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Nature16.03.1876
  • Datum
    Donnerstag, 16. März 1876
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] space so conclusively proved by Agassiz and others. The longest of the five papers in this collection is the most recent : “On the Physical History of the Valley of the Amazons,” in which he gives his reasons for considering the whole of that valley to have been filled with ice, and [...]
[...] out between the form of the stones in these deposits, and those in common boulder-clay. It should be noted also that in many cases these breccias occur in old valleys, and bear many of the characters of valley-moraines. Such are those to the east of Ullswater, and those which [...]
[...] forward, involving, as he believes it would, if carried out, the conversion of the “fertile meadows’ of the Thames Valley into “arid wastes,” and the utter destruction of “watercress beds, now of fabulous value; ” he adds that “even the canals and navigable rivers will become liable [...]
[...] dire results, he doubts whether his “judgment is seriously distorted,” although he admits being deeply interested in the water power of one of the threatened valleys, and protests that no one can submit silently to an insidious (?) attack upon his property. [...]
[...] attack upon his property. Having carefully studied for many years the hydrogra phical features of the Thames and other valleys, I have no hesitation in saying that Mr. Evans's fears are, for the most part, entirely unsupported by experience. Sterility [...]
[...] grown city,” as Mr Evans contemptuously terms it, drink the pure spring water which nature offers them in singular abundance in the Thames valley, or shall they not be permitted to taste this sparkling beverage until the paper manufacturers, in the exercise of what they call their [...]
[...] the valley of the Indus. As soon as we reached vege tation, at a distance of only two marches from the above [...]
[...] affects its colour and distinctness, and through it you get a standard for judging distances. Without vegetation, even at a lower height, as, for instance, in the valley of the Bagha (Lahoul), you seem to look through a vacuum. In the upper part of the valley of the Indus, of which I am [...]
[...] striking result. That the absence of any rain or deposit of any kind must not be left out of account is clear. The air in the side valleys of Cashmere, although rich in vege tation, is particularly transparent. Strange enough the principal valley of Cashmere, i.e. the valley of the Jehlum, [...]
[...] was seen, with the sun as centre. It stood on the white edge of a dark cloud. 2. Aug. 1.-At Dwara, in the Kulu Valley, almost the exact reproduction of the above phenomenon was seen on a cloud hanging on the side of a mountain. It was [...]
Nature27.01.1870
  • Datum
    Donnerstag, 27. Januar 1870
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] The levels of the river also appear to present a great obstacle to its joining the Nile lakes. Leaving the Valley of the Loangwa, Dr. Livingstone tells us that he ascended to a great plateau which extends for 350 miles square, southward of Tanganyika. This table-land is at an ele [...]
[...] that he ascended to a great plateau which extends for 350 miles square, southward of Tanganyika. This table-land is at an ele vation of from 3,000 to 6,oco feet above the sea. The valley of the Chambeze crosses this plateau from east to west, and the river descends from it into the great valley of the Lakes Bang [...]
[...] sandstone. 2. “On the superficial deposits of portions of the Avon and Severn Valleys and adjoining districts.” By Mr. T. G. B. Lloyd, C. E., F.G.S. The author, after describing the general characters of what he termed the Drifts of the Upper and Lower [...]
[...] characters of what he termed the Drifts of the Upper and Lower series, and the freshwater gravels of the Lower Avon, comprised within the district of the Avon Valley between Tewkesbury and Rugby, and of the Severn. Valley above and below the town of Worcester, endeavoured to show that there was a balance of [...]
[...] Strickland. Further, that there was no evidence to warrant the supposition of the existence of high and low level river-gravels in those portions of the Severn and Avon Valleys under review, and that the apparent absence of any freshwater shells in the gravels of the Severn Valley between Bridgnorth and Tewkes [...]
[...] bury led to the inſerence that the freshwater gravels of the Avon were not represented in the adjoining portions of the Severn Valley, although remains of some of the same species of mam malia occurred in both localities. Aſter stating his opinion that the time had not yet arrived for indulging in theoretical specula [...]
[...] noticing the general configuration of the surface of the district under review, which he stated to consist of an elevated plateau, bounded and rendered irregular in its outlines by valleys. The district consists chiefly of Lower Lias, with a few patches of Middle Lias. The surface-deposits on the plateau and on similar [...]
[...] quartzose drift ; 2. Sugary sand, with grains of chalk ; 3. Clay, with pebbles, principally of chalk, and distinctly striated. The valleys bounding the plateau were described as belonging to two systems, those of the Avon and Leam. The bottom of each valley is generally a narrow strip of alluvial soil, bordered by [...]
[...] same age. Mr. Gwyn Jeffreys was doubtſul as to the authen ticity of some of the shells which had been brought to Mr. Maw. The fossil shells from the Severn Valley, Wolverhamp ton, Manchester, and Moel Tryſaen were nearly identical, and indicated raised beaches. He thought it possible that a [...]
[...] through that part of England. Mr. W. Boyd Dawkins did not consider that there was any marked difference in the mammalian fauna of the Avon and Severn Valleys. He had failed to discover any traces of Ælephas antiquus in either. Mr. Prestwich thought that the author had probably divided [...]
Nature29.09.1870
  • Datum
    Donnerstag, 29. September 1870
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] It would appear that man followed up the retreating ice of the north of Europe, for the remains of his works are ſound high up in many British valleys, which must then have begun to le formed by the natural drainage out of the deposits of the Glacial Period. [...]
[...] with Crete and Northern Africa north of the Sahara. 2. The formation of a volcanic tuſa on the hills bordering the present valleys of the Tiber and its tributaries; the excavation of those valleys by the river and its streams; the last eruption of the volcanoes of Latium, and their permanent extinction. [...]
[...] The space included in the Roman territory has received its con tour, and vast tracts near the coast have been worn away. 3. The formation of valleys in the Alpine detritus, which covered up large tracts of Northern Italy, and the re-excavation of old valleys, which had been mºre or less filled with the de [...]
[...] tion of valleys in this gravel or silt, and the production of such heights as those which bound such plateaux as Rivoli. 4. Considerable local alterations in the relative level of land [...]
[...] and sea along the west Neapolitan coast. 5. The formation of the straits of Gibraltar. 6. The excavation of such valleys as that of the Manganores in Central Spain, the formation of gravels containing flint imple ments and mammalian bones near Madrid, and therefore far [...]
[...] as those in the neighbourhood of Tarascon; the dispersion of the results of the wear and tear of the second extension of the Pyrenean glaciers, and the filling up of the old valleys with it; the re-excavation of the valleys, and the carrying down of their silt or loess to the plains; the formation of streams and water [...]
[...] silt or loess to the plains; the formation of streams and water courses through this deposit. - 8. The formation of certain valleys in the Perigord by streams to a certain extent, but principally by the gradual effects of rain, heat, frost, and other meteorological actions. [...]
[...] to a certain extent, but principally by the gradual effects of rain, heat, frost, and other meteorological actions. 9. The excavation of the valleys of North and Eastern France, and the denudation and retrogression of their watersheds. Io. The dispersion of Alpine rocks, gravels, and rocks to the [...]
[...] Aſter the retirement of the glaciers, subsequent to this second extension, the wash-down of the Alps, Vosges, and Ardennes was spread over the older gravel. It filled up the valleys, and extended with a thickness varying from a few yards to a thousand feet and more, all down and over what is now the valley of the [...]
[...] 11. The separation of the coasts of France and England about Dover and Calais. 12. The excavation of nearly all the valleys in the district east of a line drawn from King's Lynn to Portland, the denudation of their watersheds, and retrogression of the river sources. [...]
All the year round08.05.1869
  • Datum
    Samstag, 08. Mai 1869
  • Erschienen
    London
  • Verbreitungsort(e)
    London; New York, NY
Anzahl der Treffer: 10
[...] throughout New Mexico, Arizona, and Northern Mexico. There is scarcely a valley in the Rio Grande basin in which the stone or adobe foundations of villages are not to be found; there is scarcely a [...]
[...] of the west, amongst which our parties found abundance of pottery; and there are most extensive ruins in the main valley, both above the falls and between the falls, and the entrance of the cañon of the Chi [...]
[...] this river on the north, draining a country very little known, but of great interest, and containing many fertile valleys. The chief of these tributaries are the Rios Preito, Bonito, San Carlos, Salinas, and [...]
[...] of stone houses and regular fortifications. They were built on the most fertile tracts of the valley, where were signs of acequias and of cultivation. The walls were of solid masonry, of rectangular form, some twenty [...]
[...] drained by a tributary of the Salinas. Of many of the ruins on the Gila itself, and in the valleys of its southern tribu taries, I can speak from personal know ledge. A little west of the northern ex [...]
[...] leaves the Santa Rita, and other ranges, and meanders for a distance of from seventy to a hundred miles through an open valley of considerable width. This long strip of fertile land is studded throughout with [...]
[...] of a steep hill which guarded the entrance to the Aravaypa cañon. All along the San Pedro valley, through which Mr. Runk's party travelled for one hundred and sixty miles, ruined pueblos were frequently met [...]
[...] the ruins found on the Gila; but after the destruction of their kingdom they travelled southward, and settled in the valley, where they now dwell; fearing lest they should again become an object of envy to a future [...]
[...] tural purposes. There is none equal to it from the lowlands of Texas, near San Antonio, to the fertile valleys of California, near Los Angelos, and, with the exception of the Rio Grande, there is not one valley [...]
[...] north to the valley of Mexico. I met with no Indian ruins in Sonora, nor have I heard of any other similar ones [...]
Nature21.06.1877
  • Datum
    Donnerstag, 21. Juni 1877
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] mountains belonging to the Tian Shan system. Two main ridges, which both run north-east to south-west, and are divided by the broad valley of the Surhan,' form the backbones of this hilly tract. Secondary ridges, either parallel to the main ones, or spreading out of them, fill [...]
[...] of the Vaksh, seems to be higher, but yet far below the highlands of Kokand or of Eastern Turkestan. Besides, tne highlands are deeply cut into by large and broad valleys which have in their lower parts a prevailing direction south by west, running thus to the Oxus. The north [...]
[...] the valley of the Surhan river which, as well as the Guzar and the Shir-abad, rises in the snow-covered ridge Meshai Kentely, and receives many affluents. Some time before [...]
[...] roofs of the dwellings from Denau to the Amu. Now, the population is concentrated in the upper, better watered parts of the valley, where we find the towns Kara-tag, Sary djui, Yourchi, and Denau. Further east we have the valley of the Kafirnagan (the Ramid of Ibis-Dast), the [...]
[...] source of which is about Paldorak, this river being second in size to the Surhan. An enlargement in the upper parts of its valley, running east and west, is well peopled, and contains the towns Hissar, Fyzabad, Kafirnagan, and Doshambe. Then, below Hissar, the river enters a deep [...]
[...] affluents of the Pandj, the KChi-Surhab (little Surhab), was explored by M. Maïeff; it is formed by two rivers, the Baldshoan and Kolab, the valley of the latter being well peopled and cultivated, notwithstanding the exten sive marshes which have given their name to the town, [...]
[...] The population of the country consists of Usbecks and Tadjicks, the former occupying, mostly the lower and better parts of the valleys, having driven the Tadjicks back to the upper parts. The banks of the Amu-daria, and especially the western parts of the country, are mostly [...]
[...] more numerous to the east. The towns contain, as usual, a very mixed population. The lower parts of the Vaksh and the Kolab valley are mostly peopled by Usbecks of the Katagan tribe. Some Kirgises have begun to found settlements in the lower parts of the Vaksh and Pandsh [...]
[...] the Katagan tribe. Some Kirgises have begun to found settlements in the lower parts of the Vaksh and Pandsh valleys; and some miserable, Turkomans are strewn among the Usbecks on the shores of the Amu. Jews, Hindoos, and Afghans form a very small percentage of [...]
[...] As to the climate of the country, it is easy to perceive that it must be comparatively mild. In the higher parts of the Kafirnagan valley there are occasionally falls of snow about two feet deep, but the lower parts of the valleys have a mild, rainy winter. Figs grow at Shir [...]
Nature01.05.1873
  • Datum
    Donnerstag, 01. Mai 1873
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] to be applicable also to the Eastern Alps. He then proceeded to examine a number of lakes in detail. The Königsee lies in a remarkably deep, steep-sided valley, terminated by a cirque, with cliffs full a thousand feet high, and has no large supply area behind. The Hallstadtersee is similarly situated, has a cirque at [...]
[...] with cliffs full a thousand feet high, and has no large supply area behind. The Hallstadtersee is similarly situated, has a cirque at the head, and two lateral valleys nearly at right angles to the lake, up which arms of it have formerly extended. These are not likely to have furnished glaciers which could have excavated [...]
[...] not likely to have furnished glaciers which could have excavated the lake ; and above the cirque there is no large supply area. The Gasauthal consists of lake-basins separated by valleys of river-erosion. The Fuschelsee and Wolfgangersee, on the south side of the Schafberg, are separated by a narrow sharp ridge of [...]
[...] primarily by glaciers. He considered a far more probable ex planation to be, that the greater lake-basins were parts of ordi nary valleys, excavated by rain and rivers, the beds of which had undergone disturbances after the valley had assumed approxi mately its present contour. He showed that the lakes were in [...]
[...] obtain, no lake offered any against it, and one, the Königs-e, was very ſavourable to it.—“On the Effects of Glacier-erosion in Alpine Valleys,” by Signor B. Gastaldi. The author de scribed the occurrence in the valley of the Lanzo and other Alpine valleys, at heights between 2,000 and 3,000 metres [...]
[...] Alpine valleys, at heights between 2,000 and 3,000 metres (6,700 and io,000 feet), of large cirques, in two of which, in the valley Sauze de Césanne, the bottom was occupied in the autumn [...]
[...] hard rocks, such as felspathic, amphibolite, and chlorite-schists, he considered to be proved. The author then referred to the mouths of the Alpine valleys opening upon the plain, which he described as being generally very narrow in proportion to their length, width, and orographical importance; and he pointed [...]
[...] described as being generally very narrow in proportion to their length, width, and orographical importance; and he pointed out that in the case of the valley of the Stura, at any rate, the outlet of the valley has been cut out by the river. This pecu liarity he accounts for by the fact that whilst the calcareous and [...]
[...] of these rocks in the region under consideration, by reason of which portions of them occupied the points which are now the mouths of the valleys. [...]
[...] Roy AL INSTITUTIox, at 2. —Annual Meeting. AºA 1/9A P. MAY 2. Geologists' Association, at 8.-On the Valley of the Vézère º, its Limestones, Caves, and Pre-historic Remains: T. Rupert Jones. Roy Al INSTITUrios, at 9.-Alcohols from Flints: Prof. Reynolds. [...]
Nature27.06.1872
  • Datum
    Donnerstag, 27. Juni 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] described by Gervais. A second fossil, part of a mandible, belonging to the same species, has been found by M. Cocchi in the Upper Arno valley. A third, also a mandible and also discovered in Tuscany, at Monte Bamboli, has [...]
[...] 18 sºils, Macacies friscus, Montpellier. 1871 Gervais, Cercopithecus, Monte Bamboli. 1872 F. Major, Macacus inuus(?) Valley of the Arno. From the restricted geographical distribution of the Iemurida, it is not surprising that no remains of this [...]
[...] of Asia Minor, beginning from Amastri, one hundred and fifty miles east of the Bosphorus, up to the Georgian valley and the Russo-Caucasian frontier, abounds in mineral springs, varying as to temperature and con stituents, but generally endowed with hygienic properties, [...]
[...] About six miles east of Trebizondon the sea-coast stands the little fishing village of Covata, at the entrance of the valley which, as also the stream that flows down it, bears the same name. Following the valley some way inland towards the mountains where it originates, we come on the [...]
[...] driving out the cork, and even bursting the bottle. Near this semi-artificial basin, and placed on a line with it one after another in the axis of the valley, are two other natural rock-hollows, one of several feet in extent, the other less; whence the same description of ferru [...]
[...] wide distribution, extending from the mountain valleys and neighbouring plains to the edge of the glaciers; very few being found only in the mountain valleys, [...]
[...] cultivated districts. None of the insects found belong to extra-Alpine species, none of the kinds peculiar to the warm valleys of the southern Alps are represented; and the inference is unavoidable, that all the animals found on the glaciers have either strayed voluntarily, or have been [...]
[...] plant on the moraine, which does not belong to a species inhabiting the immediately adjacent mountain slopes or valleys. The conclusion from these facts seems inevitable, that the conveyance of seeds, even when provided with apparatus calculated for being floated in the air by hori [...]
[...] “We may conceive, therefore, if at some former time the whole mass of Santorin stood at a higher level by 1,200 feet, that this single ravine or narrow valley, now forming the northern entrance, was the passage by which the sea entered a circular bay. But at a still earlier [...]
[...] outer islands are the remains—was still more elevated above the level of the sea, there may have been a deep valley of subaerial erosion cut by the principal river which then drained Santorin, which may have consisted of one lofty volcanic cone, afterwards truncated by a paroxysmal [...]
Saturday review28.08.1858
  • Datum
    Samstag, 28. August 1858
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] authentic information of another “Own Correspondent” of the Times who has turned up so opportunely in the Utah valley. Perhaps the most remarkable fact ascertained is that the settled Mormon population does not exceed 35,000 persons; [...]
[...] which entry in the next column answers to the station. Thus, train No. 19 leaves London at 11:45; it gets on pretty well till it reaches Rugby; but then comes the Trent Valley line, as to which its doings are not represented by mere dots, but by a zigzag [...]
[...] Bletchley at 7:25. The next entry is Dudley—12'o-with a cross reference to page Ioo. From Rugby we go down the Trent Valley, which takes us to Stafford, then we go back to Rugby, and get on to Birmingham and Wolverhampton, though brackets on opposite sides of the names—one with “Stour Valley” on it, [...]
[...] able height, and then rolled down like a river along the flanks of the mountain towards the valley of the Rhone. On entering the valley it crossed a precipitous rock barrier, down, which it poured like a cataract; but long before it reached the bottom it [...]
[...] of this may be mentioned by way of example. The most important feature for the restoration of the ancient Jerusalem is undoubtedly the Valley of the Cheese-makers, described by Josephus as traversing the city, and separating the Upper from the Lower Market. This valley has been drawn by [...]
[...] bankment, from the Jaffa Gate on the west to the Temple Close on the east, and then at right angles to its former course, southward, to the Pool of Siloam and the Valley Ben Hinnom. Now the very existence of the upper portion of this valley—all traces of which, if they ever existed, have certainly been long [...]
[...] whole of its west side, and runs up in a north-westerly direction to, the Damascus Gate. Now the advocates of the invisible valley, while accounting for its disappearance by the ac [...]
[...] Jerusalem—of course hesitate to admit the claims of its rival to that importance which the counter-theory demands for it, as cº, the valley of the interior of Jerusalem. And although it is true that the street which traverses its whole length is called by the natives el Wäd, [...]
[...] effaced—being concealed by the long-continued accumulation of rubbish;" and he is forced to imagine that the still well marked valley, from the north, tº: by the sewer, is passed over without notice by Josephus in his minute description of the physical distribution of the terrain of the city. Numerous [...]
[...] lead or brass with which it was formerly encased;” while he looks for Solomon's Pool—here actually before his eyes—under the débris in the Valley of Jehoshaphat, where, of course, he fancies that he finds traces of it (pp. 151, 303). [...]
Nature17.11.1870
  • Datum
    Donnerstag, 17. November 1870
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] by authority of the Legislature of California. 1869. M R. J. D. WHITNEY, State Geologist of California, has prepared a guide-book to the Yosemite Valley and the adjacent country, which is a model of its kind. It is well written, and is eminently lucid in its descriptions; it is [...]
[...] The British public has been already tolerably familiar ised with the most striking characteristics of the Yosemite” Valley, Mariposa County, California, by the fine picture of Mr. Bierstadt; and some excellent photographs (by Wat kins, of San Francisco), which are now lying before us, [...]
[...] cross section of it is like the letter U, and in this respect, as well as in its length, breadth, and the steepness of its cliffs, it is comparable to the Valley of Lauterbrunnen in Switzerland, but the dimensions of its cliffs exceed those of that valley, as much as its chief waterfall (the great [...]
[...] mainder of the total height is consumed by a series of cascades between the two ; but seen from the opposite side of the valley, the effect is increased rather than diminished by the subdivision, and it well deserves all the praise which has been lavished upon it. [...]
[...] Mr. Whitney does not believe that the peculiar trough form of the valley has been even modified by glacier action. There are no proofs, he says, “that glaciers have ever occupied the valley, or any part of it,” and he scouts [...]
[...] or fissures crossing each other somewhat nearly at right angles. In other and more simple language, the bottom of the valley sank down to an unknown depth, owing to its support being withdrawn from underneath, during some of those convulsive movements which must have [...]
[...] chain, no matter how slow we may imagine the process to have been.” It should be mentioned that the Yosemite Valley is exclusively granite, no remains of sedimentary rocks having been found within it. Although the Yosemite Valley itself is not ice-ground, [...]
[...] terms the Coast Ranges, and the Sierra Nevada. They are roughly parallel to each other, and to the coast line; and they are divided by the valleys of the Sacramento and San Joa quin rivers. The coast ranges are, geologically speaking, younger than the Sierra Nevada, and they are chiefly [...]
[...] thusiasm of Mr. Whitney for the mountains of Cali fornia, and we heartily hope with him, that neither the Yosemite valley nor the grove of Sequoias which—by a unique act of Congress—were ceded to the State for public use, resort, and recreation, for all time, will be suffered [...]
[...] which lead to variation are not difficult to perceive. We to not know all the laws and causes that have given their peºuliar form to each mountain or each valley, but we know a good deal of the general causes which have pro duced them, and we can perceive that the reason no two [...]
Nature22.06.1876
  • Datum
    Donnerstag, 22. Juni 1876
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] gated by Prince Max. of Neuweid, Burmeister, Rein hardt, and other well-known naturalists, is very distinct from that of the great Amazonian valley, and the adjacent flats of Guiana and the Orinoco. Many genera are pecu liar to each of them, and a whole host of representative [...]
[...] puzzling, and in some respects contradictory. Arrived at Monts Dore des Bains we searched carefully for glacier evidences in the valley of the Dordogne and the gorges de l'Enfer and de la Cour, and though some of the knolls are rounded, and there is a vast amount of débris from the [...]
[...] Again, and I must here state that I arrived at conclu sions contrary to those of my friends, I believe that a glacier has descended, in long ago ages, down the valley of the Dordogne, but so long since that the vast masses [...]
[...] of débris which have fallen from the rocks which skirt the valley, combined with the wear and tear of atmospheric agencies, the constant shifting of the bed of the Dordogne and its hundreds of tributary rills which during the [...]
[...] tºº, as on the platform below the Rochers de Beauzac, &C. The Tranteine valley, where Dr. Hooker discovered the transported rock-masses and which he has already described in NATURE, lies at right angles to the [...]
[...] the transported rock-masses and which he has already described in NATURE, lies at right angles to the Dordogne valley, runs due south, and faces the Cantal. It is difficult to understand why glacier relics should be preserved in this valley and none in that of the Dordogne. [...]
[...] the great rock-masses are stranded, consisting of moraine matter overlying beds of basaltic lava. The Tranteine valley may be reached by passing over the Col between the Pic de Sancy and Puy Ferrand, and turning down the gorge to the south, or by the long roundabout route [...]
[...] is a fine section on the Tranteine stream, en route to Picherande, where large transported rock-masses may be seen resting on glacial till. Following the valley down to the bridge which crosses the Tranteine river between Latour and Picherande, the observer will find rounded [...]
[...] of atmospheric weathering has gone on since the days when the ice passed away. Travelling down the valley of Besse to Lake Pavin, I thought I recognised glacier action; and again at the head of the valley of Chambon ; but if glaciers ever flowed [...]
[...] thought I recognised glacier action; and again at the head of the valley of Chambon ; but if glaciers ever flowed down these valleys, it is evident that they must have done so before the eruption of the Puy de Tartaret or the Puy d'Eraignes. The occurrence of the volcanic cone of Tar [...]