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The tatler16.08.1709
  • Datum
    Freitag, 16. August 1709
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 2
[...] D'Albigni. Small parties arc left in several posts from thence to Little Si. Bernard, to preserve the communication with Piedmont by the valley of Aosta. Some forces are also posted at Taloir, and in the castle of Doitt, on each side of the lake of [...]
[...] in the castle of Doitt, on each side of the lake of Anneci. General Rhebinder is encamped in the! valley of Oulx with ten thousand foot, and some detachments of horse: his troops are extended from Exilles to mount Genevre, so that he may easily [...]
Nature22.07.1875
  • Datum
    Donnerstag, 22. Juli 1875
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] and 1873 is in the press, and that concerted action of several departments by regions is, if slowly, yet gradually being inaugu rated in different directions, particularly in the valleys of the Seine, Gironde, Rhône, and Meuse, and the Mediterranean sea-board. M. Fron resumes the discussion of thunderstorms, [...]
[...] 167 feet; June 1854, 18°o feet; June 1855, 23-6 feet; and on the 24th June, 1875, 26.2 feet, the last being thus a foot and a haſ higher than any flood that has occurred in this valley during the past seventy-one years, and 33 feet higher than the historic flood of 1772. [...]
[...] transverse watersheds slopes gradually eastward, but is divisible into three prairie steppes or plateaus of different elevations. The lowest includes Lake Winnipeg and the valley of the Red River; its average altitude is 800 feet. The second, or the “Great Plains,” properly so called, has an average elevation of 1,690 [...]
[...] of Upper Silurian is concealed by the drift deposits in the Lake of the Woods region. Lowest Prairie Zezel and Valley of the Red River.—This prairie presents an appearance of perfect horizontality. The soil con sists of fine silty deposits arranged in thin horizontal beds resting [...]
[...] entirely composed of material derived from them. The Rocky Mountains themselves show abundant traces of glaciation. Nearly all the valleys hold remnants of moraines, some of them still very perfect. The harder rocks show the [...]
[...] usual rounded forms, but striation was only observed in a single locality, and there coincided with the main direction of the valley. The longer valleys generally terminate in cirques, with * perpendicular rock-walls, and containing small but deep a KeS. [...]
[...] the Rocky Mountains. On some important facts connected with the Boulders and Drifts of the Eden Valley, and their bearing on the theory of a Melting Ice-sheet charged throughout with rock-fragments, by I). Mackintosh. In this paper the main object of the author is [...]
[...] This absence of drift on the eastern side might, the author con siders, be satisfactorily accounted for by supposing that the transverse valleys of the chain were, during the glacial epoch, completely blocked up with congealed snow or ice, by which means all communications between the opposite sides of the [...]
[...] mined by faults and anticlinals. These were shown in a second series of diagrams in which the actual relation of numerous valleys, gorges, &c., to faults, &c., was pointed out. The various agents of erosion such as sea-water, rain-water, and ice had modified, and in some cases altered, the features due to dis [...]
[...] coagulation of the blood on issuing from the organism, by M. F. Glenard.—On the hailstorm which burst over Geneva and the Rhône valley on the night of July 7–8, by M. Colladon.—On clouds of ice observed during an aerostatic elevation on July 4, by M. W. de Fonvielle. - [...]
Nature30.03.1876
  • Datum
    Donnerstag, 30. März 1876
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] but are not an identical, race. The two chief tribes in the hills of the Tapeng valley are the Lakone and Kowrie or Kowlie, but numerous subdivisions of clans occur. All are said to have originally come from the Kakoos' country, [...]
[...] north-east of Mogoung ; and Shans informed us that two hundred years ago Kakhyens were unknown in Sanda and Hotha valleys. To give one instance of their migrations. The Lakone tribe have at a very recent period driven the Kowlies from the northern to the southern banks of the [...]
[...] “The Shans proper of these valleys are a fair race, somewhat sallow like the Chinese, but of a very faintly darker hue than Europeans, the peasantry, as a rule, [...]
[...] and streams, in order to supply our vast metropolis, which I am told it is contemptuous to term “overgrown.” I never spoke of the fertile meadows of the Thames valley, about which Dr. Frank land makes merry, and I never intentionally alluded in the slightest degree to the main valley of the Thames, except to say [...]
[...] verted into “arid wastes” by the abstraction of the water with which they are now charged up to within a very few feet of their surface. In the valley in which I live I have known the peaty soil above such gravel, even without the artificial abstraction of the moisture below, become during a dry summer sufficiently [...]
[...] to imbibe all the rain that falls, except when by chance the sur face is frozen. The lowering of the water which, except in the valleys, is now usually from Ioo to 200 feet below the surface, would make no difference in the receptive power of the soil on the hills, and could not be effected in the valleys without laying [...]
[...] have induced me to accept the invitation of friends, who also enjoy such researches, to again visit Auvergne for the purpose of examining the Mont Dore valley for glacial traces, and I would gladly avail myself of any observations made by other geologists in that region, if they would do me the favour of sending me the [...]
[...] examined the nature of the foundation,” and he then proceeded to inquire into the nature of the evidence upon which the calcu lations have been made, as to the rate of denudation of valleys, the wearing back of sea coasts, the growth of peat-mosses, and the deposition of alluvium. He endeavoured to show by [...]
[...] grass tree flourish at some distance from the stream. He crossed the Amama several times, and describes it as flowing through a large and fertile valley, apparently uninhabited, and well adapted for pastoral purposes. Nowhere did he find the natives pos sessing any knowledge of gold, silver, or any other metal. He [...]
[...] stone, and containing crystals of selenite, pseudomorphs of salt, and numerous small fish-scales. A single insect wing was obtained from it. This bed extends across the valley of the Willow Brook, and forms the base of Crown Hill. Above it comes the Bone-bed, from 2 to 3 inches thick, containing [...]
Saturday review19.11.1870
  • Datum
    Samstag, 19. November 1870
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] falsehood. Whether opaque colour be here present is a trivial matter compared with the question whether a hill has not been thrust into the midst of the Valley of Jehoshaphat which has no existence whatever. The writer, who isnows Jerusalem well, could with difficulty in this drawing identify a single point save [...]
[...] Nevada mountain, situated in the county of Mariposa, in the State aforesaid, and the head-waters of the Merced River, and known as the Yosemite Valley, with its branches and spurs, in estimated length fifteen miles, and in average width one mile back from the precipice on each side of the valley,” to be held by the [...]
[...] * The Posemite Guide-book: a Description of the Posemite Valley and the Adjacent Region of the Sier- Nevada, and of the Big Trees of California. By J. D. Whitney, State Geologist. Published by Authority of the Legis [...]
[...] selected from those executed for the author's Geology of Cali Ozºza. f The real name of this remarkable valley seems to be uncertain, both in its origin and its orthography. By the aboriginal Indians it was known as Ahwahnee or Auwoni. It is only of late years [...]
[...] alls in pronunciation), meaning “grizzly bear.” This may very probably have been the name of a chief, or it may have been given to the valley by bands of Indians driven out by the whites in 1851. The native denizens of the valley and its neighbourhood are said to have been a mixed race made u [...]
[...] “Bridal Veil” Fall; Totokónula (the towering rock now called “El Capitan”), imitated, say the natives, from the cry of the crane, which in winter enters the valley by flying over that rock; Loya, the “Sentinel” peak; Tululowehäck, the cañon of the South Fork of the Merced, called the Illilouette in the Californian [...]
[...] débris, the water rushes down in a series of cascades for a down ward distance of 3oo feet more. Its base being concealed by the trees of the valley, the effect of the fall is as though it were over 90o feet in vertical º: The “Virgin's Tears,” directly facing it across the valley, makes also a fine fall of over 1,000 feet, in [...]
[...] part of the range, are most abundant and defined about the heads of Kern and King's Rivers in the region above the Yosemite, from the valleys in º the Merced, San Joaquin, and Tuolumne take their rise. Of these ice masses the most striking must have been that which came down the valley of the Tuolumne, above thirty [...]
[...] of Walker, Pyramid, and the other lakes on that side of the Sierra. No doubt, as Mr. Whitney argues with reason, at that time the now arid valleys of the Nevada were beautiful inland seas, which filled the spaces between the lofty parallel ridges by which that State is traversed:— [...]
[...] unprovided with any exact parallel in nature. This is the sub sidence, from some unknown cause, of the limited area forming the Yosemite; the bottom of the valley sinking down to an indeter minate depth, owing to its support being somehow withdrawn from underneath during some of those convulsive oscillations [...]
Nature30.04.1874
  • Datum
    Donnerstag, 30. April 1874
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] a watershed, it would d priori appear more likely that a double outfall, if it exist, should lie in or towards adjacent districts than connected with opposed valley systems. The following in stance, which I observed in Norway last summer, is, in view of Colonel Greenwood's letter (NATURE, vol. ix. p. 441), worth [...]
[...] many Norwegian lakes, it presents a facies different to what we are most familiar with in Britain. Instead of occupying a single valley-basin, it consists of a chain of minor basins strung along an axis of depression (probably a pre-existing valley), and each separated from its neighbours by the subsided walls of the valley [...]
[...] authenticated instances of lakes with several outfalls could be referred to districts which have been traversed by a continuous sheet of glacier ice. When glaciers were confined within valley boundaries, as in Britain, their force was of necessity concen trated along lines, but upon level tracts or plateaux they [...]
[...] observed, however, that the actual mean annual outflow of the lakes would be a better criterion, and that from the form of the river valleys giving exit to the waters, this must necessarily increase in a much greater ratic than the measured change of level in the lake itself. It is [...]
[...] into the fertile and sheltered valley of Salcombe, so that in one [...]
[...] Richardson and Townsend, were to flow from it. Under Mr. Richardson's direction he spent a large portion of his time in searching for fossils through the valleys around Farley, and in making drawings of the fossils he found and of the recent forms that were most nearly [...]
[...] by Smith had one or more shelves sloping to represent the dip as he knew them in the typical ground of the Dunkerton Valley, near Bath, where he first studied them. This was the collection from which young Phillips first derived his ideas of a geological museum for teaching [...]
[...] in 1855. His contribution to the Palaeontographical Society on the Belemnitidae, and his “Geology of the Thames Valley,” are well known ; and he has also written many smaller works which we have not space to notice. [...]
[...] rence of Jade in the Karakash Valley, on the southern borders of Turkestan, by Dr. Ferdinand Stoliczka, Naturalist attached to the Yarkund Mission. In this paper the author described [...]
[...] was the fungus published by Kunze as Rhizomorpha corynephora. —Mr. Andrew Murray exhibited a fungoid production existing on trees over a considerable space in the Yosemite Valley, in California. Mr. Berkeley considered it near to the fungus called Dothidea morbosa, but there was also a gall on the same shoot.— [...]
Nature30.12.1875
  • Datum
    Donnerstag, 30. Dezember 1875
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 9
[...] The landslip to which Mr. Scrope refers, and which he de scribes as having occurred in 1859, under cliffs nearly a thousand feet high “on the left flank of the valley looking upwards,” is in a very different position from that of the blocks to which I have directed attention. There are no cliffs whatever such as [...]
[...] in a very different position from that of the blocks to which I have directed attention. There are no cliffs whatever such as Mr. Scrope describes on the left flank of the valley anywhere near their position, nor for half a mile above it. The left flank of the valley for half a mile above them forms a very gentle [...]
[...] north to south, the summit of the mountain being nearly level for that distance. To the east of the pass and 1,000 feet below is Lake Valley, fifty miles long from north to south, and twenty miles broad in some parts; this valley contains the basin of Lake Tahoe, which has a depth of 1,600 feet. The topography [...]
[...] Lake Tahoe, which has a depth of 1,600 feet. The topography of the pass is such that no moraine matter would reach the head of it until the basin of Lake Valley was filled by ice above the level of the pass, or by a glacier 1,000 feet thick, nor during the decline of the cold would any extensive glacier form there after [...]
[...] level of the pass, or by a glacier 1,000 feet thick, nor during the decline of the cold would any extensive glacier form there after the level of the ice in Lake Valley had fallen below the level of the pass. Such being the case, we have at the head of the American valley the results of glacial action during the middle [...]
[...] American valley the results of glacial action during the middle of the glacial epoch, or at least during the time the glacier in Lake Valley was increasing from a thickness of 1,000 feet to a thickness of 1,600 or 1,709, and also whilst it was diminishing from its maximum depth down to the level of the pass. The [...]
[...] founded are, first, the fact that no permanent ice-covering could have existed at the head of the pass at the time the Lake Valley, glacier had already reached a thickness of 1,000 feet, otherwise moraine matter could not have been deposited in [...]
[...] not increased by inflowing glaciers. Another fact indicating the existence of a high summer temperature is the comparatively small extension of the glacier down the valley of the American river. During the height of the glacial epoch the thickness of the glacier at the head of the valley must have been 600 or 7oo [...]
[...] feet above the level of the pass, and yet the bulk of the moraine matter it transported has been deposited as terminal and lateral moraines within eight miles of the summit. As the valley in this distance has only fallen about 800 feet the melting of the ice must have been much more rapid than it would be with our pre [...]
Nature08.08.1872
  • Datum
    Donnerstag, 08. August 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] extremely beautiful, but difficult to travel over. The mountains of light grey granite stand like islands in new red sandstone, and mountain and valley are all clad in a mantle of different shades of green. The vegetation is indescribably rank. Through the grass—if grass it can [...]
[...] fairly set in by November, and in the mornings, or after a shower, these leaves were loaded with moisture, which wet us to the bone. The valleys are deeply undulating, and in each innumerable dells have to be crossed. There may be only a thread of water at the bottom, but the [...]
[...] would resemble the frost vegetation on window-panes. They all begin in an ooze at the head of a slightly de pressed valley. A few hundred yards down, the quantity of water from oozing earthen sponge forms a brisk peren nial burn or brook a few feet broad and deep enough to [...]
[...] require a bridge. These are the ultimate or primary sources of the great rivers that flow to the north in the great Nile valley. The primaries unite and form streams in general larger than the Isis at Oxford or Avon at Hamilton, and may be called secondary sources. They [...]
[...] ferent directions in the Manyema country are briefly as follows:– The great river, Webb's Lualaba, in the centre of the Nile valley, makes a great bºnd to the west, soon after leaving Lake Moero, of at least 180 miles; then turning to the north for some distance, it makes another [...]
[...] members were entertained at a soiré given by H. Salway, Esq., of “The Cliff,” Ludlow. During Wednesday the Upper Lud. low rocks in the valley of the Teme were subjected to ſurther examination, and the party proceeded as far as Downton, where the uppermost members of the series are seen at the Tin Mills [...]
[...] “Pentamerus limestone,” with its characteristic Pºntamerits oblongus, was also seen. The party then proceeded to the quarries of Caradoc sandstone in the Onney valley, at one of which Prof. Morris gave a general description of the Silurian system and the extension in England of its various members. [...]
[...] and beauty. The members were then entertained at lun cheon, aſter which they left Linley Hall and traversed a long, narrow, and very beautiful valley in the park, and ter minating at the Stiper Stones. At a little distance from the park enclosure a mass of felspathic ash in Lower Llandeilo [...]
[...] Lingula flags. The Longmynds ridge, extending ſor nearly fifteen miles, bounds the view to the east, and this range had now to be crossed. The intervening valley affords several sections, at one of which was seen what was considered by Murchison to be the junction of the Silurians with the Cambrians. Near the [...]
[...] and picturesque. Caer Caradoc stands boldly out at a littie disſance to the north-east, with the Wenlock and Aymestry lime stone ridges beyond, and bounding a valley of great beauty at d extent, terminated northwards by the volcano like cone of the Wrekin, at the foot of which the Severn flows through a deep [...]
Nature12.09.1872
  • Datum
    Donnerstag, 12. September 1872
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] valley, as in the valleys of all the streams of the West, there is a chain of lake basins that must have existed during the Pliocene period. There was a continuous [...]
[...] The term Yellowstone Basin is sometimes applied to the entire valley; but the basin proper comprises only that portion enclosed within the remarkable ranges of mountains which give origin to the waters of the Yellow [...]
[...] line having then been high up on the sides of the sur rounding mountains. Warm springs are not uncommon in the valley of the lower Yellowstone, but the temperature is seldom higher than 60° or 80°. It is not until we reach Gardiner's [...]
[...] left side, opposite the third cañon, that the true hot springs commence in their full force. About three miles above its junction with the Yellowstone, the valley bottom is [...]
[...] they may therefore be called calcareous springs. There are two classes of springs in the Yellowstone valley, one in which lime predominates, in the other silica. With the exception of the White Mountain Spring in Gardiner's River, and one or two of not much importance, [...]
[...] intervals that throws the mud up several feet. The water in the vicinity, as well as the mud, seems to be thoroughly impregnated with alum. In an adjoining valley are little mud or turbid water vents, which keep up a simmering noise, showing the nature of the earth beneath the crust. [...]
[...] Only one other shaft has been met with at all suitable for observation. It is called Brandon Walls shaft, and belongs to the Rookhope Valley Mining Company, to the courtesy of whose agent we are indebted for liberty to take observations. This shaſt is some 6 miles east of those reported on last year, and is [...]
[...] about 175 species, represented by 700 or 8oo varieties. The average area occupied by each species is about 5 or 6 square miles, though many are restricted to half that area. The valleys that lie on one side of the mountain range that traverses this district preserve, as far as we can observe, the same conditions; [...]
[...] district preserve, as far as we can observe, the same conditions; but the varieties, and in some cases the species, ſound in each valley, differ from those ſound in any other.” If we would account for these facts on the hypothesis of evo lution, it seems necessary to suppose: First, that these molluscs [...]
[...] petitors, to struggle with, , and no enemies, quadrupeds and reptiles being absent, and birds few. The rivers were small and would only distribute any 'form through the same valley. All these conditions favoured this remarkable persistence of closely linked forms. [...]
Saturday review22.09.1860
  • Datum
    Samstag, 22. September 1860
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 10
[...] headdresses of many of the native women on a Sunday giving them a resemblance to cherubs whose wings are in mourning, mais qui ont de quoi. Across the meadows, down in the valley, half hid among apple and walnut trees, gleams the many-gabled village of Oberweiler, where the Baden Government maintains [...]
[...] fifty feet in height. It was in a fine summer afternoon that we walked up this valley by the side of a tumbling stream. On either hand the crumbling hills of granite and gneiss speak strongly of decay, and every side valley has that peculiar appearance which tells the geo [...]
[...] to the North Sea, through the unnumbered islands that lie between Baden and France. When satisfied with gazing, we proceeded to examine the deep rocky valleys scooped in the sides of the mountain. Patches of snow lay here and there on the slopes at the upper ends of the valleys, hinting that a change in [...]
[...] southerly direction to the Rhine, which the river Alb enters at Albruck, about forty miles below the Rhine-falls at Schaffhausen. Tramping along the road that winds down the valley, we passed through the flourishing villages of Ober, and Nieder Menzensch wand, lying among vivid green meadows, the mountains on [...]
[...] peaks, converting all their ravishing panoramas into so many monotonous abysses of cold white steam. Drizzle and inunda tions fill the valleys—sulky and damp pedestrians fill the hotels. Back along the railways are º of despairing demi semi-Alpinists, whose modest powers of enjoyment are not worthy [...]
[...] * The Eagle's Nest in the Valley of Sirt, together with some Ercursions among the Great Glaciers. By A. Wills. London: Longmans. 1869, [...]
[...] matter of mountains, and hopes to persuade some of these punc tilious devotees that there is †: worth seeing in Northern Savoy out of sight of Chamounix. The little Valley of Sixt, whose cause he especially pleads, lies just two ridges north of the Valley of Chamounix, on the western slopes of the Buet. The [...]
[...] corner of the Alps so well, ought to be an ample voucher. The book, which is full of descriptions almost as warm of the scenery by which this happy valley is surrounded, is published avowedly for the purpose of drawing into it some portion of the throngs that yearly stream into the desolate and rugged valley of Cha [...]
[...] enjoyments that this agreeable little collection of verbal land scapes has been written. His intense admiration has induced the author to become a landowner in the Valley of Sixt, and he confesses to a neighbourly desire to divert, for the benefit of its [...]
[...] struggling population, a little English gold from the plethoric prosperity of Chamounix guides and hotels. During the present season, when the lower Alpine valleys have consisted more of water than of anything else, there have been comparatively few visitors to divert. The unfortunate inhabitants of Sixt suffered [...]
Nature22.02.1877
  • Datum
    Donnerstag, 22. Februar 1877
  • Erschienen
    London
  • Verbreitungsort(e)
    London
Anzahl der Treffer: 9
[...] boast one natural phenomenon which is certainly exceptional, and at the same time very effective. In the East Island most of the valleys are occupied by pale-grey glistening masses, from a few hundred yards to a mile or so in width, which look at a distance much like [...]
[...] Far down below, under the stones, one can hear the stream of water gurgling which occupies the axis of the valley ; and here and there, where a space between the blocks is unusually large and clear, a quivering reflection is sent back from a stray sunbeam. [...]
[...] blocks is unusually large and clear, a quivering reflection is sent back from a stray sunbeam. At the mouth of the valley the section of the “stone river” exposed by the sea is like that of a stone drain on a huge scale, the stream running in a channel arched [...]
[...] believe, very much underrated. There can be no doubt that the blocks of quartzite in the valleys are derived from the bands of quartzite in the ridges above, for they correspond with them in every respect; the difficulty is to account for their flowing [...]
[...] ridges above, for they correspond with them in every respect; the difficulty is to account for their flowing down the valley, for the slope from the ridge to the valley is often not more than six to eight degrees, and the slope of the valley itself only two or three, in either case much [...]
[...] in the soil-cap and piled in the valley below. The only other question is how the soil is afterwards removed and the blocks left bare. This, I have no doubt, is effected [...]
[...] other question is how the soil is afterwards removed and the blocks left bare. This, I have no doubt, is effected by the stream in the valley altering its course from time to time, and washing away the soil from beneath. This is a process which, in some of the great “stone [...]
[...] quently piling these in moraine-like masses, where the progress of the earth-glacier is partially arrested, as at the contracted mouth of a valley, when the water perco lating through among them in time removes the inter vening soil. As the avalanche is the catastrophe of ice [...]
[...] F.R.S.—The remains noticed in this paper were obtained by MM. O'Reilly and Sullivan in a cavern discovered at about twelve metres from the surface, in the valley of Udias, near Santander, by a boring made through limestone in search of calamine. They were found close to a mound of soil which had [...]