scholarly journals The Contexts of Osip Mandelstam’s Works in Tomas Venclova’s Diptych “Two Poems about Love”

Literatūra ◽  
2020 ◽  
Vol 62 (2) ◽  
pp. 129-137
Author(s):  
Donata Mitaitė

The article analyzes a diptych “Two Poems about Love” written by Tomas Venclova in 1973 and its contexts. The article refers to the archived manuscript and the translation of Mandelstam’s poem “Za to, chto ia ruki tvoi ne sumel uderzhat‘…” (“For I failed to keep your hands…”) that Venclova first released in 1967. In this case, Mandelstam’s poem is important to Venclova both as a text about a city doomed for collapse, and as a work about love. It is noted that in the diptych this is not the only important poem by Mandelstam (although it was noted in the comments); images from the other poems (“Swallow,” “Leningrad”) were also quoted and reinterpreted by Venclova. Just like Mandelstam, Venclova was also opposed to totalitarianism. For Mandelstam, the post-revolutionary St. Petersburg, and for Venclova the Soviet Vilnius, represent a dying city – in the first poem of the diptych it is moved to the ocean, in such a way highlighting the threatening situation. In the first poem, the source of life is love disguised with a musical theme; the second one already talks about passing lovers – their bodies now “like stones lay next to each other.” Some poetic images are modified in Venclova’s later works. Mandelstam is still as important and will appear next to Ovid, who is only mentioned in the manuscript, in the poem “Tristia” from 1997.

2021 ◽  
Vol 6 (16) ◽  
pp. 104-112
Author(s):  
Zulfiyye HUSEYNOVA

The art of minstrel, whose etymological meaning is "ash", "light", "love", is common in all Turkic peoples, including Azerbaijan, Göyçe, Borchali, Nakhchivan, Yerevan, Ağbaba, Çıldır, Derbent, Karabakh, Ganja, Tovuz, Gazakh, Shamkir, Shamahhi, It was developed in Ismayilli, Agsu, Goychay, Khizi, Guba, Tabriz, Urmia, Khorasan regions. Although the Shirvan minstrel environment has been included in the research of philologists, it has been little studied in musicology. From this point of view, the works of K. Akhundova (Dadaşzade), Ahliman Rahimov, Aliyeva Hanim devoted to examining the Shirvan ash circle are quite remarkable. Shirvan ashik environs have spread over a wide area, including Shamakhi, Ismayilli, Agsu, Goycay, Hızi, Ujar, Gobustan, Mugan region, Salyan, Sabirabad and Belasuvar regions. Shirvan minstrels always responded to cultural events with their art, and took an active role in minstrel congresses and other important state events that played an important role in the development of this art. Shirvan ashik’s have always come to the fore with their musical creations. In Shirvan's minstrel environment, air is played in the accompaniment of various instruments, unlike other regions. It included two balabans, a percussion instrument (double drum) and a ashik singer, including a ashik. In this respect, the group of Shirvan ashik’s can be called a community. One of the characteristic features of the representatives of the environment is that the mugham is performed at the beginning of the air, sometimes between the second and third lines, which shows the skill of the minstrel. Balaban performers also have other responsibilities within the group. It adds color to the general sound of the air accompanied by two bitterns. While one of the balaban players plays a musical theme, the other has a kind of "helper" structure and takes exemplary notes in accordance with the mood and melody of the air. The inclusion of the percussion instrument in the backing demonstrates the uniqueness of this setting not seen in other regions. Although they can be found in other environments such as Güzell?, sikeste, keremi, muhammes, gerayli, they are completely different from Shirvan airs in terms of melody. Peşrov and Shesangi melodies belong only to Shirvan ashik’s and are not performed in other settings. Shirvan ash tunes are also very rich in terms of musical style and contain developed moments, melodies and rhythms.


2020 ◽  
Vol 17 (2) ◽  
pp. 171-182
Author(s):  
Peter Bofinger

The paper discusses the monetary policy of the European Central Bank (ECB) under the presidency of Mario Draghi. It first shows the serious mistakes made under his predecessor, Jean-Claude Trichet, during which period the ECB destabilized rather than stabilized. Draghi, on the other hand, embarked on a more expansive course immediately after taking office, thereby securing the existence of the euro in a very threatening situation. In 2014, he then identified the deflationary risks for the eurozone at an early stage and successfully countered them with massive bond purchases. The undesirable developments for the financial system and especially the banks predicted by his critics, who are to be found primarily among German economists, have not materialized.


1988 ◽  
Vol 62 (03) ◽  
pp. 411-419 ◽  
Author(s):  
Colin W. Stearn

Stromatoporoids are the principal framebuilding organisms in the patch reef that is part of the reservoir of the Normandville field. The reef is 10 m thick and 1.5 km2in area and demonstrates that stromatoporoids retained their ability to build reefal edifices into Famennian time despite the biotic crisis at the close of Frasnian time. The fauna is dominated by labechiids but includes three non-labechiid species. The most abundant species isStylostroma sinense(Dong) butLabechia palliseriStearn is also common. Both these species are highly variable and are described in terms of multiple phases that occur in a single skeleton. The other species described areClathrostromacf.C. jukkenseYavorsky,Gerronostromasp. (a columnar species), andStromatoporasp. The fauna belongs in Famennian/Strunian assemblage 2 as defined by Stearn et al. (1988).


1967 ◽  
Vol 28 ◽  
pp. 207-244
Author(s):  
R. P. Kraft

(Ed. note:Encouraged by the success of the more informal approach in Christy's presentation, we tried an even more extreme experiment in this session, I-D. In essence, Kraft held the floor continuously all morning, and for the hour and a half afternoon session, serving as a combined Summary-Introductory speaker and a marathon-moderator of a running discussion on the line spectrum of cepheids. There was almost continuous interruption of his presentation; and most points raised from the floor were followed through in detail, no matter how digressive to the main presentation. This approach turned out to be much too extreme. It is wearing on the speaker, and the other members of the symposium feel more like an audience and less like participants in a dissective discussion. Because Kraft presented a compendious collection of empirical information, and, based on it, an exceedingly novel series of suggestions on the cepheid problem, these defects were probably aggravated by the first and alleviated by the second. I am much indebted to Kraft for working with me on a preliminary editing, to try to delete the side-excursions and to retain coherence about the main points. As usual, however, all responsibility for defects in final editing is wholly my own.)


1967 ◽  
Vol 28 ◽  
pp. 177-206
Author(s):  
J. B. Oke ◽  
C. A. Whitney

Pecker:The topic to be considered today is the continuous spectrum of certain stars, whose variability we attribute to a pulsation of some part of their structure. Obviously, this continuous spectrum provides a test of the pulsation theory to the extent that the continuum is completely and accurately observed and that we can analyse it to infer the structure of the star producing it. The continuum is one of the two possible spectral observations; the other is the line spectrum. It is obvious that from studies of the continuum alone, we obtain no direct information on the velocity fields in the star. We obtain information only on the thermodynamic structure of the photospheric layers of these stars–the photospheric layers being defined as those from which the observed continuum directly arises. So the problems arising in a study of the continuum are of two general kinds: completeness of observation, and adequacy of diagnostic interpretation. I will make a few comments on these, then turn the meeting over to Oke and Whitney.


1966 ◽  
Vol 24 ◽  
pp. 337
Author(s):  
W. Iwanowska

A new 24-inch/36-inch//3 Schmidt telescope, made by C. Zeiss, Jena, has been installed since 30 August 1962, at the N. Copernicus University Observatory in Toruń. It is equipped with two objective prisms, used separately, one of crown the other of flint glass, each of 5° refracting angle, giving dispersions of 560Å/mm and 250Å/ mm respectively.


2020 ◽  
Vol 43 ◽  
Author(s):  
Philip Pettit

Abstract Michael Tomasello explains the human sense of obligation by the role it plays in negotiating practices of acting jointly and the commitments they underwrite. He draws in his work on two models of joint action, one from Michael Bratman, the other from Margaret Gilbert. But Bratman's makes the explanation too difficult to succeed, and Gilbert's makes it too easy.


1999 ◽  
Vol 173 ◽  
pp. 249-254
Author(s):  
A.M. Silva ◽  
R.D. Miró

AbstractWe have developed a model for theH2OandOHevolution in a comet outburst, assuming that together with the gas, a distribution of icy grains is ejected. With an initial mass of icy grains of 108kg released, theH2OandOHproductions are increased up to a factor two, and the growth curves change drastically in the first two days. The model is applied to eruptions detected in theOHradio monitorings and fits well with the slow variations in the flux. On the other hand, several events of short duration appear, consisting of a sudden rise ofOHflux, followed by a sudden decay on the second day. These apparent short bursts are frequently found as precursors of a more durable eruption. We suggest that both of them are part of a unique eruption, and that the sudden decay is due to collisions that de-excite theOHmaser, when it reaches the Cometopause region located at 1.35 × 105kmfrom the nucleus.


1975 ◽  
Vol 26 ◽  
pp. 395-407
Author(s):  
S. Henriksen

The first question to be answered, in seeking coordinate systems for geodynamics, is: what is geodynamics? The answer is, of course, that geodynamics is that part of geophysics which is concerned with movements of the Earth, as opposed to geostatics which is the physics of the stationary Earth. But as far as we know, there is no stationary Earth – epur sic monere. So geodynamics is actually coextensive with geophysics, and coordinate systems suitable for the one should be suitable for the other. At the present time, there are not many coordinate systems, if any, that can be identified with a static Earth. Certainly the only coordinate of aeronomic (atmospheric) interest is the height, and this is usually either as geodynamic height or as pressure. In oceanology, the most important coordinate is depth, and this, like heights in the atmosphere, is expressed as metric depth from mean sea level, as geodynamic depth, or as pressure. Only for the earth do we find “static” systems in use, ana even here there is real question as to whether the systems are dynamic or static. So it would seem that our answer to the question, of what kind, of coordinate systems are we seeking, must be that we are looking for the same systems as are used in geophysics, and these systems are dynamic in nature already – that is, their definition involvestime.


1976 ◽  
Vol 32 ◽  
pp. 577-588
Author(s):  
C. Mégessier ◽  
V. Khokhlova ◽  
T. Ryabchikova

My talk will be on the oblique rotator model which was first proposed by Stibbs (1950), and since received success and further developments. I shall present two different attempts at describing a star according to this model and the first results obtained in the framework of a Russian-French collaboration in order to test the precision of the two methods. The aim is to give the best possible representation of the element distributions on the Ap stellar surfaces. The first method is the mathematical formulation proposed by Deutsch (1958-1970) and applied by Deutsch (1958) to HD 125248, by Pyper (1969) to α2CVn and by Mégessier (1975) to 108 Aqr. The other one was proposed by Khokhlova (1974) and used by her group.


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