scholarly journals Góry i wspinaczka w „Boskiej komedii” Dantego

2021 ◽  
Vol 15 ◽  
pp. 11-43
Author(s):  
Jacek Kolbuszewski

The study uses a variant of the geocritical methodology combined with humanistic mining studies. It was pointed out that in Dante’s poem there were numerous references to the realities of real space (the Alps and the Apennines, which, appearing as a separate part of the mountain world, in the poem at the same time constitute a kind of props room of mountain motifs, used in the construction of Purgatory Mountain). Also, the journeys of the heroes, Dante and his guide Virgil, can be perceived realistically as an actual journey, made in a difficult mountain terrain. It was specified in the realities of Hell, Purgatory Mountain, and Paradise. In this way, using specific Earth realities, Dante created a powerful vision largely made of mountain realities. Mount Purgatory, the target of Dante’s ascent, created when Lucifer, thrown from the heavens, struck the depths of the Earth deep into its center, which changed the hemisphere and pushed up the land masses, throwing them over the surface of the ocean covering the southern hemisphere. Locating the Mount of Purgatory in the center of the southern hemisphere, and at the antipodes of Jerusalem, as a mountain rising on a small island from the vastness of the seas covering this part of the world, Dante used elements of the Muslim tradition (perhaps known to him) with its notions of a lofty, pyramidal shape, which is considered to be the holy Mount of Adam (2243 m) in Ceylon (Sri Lanka). The poet, however, never once described the Purgatory Mountain as a whole, creating a vision of its enormity seen from under its steep walls, but he introduced into the poem numerous details about the surface of this mountain and how to climb it. He filled his abstract vision with real details. From the very first songs of Purgatory, the narrative runs in the order of the characters’ ascent towards the summit Paradise. The work hypothesized that the famous poet Bismantova became the prototype of the Dante Mountain of Purgatory, such a judgment is almost universally approved. That Dante saw this mountain is certain: he was in Lunigiano and Casentino (Bismantova rises right next to it) in 1306, and certainly before 1315, at the time when Divine Comedy was being written. For the accuracy of this hypothesis, the shape of this vast rock mass (culmination in 1047), rising above the level of the surrounding valleys by about 400 m in height with almost vertical rock walls, is of great importance for the accuracy of this hypothesis. The peak landscape largely corresponds to the ideas of an ancient idyllic grove. These realities of the mountain landscape meant that the thought about them found literary expression in the pages of Dante’s poem, which prompts me to share my opinion that the sight of the boatswain and his presence in it gave Dante a vision of the Purgatory Mountain as a “hybrid” creation, partially a description of a real landscape and in part a fantastic, syncretic vision based on elements of ancient literary tradition. The description of climbing this mountain leads us through a narrow chimney, overhang, and other rock formations, forming terraces in the structure of the mountain. The conclusion of the work are the words of Italian literary researcher Filippo Zolezzi, who wrote that “Mount Purgatory appears as an absolute ideal of a mountain, because on its top there is an earthly Paradise — a space of direct contact with the divine, hence even the most beautiful earthly mountains are merely a copy of them. However, the very fact that a poet — a man — to reach this summit, has to climb, climb, makes it an ideal prototype for mountain climbing”.

1968 ◽  
Vol 57 (4) ◽  
pp. 567-604 ◽  
Author(s):  
R. W. Paine

The stick-insect Graeffea crouanii (Le Guillou) is a pest of coconuts of local and sporadic importance in the south Pacific and there have been recent outbreaks on Taveuni Island, in the Fiji group. As there appear to be virtually no parasites of the nymphal stages, a preliminary search was made in 1960 for parasites of other palm-feeding Phasmatids in Melanesia. This revealed the presence of Tachinidae parasitising species of the genera Ophicrania and Megacrania, and in 1963–64 these were studied in the Solomon Islands. The Tachinidae comprise at least two species of Mycteromyiella: M. laetifica (Mesnil) attacking both O. leveri Günth. and a species of Megacrania in the western Solomons, and M. phasmatophaga Crosskey attacking 0. leveri and some other Phasmatid hosts on Guadalcanal. The early stages of both species of Mycteromyiella are briefly described and compared, with notes on their bionomics. There was no evidence of any egg parasite attacking Ophicrania in the Solomons.O. leveri, which is very closely related to G. crouanii, has never caused significant damage to coconuts in the Solomon Islands, except on the small island of Savo, from which its Tachinid parasites appear to be absent. It is concluded that Mycteromyiella, especially M. laetifica, which appears to be fairly specific, may be an important factor in the control of O. leveri in the Solomons.The principal hosts of O. leveri are the sago palm (Metroxylon salomonense) and species of arecoid palms in the forest, on all of which the insect has better scope for concealment than on coconuts. Collections of nearly 6,000 examples of O. leveri from sago palm on Kolombangara island, in the western Solomons, in August 1963-February 1964 showed an average parasitism by Mycteromyiella laetifica of 28 per cent. Eggs of the Tachinid are laid on nymphs of all instars as well as on adults. The host-survival rate was about 30 per cent, for nymphs and 50 per cent, for adults.A small number of parasitised specimens of O. leveri from Kolombangara were released on Savo, but there was no evidence six months later that M. laetifica had become established there.Breeding trials at Honiara showed that O. leveri could be reared successfully in captivity but not M. laetifica, which shows reluctance to mate in cages and has a narrow range of environmental tolerance in the pupal stage, in which a mortality of at least 70 per cent, seems unavoidable under the conditions practicable for transportation of this stage by air.Between October 1963 and March 1964 nearly 960 puparia of M. laetifica were sent to Fiji. About half of them were used for breeding trials, which showed that the Tachinid could be reared through G. crouanii in captivity but could not be maintained. The rest were released on Taveuni, but a further outbreak of G. crouanii during 1965 yielded no evidence that M. laetifica had become established.Material of M. phasmatophaga, which has a more restricted choice of environment than M. laetifica, but also a somewhat greater potentiality for killing its host, was obtained by exposing O. leveri on seedling coconut palms planted in the forest at Honiara. Quantities were insufficient for transmission to Fiji; 150 parasitised hosts were released on Savo but samples of O. leveri collected there six months later gave no indication of its establishment.Despite this initial failure, it is considered that Mycteromyiella could bring about the control of G. crouanii in Fiji and other affected Pacific islands, and the means by which this might be achieved are discussed.


1989 ◽  
Vol 3 (6) ◽  
pp. 721
Author(s):  
DA Duckhouse

Australasian pericomoids, psychodids resembling northern hemisphere species of Pericoma Walker (tribe Pericomini), are mostly members of the tribe Maruinini, here re-defined. Amongst Maruinini, they are like several neotropical genera named by Enderlein (1937), but their actual relationship to Enderlein's genera, and hence their identity, has been a long-standing taxonomic problem. Consideration of extensive new collections and observations made in the southern hemisphere now shows that they consist of the following: Genus Notiocharis Eaton. Tribe Maruinini: genus Didicrum Enderlein, and five new genera, Eremolobulosa, Rotundopteryx, Alloeodidicrurn, Satchellomyia and Ancyroaspis. Of these, the Australian Eremolobulosa is the possible sister group of the European Lobulosa Szabo, and the New Zealand genera Satchellomyia and Ancyroaspis are possible sister groups. Of Enderlein's neotropical genera, five classified by Quate (1963) as synonyms, or in one case a subgenus, of Pericoma (Didicrum, Desmioza, Synmormia, Syntomolaba and Podolepria) are recognised as full genera. A key to Australasian pericomoid genera is provided.


1950 ◽  
Vol 31 (3) ◽  
pp. 79-84 ◽  
Author(s):  
C. M. Cross

The behavior of slope and valley winds near the town of Trail in the Columbia River valley system in southern British Columbia was studied, and the results compared with those obtained from similar studies made in the Alps. The hourly wind velocities for two stations—one in the main valley, the other in a side valley—were resolved into components parallel to and at right angles to the valley. This procedure gives the valley and slope winds respectively. The usual diurnal wind pattern was found to prevail in most instances, with up-slope and up-valley winds during the day, and down-slope and down-valley winds at night. These systems were much better developed during the summer than in winter, and approximated the ideal pattern more closely on sunny days when the overall pressure gradient was weak.


2009 ◽  
Vol 37 (1) ◽  
pp. 43-66 ◽  
Author(s):  
Ann C. Colley

Most readers either overlook or dismissJohn Ruskin's climbs in the Alps as being insignificant compared to his avid interest in geology and mountain form. However, I want to suggest that Ruskin's climbing – his physical and kinetic relationship to the mountains – is essential to his understanding of them. His numerous and repeated ascents in the lower Alps were not always easy: in fact, they were often tough and sometimes dangerous. Through a few select examples, in the first part of the essay, I establish just how difficult many of these scrambles were so that I may proceed, in the body of the paper, to talk about how these strenuous experiences influenced his way of seeing the mountain landscape he admired, and how, in turn, they helped shape his concept of imperfect vision.


1828 ◽  
Vol 118 ◽  
pp. 113-151 ◽  

The following nebulæ and clusters of stars in the southern hemisphere were observed by me at my house in Paramatta, situated about 6″ of a degree south and about I 8 .78 of time east of the Brisbane Observatory. The observations were made in the open air, with an excellent 9-feet reflecting telescope, the clear aperture of the large mirror being nine inches. This telescope was occasionally fitted up as a meridian telescope, with a strong iron axis firmly attached to the lower side of the tube nearly opposite the cell of the large mirror, and the ends of the axis rested in brass Y’s, which were screwed to blocks of wood let into the ground about 18 inches, and projecting about 4 inches above the ground; one end of the axis carried a brass semicircle divided into half degrees and read off by a vernier to minutes. The position and index error of the instrument were ascertained by the passage of known stars. The eye end of the telescope was raised or lowered by a cord over a pulley attached to a strong wooden post let into the ground about two feet: with this apparatus I have observed a sweep of eight or ten degrees in breadth with very little deviation of the instrument from the plane of the meridian, and the tremor was very little even with a considerable magnifying power. I made drawings or representations of a great number of the nebulæ and clusters at the time of observation, several of which are annexed to this paper; and also very correct drawings of the Nebulæ major and minor, together with a representation of the milky nebulosity surrounding the star η Robur Caroli. The places of the small stars in the Nebulæ major and minor, and also those accompanying the η Robur Caroli, I ascertained by the mural circle in the year 1825, at which time I was preparing to commence a general survey of the southern hemisphere. These stars being laid down upon the chart, enabled me to delineate the nebulosity very accurately. The nebulæ are arranged in the order of their south polar distances to the nearest minute for 1827, and in zones for each degree in the order of their right ascension. The column on the right hand shows the number of times the object has been observed.


1956 ◽  
Vol 46 (1-2) ◽  
pp. 37-45 ◽  
Author(s):  
F. W. Walbank

Few historical problems have produced more unprofitable discussion than that of Hannibal's pass over the Alps. But if there is still no clear answer, some headway had at least been made in defining the question—which is half the battle. Kahrstedt put the matter as succinctly as anyone. ‘Mit Topographie ist nicht zum Ziele zu kommen, weisse Felsen and tiefe Schluchten, Flusstäler und steile Abhänge gibt es uberall. Das Problem ist literarhistorisch, nicht topographisch.’ Hence a feeling of dismay at finding the question reopened without, apparently, any realization of what sort of question it is. For in fact Sir Gavin de Beer's forthright and attractive little book, despite its ingenious attempt to introduce new kinds of evidence, never comes to grips with the fundamental issue—the relationship between Polybius' account and Livy's. This central question is dismissed with a fatal facility : ‘each account complements and supplies what was missing from the other ‘(p. 33). If one is to get anywhere with this problem one must treat it more seriously than that; and it may therefore perhaps be worth while, yet again, to reconsider the evidence and to indicate the limits within which the answer is to be sought (without any guarantee that it will necessarily be found). Such a survey can offer none of the ‘certainties’ or the excitement to be found in Alps and Elephants; it will propose no novelties; and if it is not to become unreadable, it had better avoid all but the most obvious and necessary references to a fantastically inflated modern literature.


1887 ◽  
Vol 4 (12) ◽  
pp. 531-540
Author(s):  
T. Sterry Hunt

The present writer in 1883 reviewed the history of the rocks of the Alps and the Apennines with especial reference to the geological relations of serpentine and its associates, in a paper which appeared in the first volume of the Transactions of the Royal Society of Canada, and is reprinted, revised and with some additions, as the tenth chapter of his volume entitled “Mineral Physiology and Physiography” (Boston, 1886). Therein he gave a somewhat detailed account of the labours in Italian geology of the late Professor Bartolomeo Gastaldi, of Turin, a list of whose publications on that subject from 1871 to 1878, so far as known to the writer, will there be found, including his letter to Quintino Sella, in 1878, on the general results of explorations made in 1877 (loc. cit., 458).


2020 ◽  
Vol 13 ◽  
pp. 19-34
Author(s):  
Jacek Kolbuszewski

If a route is understood to be a selected or marked sequence of places within a given space, the term can also encompass a climbing route, which is a sequence of places in the mountains, on a rock, ice wall or arête through which we can reach a specific destination — in the case of climbing it is usually the top of a mountain or an element in the structure of a mountain that stands out. Thus a route is an order of the places through which a climber is pursuing his or her goal — a top or an arête. In the physical sense this route, blended in the mountain landscape, does not exist, although it can be marked by a painted trail, small mounds, but not ladders and stairs, because these are elements of a route existing in the physical sense, while a climbing route is an intentional, virtual being existing only in the climber’s mind, first as a project of traversing a given rock formation, obviously large enough, i.e. requiring movement in this space, and then as the above mention order (sequence) of places — rock formations, from large to the smallest ones (grip). Not existing physically in reality (a designated fragment of space to move from place to place), a climbing route appears as a man-designed imagined line, a sequence of places marking the direction in which to move. The real sense of the existence of a route lies in its use: a route is alive, when there is movement on it — in this case mountain climbing.


2020 ◽  
Vol 13 ◽  
pp. 343-355
Author(s):  
Jan Pacholski

The present article focuses on eighteenth-century German-language descriptions of the Giant Mountains and Izera Mountains included in selected eighteenth-century accounts of trips to the high est mountains of Silesia and Bohemia by travellers from various German-speaking countries. The analysed fragments refer primarily to sites on the Silesian side of these mountain ranges, although the Bohemian part is mentioned in one case. Differing in terms of their countries of origin, the authors of these works — who included Silesians, a German from Bohemia as well as a man from Berlin and a man from Saxony — liked to refer in their accounts to well-known Swiss models, primarily to the poetic works of Albrecht von Haller and scholarly works of Johann Jakob Scheuchzer, comparing the Giant Mountains to the Alps and using in their descriptions of nature metaphors inspired by the famous Swiss authors, whose oeuvres were quite popular across the entire civilised Europe. The present article provides a detailed analysis of the descriptions of the various natural sites and phenomena, in which the authors use the vocabulary of the history of art and culture, comparing, for example, the view of valleys seen from a mountain top to miniature painting, a waterfall to a performance and music, and rock formations to architectural objects and ancient ruins.


1830 ◽  
Vol 120 ◽  
pp. 223-237 ◽  

The discovery in sea-water of iodine and bromine, two principles which, although in minute proportions, are said to be generally diffused throughout the present ocean, naturally suggested the inquiry, as to whether these same ingredients might not be found to exist in springs occurring in inland situations when containing a similar saline impregnation. This accordingly has been already determined by Stromeyer, Liebig, and others, to be the case in many of the brine-springs of Germany, France, and Italy; but at the time my attention was first directed to the subject, I was unacquainted with any trials of the kind having been instituted with reference to those of this country, except by Professor Turner of the London University, regarding the presence of iodine in the mineral waters of Scotland; in only one of which, that of Bonnington near Leith, he appears to have detected it. I was therefore induced in the course of last spring and summer to undertake a pretty extensive survey of such English springs as are known to contain a considerable proportion of common salt; and having succeeded in detecting in several of them traces of one or both the substances alluded to, I inserted a brief account of the results obtained, in the Philosophical Magazine and Annals of Philosophy for September last. An article that has appeared in a subsequent number of the same periodical work has, however, been the means of drawing my attention to a little work by Mr. Murray, entitled “Experiments on Chemical Philosophy,” which had not before fallen in my way; and from this it is clear, that the detection of iodine in the Gloucester Spa water had been made by that gentleman some time before I had engaged in the inquiry. I am unable, however, to discover in his publication, although it bears so late a date as 1828, any thing that can substantiate the assertion which its author has made in the number of the Philosophical Magazine and Annals referred to, as to his having anticipated me in the discovery of iodine in the springs at Cheltenham*, or in that of bromine in those of Ingestrie. I consider myself, therefore, still warranted in claiming as my own the first public announcement of the existence of bromine in our English springs; but I am far from attaching importance to a discovery which had been previously made in so many similar situations abroad, and would wish it to be understood, that my only pretence for offering to the Royal Society the present communication, is the circumstance of my having examined on the spot most of the mineral springs hereafter enumerated, and having undertaken, wherever it appeared practicable, to obtain an approximation at least to the proportion which these principles bore to the other ingredients present, and to estimate their comparative frequency and abundance in the several rock-formations.


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