Roumania Past and Present - James Samuelson (13 ebook reader .TXT) 📗

brownish-yellow translucent crystalline hydrocarbon, which softens with the warmth of the hand, and burns with a bright light. It has never been industrially applied, excepting in small quantities by the peasantry, who themselves fabricate rude candles from it; but this is owing rather to want of enterprise than to scarcity of the deposit. Anthracite, too, is present in various places, but it is not worked. Of the existence of iron there is no doubt whatever. Not only are there indications of it in the ferruginous brooks and springs, but it has been found in association with coal in various parts of the country.[18] Specimens of hæmatite have several times been submitted to analysis, but the results were very unsatisfactory. One sample tested by M. Hanon gave only 35.5 per cent., and another by Dr. Bernath yielded 40 per cent., of metallic iron. That gold has been found and was worked in the Carpathians as far back as the Dacian age is well known; and, according to modern writers, cobalt, sulphur, arsenic, copper,[19] and lead are also present in different districts, but the workable minerals of Roumania are at present limited to salt, petroleum, and lignite; and, looking to the importance of the subject, it is much to be regretted that the Government does not take the same means to instruct the population in practical geology and mineralogy as are employed to disseminate agricultural knowledge at the excellent institution to which reference will be made hereafter. If the people are only allowed to develop their industries in peace, it will no doubt soon become apparent that the strata are charged with considerable stores of mineral wealth.

[Footnote 15: The chief are R.F. Peters ( Die Donau und ihr Gebiet . Leipzig: Brockhaus, 1876. Cap. xii. p. 313), Fuchs, Bernath, and D.T. Ansted. There have also been isolated memoirs published by Roumanians, but, so far as we could ascertain, no systematic work is extant. The best general works, touching also on geology, are those of Aurelian and Obedenare.]

[Footnote 16: Principles of Geology , vol. i. p. 209.]

[Footnote 17: We believe this is really all that is known of the general stratification, and although little that is positive has been revealed, writers have made up for the deficiency by any amount of negative description. Such writers as Aurelian and Obedenare simply deplore the paucity of information, whilst Fuchs, an able and industrious geologist, says: 'It is difficult to describe the country because there are such vast tracts which have a character of despairing monotony; because fossils are rare and badly preserved, if not entirely wanting; and the different elevations present exactly similar petrographic appearances;' in fact, he says that the prominent data are wanting to enable a geologist to make a classification of the various strata.]

[Footnote 18: See Obedenare, 16-19. Also Cantacuzeno, Cenni sulla Romania , Bucarest, 1875; and Ansted.]

[Footnote 19: Copper exists at Baia d'Arana.]


CHAPTER II.

GEOGRAPHICAL--ARCHÆOLOGICAL.

The river system of Roumania--The 'beautiful blue
Danube'--Appearance of the Lower Danube comparable to the Humber or
Mississippi--Floating mills--The Danube in the Kazan Pass--Grand
scenery--The 'Iron Gates,' misconceptions concerning them--Their
true character--Archæological remains--Trajan's road--His
tablet--His bridge at Turnu-Severin--Its construction and
history--The tributaries of the Danube and towns upon them--The
fishes of the Roumanian rivers--Lakes--Mineral waters of Balta
Alba--Roman roads--Bridge of Constantine--Roman streets, houses,
temples--Statue of Commodus--Gothic and prehistoric
remains--Climate--Great extremes of heat and cold--Beautiful
autumn--Rainfall-Comparison with other countries--Russian
winds--Sudden daily alternations--Comparison of the country
generally with other European states--Résumé of its productions,
resources, and attractions for visitors.


I.

The river system of Roumania constitutes one of the most remarkable features in its geography, has played an important part in its past history, and promises to exercise a powerful influence on its industrial and political future. This system comprises the great main artery, the Danube, with numerous confluents which take their rise in the Carpathians, and, rushing at first in torrents, then How as sluggish, often as half-dry streams, across the country before they empty themselves into the parent river.

The 'beautiful blue Danube' has been so bepraised that to a traveller who visits it for its scenic attractions it is likely to prove a bitter disappointment. It is not blue, although during certain seasons it is said to have a blue tinge, but a great part of the way from Vienna to the defile of Kazan, and the whole distance from Orsova to the Black Sea, it resembles in colour and appearance our river Humber, and we have heard American travellers compare it to the Mississippi. For hours and hours at a time it flows between perfectly flat banks, on which nothing is visible but reeds and willow bushes. The surface of the river is enlivened by innumerable floating water-mills, which lie at anchor either in midstream or close to the banks, and obtain their motive power from the rapidly flowing current. These are used for grinding the maize and other cereals of the country. Here and there a small town or fortification presents itself on either bank. On the Bulgarian side are the towns of Vidin, Nicopolis, Sistova, and Rustchuk, with their domes and minarets, and idle laughing crowds of gazers, either men picturesquely clad, or women sitting perched, on the rocks, and looking like so many sacks of floor all in a row. These certainly break the monotony of the great stream, but the general appearance of the river from Verciorova, where it begins to bathe the Roumanian shore, to its mouth at Sulina is one long flat reach, higher, as we have already said, on the Bulgarian than on the Roumanian side.

[Illustration: TERMINAL PIER OF TRAJAN'S BRIDGE ON ROUMANIAN SHORE. (FROM A SKETCH BY THE AUTHOR.)]

But although that is the stretch of the river which comes strictly within the scope of our survey, there is another portion, lying immediately above it, that well merits a passing notice, more especially as we know that it played an important part in the Roman conquest and the subsequent colonisation of ancient Roumania. There is perhaps no river scenery in Europe to equal, and certainly none which excels, that part of the Danube stretching for about seventy-five miles from Bazias--the terminus of a branch of the railway from Vienna to Verciorova--to the so-called 'Iron Gates.' It is here that the river cuts its way through the Carpathians, and whilst along its general course it varies in width from half a mile to three miles or more, in the Kazan Pass, a defile having on either side perpendicular rocks of 1,000 to 2,000 feet in height, it narrows in some parts to about 116 yards, and possesses a depth of thirty fathoms. The banks closely resemble those of a fine Norwegian fiord, rising more or less precipitously, and being covered with pines and other alpine trees, and occasionally, as in Norway or even in Scotland, the steamer appears to be crossing a long mountain-locked lake. At the lower end of this reach of the Danube are what the metaphor-loving Ottomans first called the 'Iron Gates,' and they no doubt found them an insurmountable barrier to their western progress up the river. Considerable misapprehension, however--which is certainly not removed by the accounts of modern writers, who have apparently copied from one another without visiting them--exists concerning these same 'Iron Gates.' Some of the writers referred to speak of 'rocks which form cascades 140 mètres' (or about 460 feet) high, 'and which present serious obstacles to navigation.' Where these cascades are we were not able to discover. The fact is that the whole descent of the river throughout this portion does not exceed twenty feet, and where it issues from the outliers of the Carpathians the banks slope more gently than higher up, and the summits are simply high hills. The 'Iron Gates' themselves consist of innumerable rocks in the bed of the river. Here and there they appear above the surface, but generally they are a little below it, and they break up the whole surface for a considerable distance into waves and eddies, through which only narrow passages admit of navigation, insomuch that in certain states of the river the passengers and cargoes of the large steamers have to be transferred to smaller boats above, and retransferred to the larger class of steamers below, the 'Iron Gates.'


II.

But by far the most distinctive, and for us the most interesting, features of the Danube about here, are its historical reminiscences. Almost the whole way from Golubatz (Rom. Cuppæ) to Orsova, there are traces on the right (southern) bank of the remarkable road constructed by Trajan (and probably his predecessors) for his expedition into Dacia, and at one place opposite to Gradina is a noted tablet inserted in the rock to commemorate the completion of the road. This tablet has been the subject of much controversy, and it bears the following inscription:--

IMP. CÆSAR. DIVI. NERVÆ. F. NERVA. TRAJANUS. AUG. GERM. PONTIE.
MAXIMUS. TRIB. POT. IIII. PATER. PATRIÆ.[20]

The Servian peasants, however, have little respect for heroes--at least, for ancient ones--and the barbarians of seventeen or eighteen centuries appear to have lighted their fires and cooked their 'mamaliga'[21] against the tablet until it presents the appearance of a blackened mass. Of the road itself we shall speak hereafter at some length in connection with Trajan's expedition, but a few words concerning his bridge at Turnu-Severin may still be added. All that remains visible to the traveller to-day are the two terminal piers, of which sketches are here given; but between those piers the bridge spanned the river, and a very low state of the water discloses the tops of several other piers still standing. In speaking of one bridge we have taken rather a liberty with the facts, for it is now pretty generally admitted that there were really two structures. Further down the river is a small island which, in former times, is said to have extended to where the remains of the bridge are found, and upon this tongue of land the ends of the sections starting from either shore rested. The land is supposed either to have sunk or to have been washed away by the current.[22] The bridge, to which further reference will be made in our historical sketch, was built after the plans of Apollodorus, the architect of Trajan's Column at Rome. It was commenced about 103 A.D., and probably consisted of twenty piers, each 150 Roman feet high and 60 feet broad, and the distance between the two terminal piers on the banks is about 3,900 English feet. The piers were of stone, but the upper part of the bridge was wood. In the northern pier the stone consists of rubble, or artificial conglomerate composed of small roundish stones and cement, and this was probably cast into blocks, but the one on the right (southern) bank is of hewn stone. On the northern side there is an old wall running up from the pier to the ruins of a tower which was evidently connected with the bridge.

[Illustration: TERMINAL PIER ON SERVIAN SIDE. (FROM A SKETCH BY THE AUTHOR.)]

But it would be better that we should reserve any further remarks concerning the archæological relics of Roumania, and also some observations of immediate interest in connection with the Danube, until we have completed a brief account