Relevant bibliographies by topics / Dniester

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Dniester'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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Journal articles on the topic "Dniester"

1

Adamenko, Оleg. "Causes and consequences of floods in the Dniester valley." Visnyk of the Lviv University. Series Geography, no. 48 (December 23, 2014): 141–49. http://dx.doi.org/10.30970/vgg.2014.48.1302.

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Catastrophic floods in r. Dniester led to the creation of the Dniester engineering and ecological flood polygon-model sites in the Dniester within the Galician and Tysmenytsia areas centered on the village Mariyampil Galician region. Based on comprehensive studies of the Dniester area flood polygon possible to develop effective measures to prevent and reduce the negative effects of catastrophic floods and improve environmental security in the region. Key words: flood, flood Dniester ground, geoecological research.
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Yatsyshyn, Andriy, and Piotr Gębica. "STUDY OF THE HOLOCENE STAGE OF FORMATION OF THE DNIESTER VALLEY IN THE EASTERN CARPATHIAN FORELAND." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 11(01) (December 2020): 118–39. http://dx.doi.org/10.30970/gpc.2020.1.3204.

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The article describes the main stages of studying of the floodplain and the first floodplain terrace of the Dniester river within the Eastern Carpathian Foreland fragment of the valley, and evaluates the results of existing studies. It is discovered that during all the stages of the research morphological and morphometric parameters of the floodplain and the first floodplain terrace of the Dniester river, morphology and facie structures of the alluvial accumulations, as well as palynological analyses of biogenic accumulations buried in an alluvial series are performed. The results obtained during the palynological analyzes are used to date the erosion-accumulation cycles and to reconstruct the physical-geographical conditions of the time of the floodplain and the first floodplain formation of the Dniester terrace. The radiocarbon dating of biogenic sediments buried in alluvial series is also actively conducted at the last stage of the research. The array of geological and geomorphological information collected at the first two stages of research made it possible to establish that, first, the first floodplain terrace and floodplain were formed during the Holocene in the Dniester Valley. The first floodplain terrace (the height of which reaches 4–6 m above the Dniester riverbed) can be considered as a high floodplain which is often covered by high floods. The terrace is accumulative, but unlike all other terraces of the Dniester it is devoid of the loess cover. In the cross-sections of its accumulations the deposits of the alluvium of the channel facies builted of pebbles are exposed and covered with the alluvium of the floodplain facies composed of sands, sandy loams and loams. The total thickness of alluvium reaches 9–10 m and it doesn’t varysignificantly downstream of the Dniester. Except the Upper Dniester basin, where the thickness of the alluvium increases to 10–18 m, and the layers of peat are found. The floodplain is 4–5 m above the Dniester riverbed and is built of alluvium of the channel facies, dominated by sand and pebble series. In someplaces floodplain is covered with sandy or loamy deposits of floodplain facies. Secondly, in the Eastern Carpathian Foreland part of the Dniester valley the course of fluvial morpholitogenetic processes was regulated not only by climatic changes and neotectonic movements, but also by human economic activity. During the XIX–XX centuries especially large-scale human influence was on the Dniester riverbeds by construction of flood ramparts, reclamation canals, etc. The results of recent geomorphological research conducted within the studied fragment of the river valley particularly palynological and radiocarbon dating have significantly improved the idea of morphology, structure and history of floodplain formation and the first floodplain terrace of the Dniester. The research revealed that the accumulation of alluvium of the first floodplain terrace which is above the Dniester riverbed reaches 5,5–6,5 (7) m and started to develop in the late Pleistocene (Bølling–Allerød interstadial) (13 000–11 000 years ago (GI–1)). Presumably in the early Dryas (11 000–10 000 years ago (GS–1)), the first floodplain terrace was dissected by the meandering channel of the Dniester. The alluvial deposits that fill these large paleomeanders are still well preserved and are often exposed in the ledges of the first terrace. The further development of the floodplain and first floodplain terrace of the Dniester river was taking place in several stages such as the end of the boreal, the beginning of the atlantic, the end of the atlantic, subboreal, the beginning of the subatlantic, as well as during V–VI, X–XII and XIV–XVI centuries. These stages are identified in correlation with the cycles of humidification of the climate and the growth of fluvial activity of riverbeds (flood phases). As a result of the intensification of erosion-accumulation activity of the Dniester the two – three levels of Holocene floodplain were formed up to 4–5 m and 3–4 m high. The first traces of human activity within the studied fragment of the Dniester valley were dated by subboreal and recorded by the presence of grain pollen in the spore-pollen diagrams of Mainych (Upper Dniester Basin) and Tsvitova (Galician-Bukachiv Basin) sections. Key words: Dniester valley; floodplain; the first floodplain terrace; alluvium; phases of floods; Allerød; early Dryas; Holocene.
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Gazyetov, Ye І., V. І. Medinets, S. M. Snigirov, N. V. Kovaleva, and S. V. Medinets. "HYDROLOGICAL CHARACTERISTICS OF THE DNIESTER ESTUARY BY SURVEYS IN THE SUMMER’S OF 2003–2019." Odesa National University Herald. Geography and Geology 26, no. 1(38) (September 4, 2021): 28–42. http://dx.doi.org/10.18524/2303-9914.2021.1(38).234645.

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Problem Statement and Purpose. The Lower Dniester delta and the Dniester estuary are very important because they are natural filters of the river water from pollution and suspended matter, as well as they are the habitat of a large number species of flora and fauna. The construction of reservoirs on the Dniester River in past completely changed the hydrological regime of the river itself and of the Dniester estuary. For these reasons a constant environmental monitoring of the aquatic environment are required. Since 2002 Odessa I. I. Mechnikov National University has been carrying out a wide range of environmental studies in the Dniester estuary, one of aspects of which is observation of hydrological characteristics. The purpose of this paper is to study long-term changes in transparency, temperature and electrical conductivity of the Dniester estuary water in the summer periods of 2003–2019. Materials & Methods. Measurements of transparency, temperature and electrical conductivity of water in the Dniester estuary in the indicated years were carried out according to standard methods at 19 ecological stations. Statistical processing, analysis and mapping of the measurements results were conducted in EXCEL, ARCGIS, SURFER software’s. Data analysis was based on a graphical representation of the spatial distribution of characteristics, as well as by identifying the features of long-term changes in these characteristics. Main Results and Conclusions. On the basis of the summer surveys during 2003–2019 more than double decrease of water transparency mean values in the Dniester estuary has been established. It was found that the maximum transparency values were observed in the central parts of the estuary, far from settlements. For theseyears, an increase of the mean water temperature for the estuary northern part and its decrease in the middle and southern parts has been recorded. Also, for the summer period of these years, an increase of the mean water electrical conductivity in all parts of the estuary was established. The established features of spatial distribution of hydrological characteristics indicate to the river runoff, intrusion of seawater into the estuary, and wind activity as the determining factors in formation of the estuary hydrological regime. Recorded long-term trends of the means transparency values decreasing and the means temperature and electrical conductivity increasing of the Dniester estuary water in the summer of 2003–2019 are considered as consequences of the river discharge decreasing due to long-term climatic changes over Europe and man regulation of river flow.
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Tomeniuk, O. "Yuriy Polians’kyi as a researcher of terraces of Dniester river." Visnyk of the Lviv University. Series Geography, no. 38 (December 15, 2010): 340–56. http://dx.doi.org/10.30970/vgg.2010.38.2287.

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Yuriy Polians’kyi’s contribution to the investigation of geologic and geomorphologic structure of Dniester River on the basis of detailed analysis of his scientific publications was characterized. Works of the scientists who were the predecessors and the successors of Yuriy Polians’kyi in the field of study of terraces of Upper and Middle currents of Dniester River also was analyzed. The principal achievements of Yuriy Polians’kyi that have got the further development in present geomorphology were corroborated at the article. Key words: floodplain terrace, alluvium, Pleistocene, relative elevation, geological and geomorphological researches, Dniester, Podillya.
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A. Chebanova, Lydia, Lyudmila A. Novikova, Lyudmila K. Ushakova, and Irina A. Karnilovi. "Migration Processes in the Trans-Dniester Region of the Republic of Moldova and Their Impact on the Socio-Economic Situation." International Journal of Engineering & Technology 7, no. 3.15 (August 13, 2018): 226. http://dx.doi.org/10.14419/ijet.v7i3.15.18677.

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The purpose of the study is revealing the content and causes of migration processes in Trans-Dniester Region and their impact on the socio-economic situation in the region. From this perspective the main objectives of the study consisted in disclosing the reasons of considerable population outflow over the past two decades, the study of the peculiarities of different forms of migration in Trans-Dniester Region, identifying trends in migration of population, regulation of the migration mechanism at the present stage, the assessment of the current system of migration flows accounting in Trans-Dniester Region and the definition of its optimization directions. Particular attention is paid to the consideration of the migration scale and the main areas of emigration. The loss of immigration attractiveness of the region and outflow of highly qualified young and active population from Trans-Dniester Region causes a steady reduction in the population, creates a significant imbalance in the demographic structure of the population (in terms of age and profession). Besides, the Trans-Dniester Region turned out to be actively involved in migration processes due to its relative geographical proximity to both Russia and the EU countries. Currently, the predominant role is played by labor migration.
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Brusak, Vitaliy, and Sofia Paljanycja. "Non-living nature monuments of Halych-Dniester region: state of protection and perspectives of geotouristic application." Visnyk of the Lviv University. Series Geography, no. 47 (November 27, 2014): 30–41. http://dx.doi.org/10.30970/vgg.2014.47.814.

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The list of non-living nature geological, geomorphological, hydrological monuments of Halych National Park in Halych-Dniester region is submitted in this article and its current state of protection is characterized. The opportunities of application of non-living nature monuments in recreation and tourism activities of Halych National Park are analyzed. The network of one-day and multi-day geotouristic trails are developed. The perspectives of creation of National geopark “Halych-Dniester region” are regarded. Key words: monuments of non-living nature, geological, geomorphological and hydrological monuments of nature, geotouristic trails, National geopark, Halych-Dniester region, Halych National Park.
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Bosatikova, Nadezhda. "Summer in the Trans-Dniester." Index on Censorship 22, no. 4 (April 1993): 16–18. http://dx.doi.org/10.1080/03064229308535542.

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Kravchuk, Yaroslav, and Yuriy Zinko. "STEPAN RUDNITSKY'S STUDIES OF THE PODILLYA RELIEF: ITS MORPHOLOGY, GENESIS AND HISTORY OF DEVELOPMENT." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 3–20. http://dx.doi.org/10.30970/gpc.2019.1.2796.

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S. Rudnitsky’s research continued in Podillya; he went on studying the morphology of genesis and history of the relief of the Carpathian and pre-Carpathian Dniester basins. Many years of expeditionary research (1903-1912) resulted in the monograph “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester”, which was recommended for publication at the meeting of the Mathematical & Nature Descriptive section of the Shevchenko Scientific society (NTSh) on April 17, 1912. This work provides detailed morphographic and morphometric characteristics of the Galician Podillya relief. The monograph also reports on the formation of the Dniester basin river system, geological structure, paleogeomorphology, as well as morphological & genetic problems. In studying the Podilsky Dniester Basin, S. Rudnytsky made numerous conclusions on the problems of morphological regionalization, the relief history, in particular the formation of the Dniester valley and its Podilsky tributaries, which have not lost their relevance to this day. We can distinguish the following major points among the main findings of S. Rudnitsky's research of morphogenesis and the evolution of the Podilsky Dniester basin relief: (1) Geomorphological division of the Galician Podillya with districts allocation: Roztochya, Vereshchytsky-Shchyrets lowland, Mykolayiv-Bobretskyi “horbovyna” (land surface with hills) (Pidopillya), Opilsky “horbovyna”, Podnistriya, Podillya and Gogoloro-Kremenetsk Ridge; (2) Clarification of the history of individual regions development: the erratic Scandinavian material in Roztochya is mixed (Scandinavian-Carpathian); it is deposited by fluvia-glacial flows and represented up to altitudes of 380 m; (3) In the periglacial Pleistocene period, almost all the sands of the main areas had eolian processes; (4) Confirmation of the Podillya geological division into western and eastern with five morphological bands, proposed by W. Teisseyre; (5) Justification of the morphotectonic scheme of Podillya development, connected with tectonic elevations of the Hologoro-Kremenets Ridge, which caused the current inclination of the Podolsk hills to Southeast-East; (6) Statement that the tectonic lines of Berdo-Nârul and Kovalivka-Smykivtsi characterize the Paleozoic Platform of Podillya as a typical tectonic horst; (7) Detailed description of the Dniester “rinyshcha” (alluvial deposits) with the Carpathian material present in Podniester, Opil and Podillya itself, which are present as a strip at a distance of 14-20 km from the modern Dniester river bed; (8) Based on literary sources and his own research, the scientist came to the conclusion that there is “eolian” loess in the “rinyshcha”, sands and alluvial clay; (9) It is argued that the old Nadnistryan rivers cannot be older than the planation surfaces of the Carpathians and Pre-Carpathians; (10) Formation of the Dniester valley pattern in Pliocene and Pleistocene, which determined the direction of the flows of the left tributaries and their capture by the Western (Zakhidny) Bug river sources. Finally, in his “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester” S. Rudnitsky managed to use a complex morphogenetic approach to studying the region relief for the first time geomorphological literature: from standardized morphological descriptions through systematization of the morphological structure of the region to the historical genetic interpretation of the main features of relief morphology. Key words: morphological districts; Dniester catchment area (basin); Naddnistriansky “rinyshcha” (alluvial deposits); glacial erratic material; fluvia-glacial deposits; free and entrenched meanders; “horbovyna” (land surface with hills); Podillya.
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Jacyshyn, A. "The principal stages high pliocene and low pleistocene morpho and lithogenesis of the Dniester basin in the Halician Dniester region." Visnyk of the Lviv University. Series Geography, no. 38 (December 15, 2010): 379–94. http://dx.doi.org/10.30970/vgg.2010.38.2290.

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The principal stages of high Pliocene and low Pleistocene history of the Dniester basin development in Halicia and Ivano-Frankivsk region on the basis of the detailed morphological, morphometric analysis of the Dniester terraces as well as its Carpathian streams and the analysis of cut terraces. The fundamental geomorphological research of Loyeva, Krasna rivers levels has been done and some determined provisions about their structure, development and time of formation were defined. Paleogeographic events are related with the stages of isotopic-oxygen scale, paleomagnetic rappers, stratigraphic horizons of loess and soil series of the Halician Dniester region. Key words: level of Krasna river, level of Loyeva river, terrace, isotopic-oxygen stage, tectonic raising, erosive cutting, alluvium accumulation.
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Yatsyshyn, Andriy, Maciej Bąbe, Danuta Olszewska-Nejbert, Andriy Bogucki, and Kateryna Dran. "Lithological characteristics of the alluvium of the seventh terrace of the Dniester River in the Kunysivtsi and Ivane-Puste sections (Podillia-Dniester region)." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 367–78. http://dx.doi.org/10.30970/vgg.2013.42.1897.

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The main lithological characteristics of the sands, gravels and pebbly deposits in the particular layers of the seventh terrace of the Dniester River in the investigated part of its Podillian valley have been analyzed. The texture and the granulometrical and petrographical composition of the sands, gravels and pebbly materials has been described, including the roundness of the grains and some other features. The conditions of sedimentation of the alluvial sands, gravels and pebbly deposits of the seventh terrace of the Dniester River have been reconstructed and direction of the palaeo-Dniester flow and some other features interpreted. Key words: terraces over the canyon, alluvium, granulometrical composition, petrographical composition, sandstone, aleurolite, quartz, siliceous rocks, roundness.
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Dissertations / Theses on the topic "Dniester"

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Varzari, Alexander. "Population History of the Dniester-Carpathians: evidence from Alu insertion and Y-chromosome polymorphisms." Diss., [S.l.] : [s.n.], 2006. http://edoc.ub.uni-muenchen.de/archive/00005868.

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Marinuta, Vitalie Nicon. "Evolution of Transdniestrian conflict in the Republic of Moldova: prospects for its solution." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2004. http://library.nps.navy.mil/uhtbin/hyperion/04Jun%5FMarinuta.pdf.

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Thesis (M.A. in International Security and Civil-Military Relations)--Naval Postgraduate School, June 2004.
Thesis advisor(s): Jessica Piombo, Anne Clunan. Includes bibliographical references (p. 117-124). Also available online.
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Mija, Valeriu. "A solution to Moldova's Transdniestrian conflict : regional complex interdependence /." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Jun%5FMija.pdf.

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Thesis (M.A. in International Security and Civil-Military Relations)--Naval Postgraduate School, June 2003.
Thesis advisor(s): Jeff Knopf, Mikhail Tsypkin. Includes bibliographical references (p. 77-85). Also available online.
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Raileanu, Victoria. "Les figures de la propagande : le temps, l'espace et le héros dans le documentaire historique produit à la télévision de la République soviétique socialiste moldave (1961-1989)." Thesis, Université Laval, 2013. http://www.theses.ulaval.ca/2013/29812/29812.pdf.

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Cette thèse a pour objet les significations produites par la propagande soviétique au moyen du documentaire historique réalisé entre les années 1960 et 1980 à la station de télévision de la République Soviétique Socialiste Moldave. À partir d’un corpus de base de 32 documentaires, la thèse vise trois types de représentations filmiques investies d’une forte connotation idéologique : les figures du temps historique, les métaphores de l’espace et l’image du héros soviétique. Nous considérons également les représentations connexes qui constituent le contexte narratif et filmique des trois catégories principales d’images de manière à révéler le réseau entier de significations de l’idéologie soviétique. Notre étude s’inscrit dans la lignée des études des sociétés communistes en même temps qu’elle appartient au domaine théorique de l’histoire de l’imaginaire et des idées. Elle répond à une triple problématique. Premièrement, elle explique la portée et les usages politiques et idéologiques des représentations véhiculées par la propagande télévisée. La recherche rend compte des objectifs et des stratégies propagandistes en Moldavie, alors en cours de soviétisation. Elle révèle notamment les normes officielles de représentation, leurs variations à la suite des changements politiques et dresse un inventaire des moyens discursifs mis en œuvre dans l’élaboration des symboles clés de la propagande de Parti. Ensuite, la recherche montre les différents degrés d’implication des cinéastes et des historiens dans la construction des codes de l’idéologie soviétique. Elle cerne les rapports entre le pouvoir soviétique et les intellectuels, contraints d’être des idéologues et des propagandistes professionnels. L’étude constate une tendance épisodique parmi les producteurs culturels à échapper au registre propagandiste afin d’exprimer une vision hétérodoxe. Enfin, nous sondons l’ancrage des représentations propagandistes dans les structures durables de l’imaginaire. La recherche puise ses données empiriques dans la presse soviétique écrite, dans des documents d’archives visant le fonctionnement institutionnel de la télévision moldave, et dans une série de 16 entretiens de cinéastes et de responsables administratifs et idéologiques. Elle recourt à une ample contextualisation historique afin de montrer l’évolution des structures archétypales à travers les différents systèmes de représentations et leur adaptation aux réalités culturelles changeantes.
The work presented in this thesis investigates the contents of Soviet propaganda as it appeared in historical documentaries produced from 1960 through 1990 by the local television broadcaster of the Moldavian Soviet Socialist Republic. From a base corpus containing 36 documentaries, it centers itself on three types of filmic representations with high ideological connotation: the figures of historic time, the metaphors of space and the soviet hero's image. It also considers the related representations that create the narrative and cinematic context of the three main categories of images in order to reveal the entire network of meanings of Soviet ideology. Our study falls in line with soviet studies research while also belonging to the theoretical field of the history of imagination and ideas. It addresses three problems. First, it reveals the scope and the political and ideological purpose of the representations conveyed by television propaganda. The research reflects the objectives and strategies of official propaganda in Moldova, a territory under sovietization. It unearths the official standards of representation, their variations due to political changes and makes an inventory of discursive means used in the development of the key symbols of Party propaganda. Second, the research shows the different degrees of involvement of filmmakers and historians in the construction of the codes of Soviet ideology. It identifies the relationships between Soviet power and intellectuals, reduced to the rank of ideologists and professional propagandists. The study finds an occasional tendency among cultural producers to escape the mandatory propagandist registry and express an unorthodox view. Finally, we survey the rooting of propagandist representations in the lasting structures of the imagination. The research draws its empirical data from Soviet print media, from archive documents related to the institutional inner workings of Moldovan television, and from a series of 16 interviews with filmmakers and administrative and ideological executives. It makes use of the long historical detour to show the evolution of archetypal structures across various systems of representation and their adaptation to changing cultural realities.
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Varzari, Alexander [Verfasser]. "Population history of the Dniester-Carpathians : evidence from Alu insertion and Y-chromosome polymorphisms / vorgelegt von Alexander Varzari." 2006. http://d-nb.info/981561349/34.

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Books on the topic "Dniester"

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Dailey, Erika. Human rights in Moldova: The turbulent Dniester. New York, N.Y: Helsinki Watch, 1993.

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John, Philipps. The Germans by the Black Sea between the Bug and Dniester rivers. Fargo, N.D: Germans from Russia Heritage Collection, North Dakota State University Libraries, 2000.

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Azyl nad Dniestrem. Warszawa: Wydawn. Ministerstwa obrony narodowej, 1986.

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Externe, Romania Ministerul Afacerilor, Romania Securitatea, and Institutul de Istorie "George Bariț" din Cluj-Napoca, eds. Chestiunea refugiaților depeste Nistru: Documente diplomatice și ale servicilor române de informații, 1919-1936 = The question of the refugees across the Dniester in diplomatic and Romanian intelligence documents, 1919-1936. Cluj-Napoca: Argonaut, 2011.

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Chirica, Vasile. Gisements du paléolithique supérieur ancien entre le Dniestr et la Tissa. Iași: Ed. Helios, 1996.

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Sulgostowska, Zofia. Prahistoria międzyrzecza Wisły, Niemna i Dniestru u schyłku plejstocenu. Warszawa: Państwowe Wydawn. Nauk., 1989.

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Sulgostowska, Zofia. Prahistoria międzyrzecha Wisły, Niemna i Dniestru u schyłku plejstocenu. Warszawa: Państwowe Wydawn. Nauk, 1989.

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Stempowski, Jerzy. W dolinie Dniestru i inne eseje ukraińskie ; Listy o Ukrainie. Warszawa: LNB, 1993.

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Stempowski, Jerzy. W doline Dniestru i inne eseje ukraińskie ; Listy o Ukrainie. Warszawa: LNB, 1991.

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Grodziski, Stanisław. Wzdłuż Wisły, Dniestru i Zbrucza: Wędrówki po Galicji dyliżansem, koleją, samochodem. Kraków: Grell, 1998.

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Book chapters on the topic "Dniester"

1

Shulyarenko, A., M. Yatsyuk, and L. Shulyarenko. "Causes and Peculiarities of Recent Floods on the Dniester River." In Flood Issues in Contemporary Water Management, 95–100. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4140-6_10.

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Jeleapov, Ana, Orest Melniciuc, and Iurie Bejan. "Assessment of Flood Risk Areas in the Dniester River Basin (in the Limits of the Republic of Moldova)." In Water Science and Technology Library, 157–73. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-02708-1_8.

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Markova, Anastasia K. "A New Early Middle Pleistocene Locality of Small Mammals (Lower Dniester River) and its Position in the Early Middle Pleistocene Sequence." In Springer Geology, 1017–18. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_193.

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Mudrovska, I. V., I. E. Merkushin, A. A. Lysenko, and A. B. Bobrov. "The Savran ore field of the Dniestr-Boug domain, Ukrainian Shield: A rare example of Paleoproterozoic (ca 2 Ga) orogenic gold mineralization related to retrogressive alteration of Archaean (> 3 Ga) granulite-facies host rock." In Mineral Deposit Research: Meeting the Global Challenge, 1021–24. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_261.

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Filippov, V., I. Shestakov, and V. Kharchenko. "Dniester Notebook." In Lecture Notes in Pure and Applied Mathematics, 461–516. Chapman and Hall/CRC, 2006. http://dx.doi.org/10.1201/9781420003451.axb.

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"Bug/Dniester." In Encyclopedic Dictionary of Archaeology, 204. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_20725.

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"Bug-Dniester." In Encyclopedic Dictionary of Archaeology, 204. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_20724.

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Demediuk, Mykola S., and Yuriy N. Demediuk. "Lithological characteristics of the Dniester Glacial Complex deposits in the Carpathian Foredeep." In Glacial Deposits in North-East Europe, 221–24. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077695-32.

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"Chapter Two. The Political History Of The Carpathian-Dniester Region And Of The Neighbouring Territories." In The Romanians and the Turkic Nomads North of the Danube Delta from the Tenth to the Mid-Thirteenth Century, 47–175. BRILL, 2009. http://dx.doi.org/10.1163/ej.9789004175365.i-482.8.

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BRAUND, DAVID. "Greater Olbia: Ethnic, Religious, Economic, and Political Interactions in the Region of Olbia, c.600-100 bc." In Classical Olbia and the Scythian World. British Academy, 2007. http://dx.doi.org/10.5871/bacad/9780197264041.003.0005.

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This chapter discusses the ethnic, religious, economic and political interactions of Olbia with other communities during the 600–100 century BC. It focuses on the various relationship of the Greater Olbia with both Greeks and non-Greeks. Greater Olbia pertains to Olbia's mini-empire in the northwest Black Sea and spans across the estuary of the lower Bug, the lower Dnieper, the north-west Crimea, the outer estuary of Dnepier or Hylaea, the Berezan, the island of Lueke, and the settlements along Dniester. Greater Olbia was largely dependent on the maintenance of broadly symbiotic relationships with non-Greeks. These relationships and interactions with other non-Greek communities are reflected in the existence of a rich mix of traditional Greek and barbarian names in the personal names of Greeks. However distinct and Greek the Olbiopolitans may have perceived themselves, they were subjected to extensive cultural osmosis between Greeks and non-Greeks in and around the city. This osmosis and symbiosis can be seen in the religion, the pottery, the names and other aspects of the Olbiopolitan living such as the observation of Dio Chrysostom where he made note of a young Olbiopolitan cavalryman in a garb of a barbarian yet with his head full of Achilles.
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Conference papers on the topic "Dniester"

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Sandu, Maria, Anatolie Tarita, Raisa Lozan, Elena Mosanu, Sergiu Turcan, and Tatiana Goreacioc. "Indicele de nitrificare a ionilor de amoniu în apele din fluviul Nistru." In Provocări şi tendinţe actuale în cercetarea componentelor naturale şi socio-economice ale ecosistemelor urbane şi rurale. Institute of Ecology and Geography, Republic of Moldova, 2020. http://dx.doi.org/10.53380/9789975891608.30.

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The paper presents the fluctuations of the river Dniester Water Nitrification Index, which denotes that downstream of Naslavcea village the nitrification process is intensely (98%), similar to that calculated according information of 2016-2019 years, and towards Palanca village is of 72-79%. Initrif of river Dniester water has a negative correlates with COD-Cr and BOD5, being evidenced the influence on the nitrification process of chemical and biochemical degradable substances, which is attes
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Malyukevitch, Alexander, and Sergey Agulnikov. "Barrow necropolis of the Dniester Right Bank." In ANCIENT NECROPOLISES — FUNERAL AND MEMORIAL RITUALISM, ARCHITECTURE AND PLANNING OF NECROPOLISES. Institute for the History of Material Culture Russian Academy of Sciences, 2018. http://dx.doi.org/10.31600/978-5-93572-816-8-86-91.

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Sirodoev, Ghenadie, and Efrem Mitul. "The typology of water body delineation in the Prut river basin (Moldova)." In Starea actuală a componentelor de mediu. Institute of Ecology and Geography, Republic of Moldova, 2019. http://dx.doi.org/10.53380/9789975315593.10.

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Jeleapov, Ana, and Daniela Burduja. "Resursele de apă ale râurilor din Regiunea de Dezvoltare Nord." In Provocări şi tendinţe actuale în cercetarea componentelor naturale şi socio-economice ale ecosistemelor urbane şi rurale. Institute of Ecology and Geography, Republic of Moldova, 2020. http://dx.doi.org/10.53380/9789975891608.12.

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The research is dedicated to assessment of rivers and their resources from the North Development Region of the Republic of Moldova. Main methods used in the study are the statistical ones utilized for estimation of main hydrological characteristics, monitored at gauging stations of national monitoring network. Also, GIS technologies were applied in order to evaluate main rivers characteristics and to perform spatial representation of the area. Main rivers of the pilot area are the Dniester and the Prut transboundary rivers. Analysis of their time series shows that flow is slowly decreasing. The measurements of the flow of main tributaries of the Dniester and Prut rivers show a flow slow increase in the northern part and a slow decrease in the southern part of the region. These rivers do not represent big economic value in comparison with large rivers and groundwater resources.
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Bubniak, A. M., I. M. Bubniak, and A. I. Zyhar. "Lineaments analysis of the Dniester area (between Bakota and Novodnistrovsk)." In Geoinformatics: Theoretical and Applied Aspects 2020. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.2020geo110.

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Topal, Denis. "Patterns of kurgan landscape between Dniester, Prut and Danube rivers." In Antiquities of East Europe, South Asia and South Siberia in the context of connections and interactions within the Eurasian cultural space (new data and concepts). Institute for the History of Material Culture Russian Academy of Sciences, 2019. http://dx.doi.org/10.31600/978-5-907053-35-9-29-32.

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Telnov, N. "CHOBRUCHY CROSSING ON THE DNIESTER IN THE LIGHT OF ARCHAEOLOGICAL AND HISTORICAL SOURCES." In Man and Nature. Socio-natural interaction in the world-historical process. LLC MAKS Press, 2020. http://dx.doi.org/10.29003/m1976.s-n_history_2020_43/264-270.

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Medinets, S., A. Mileva, S. Kotogura, I. Gruzova, N. Kovalova, O. Konareva, E. Cherkez, et al. "Rates of atmospheric nitrogen deposition to agricultural and natural lands within the Lower Dniester catchment." In XIV International Scientific Conference “Monitoring of Geological Processes and Ecological Condition of the Environment”. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202056053.

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Medinets, V., T. Pavlik, Ye Gazyetov, S. Medinets, N. Kovalova, E. Cherkez, and T. Kozlova. "Use of Landsat Space Images to Assess Wildfire Areas in the Dniester Delta in 2010-2020." In XIV International Scientific Conference “Monitoring of Geological Processes and Ecological Condition of the Environment”. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202056025.

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Salyha, V., and L. Davybida. "Regional Assessment of Groundwater Resources within the Dniester Basin Based on the Mathematical Modeling and Geoinformation Approach." In Geoinformatics. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.20215521068.

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