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Статті в журналах з теми "Karsts – Turkey":

1

Sağır, Çağdaş, Bedri Kurtuluş, and Moumtaz Razack. "Hydrodynamic Characterization of Mugla Karst Aquifer Using Correlation and Spectral Analyses on the Rainfall and Springs Water-Level Time Series." Water 12, no. 1 (December 25, 2019): 85. http://dx.doi.org/10.3390/w12010085.

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Karst aquifers have been an important research topic for hydrologists for years. Due to their high storage capacity, karst aquifers are an important source of water for the environment. On the other hand, it is safety-critical because of its role in floods. Mugla Karst Aquifer (SW, Turkey) is the only major water-bearing formation in the close environs of Mugla city. Flooding in the wet season occurs every year in the recharge plains. The aquifer discharges by the seaside springs in the Akyaka district which is the main touristic point of interest in the area. Non-porous irregular internal structures make the karsts more difficult to study. Therefore, many different methodologies have been developed over the years. In this study, unit hydrograph analysis, correlation and spectral analyses were applied on the rainfall and spring water-level time series data. Although advanced karst formations can be seen on the surface like the sinkholes, it has been revealed that the interior structure is not highly karstified. 100–130 days of regulation time was found. This shows that the Mugla Karst has quite inertial behavior. Yet, the storage of the aquifer system is quite high, and the late infiltration effect caused by alluvium plains was detected. This characterization of the hydrodynamic properties of the Mugla karst system represents an important step to consider the rational exploitation of its water resources in the near future.
2

G., Günay. "Gypsum karst, Sivas, Turkey." Environmental Geology 42, no. 4 (July 1, 2002): 387–98. http://dx.doi.org/10.1007/s00254-002-0532-0.

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3

Özler, Murat. "Karst hydrogeology of Kusluk-Dilmetas karst springs, Van-Eastern Turkey." Environmental Geology 41, no. 3-4 (December 1, 2001): 257–68. http://dx.doi.org/10.1007/s002540100401.

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4

TAYLAN, MEHMET S., CLAUDIO Di RUSSO, MARINA COBOLLI, and Marina Cobolli. "The Dolichopodainae and Troglophilinae cave crickets of Turkey: an update of taxonomy and geographic distribution (Orthoptera, Rhaphidophoridae)." Zootaxa 2829, no. 1 (April 22, 2011): 59. http://dx.doi.org/10.11646/zootaxa.2829.1.3.

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In this note we report a new series of data on Dolichopodainae and Troglophilinae cave crickets of Turkey, after an extensive survey conducted between the years 2006 and 2010 in the main Anatolian cave systems. These new data, including the identifications of some undescribed taxa, are discussed in the framework of climate regions, vegetation and karst distribution of Turkey, contributing to the study of diversity and geographical distribution of Rhaphidophoridae cave crickets from Turkey.
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Gökkaya, Ergin, Francisco Gutiérrez, Mateja Ferk, and Tolga Görüm. "Sinkhole development in the Sivas gypsum karst, Turkey." Geomorphology 386 (August 2021): 107746. http://dx.doi.org/10.1016/j.geomorph.2021.107746.

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6

Ilhan, Aydin, Aynur Bayhar, and Hayrettin Gumusdag. "Investigation of Body Perceptions of Karate Athletes." Pakistan Journal of Medical and Health Sciences 15, no. 7 (July 30, 2021): 2190–92. http://dx.doi.org/10.53350/pjmhs211572190.

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Background: Sports are part of the social life we live in. Sports have an important role in the social, physical, mental and spiritual development of individuals. It has a significant effect on the individual's self-confidence, development of his character, being a social person, development of practical thinking ability, and mental and physical development. One of the ways used for the desired body structure is physical activity. They had the chance to reach a new physical appearance through physical activities. They have a new physical appearance and positive thoughts [1]. Self-perception is positively affected by participation in sports. From this point of view, examining it with different variables causes us to learn various ways to increase the effect of self-concept. Aim: The aim of this study is to examine the relationship between the body perceptions of karate athletes, gender, sport age, and generation levels. Place & Duration: Data was collected in Turkey. Study duration September 2019 to May 2020. Methods: The research group consisted of 303 people between the ages of 12 and 20 who practiced karate in Turkey. Data collection tools 'Personal Information Form' and 'Physical Self-Perception Inventory for Children and Adolescents' scale were used. The relationships between the body perceptions of karate athletes, gender, sport age and generation levels were examined. The obtained data were made according to Shapiro Wilk normality analysis and it was determined that all variables did not show normal distribution. All analyzes were performed non-parametrically Results: The differences in body perceptions of 303 karate athletes in Turkey according to gender, sport age and generation levels were examined in this study, no statistically significant difference was found between the genders, sport ages and generation levels of the participants. Conclusion: There was no significant difference between body perceptions and gender, sport age and generation levels in karate athletes. Keywors: Karate, Body Image, Adolescence
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Demiroglu, Muhterem. "Classification of karst springs for flash-flood-prone areas in western Turkey." Natural Hazards and Earth System Sciences 16, no. 6 (June 27, 2016): 1473–86. http://dx.doi.org/10.5194/nhess-16-1473-2016.

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Abstract. Flash floods are caused by heavy rainfall that has become more frequent. They are more prominent in low-storage karst regions, although karst terrain often acts as a natural flood control particularly when it is bare and dominated by conduits. A study using a hydrogeochemical approach and assessing data from several springs in different carbonate rock in western Turkey has made it possible to classify karst aquifers based on their response to heavy rainfall events. According to this aim, physico-chemical measurements in wet and dry seasons and discharge rates in springs are compared in order to explain aquifer characteristics. Groundwater samples have a pH ranging from 6.3 to 8.9, temperature (T) varying from 7 to 35 °C and electrical conductivity (EC) ranging from 140 to 998 µs cm−1. Groundwater samples with high EC, high T and low dissolved oxygen (DO) represent the deep circulating water, while low EC, low T and high DO are linked to the shallow circulating water. Lower variability between wet and dry seasons reveals that fracture permeability is predominantly controlled by diffuse groundwater flow with low or high storage, and conduit permeability with high storage. However, variability of the physico-chemical characteristics is higher in a conduit permeability with low storage. These types of aquifers with high transfer capability, predominantly controlled by turbulent groundwater flow, affect flash floods.
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Doğan, Uğur, and Sadettin Özel. "Gypsum karst and its evolution east of Hafik (Sivas, Turkey)." Geomorphology 71, no. 3-4 (November 2005): 373–88. http://dx.doi.org/10.1016/j.geomorph.2005.04.009.

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9

Elhatip, H. "The influence of karst features on environmental studies in Turkey." Environmental Geology 31, no. 1-2 (May 26, 1997): 27–33. http://dx.doi.org/10.1007/s002540050160.

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10

Günay, Gültekin, and Petar Milanović. "Karst engineering studies at the Akköprü Reservoir area, southwest of Turkey." Environmental Geology 51, no. 5 (July 28, 2006): 781–85. http://dx.doi.org/10.1007/s00254-006-0395-x.

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Дисертації з теми "Karsts – Turkey":

1

Hay, Anne Persida. "Physical and metaphysical zones of transition : comparative themes in Hittite and Greek Karst landscapes in the Late Bronze and Early Iron ages." Diss., 2021. http://hdl.handle.net/10500/27463.

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English, Afrikaans and Zulu summaries
While there is increasing interest in the effect of landscape on ancient imagination, less attention has been paid to the impact of restless karst hydrology on ancient beliefs. By identifying shared themes, this study compares and contrasts the way Hittites and Aegean people in the Late Bronze and Early Iron Ages reshaped peripheral karst landscapes into physical and imagined transitional zones. Karst geology underpins much of the Aegean and Anatolian landscape, allowing subterranean zones to be visible and accessible above ground via caves, springs, sinking streams, sinkholes and other unusual natural formations. In both cultures, certain dynamic landscapes were considered to be sacred porous points where deities, daemons, heroes and mortals could transit between cosmic realms. Evidence suggests that Hittites and Aegean people interpreted dramatic karst landscapes as liminal thresholds and spaces situated between the world of humans and the world of deities. Part One investigates physical zones of transition via the karst ecosystems of rural sanctuaries. Part Two considers the creative interpretation in myth and iconography of karst phenomena into metaphysical zones of transition. The examples reveal the way in which Hittites and Aegean people built their concept of the sacred on the extraordinary characteristics of karst geology. Numinous karst landscapes provided validity and a familiar reference point for the creation of imagined worlds where mortal and divine could connect.
Vandag is daar toenemende belangstelling in die effek van die landskap op die verbeelding van die mensdom in die oudheid - maar minder aandag word bestee aan die impak van die rustelose karst landskap op die mens se gelowigheid in die oudheid. Deur die identifisering van sekere gemene temas, vergelyk hierdie verhandeling die manier waarop die Hetiete en die Egeïese volkere in die Laat Brons- en vroeë Ystertydperke die omliggende karstlandskap herskep het in fisiese en denkbeeldige oorgangszones. Die Egeïese en Anatoliese landskap bestaan grotendeels uit karst geologie, met tot gevolg dat ondergrondse zones bo die grond sigbaar en toeganklik is in die vorm van grotte, bronne, sinkgate en ander uitsonderlike natuurlike formasies. In beide bogenoemde kulture is sekere landskapstonele beskou as heilige en poreuse punte waar gode, demone, helde en sterwelinge tussen die kosmiese zones kon beweeg. Die getuienis van die tyd suggereer dat die Hetiete en die Egeïese volkere die dramatiese karst landskappe as grense of drempels tussen hulle wêreld en dié van die gode beskou het. Deel Een ondersoek die fisiese oorgangszones deur te kyk na die karst ecostelsels waarin plattelandse heiligdomme hulle bevind het. Deel Twee beskou die kreatiewe gebruik van karst verskynsels as voorstellings van metafisiese oorgangszones in die gekrewe bronne en ikonografie. Die geselekteerde voorbeelde dui aan die manier waarop die Hetiete en Egeïese volke hulle konsepte van heiligdom gebaseer het op die buitengewone verskynsels van karst geologie. Numineuse karst landskappe het hulle idees gestaaf en ‘n bekende verwysingspunt uitgemaak waar die menslike en die goddelike met mekaar in kontak kon kom.
Ngenkathi intshisekelo ekhulayo yethonya lokwakheka komhlaba emcabangweni wasendulo, kunakwe kancane umthelela we-karst hydrology engenazinkolelo ezinkolelweni zasendulo. Ngokukhomba izingqikithi okwabelwana ngazo, lo mqondo uqhathanisa futhi uqhathanise indlela amaHeti nabantu base-Aegean kweLate Bronze kanye ne-Early Iron Ages abuye abuye abumbe kabusha imigwaqo ye-karst yomngcele ibe yizingxenye zesikhashana zomzimba nezicatshangwe. I-Karst geology isekela kakhulu indawo yezwe i-Aegean ne-Anatolian evumela ukuthi izindawo ezingaphansi komhlaba zibonakale futhi zifinyeleleke ngaphezu komhlaba ngemigede, iziphethu, imifudlana ecwilayo, imigodi yokushona nokunye ukwakheka okungokwemvelo okungajwayelekile. Kuwo womabili amasiko izindawo ezithile eziguqukayo zazithathwa njengezindawo ezingcwele zokungena lapho onkulunkulu, amademoni, amaqhawe nabantu abafayo bengadlula phakathi kwezindawo zomhlaba. Ubufakazi bukhombisa ukuthi amaHeti nabantu base-Aegean bahumusha imidwebo emangazayo yekarst njengemikhawulo yemikhawulo nezikhala eziphakathi komhlaba wabantu nezwe lonkulunkulu. Ingxenye yokuqala iphenya izindawo eziguqukayo zomzimba ngokusebenzisa imvelo ye-karst yezindawo ezingcwele zasemakhaya. Ingxenye Yesibili ibheka ukutolikwa kokudala kunganekwane nakwizithonjana zezinto ze-karst kube izingxenye eziguqukayo zenguquko. Izibonelo ziveza indlela abantu abangamaHeti nabantu base- Aegean abawakha ngayo umqondo wabo ongcwele ngezimpawu ezingavamile ze-karst geology. Amathafa amahle we-karst ahlinzeka ngokusebenza kanye nephuzu elijwayelekile lesethenjwa lokwakhiwa kwamazwe acatshangelwe lapho abantu abafayo nabaphezulu bangaxhuma khona.
Biblical and Ancient Studies
M. A. (Ancient Near Eastern Studies)
2

Koçer, Banu Aysu. "Eight Karats of Justice: Analysis of the Grassroots Resistance Movement Against Goldmining in the Villages of Bergama, Turkey." 2007. http://trace.tennessee.edu/utk_graddiss/216.

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This study explores and analyzes the grassroots movement against goldmining in the villages of Bergama, Turkey. The struggle of Bergama villagers started out as a local ecological resistance movement in the early 1990s and gradually transformed into an environmental justice movement with national implications when activists adopted a rights-based discourse by incorporating into their claims the notions of justice, democratic participation, and citizenship rights. Since goldmining investment in Bergama was a manifestation of significant shifts in the global corporate mining industry starting in the 1980s, and of changes in the world political economy, an account of these shifts is presented as the global political-economic background for the grassroots resistance movement in Bergama. This global perspective is complemented by an account of the domestic socio-economic and political context in which the Bergama villagers’ resistance movement unfolded. The study employs two reference frames for the conceptual and theoretical analysis of the Bergama villagers’ movement. The Environmental Justice Movement (EJM) Literature is reviewed for conceptual clues pertaining to the transformation process of the movement under investigation. As the theoretical reference frame, the New Social Movements (NSM) approach to contemporary social movements is employed in an attempt to assess the applicability of this theoretical approach to the resistance movement of Bergama villagers, as well as the EJM in the United States. NSM theories are inadequate in explaining these movements. Based on the weaknesses of the NSM and the similarities identified between the Bergama villagers’ movement and the EJM, I assert that a new approach to theorizing social movements, which takes as its point of departure these similarities, is necessary. I argue that such an approach will guide not only social movement scholars in understanding ecological grassroots movements in the global North and South but also movement activists in their struggle for social change. In contrast, an exclusive focus on the distinctions between the ecological grassroots movements in the global South, on the one hand, and in the North, on the other, based merely on their economic and cultural differences, will be counter-productive in challenging the systemic root causes of ecological problems plaguing the people of the world today.
3

Koçer, Banu Aysu. "Eight karats of justice analysis of the grassroots resistance movement against goldmining in the villages of Bergama, Turkey. /." 2007. http://etd.utk.edu/2007/KocerBanu.pdf.

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Книги з теми "Karsts – Turkey":

1

Yamaç, Ali, Eric Gilli, Ezgi Tok, and Koray Törk. Caves and Karst of Turkey - Vol. 1. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65501-3.

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2

International Symposium and Field Seminar on Karst Waters and Environmental Impacts (5th 1995 Antalya, Turkey). Karst waters & environmental impacts: Proceedings 5th International Symposium and Field Seminar on Karst Waters and Environmental Impacts : Antalya, Turkey, 10-20 September 1995. Rotterdam, Netherlands: A.A. Balkema, 1997.

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3

Hydrogeological processes in karst terranes: Proceedings of the international symposium and field seminar held at Antalya, Turkey, 7-17 October 1990. Wallingford, Oxfordshire: International Association of Hydrological Sciences, 1990.

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4

Back, William, A. Ivan Johnson, and Gultekin Gunay. Series of Proceedings and Reports: Hydrogeological Processes in Karst Terranes -Proceedings of a Symposium and Field Seminar Held at Antalya, Turkey, October 1990 (Series of Proceedings and Reports). IAHS Press, 1993.

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5

Eslick, Christine. Elmali-Karatas V: The Early Bronze Age Pottery of Karatas - Habitation Deposits. Archaeopress, 2009.

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6

Gevorg, Hazěchyan, та Hovsepʻyan Garegin 1867-1952, ред. Ogun chʻapawinelu ardiwnkʻě: Karsi ankumě 1920tʻ Hoktemberi 30-in - Garegin Arkʻ. Hovsēpʻeantsʻi hushagrutʻiwně ev pʻastatʻghtʻer. Erevan: "Azgaynakan" Akumb, 2002.

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Частини книг з теми "Karsts – Turkey":

1

Yamaç, Ali, Eric Gilli, Ezgi Tok, and Koray Törk. "Speleology in Turkey." In Caves and Karst of Turkey - Vol. 1, 1–10. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65501-3_1.

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Yamaç, Ali, Eric Gilli, Ezgi Tok, and Koray Törk. "Cave Archaeology in Turkey." In Caves and Karst of Turkey - Vol. 1, 11–26. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65501-3_2.

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3

Günay, G., İ. Çörekçioğlu, S. O. Eroskay, and G. Övül. "Konya Karapınar Obruks (Sinkholes) of Turkey." In Advances in Research in Karst Media, 367–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-12486-0_57.

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4

Yamaç, Ali, Eric Gilli, Ezgi Tok, and Koray Törk. "Natural Sciences in the Caves of Turkey." In Caves and Karst of Turkey - Vol. 1, 27–40. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65501-3_3.

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5

Bayarı, C. Serdar, N. Nur Özyurt, A. Koray Törk, Pınar Avcı, İ. Noyan Güner, and Emrah Pekkan. "Geodynamic Control of Hypogene Karst Development in Central Anatolia, Turkey." In Hypogene Karst Regions and Caves of the World, 449–62. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-53348-3_27.

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6

Günay, Gültekin. "Natural Recharge of Karst Aquifers in Western Taurus Region (Southwestern Turkey)." In Estimation of Natural Groundwater Recharge, 405–22. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-015-7780-9_26.

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7

Lewin, John, and Jamie Woodward. "Karst Geomorphology and Environmental Change." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0022.

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Whilst about 12 per cent of the earth’s dry and ice-free land is covered by carbonate rocks (limestone, marble, and dolomite), the proportion is significantly higher in the landscapes that border the Mediterranean Sea. These rock types are especially widespread in the northern part of the region and limestones in particular reach great thicknesses in Spain, southern France, Italy, the Balkan Peninsula, and Turkey and in many of the Mediterranean islands. Abundant precipitation in the uplands of the Mediterranean has encouraged solutional weathering of these carbonate rocks for an extended period. The region contains some of the deepest karst aquifers in the world, with many extending deep below present sea level (e.g. Bakalowicz et al. 2008). The regional fall in base level associated with the Messinian Salinity Crisis allowed the formation of very deep, multiphase karst systems in several parts of the Mediterranean basin (e.g. Mocochain et al. 2006). Thus, karst terrains and karstic processes are very significant components of the physical geography of the Mediterranean basin. Indeed, along with the climate and the vegetation, it can be argued that limestone landscapes (including limestone bedrock coasts) are one of the defining characteristics of the Mediterranean environment. Much of the northern coastline is flanked by mountains with bare limestone hillslopes (Figure 10.2) drained by short and steep river systems whose headwaters commonly lie in well-developed karst terrain. Karst terrains are also well developed in the Levant and in the Atlas Mountains of Morocco and Algeria, while relict karst features can be identified in the low-relief desert regions of Libya and Egypt (Perritaz 2004) (Figure 10.1). Mediterranean karst environments are also associated with distinctive soils, habitats and ecosystems as described in Chapters 5, 6, and 23. The nature and evolution of the karst landscapes across the Mediterranean region displays considerable spatial variability due to contrasts in relief, bedrock composition and structure, climatic history, and other factors. The karst geomorphological system is distinguished from other systems (e.g. glacial, fluvial, coastal, and aeolian) because of the dominant role of dissolution which results in water flowing in a subterranean circulation system rather than in surface channels (Ford 2004).
8

Foster, David R., and B. L. Turner II. "The Long View: Human–Environment Relationships in the Region, 1000 BC–AD 1900." In Integrated Land-Change Science and Tropical Deforestation in the Southern Yucatan. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780199245307.003.0010.

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The Yucatán Peninsula is a thick, low-lying, limestone shelf that rose fully above the Caribbean Sea and Gulf of Mexico during the Pleistocene (Folan 1983; Wilson 1980). Given its calcite and dolomite base, the entire peninsula northward from the Libertad Arch, which extends east–west across the central Petén, is a karstic landscape of coastal plains and interior uplands or hills dominated by solution features and subsurface drainage (Finch 1965; Jennings 1985; Weidie and Ward 1976; Wilhemy 1981). Permanent rivers and streams appear only in the southern, high rainfall, portion of the peninsula, largely along the lower-lying coastal plains and adjacent edges of the interior uplands. For the most part, the southern Yucatán peninsular region constitutes an undulating upland (about 80% of the landscape) composed of ridges and, to the south, cone karst (Figs. 2.1 and 2.2: upland-bajo distribution). Interspersed among the uplands are large, surface solution sinks or poljes (Weidie and Ward 1976), locally known as bajos (sometimes, akalches). These features infill with sediments, predominately montmorillonite clays, which impede subsurface drainage and retain surface water built up during the rainy season, creating seasonal wetlands. Otherwise, water percolates through the upland karst to subterranean aquifers, which generally lie deep below the surface. In the uplands proper, these aquifers may be more than 200m below the surface (Turner, 1983). The region occupies a transitional position between tropical monsoon (Am, Köppen classification) and tropical wet-dry (Aw) climates to the south and north respectively. The critical distinction between the two is the length and severity of the dry season, which increases northward. Overall, the climate is characterized by hot, humid summers and warm, dry winters, in which nortes (cold northern airstreams) penetrate the region for brief periods. Average annual precipitation ranges from about 900mm to in excess of 1,400mm, increasing to the south, the large majority of which falls during the wet season (mid-May through October) (Garcia 1970). Water deficits exist throughout the region during the mid-to-late dry season, stressing vegetation, wildlife, agriculture, livestock, and human settlement.
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Özel, Sevda. "Identification and Assessment of Hazard of Development in Gypsum Karst Regions: Examples from Turkey." In Natural Hazards - Risk, Exposure, Response, and Resilience. IntechOpen, 2019. http://dx.doi.org/10.5772/intechopen.83684.

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10

Roberts, Neil, and Jane Reed. "Lakes, Wetlands, and Holocene Environmental Change." In The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.003.0021.

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The Mediterranean regions of the world are defined on the basis of their climate, with a distinct hot, dry summer season and a warm, wet winter (Grove and Rackham 2001; Chapter 3). Spring and autumn seasons are less well defined but often contribute significantly to annual precipitation. Strictly defined in this way, the Mediterranean region is confined to parts of Italy, Greece, southern France, the south and east of Spain (non-Atlantic climate), the Maghreb and Cyrenaica in North Africa, and narrow coastal strips running through the Balkans, southern and western Turkey, and the Levant (Syria, Lebanon, and Israel-Palestine). Outside these areas, climate becomes humid temperate (western Europe, Black Sea), arid (Sahara, northern Arabia), or continental (interior areas of the Balkans, Turkey and Iberia, the Zagros mountains of Iran/Iraq). Even within the strict definition are found subalpine mountain zones, so it is a difficult study region to demarcate absolutely. In a similar vein to the volume by Zolitschka et al. (2000), this chapter extends the scope to important wetlands in some neighbouring regions, and deals effectively with the circum-Mediterranean. Thus, we include lakes Ohrid and Dojran in the Balkans, wetlands of the continental interior of Turkey, north-western Iran and the Caucasus (e.g. Lakes Van, Urmia, and Sevan), the climatically dry Jordan rift valley which includes the Dead Sea, and the subalpine northern Italian lakes such as Como and Maggiore. The Mediterranean basin is geologically complex and has its origin in the progressive closure of the Sea of Tethys during the Tertiary (Laubscher and Bernoulli 1977). Plate convergence between Africa and Eurasia led to a major phase of orogenesis and the creation of fold mountains including the Atlas, Sierra Nevada, Alps, Apennines, and Taurus, and to plateau uplift in Iberia and Anatolia (Chapter 1). These mountain ranges are commonly dominated by massively deformed Mesozoic limestones that now form karst landscapes (e.g. Dinaric Alps; Ager 1980; Chapter 10). Tectonic movement also led to extensive late Cenozoic volcanism, notably in southern and central Italy, the Hellenic arc, Anatolia, and around the Jordan rift (Chapter 15).

Тези доповідей конференцій з теми "Karsts – Turkey":

1

Emanet, Hakan. "The Contribution of Baku-Tbilisi-Kars Railway to International Trade between Turkey and Turkish Republics." In International Conference on Eurasian Economies. Eurasian Economists Association, 2017. http://dx.doi.org/10.36880/c08.01953.

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This study examines the potential contribution of the Baku-Tbilisi-Kars (BTK) railway, which is planned to be in service in 2017, to the commercial relationship between Turkey and five Turkish republics (Azerbaijan, Kazakhstan, Uzbekistan, Kyrgyzstan and Turkmenistan). First, the general structure of the last five years of foreign trade between Turkey and these states will be revealed. In the second stage, transport routes which are used extensively in the physical transport of goods in the current trade, and the benefits and drawbacks of these routes will be mentioned. In the third stage, the characteristics of the BTK railway will be specified as a new route option. In the last part, the future contribution of the BTK railway to the trade between Turkey and these states will be evaluated.
2

Pekbey, Gamze, and Zeliha Eroğlu. "Sarcophagidae (Diptera) fauna of Artvin, Iğdır and Kars provinces of Turkey." In II. INTERNATIONAL CONFERENCE ON ADVANCES IN NATURAL AND APPLIED SCIENCES: ICANAS 2017. Author(s), 2017. http://dx.doi.org/10.1063/1.4981712.

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3

Field, Malcolm S. "Fortran Processing of Fluorometric Data Logged by a Turner Designs Field Fluorometer." In Ninth Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. Reston, VA: American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40698(2003)18.

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4

Yilmaz, D. G. "Stone masonry walls and woodworks as architectural heritages in rural areas of the Eastern Anatolia Region, Turkey: case studies from Erzurum, Kars and Ardahan." In STREMAH 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/str130051.

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