Volltextsuche ändern

447 Treffer
Suchbegriff: Valley

Über die Volltextsuche können Sie mit einem oder mehreren Begriffen den Gesamtbestand der digitalisierten Zeitungen durchsuchen.

Hier können Sie gezielt in einem oder mehreren Zeitungsunternehmen bzw. Zeitungstiteln suchen, tagesgenau nach Zeitungsausgaben recherchieren oder auf bestimmte Zeiträume eingrenzen. Auch Erscheinungs- und Verbreitungsorte der Zeitungen können in die Suche mit einbezogen werden. Detaillierte Hinweise zur Suche.

Datum

Für Der gerade Weg/Illustrierter Sonntag haben Sie die Möglichkeit, auf Ebene der Zeitungsartikel in Überschriften oder Artikeltexten zu suchen.

Nature14.03.1872
  • Datum
    Donnerstag, 14. März 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] and having this definite trend, are found to extend over the whole plateau area uninfluenced by the more tortuous deeper river-valleys which intersect the same area at various angles to their course. The river-valleys are covered with gravel formed of the dºri's of the rocks [...]
[...] covered with gravel formed of the dºri's of the rocks through which the present rivers flow, while the plateau valleys and plains are free from such dºris, but are covered with a uniform layer of red clay or loam. Whence M. Belgrand concludes that the two systems of valleys [...]
[...] M. Belgrand considers that the only explanation which will account for the phenomena presented by these higher-level valleys and hills, is the rapid and transient passage of a large body of water over the surface; and as the excavation of these higher valleys took place after [...]
[...] course were turned off at acute angles, until they reached the main channel of the Seine, tending thereby to form secondary or tributary valleys, which, when the deluge had passed, contributed, with the Seine valley, to form the pre sent lines of river drainage. Such volumes of water as we [...]
[...] the nature of that cause. Without going far into the argument, we may mention that the well-known fact of the gravel found in each tributary of the valley of the Seine, consisting of the débris of those rocks only through which that tributary flows, while in the Seine valley are [...]
[...] such exist. Not only is the débris of each great Lasin restricted to its own rocks, but even each tributary river valley has its own special rock débris and no other. M. Belgrand remarks, it is true, of the Somme Valley, which lies on the line of his third great diluvial water channel, [...]
[...] lies on the line of his third great diluvial water channel, and which prolonged south-east passes across the Oise valley and up that of the Aisne, that some debris of the older rocks of the latter areas have been found in the chalk valley of the Somme. But we must confess we have never [...]
[...] as just suggested. With regard to the ingenious suggestion of M. Belgrand that some south-east and north-west valleys of the table lands are faced on the opposite side of intersecting river valleys by a bay in the hills due to the violence of the [...]
[...] M. Ed. Lartet. Here again we cannot, however, agree with him in his modus operandi. The great boulders of sand stone, meulière, granite, &c., found in the valley gravel of the Seine, are attributed by M. Belgrand in the first place to removal to the line of the Seine valley by diluvial action, [...]
[...] leaving the rivers clearer and under conditions favourable for the growth of peat, which he shows never takes place in river valleys subject to frequent and heavy floods, but always in valleys where springs abound, and the floods are few and not turbulent. [...]
Nature07.06.1877
  • Datum
    Donnerstag, 07. Juni 1877
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] pointing out the evidence for the former greater extension of the ice-fields of New Zealand, and dwelling especially on the proofs of enormous erosion shown by the valleys and lake-basins. [...]
[...] most deafening roar. No solid matter, however, was borne along with the vapour. Not far from the crater an extensive depression in the valley of Askja has taken place, and the fresh surfaces of rock exposed thereby give a clear picture of the peculiar formation of the valley by [...]
[...] plements have been so largely found ; therefore he believed that in all that area man is of post-glacial age. If we got two levels on either side of a valley, so many feet above sea-level, with the boulder clay cut off on either side, then of course the dººris at the bottom of the valley would consist of gravel, and so on, [...]
[...] at the bottom of the valley would consist of gravel, and so on, derived from materials which had been formed by the destruction of the several strata which originally traversed that valley. The materials so spread out were necessarily newer than the boulder clay; consequently man in the valleys was post-glacial. There [...]
[...] clay; consequently man in the valleys was post-glacial. There were sometimes two or three successive levels of gravels in those valleys. If a valley was excavated to a certain depth, and a deposit was formed in which they could find no traces of the existence of man, whilst at another and deeper level flint imple [...]
[...] mammalian remains and implements are found in the low-level gravel but none in the higher. Thus at the entrance of the Thames valley near to France we find evidence of man in the later high-level gravels, but man had not then penetrated into the Upper Thames valley. It was evident that at the period that [...]
[...] a few facts from personal observation tending to show that some modification of the theory was necessary. With respect to the valley of the Somme, there was evidence afforded by relics of the Roman and bronze age found in the peat in the bottom of the valley, that the river had not materially lowered its bed since [...]
[...] Mr. Tiddeman, man existed in these parts during the subsidence of the glacial epoch, that would account, he thought, for a much greater flow of water having passed down these valleys in palaeo lithic times than was the case at present. In the valley of the Solent the same class of evidence was obtained. Mr. Evans had [...]
[...] Solent the same class of evidence was obtained. Mr. Evans had shown what a large amount of depression and erosion must have taken place in this valley since drift implements were deposited on the hill at Southampton. The valley of the Solent, from Portsdown to the Isle of Wight, is nine miles wide, and we have [...]
[...] enormous lapse of time comprised in the palaeolithic period, which was evidenced by the amount of time requisite for the erosion of river valleys, he thought they would eventually be able to establish some chronology. If they could form any idea of the amount of time requisite for the excavation of a valley such as [...]
Nature04.07.1872
  • Datum
    Donnerstag, 04. Juli 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] end of the Longmynds, where the Wenlock Shales will be examined, and the physiography of the district formed by the Llandeilo Rocks observed. Walk back through the Valley of the Onney, observing on the way sections of Silurian Rocks from the Lower Caradoc to the Wenlock. On Friday, proceed [...]
[...] gravels in the neighbourhood of Acton have been divided by Mr. Prestwich into two principal groups—viz, the high-level gravels on the hills above the valley, and the valley-gravels on the sides and bottom of the valley itself. The valley-gravels have been again divided by Mr. Whitaker into three terraces—viz., a high [...]
[...] which is laid bare at an average level of 5oſt. The London Clay is also laid bare on the sides of the tributary streams running into the valley on both sides of the river, thus dividing the high terrace gravel into patches. The mid terrace is continuous, and follows the sinuosities of the valley on both sides up to the strip [...]
[...] and consequently about 50ft. lower than the implements of the high terrace, I } mile to the north. The section across the valley, taken through the two places, here shows the strip of the London Clay intervening between the two terraces. The chief points of interest which the author submitted to the [...]
[...] base theories upon merely negative evidence. It was to be hoped that other investigators would extend similar discoveries to other parts of the valley of the Thames. Mr. Godwin-Austen did not think that the presence of the young Hippopotamus was absolutely conclusive of its having been born in this country. [...]
[...] existence of man with the Pleistocene ſauna. Under any cir cumstances the gravels containing the implements could only have been deposited at a time when the Thames valley had not been excavated to anything like its present depth ; and they were therefore of great antiquity. . There was, moreover, a [...]
[...] wide; but there was at Croydon, 12 miles distant, a deposit of gravel capped with loess, containing elephant remains, and exactly resembling the Thames valley-gravels, and communicating with them. This evidently formed part of the Thames valley system, whatever that system might be taken to be ; and if so, [...]
[...] high, called the Rossendale Anticlinal, which forms the water shed between the basins of the Mersey and the Ribble; (2), the valley of the Burnley and Blackburn Coal-field, which drains north through gorges in (3) the Pendle chain of hills into (4) the broad valley of the Ribble; (5), a group of Fells rising to a gene [...]
[...] north through gorges in (3) the Pendle chain of hills into (4) the broad valley of the Ribble; (5), a group of Fells rising to a gene ral level of 1,800 feet, between the valleys of the Ribble and the Lune, called, for the purpose of this paper, “The Central Fells;” (6), north of this the valley of the Lune and the estuary of the [...]
[...] robably belongs to the same animal. From the outer part of its crown three folds project into the bottom of the median valley. The tooth measures 1 inch and Io lines wide. The species may be named Ahinoceros pacificus. Another fossil specimen, labelled “Crooked River,” consists of an isolated ver [...]
Nature14.09.1876
  • Datum
    Donnerstag, 14. September 1876
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] peninsula. The paper by Mr. A. Helland, “On “Cirques’ and Sack-valleys,” and on their importance in the theories of the Formation of Valleys,” will certainly be perused with profit by the geologist.” After a description of [...]
[...] of the Formation of Valleys,” will certainly be perused with profit by the geologist.” After a description of cirques and sack-valleys, and of the forms intermediate between the two, Mr. Helland remarks that the openings of the cirques are generally directed towards the north. [...]
[...] dalenes dannelse.” A “botn,” a semi-circular indentation in the mass of the field, is what is called in the Alps a “cirque.” . A “sack kedal," i.e., a valley, the head of which presents a semi-circular enlargement, or , a “cirque,” a valley which ends in a cul-de sac, might be called a “sack valley,” a literal translation of the word “sackkedal." [...]
[...] pointing even due south, but these are only exceptions to the general rule. Besides, when a valley has a west-east direction, or when the slope of a fjeld follows this direc tion, it is on the slope which faces to the north that semi [...]
[...] tion or in the clearing of cirques. The conclusions arrived at by Mr. Lorange, and supported by Mr. Helland are, that cirques, as well as sack-valleys, were necessarily excavated with the aid of glacier-ice. But the ice did not act as a direct excavating agent ; it only [...]
[...] cirques, the rock being disintegrated by the incessant intermittence of the freezing and thawing of water in the fissures. Doing little to excavate the valley, the glacier acts as a powerful means of transport of the disinte grated parts of the rock, where such a means is want [...]
[...] accumulates and protects the underlying rock from further disintegration. The tarns, so numerous at the bottoms of cirques and of sack-valleys, were formed, the author supposes, by the same process, the rocks being disintegrated when the water freezes under the glacier [...]
[...] cosity, with all the consequences of this theory, certainly will not find the question extravagant; they will remem ber that the motion of ice ºf the valleys, and even a motion on slopes from 20° to 63° is an established fact. [...]
[...] In the valleys which have, for example, a west-to-east direction, and which were crossed by the ice moving from north to south, the plastic ice ascended the slopes which [...]
[...] north to south, the plastic ice ascended the slopes which faced towards the north ; and also did it ascend on the fjelds when it moved up a valley, a phenomenon which, we know, is not at all uncommon. A second short paper, by Mr. Helland, gives a table of [...]
Nature16.04.1874
  • Datum
    Donnerstag, 16. April 1874
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] valley from early times to the present day. . For many years I had an ambition to work out the history of the Rhine. I have known it now for more than twenty years; going often up and [...]
[...] worked it out, with the result which is now to be explained. First, with regard to the great main features of the Rhine valley; it has its sources, as every one knows, in the mountain regions of Switzerland, one of which is in the valley of the Vor der Rhine, and the other in that of the Hinter Rhine, both glacier [...]
[...] that of the mountains of the Schwartzwald–-I found that none of the glaciers of that region (and there are proofs that glaciers once existed there) even extended well down into the valley of the Rhine. And on the opposite side of the Rhine Valley, that of the old glacier region of the Vosges, I found no proof that [...]
[...] fossils contained in the rocks, it is possible to form some con ception of the appearance of the country. On the east and west of the great valley were mountainous ranges now called the Schwartzwald and the Vosges, while far to the south rose the high mountains of the pre-Miocene Alps, more [...]
[...] I now come to the chief part of this lecture, which is to account for the origin of the Rhine : for at that earlier time the Rhine had no existence in this valley, and indeed there is proof that instead of the main drainage of the area, flowing from south to north as it does now through this valley, the waters drained [...]
[...] Rhine was established flowing at a height which we may roughly speak of as having been 500 ft. higher than now, because at that time all the great valley between Basle and Bingen was filled to that height with Miocene strata. We know this to be a fact by an examination of the valley on the right hand and the left, from [...]
[...] fact is plain to anyone accustomed to reason on geological pheno mena. The strata forming scarped slopes on opposite sides of the valley were once united, and their early continuity has been destroyed, simply by long-continued watery waste and denuda tion. They are indeed only the relics of an older phase of the [...]
[...] terraced hills on either bank still remain to attest the amount of watery degradation that the area has undergone. So much for the scooping out of the valley. But there is another point which I would like to impress upon you. On each side of the Rhine there are important tributary [...]
[...] rivers. Thus, for example, above the gorge we have the Maine, the Neckar, the Kinzig, the Elz, and other streams, flowing through deep steep-sided valleys; and these rivers have from a very early period been tributaries of the Rhine. It follows, then, that when the level of the Rhine was [...]
[...] 4oo or 500 ft. higher than at present the levels of the bottoms of these rivers must also have been 400 or 500 ft. higher than at present; and therefore, just in proportion as the great valley of the plain of the Rhine was being cut down and lowered, so in proportion must the valleys in which these rivers run have [...]
Nature27.02.1873
  • Datum
    Donnerstag, 27. Februar 1873
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] (hough 600 miles from the sea, is one and a half # breadth during the heavy rains, and about a ng the dry season. Its great valley is, however, broken up by low isolated ranges which confine ters to comparatively narrow but deep channels. [...]
[...] been a comparatively recent outflow of trappean rocks, while the country to the west is exclusively granitic and metamorphic. There, as well as in the Sanda Valley, are hot springs which issue at almost the boiling-point, and at the head of the Nantin valley is the large extinct [...]
[...] able us to assign a place in chronology to the Troglodytes of the valley of the Vézère. There is not one polished hatchet [...]
[...] hardly above that of the river. Now, at the present day, it is situated twenty-seven metres above the lowest water mark; the depth of the valley is therefore considerably increased since the epoch of the Moustier Troglodytes. On the other side, the [...]
[...] the most recent, per haps the most recent of the valley, is very slightly above the level of the largest present [...]
[...] floodings. We may hence conclude that the valley of the Vézère was very much then what it is now, and that since [...]
[...] the river, to Eyzies, which is down, the distance is but eight kilometres as the crow flies; it is nearly double when you follow the windings of the valley. Between these extreme stations we see succeeding each other, on [...]
[...] will be more abundant than those of all the others put together. - The finest works in flint of the Valley of the Vézère are those of Upper Laugerie. All the implements, all the weapons of that station are in flint. They are innume [...]
[...] These carefully-wrought points, so common at Upper Laugºrje, are not to be found in the later stations of the valley of the Vézère. starce, that the workmanship of flints, after having pro gressed till the time of Upper Laugerie, had then declined. [...]
[...] of bones, such as those of Kirkdale, Liege, and Gibraltar, the last having been lately explored by Mr. Busk. Those of the Wellington Valley in Australia have afforded nu merous remains of marsupials, showing that those animals have been located there for a considerable period. Again [...]
Nature09.04.1874
  • Datum
    Donnerstag, 09. April 1874
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] tinual additions to the long list—chiefly through the exertions of collectors in various parts of the Andean Chain, where almost every valley appears to contain distinct species of birds. At a recent meeting of the Zoological Society, twenty-four new species of birds [...]
[...] ON June 22, 1863, the late Captain Speke published his map, giving (on native authority) four outlets from Lake Victoria Nyanza, converging to one valley or water-flow—the Nile. [...]
[...] modify my dictum by saying, that if by a rare possibility a lake may be found to exist on a water-parting having at opposite ends two outlets to two different valleys, I should still doubt the possi bility of a lake at its one lower end having a multiplicity of out lets converging to one valley or water-flow, as in the case of the [...]
[...] Same rate. The outlet of every lake in the wide, wide world is always being lowered from erosion, as are valleys themselves. Valleys exist only in the dissolution of hills. They are mere water-flows. They are the perpetually changing effects of atmospheric disin [...]
[...] They are the perpetually changing effects of atmospheric disin tegration, and the erosion of rain and rivers, and consequently every water-parting is a valley-parting. [...]
[...] being experienced during almost the entire voyage. In the first 1oo miles west from San Diego, there ap pear to be two valleys and two peaks. The first valley is from 622 to 784 fathoms depth; the first peak 445 fathoms, the second valley 955 fathoms, the second peak 566 [...]
[...] more than twelve miles by six, comparatively flat in the centre, but surrounded by higher land. This range of high land is divided by a series of deep valleys, forming ridges which are again divided into transverse valleys. Most of the hills are from 7oo to 1,200 ft. high, but one in [...]
[...] gravelly, and though seen only in this one spot in St. Vincent, it grows abundantly in St. Jago by the stream in St. Domingo Valley. As seen from the sea, the rocks of St. Vincent present a singular appearance, owing to the presence of a thick [...]
[...] nomena (especially periodic) of vegetation; embryonal develop ment of Tunicata; composition and mutual relations of albumi noid substances; coal system of the Liège valley. [...]
[...] human fossils from the same valley of Vézère, from Bruniquel (caves of Lafaye and Forges), from the south towards the Pyrenees (the cave of Aurignac), and from the cave of Gourdon [...]
Nature11.07.1872
  • Datum
    Donnerstag, 11. Juli 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] of expression have been mastered (and it must always be remembered that line engraving is necessarily conven tional), the peaks detach themselves from the valleys and soar aloft, and the mountaineer sees the Alps before him with all their marvellous diversity of architecture ; nay, [...]
[...] His map was published at the expense of the Alpine Club, and it is, I believe, the only one which at all fairly repre sents the southern side of Monte RCsa, the valleys of Val pelline, Barthelemy, and Tournanche, and the ranges which divide those valleys. Mr. R. C. Nichols has de [...]
[...] and it does not extend quite so far to the north as the Swiss map, but in the south it embraces the important groups of the Graian Alps to the south of the Valley of Aosta, which include the Valleys of Locana, Cogne, Savaranche, Rhêmes, Grisanche, and the Tsere, with their [...]
[...] But since the discoveries in the Somme Valley were recognised, a flood of light has been shed upon the sub ject. These dry bones live, and these rude stones are [...]
[...] other able writers of their time, that the general dispersion of gravel, sand, and loam, over hills and elevated plains, as well as valleys, was the result of a universal deluge, which is described as transient, simultaneous, and of a date not very remote ; that the existing system of valleys [...]
[...] date not very remote ; that the existing system of valleys was mainly due to the same cause, and that thus both valleys and gravels preceded our present river systems, Cuvier, and the French geologists generally, have held the same opinion, but of late years it seems to have been [...]
[...] the implements which, so far as they are concerned, are at variance with the theory of fluviatile transport. For instance, when met with in valleys, it appears that the im plements are not found along the whole course of those valleys, as well where flint gravels are wanting, as where [...]
[...] before they were worked. If, indeed, it had happened that these things had never been found elsewhere than in river valleys, the conclusions arrived at by Mr. Evans would have been irresistible, but so far from this being the case, it is certain that these im [...]
[...] der such circumstances it may be fairly assumed that the same forces, whatever they were, that covered the hill-tops, may have partially filled up the valleys; the presence of gravel may suggest, but cannot prove, that the river brought it, however much it may have re-arranged and [...]
[...] gravel may suggest, but cannot prove, that the river brought it, however much it may have re-arranged and sorted it; both valley and gravel may have had an exist tence before the river began its course. We have many valleys and gravels without rivers, and rivers without [...]
Nature31.10.1872
  • Datum
    Donnerstag, 31. Oktober 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] My route traversed an extensive but rarely visited tract of country, that, namely, of the great Chorok, or Harpagus river-valley from Beyboort to Artween, and the mountain lands that extend beyond that valley east and north up to the frontier of Russian Georgia, returning by the Black [...]
[...] Near Artween, long. 42,” the valley turns sharp to the north, and finds its way through a narrow and precipitous cleft to the sea. [...]
[...] other fluvial systems. Farther on the Russo-Georgian frontier follows its eastern slope. Returning to the Chorok valley—one might almost call it trench—I may as well notice that its height above sea level at Beyboort is about 5,000 feet, and at Artween only [...]
[...] partly on foot; so that I had full opportunity for the most leisurely observation. My route first followed the southern side of the Chorok valley for about seventy miles, then the northern for about fifty more, after which I traversed the eastern highlands to the Russian frontier, [...]
[...] it were, smoothed off; the sides marked with scooped depressions much too wide for their depth to be attri butable to torrent action; low down in the valley the slopes terminate in rifted precipices. That the epoch to which these moraines belong was [...]
[...] boulders, many ten or more feet in diameter. Another volcanic tract succeeds, where the path winds along a valley hemmed in by gigantic cliffs of black lava, dashed with blood-red porphyritic stains. From this point my track followed a level too low to permit of expecting or of [...]
[...] Thames during high tide at Richmond bridge, my path led to Artween, the chief village-centre of these regions, along the north-western side of the valley; that is, along the inner slope of the coast range. These Lazistan moun tains form a very lofty, but comparatively narrow ridge, [...]
[...] latter with glaciers, while it would furrow the former with torrents of the first magnitude. Leaving the Chorook valley, my road—or track, to speak more properly, for road in our sense of the word there was none—led north-east up to the great water-shed [...]
[...] an intervening ledge, 7,300 feet above the sea, composed of granite rocks, worn and marked with unequivocal ice action, though now wholly bare of snow. A valley divided this ridge from the highest of all, that called Penek, up which a difficult track, called the “Egri Yokoosh" or [...]
[...] companied by a wild rushing noise, and the crashing of the trees and branches could be heard becoming louder and louder as it advanced. It crossed the valley over the railway viaduct, close to Randalstown, fortunately avoid ing the village. It here presented the appearance of a [...]
Nature20.11.1873
  • Datum
    Donnerstag, 20. November 1873
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] rocks first appeared above the sea, they contended that the present contours of the land had arisen mainly from a process of sculpture,—the valleys having been carved out by rains, streams, and other superficial agents, while the hills were left standing up as ridges between. So [...]
[...] continents are gathered together, than of learning how the outlines of existing continents have been produced. The study of the origin of mountain and valley went out of fashion, and from the time of Playfair's Illustrations, published at the beginning of this century, received in [...]
[...] millions upon millions of cubic yards of rock have been worn off their crests and ridges, and carved out of their sides. There is not a cliff, crag, or valley along the whole chain of the Alps which does not bear witness to this great truth. [...]
[...] general surface of the country has had hundreds or even thousands of feet of solid rock worn away from it. Such a section shows moreover that our present valleys are not mere folds due to underground movements, but are really trenches out of which the solid rock has been carried [...]
[...] of opinion. The language of Hutton may be literally true of Britain —“The mountains have been formed by the hollowing out of the valleys, and the valleys have been hollowed out by the attrition of hard materials coming from the mountains.” Our British hills, unlike the chains [...]
[...] of the Jura and the Alps, are simply irregular ridges de pending for their shape and trend upon the directions taken by the separating valleys. The varying textures of the rocks, their arrangements with relation to each other, their foldings and fractures, and the other phenomena [...]
[...] potency great enough to cut down table-lands into moun tain ridges and glens, to carve out the surface of the land into systems of valleys, and in the end to waste a con tinent down to the level of the sea. (70 he consinued.) [...]
[...] Peru,” Part I. The object of the paper was to describe the “huacas” or burial-grounds, especially those lying beweent Arica and the Huatica Valley, and to expose some popular errors respecting them. ... Every bit of old wall, every heap of gravel, mound of earth, large or small cluster of ancient ruins of [...]
[...] burying-grounds of Ancon, Pasamayo, and other places where there is no elevation above the country, as to those of Pando and Ocharán, large burial mounds in the valley of Huatica. The author proceeded to describe in detail the mode of interment and the various articles discovered. The celebrated Pacha-Cámác [...]
[...] the various articles discovered. The celebrated Pacha-Cámác was described. Along the whole course of the Huatica Valley—from Callao to Chorillos—a distance of ten miles direct or sixteen miles round by Lima, there is no natural elevation that could be made available as a sub-structure for those colossal [...]
Suche einschränken
Zeitungsunternehmen
Zeitungstitel
Erscheinungsort
Verbreitungsort
Jahrhundert
Sprache