scholarly journals NADVIRNA AREA ON LINGUISTIC MAPS

2021 ◽  
pp. 52-57
Author(s):  
Lesia Kysliak

The paper is devoted to the status of dialects of the settlements in Nadvirna district, Ivano-Frankivsk region, which required a through studying of the works of well-known dialectologists of the boundaries of pokutskyi, naddnistrianskyi, hutsulskyi, boikivskyi dialects. The paper contains the analysis of the linguistic maps of AUL (Atlas of the Ukrainian language), made by S. Bevzenko, О. Horbach, Ya. Zakrevska, F. Zhylko, Ya. Yanіv, Т. Yastremska; it also includes descriptive works of the researchers of sub-dialects of a south-west dialect where dialects of settlements of Nadvirna distirct, Ivano-Frankivsk region were represented. The material, cartographed by precursors, has proved that dialects of Nadvirna area are not similar at all language levels. It was stated that researchers chose various networks of dialects which did not allow them to draw demarcation lines between hutsulskyi, naddnistrianskyi, pokutskyi and boikivskyi dialects. In descriptive works about these dialects a starting point in defining boundaries is Nadvirna, part of Nadvirna district (except for the settlements in the north), part of Nadvirna area to the north of Yaremche and others. The attention has been paid to the fact that a demarcation line can stretch for tens and hundreds of kilometers. The assumption has been made that a greater part of Nadvirna area will have a status of transitional dialects. Some own maps of lexical-semantic phenomena, which helped separate groups of dialects – a northern group, a south-eastern group, were analyzed. It has been stated that a larger number of cartographic data will enable to elaborate the boundaries of dialects which contact, to determine transitional dialects, to identify zones and groups of dialects on Naddniprianshchyna area.

2015 ◽  
pp. 289-306
Author(s):  
Tijana Surlan

Recognition is an instrument of the public international law founded in the classical international law. Still, it preserves its main characteristics formed in the period when states dominated as the only legal persons in international community. Nevertheless, the instrument of recognition is today as vibrant as ever. As long as it does not have a uniform legal definition and means of application, it leaves room to be applied to very specific cases. In this paper, the instrument of recognition is elaborated from two aspects - theoretical and practical. First (theoretical) part of the paper presents main characteristics of the notion of recognition, as presented in main international law theories - declaratory and constitutive theory. Other part of the paper is focused on the recognition in the case of Kosovo. Within this part, main constitutive elements of state are elaborated, with special attention to Kosovo as self-proclaimed state. Conclusion is that Kosovo does not fulfill main constitutive elements of state. It is not an independent and sovereign state. It is in the status of internationalized entity, with four international missions on the field with competencies in the major fields of state authority - police, judiciary system, prosecution system, army, human rights, etc. Main normative framework for the status of Kosovo is still the UN Resolution 1244. It is also the legal ground for international missions, confirming non-independent status of Kosovo. States that recognized Kosovo despite this deficiency promote the constitutive theory of recognition, while states not recognizing Kosovo promote declaratory theory. Brussels Agreement, signed by representatives of Serbia and Kosovo under the auspices of the EU, has also been elaborated through the notion of recognition - (1) whether it represents recognition; (2) from the perspective of consequences it provokes in relations between Belgrade and Pristina. Official position of Serbian Government is clear - Serbia does not recognize Kosovo as an independent and sovereign state. On the other hand, subject matter of Brussels Agreement creates new means of improvement for Kosovo authorities in the north part of Kosovo. Thus, Serbian position regarding the recognition is twofold - it does not recognize Kosovo in foro externo, and it completes its competences in foro domestico. What has been underlined through the paper and confirmed in the conclusion is that there is not a recognition which has the power to create a state and there is not a non-recognition which has the power to annul a state.


Sociobiology ◽  
2020 ◽  
Vol 67 (2) ◽  
pp. 201
Author(s):  
Francisco Jiménez-Carmona ◽  
Soledad Carpintero ◽  
Joaquín Luís Reyes-López

The ‘dehesas’ are important and vast agro-silvo-pastoral systems typical of the Iberian Peninsula that are undergoing a crisis due to their low economic profitability and environmental degradation. Thus, it is necessary to identify effective tools that provide a reliable idea of the status of these ecosystems as a starting point for future measures of conservation. In this study we analyse the possible role of ants as surrogates for epigeic arthropods, a common biodiversity indicator group. A total of 15 farms were sampled throughout Sierra Morena (Andalusia, Spain) with pitfall traps, both for the ‘dehesa’ habitats themselves and for different microhabitats within the study sites. First, we achieve a complete list of the species of ants of the area. The results indicate that the ‘dehesa’ habitats were very homogenous for all farms, while microhabitats showed differences in species richness and ant communities’ composition compared to the ‘dehesas’. To evaluate the role of ants as surrogates, the number of traps occupied by each order of arthropod and by each ant species was compared. We found a high correlation between them what confirm the surrogate character of ants for the rest of arthropods in these ecosystems.


Africa ◽  
1933 ◽  
Vol 6 (3) ◽  
pp. 259-276 ◽  
Author(s):  
Monica Hunter

The AmaMpondo are a Bantu tribe of the south-eastern group, living in a native reserve on the southern border of Zululand, and speaking a dialect of Xosa. They depend for their subsistence upon cattle farming and hoe culture. They have a typical Bantu ‘cattle complex’, cattle not only being of economic importance, but being a centre of men's interests and emotions and playing a large part in religion and marriage. They live in patrilineal kinship groups imizi (sing, umzi) which are scattered about the country at distances varying from some hundreds of yards to two or three miles. The average umzi now contains four to five adults, but formerly, when danger from man and beast made concentration necessary for defence, it is said that it was common for twenty married men, together with their wives and children, to live together in one umzi. Both chiefs and commoners practise polygyny, and a union is legalized by the passage of cattle from the groom's group to the bride's (ukulobola). Administration was organized on a territorial basis. There was a powerful paramount chief with district chiefs and sub-chiefs under him. Each sub-chief had a court, from which there was the right of appeal to his immediate superior and finally to the paramount. Cutting across the territorial groupings (amabandla) are patrilineal clans, iziduko (sing, isiduko). Iziduko are strictly exogamous, and the sense of difference between them, and oneness within them, is marked by the taboo on drinking milk, or eating sacrificial meat, of a strange isiduko, but the acceptance of either from a member of the same isiduko. Great emphasis is laid on the respect for elders, living and dead. Deceased ancestors, amatongo, are believed to have the power of blessing, or of sending sickness and poverty, and sacrifices of meat and beer are made to them. Besides being sent by ancestral spirits, sickness is thought to be caused by sorcerers, abatakati. Murder by sorcery is regarded as the worst possible crime, and was punished with torture and death. The fear of sorcery is ever present in the minds of AmaMpondo. The most powerful specialists in the society are the diviners, amagqira, who discover sorcery and who also treat sick persons.


Zootaxa ◽  
2019 ◽  
Vol 4706 (2) ◽  
pp. 255-274 ◽  
Author(s):  
FELISTA KASYOKA KILUNDA ◽  
WERNER CONRADIE ◽  
DOMNICK VICTOR WASONGA ◽  
JIE-QIONG JIN ◽  
MIN-SHENG PENG ◽  
...  

Historically Panaspis wahlbergi (Smith, 1849) has been the only assignable species present in Kenya. Recent studies have shown that it comprises multiple cryptic species and the nominal species is now restricted to southern Africa. Newly collected mitochondrial data (16S rRNA) helped to resolve the status of the Kenyan populations, which revealed the presence of two distant related species. Pairwise distances show average 5.87% differences between the two Kenyan species, and 3.58–5.27% and 8.62–9.15% to nominal P. wahlbergi and P. maculicollis Jacobsen & Broadley, 2000 respectively. Ablepharus massaiensis Angel, 1924 was described from the Maasai plains near Nairobi, but has long been considered a junior synonym of P. wahlbergi. We herein resurrect Panaspis massaiensis comb. nov. as a valid species and describe a new species, Panaspis tsavoensis sp. nov. from the Tsavo Conservation Area in south-eastern Kenya. Morphological examinations of specimens reveal minor differences from each other as well as nominal forms of P. wahlbergi and P. maculicollis. Panaspis massaiensis comb. nov. shares with the P. wahlbergi group a white ventrolateral stripe but can be distinguished by the presence of 26 midbody scale rows versus 24. Panaspis tsavoensis sp. nov. on the other hand, lacks the white ventrolateral stripe, most similar to the P. maculicollis group but differs in that P. maculicollis breeding males have a black patch on the neck with diagonal rows of white spots. Panaspis massaiensis comb. nov. is widespread in the Kenyan and northern Tanzanian highlands, isolated dryland montane forests and rocky hills, while P. tsavoensis sp. nov. occur in the expansive arid lowlands of Tsavo Conservation Area and should be present in similar arid lowlands in northern Kenya as well as in adjacent Tanzania. 


2000 ◽  
Vol 124 (1) ◽  
pp. 47-51 ◽  
Author(s):  
A. JASIR ◽  
A. NOORANI ◽  
A. MIRSALEHIAN ◽  
C. SCHALEN

We examined three populations from the Tehran region and the North part of Iran (Gilan), in all more than 5000 individuals, for carriage of Streptococcus pyogenes (group A streptococci; GAS). Children or adults with acute pharyngotonsillitis and healthy school children harboured GAS in 34·1, 20·0 and 21·0%, respectively. Typing of 421 randomly selected isolates showed a predominance of M-types M4, M5, M11, M12, as well as the provisional type 4245; however, many of the isolates were T and M non-typable. Forty-three percent of all strains were opacity factor (OF) negative. The type distribution differed markedly from that reported in 1973–4, when M types 1 and 12 were predominant.


1869 ◽  
Vol 6 (58) ◽  
pp. 167-173
Author(s):  
Henry Alleyne Nicholson

In the former portion of this paper, the Tipper or south-eastern boundary of the Skiddaw Slates, in their main area, had been traced from Troutbeck, on the N.E., as far as the head of Buttermere, onthe S.W. From this point (i.e. the north-western end of Honister Crag), the Skiddaw Slates can be traced for a very short distance across Warnscales Bottom. They are still overlaid by the felspathic trap and succeeding band of slates and breccias, which together compose Fleetwith Pike and the S.E. end of Honister Crag, and the relations between the two formations are the same as in the Gatescarth Valley. When however the pass of Scarf Gap on the south-west of Warnscales is reached, the Skiddaw Slates have disappeared and the base of the Green Slate Series now rests upon a great mass ofiatrusive felstone-porphyry (here almost a true syenite) which forms High Crag and High Stile. Though the Skiddaw Slates are absent here, it is interesting to observe that the stratification of the Green Slate Series can be particularly well made out in this region. The rugged hills to the S.E. of Scarf Gap are occupied by a prolongation of the great slaty band of Honister, but the beds have now to a great extent lost their former character, and have assumed very much the mineral aspect of trap, from which however they are easily distinguished by the fact that the bedding, in spite of a rough but well marked cleavage, is unusually distinct. The strata displayed in a number of magnificently moutonné'd crags and bosses, in which they are seen to undulate repeatedly, forming a series of small but well-preserved anticlinals and synclinals, the dips of which are N.N.W. and S.S.E. at angles of from 25° to 35°. The inclination therefore of these beds is only about half as high as that of the Skiddaw Slates in the Gatescarth Valley.


2020 ◽  
Vol 15 (4) ◽  
Author(s):  
S.V. Ryzhkova ◽  
◽  
E.V. Ponomareva ◽  
A.G. Zamiraylova ◽  
◽  
...  

For the South-Eastern regions of the West Siberian oil and gas province, a model of the structure of the Bazhenov reservoir and criteria for selecting areas that are promising for detecting oil accumulations in the productive level of the South-West Bazhenov Formation are proposed. According to the our criteria, the following characteristics of the object of research are given: the thickness of rocks of the Bazhenov Formation, the thickness of rocks with a Corg content > 7%, catagenesis degree of organic matter, the thickness of the underlying and overlying fluid barriers, current reservoir temperatures of rocks and reservoir pressures in the Bazhenov Formation. Based on a comprehensive analysis of the materials that characterize the above criteria, promising zones of two categories are identified. The Central-Nyurol zone is assigned to the 1st category (the most promising), and the North-Nyurol, East-Nyurol, South-Nyurol, West-Parabel, and Ust-Tym zones are assigned to the 2nd category.


2011 ◽  
Vol 80 (3) ◽  
pp. 237-244
Author(s):  
Agnieszka Nobis ◽  
Marcin Nobis ◽  
Alina Urbisz

<em>Lathyrus aphaca</em>, which is in Poland considered to be an ephemerophyte recorded mainly in the north-west and the south-west, has lately been observed in arable fields in the south of the country. Recent and historical data on the distribution of the taxon in Poland are presented. Original relevés conducted in arable fields in Poland are analysed and compared to those from the Czech Republic, Germany and Slovenia. The current status of <em>L. aphaca </em>in the Polish flora is discussed.


2021 ◽  
pp. 17-24
Author(s):  
Anil Kyadampure ◽  
N.D. Vagshette ◽  
M.K. Patil

We present results based on analysis of the currently available 29.86 ks Chandra data on the Bright Group-Centered Galaxy (BGG) NGC 5846 of G50 group. A pair of X-ray cavities have been detected within a radius ? 1 kpc along the North-East and South-West directions. The analysis yielded the average cavity energy, ages and mechanical power equal to ~ 3:1 x 1048 erg, 0:61 x 107 yr and, 3:78 x 1041 erg s-1, respectively. The luminosity of X-ray emitting gas within the cooling radius (20 kpc) was found to be 2.4 x 1041 erg s??1, in agreement with the mechanical cavity power. The ratio of radio luminosity to mechanical cavity power is found to be 10??4. The Bondi accretion rate of the central supermassive black hole (SMBH) is ~ 5:95 x 10-5 M? yr-1 and the black-hole mass derived using the Bondi-accretion rate was found to be ~ 3:74 x 108 M?.


1903 ◽  
Vol 10 (2) ◽  
pp. 84-85
Author(s):  
Samuel Moore

In the Summer of 1901 I found in a pasture, between Oxlow Rake and Cop Round (IX S.E.), some blocks of Toadstone in a bed of clay that has all the characteristics of decomposed Toad-stone. The clay was being dug for puddling a new mere, and the deposit is well known to natives. I traced the outcrop south-west to Starvehouse Mine, and my inference that the clay was decomposed Toadstone was soon verified by the Toadstone itself coming to day-light and replacing the clay. I did nothing more that year, but in the Summer of last year I continued to follow the bed, and have traced it as far as Bushy Heath House (XV N.E.), a distance of about two miles from its starting-point.The outcrop starts as a clay bed, at the southern end of an enclosure called Old Moor (IX S.E.), at a point about 50 yards south-east of two old mine shafts, and where a spring issues from under the limestone scarp, at a height of 1,400 feet above mean sea-level (by aneroid). Thence it runs in a general south-west direction for half a mile, along a line of five springs at the base of the limestone escarpment, to the north wall of Starvehouse Mine (IX S.E.), which it cuts at an altitude of 1,500 feet.There is no throw at the Starvehouse lode, and the bed contours round the point of Cop Round and crosses Dick Lane 30 yards from the summit gate (1,510 feet); from there it runs south-east with the dip of the limestone to Moss Rake (IX S.E.), the base passing just above the letter n of Piece Barn on the map. It reaches the lode at 1,350 feet.


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