yaila which separated them from their beloved home. How discontented was the enslaved remainder of the Zaporogs when transported to the Western Caucasus.

Now the conditions are quite changed. The great colonizing movement of the Ukrainians touched the Yaila as much as twenty years ago, and has extended the frontiers of the Ukrainian settlements along the outer mountains of the Caucasus to the Caspian Sea. And the once strange, hostile mountain-worlds have opened their doors to Ukrainian colonization.

The Yaila Mountains of Crimea are, in comparison with the Carpathians, a small mountain system hardly 150 km. long and 35 km. wide. They lie in three parallel ranges, separated by longitudinal valleys, along the southeast shores of the peninsula. The northern declivities of all the ridges are gently sloping, the southern ones steep. The southern main range exceeds a height of 1500 m. with its peaks, Chatirdagh, Roman-chosh, and Demir Kapu. This main ridge, which declines toward the sea in steep precipices, is flat and rocky on top, strewn with rock-craters; it bears the name Yaila and serves as a lean mountain pasture. Deep gorges cut the rough surface of the summit and divide it into single table mountains.

The mountains of Crimea, like the Carpathians, are mountains of plication. They are composed of Jurassic, chalk, and miocene-layers. The large blocks of lime of the Jurassic, which rest on softer slates and clays, form the main ridge of the mountains. Besides craters, we find, in the limestone mountains of the Yaila, impassable furrows and numerous hollows.

Very picturesque is the magnificent precipitous decline of the main range of the Yaila to the sea. Here the entire southern part of the range has sunk in great ravines and the resisting power of the eruptive rocks which appear here has created a coastal mountain landscape of great beauty. Protected by the mountain wall from northerly winds, a Mediterranean flora has been able to develop here at the southern foot of the range, while beautiful leafy forests partly cover the declines of the mountains.

On the peninsula of Kerch, which forms the eastern extreme of Crimea, a low steppe-like hill-country extends seemingly as a prolongation of the Yaila Range. The new tertiary clays are here laid in flat folds, which are more closely related to the Caucasus. Here, and on the quite similarly formed Taman peninsula, we find many small cone-shaped mud volcanoes which emit gases, smoke, and thinly flowing blue-gray mud from their miniature craters.

The magnificent lofty range of the Caucasus forms the boundary-post of the Ukraine on the east. Only the western part of the mountain system lies within Ukrainian territory. We shall, therefore, discuss it quite briefly.

The Caucasian Mountain system, which is 1100 km. in length, lies like a huge wall of rock between Europe and Asia. Most geographers consider the Caucasus as part of the latter continent, which is correct in so far as these mountains show many characteristics of Asiatic mountain ranges. First of all they are hard to cross, much harder than the highest mountains of Europe, the Alps. Along a stretch of 700 km., the ridge of the Caucasus descends only twice to a level of 3000 m. On the other hand, the Caucasus is not wide--on the average only 150 km.--and at the point where the Grusinian army road crosses the range, barely 60 km. Then, the Caucasus, like many mountain ranges of Asia, stretches in a straight line from the peninsula of Taman to the peninsula of Apsheron, famous for its abundance of petroleum.

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