Complex geomorphological characteristics and relief geodynamic features of morphostructural units of the southern slope of the Greater Caucasus

2021 ◽  
Vol 07 (02) ◽  
pp. 61-63
Author(s):  
Qüdrət Tərlan oğlu Məmmədli ◽  
Keyword(s):  
Key Words ◽  
Geological Structure ◽  
Southern Slope ◽  
Greater Caucasus ◽  
River Valleys ◽  
Geomorphological Analysis

According to the modern geodynamic concept of lithosphere pans, the geological structure of the Greater Caucasus in the system of geosynclinal and platform regions is very complex. This situation, along with different conditions for the geomorphological development of the area, led to the formation of a complex and diverse relief with different ridges, massifs, inland basins, river valleys and other small morphostructures and morphosculptures. Key words: Greater Caucasus, southern part of Greater Caucasus, southern slopes, mosfostructure, geomorphological analysis, relief forms

Study of factors influencing the transformation of mountain geosystems on the southern slope of the Greater Caucasus

2021 ◽  
Vol 07 (02) ◽  
pp. 75-77
Author(s):  
Zeynəb Zəkəriyyə qızı Qurbanzadə ◽  
Keyword(s):  
Key Words ◽  
Ecological Study ◽  
Southern Slope ◽  
The South ◽  
Anthropogenic Changes ◽  
Greater Caucasus ◽  
Factors Influencing ◽  
South Slope

In the article touched such issues as anthropogenic changes in the landscapes of the south slope of the Greater Caucasus, ecological study of enviromental impact, landscape optimization. There are also suggestions for more efficient use of rapidly growing anthropogenically affected landscapes. Key words: anthropogenic changes, Greater Caucasus, south slope, optimization, landscape Azərbaycanın şimal-şərq hissələrini əhatə edən təbii iqlim şəraiti, heyvanat və bitki aləminə, turizm və istirahət üçün əvəzolunmaz məziyyətlərinə, həm də zəngin yeraltı sərvətlərinə görə respublikamızın nadir ərazilərindən biri olan Böyük Qafqazın cənub yamacı getdikcə daha da intensivləşən antropogen təsirlərə məruz qalan bir tədqiqat obyekti kimi nəzəri cəlb edir.

On the possible analogy between the Dizi Series of the Southern slope zone of the Greater Caucasus and the folded basement of the plain Crimea: composition, metamorphism, magmatism and age

2021 ◽  
Author(s):  
Irakli Javakhishvili ◽  
David Shengelia ◽  
Tamara Tsutsunava ◽  
Giorgi Chichinadze ◽  
Giorgi Beridze ◽  
...  
Keyword(s):  
Middle Jurassic ◽  
Regional Metamorphism ◽  
Geological Structure ◽  
Greenschist Facies ◽  
Igneous Rocks ◽  
Contact Metamorphism ◽  
Southern Slope ◽  
Quartz Syenite ◽  
Greater Caucasus ◽  
Geological Conditions

<p>The Dizi Series is exposed within the Southern slope zone of the Greater Caucasus that occurs as a complex geological structure, which constitutes an integral part of the Mediterranean (Alpine-Himalayan) collisional orogenic belt. It is built up of terrigenous and volcanogenic-sedimentary rocks faunistically dated from the Devonian to Triassic inclusive (Somin, 1971; Somin, Belov, 1976; Kutelia 1983). Most of them are metamorphosed under conditions of chlorite-sericite subfacies of the greenschist facies of regional metamorphism (chlorite-phengite-albite±quartz, graphite-sericite-quartz phyllites and marbleized limestones), and only a minor part represented by clay-carbonaceous, phengite-chlorite-carbonaceous and prehnite-chlorite-carbonate schists underwent anchimetamorphism (Shengelia et al., 2015). The Dizi Series is intruded by numerous magmatic bodies of gabbro-diabases, diabases, diorites, diorite-porphyries, syenites, monzo-syenites and granitoids. The age of the intrusions was defined by K-Ar method at 176-165 Ma (Dudauri, Togonidze, 1998) and by U-Pb LA-ICP-MS zircon dating at 166.5 ± 4.6 Ma (authors` unpublished data) and corresponds to the Bathonian orogeny. The Middle Jurassic intrusions caused intense contact metamorphism of the rocks of the Dizi Series resulted in the formation of various hornfelses containing andalusite, cordierite, corundum, biotite, plagioclase, potassium feldspar, clinozoisite, hornblende, cummingtonite, clinopyroxene, wollastonite and scapolite. These rocks correspond to albite-epidote-hornfels, andalusite-biotite-muscovite-chlorite-hornfels and andalusite-biotite-muscovite-hornfels subfacies of the contact metamorphism (Javakhishvili et al., 2020). The analogues of the Dizi Series rocks have not previously been established either in the Greater Caucasus or in the neighboring regions. In our view, Paleozoic rocks similar to the Dizi Series occur under the Cretaceous and Jurassic deposits within the folded basement of the plain Crimea where they were recovered by wells. Most of these rocks, as in the Dizi Series, underwent metamorphism of chlorite subfacies of the greenschist facies and, to a lesser extent, deep epigenesis (clayey-carbonaceous, sericite-carbonaceous, actinolite-chlorite-prehnite, muscovite-albite-chlorite, epidote-actinolite-chlorite and graphite-talc-quartz schists) (Chernyak, 1969). These rocks are also intruded by Middle Jurassic igneous rocks, including gabbro-diabases, diabases, diorites, syenites, monzo-syenites, granite-porphyries, etc. (Shniukova, 2016; Shumlyanskyy, 2019). As a result of the contact metamorphism of the basement rocks, muscovite-quartz-cordierite and cordierite-quartz-feldspar micaceous hornfelses were formed. Quartz syenite yielded a K-Ar age of 158 Ma (Scherbak, 1981), while monzo-syenite was dated at 170 ± 5 Ma applying 40Ar/39Ar method (Meijers, 2010). Thus, based on the rock associations, the nature of metamorphism, the age of the metamorphic and igneous rocks, and on the spatial position of the Dizi Series and folded basement of the plain Crimea we assume that these units developed coevally in similar environment and geological conditions.<br><br>Acknowledgements.This work was supported by Shota Rustaveli National Science Foundation (SRNSF) [PHDF-19-159, Regional and Contact Metamorphism of the Dizi Series].</p>

BÖYÜK QAFQAZIN CƏNUB-ŞƏRQ YAMACINDA ANTROPOGEN TRANSFORMASİYANIN QİYMƏTLƏNDİRİLMƏSİ

2021 ◽  
Vol 07 (02) ◽  
pp. 53-56
Author(s):  
Jalə Ehtibar qızı Tağızadə ◽  
Keyword(s):  
Population Density ◽  
Key Words ◽  
Evaluation Criteria ◽  
Anthropogenic Factor ◽  
Southern Slope ◽  
Anthropogenic Transformation ◽  
Greater Caucasus

The article assesses the anthropogenic transformation of the southern slope landscape complexes of the Greater Caucasus. In this case, the location of settlements in the landscape (in%), population density (people / km2) were taken as evaluation criteria. Key words: Anthropogenic factor, Greater Caucasus, anthropogenic transformation, landscape Böyük Qafqazın cənub-şərq zonası 412290,65 ha sahəni əhatə edir. Həmin ərazidə kiçik və orta ölçülü 196 yaşayış məntəqəsi qeydiyyata alınmışdır. Burada yerləşən məntəqələrin 4-ü şəhər tipli, 5-i qəsəbə və 187-si isə kənd tiplidir.

The main characteristics of the wrinkled relief on the southern slope of the Greater Caucasus

2021 ◽  
Vol 09 (04) ◽  
pp. 24-26
Author(s):  
Qüdrət Tərlan oğlu Məmmədli ◽  
Keyword(s):  
Key Words ◽  
Southern Slope ◽  
The South ◽  
The Caucasus ◽  
Greater Caucasus ◽  
Mountainous Regions ◽  
South Eastern ◽  
Mountain System ◽  
Caucasus Mountains

Like other mountainous regions of the Caucasus, the South-Eastern Caucasus is an epigeosynclinal mountain system formed by the first and middle alpine folds. Between the Alpine fold stage and the orogenic stage, the South-East Caucasus Mountains were denuded and turned into hilly, low mountain plains in the Oligocene and Miocene. Wrinkled structures were destroyed by denudation and a mostly neutral relief type was formed. Key words: Greater Caucasus, southern slope of the Greater Caucasus, morphostructure, wrinkled relief, geological development

scholarly journals RELIEF AND GEOLOGICAL STRUCTURE OF CARPATHIAN BIOSPHERE RESERVE

2021 ◽  
pp. 19-38
Author(s):  
Yaroslav Kravchuk ◽  
Vitaliy Brusak
Keyword(s):  
Key Words ◽  
Biosphere Reserve ◽  
Geological Structure ◽  
Rill Erosion ◽  
Lower Tier ◽  
Gravitational Processes ◽  
River Valleys ◽  
Glacial Landforms ◽  
Longitudinal Division ◽  
Sheet Erosion

The relief and geological structure of Carpathian Biosphere Reserve represent the features of the geological and geomorphological structure of the four geomorphological regions of the Ukrainian Carpathians. The block mid-mountains of the Polonynsko-Chornohirsky Carpathians (Chornohora, Svydovets, and Uholsko-Shyrokoluzhansky massifs) and the folded mid-mountains of Marmarosy crystal massif (Marmarosy and Kuziy-Trybushansky massifs) are well protected within the reserve. The analysis of the morphostructure and morphosculpture of the reserve is carried out taking into account the longitudinal (NW–SE) and transverse divisions of the Ukrainian The analysis of the morphostructure and morphosculpture of the reserve is carried out taking into account the longitudinal (NW–SE) and transverse divisions of the Ukrainian Carpathians. The longitudinal division is associated with morphostructures of higher orders, such as second and third. The transverse division is associated with the fourth and fifth orders of morphostructures. In the analysis of morphosculpture of the reserve, the types characterized for all regions of Flysch and Crystal Carpathians are allocated. All mountain massifs and ridges could be characterized by an asymmetrical structure, such as steep northeastern slopes and acclivous southwestern slopes. The relic morphosculpture is represented by: 1) fragments of denudation surfaces of different ages such as Polonynska, Pidpolonynska, and riparian; 2) ancient glacial and extra glacial landforms; 3) areas of ancient longitudinal valleys. River valleys with a complex of different age terraces represent inherited morphosculpture. Modern morphodynamic processes are represented by height (tier) differentiation. The processes of sheet erosion, deflation, and rill erosion play an important role in the relief modeling for the tiers of strongly dissected mid-mountain relief. The lower tier of the terraced and non-terraced bottoms of the valleys are associated with the processes of leaching and erosion as well as a significant accumulation of erosion products and mudflows. Stabilized and active displacements are the most recorded among the gravitational processes and block motions. Key words: Carpathian Biosphere Reserve; Ukrainian Carpathians; relief; morphostructure; morphosculpture.

scholarly journals Ecological Distribution of Cyclemys oldhamii (Gray, 1863) from Nepal

Our Nature ◽  
1970 ◽  
Vol 2 (1) ◽  
pp. 7-12 ◽  
Author(s):  
Kalu Ram Rai
Keyword(s):  
Habitat Loss ◽  
Paddy Field ◽  
Flood Plain ◽  
Southern Slope ◽  
Ecological Distribution ◽  
Eupatorium Adenophorum ◽  
Adult Specimen ◽  
Juvenile Specimen ◽  
River Valleys ◽  
Ecological Habitats

Tangting River originates from southern slope of Murtidanda of Mahabharat range and forms a very narrow v-shaped agriculturally fertile valley in lower parts of Chure hills. It has three main tributaries merging from east and west. Water is clear with rocky bed and margin is covered with thick bushes of semi-shrubs (Eupatorium adenophorum). During the herpetological survey, a live juvenile specimen of Cyclemys oldhamii (Gray, 1983) was collected from the periphery of Banmare Khola, an eastern tributory of the river. It was found hiding in the paddy field in the flood plain of Tangting river (280 m), and another adult specimen was collected from Dhobi Khola (450 m), a western tributory of the river. Empty shells were also collected from Garuwa and Mai valleys, respectively. Tangting and Garuwa river valleys are the favourable habitats for Cyclemys oldhamii. The main reason of discontinued distribution is habitat loss by deforestation. Key words: Cyclemys, Morphology, Ecological habitats, Distributiondoi:10.3126/on.v2i1.317Our Nature (2004) 2: 7-12

scholarly journals Temporal and spatial variation of NPP and its response to climatic factors in main river valleys on the southern slope of Qilian Mountains

2019 ◽  
Vol 131 ◽  
pp. 01044
Author(s):  
Rong-rong Yang ◽  
Guang-chao Cao ◽  
Sheng-kui Cao ◽  
Yao Lan ◽  
Zhuo Zhang ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
Climatic Factors ◽  
Growing Season ◽  
Qilian Mountains ◽  
River Valley ◽  
Distribution Characteristics ◽  
Southern Slope ◽  
Qilian Mountain ◽  
Main River ◽  
River Valleys

Based on the NPP products of MODIS data, the spatial and temporal distribution characteristics of grassland NPP and its response to climatic factors in the vegetation growing season of the main river valleys in the southern slope of Qilian Mountains from 2000 to 2016 were carried out by correlation analysis and spatial interpolation. The research further provides a scientific basis for the quality evaluation of grassland ecosystems on the southern slope of Qilian Mountain and the rational use of grassland resources along the river. The results show that: (1) With the increasing distance of buffers on both sides of the river, the NPP of grassland in each year shows the characteristics of “single-peak” distribution, which is increased first and then decreased; (2) the NPP of grassland in the main river valley of the southern slope of Qilian Mountain The spatial distribution characteristics show a trend of increasing from northwest to southeast. (3) The spatial distribution of NPP and air temperature in the main river valleys of the southern slope of Qilian Mountains is gradually increasing from northwest to southeast, but the spatial distribution correlation coefficient of NPP and precipitation in the river valley grassland of vegetation growing season basically shows a trendof decreasing from northwest to southeast.

scholarly journals Comparison of southern part of Volyn and Zhytomyr Polissya river valleys (for example Horyn and Sluch)

2014 ◽  
pp. 386-394
Author(s):  
О. Budko
Keyword(s):  
Key Words ◽  
River Valley ◽  
Ukrainian Shield ◽  
River Valleys ◽  
Different Parts

At the article a Horyn and Sluch river valleys are described. Terrace levels are allocated, the structure of valleys as a whole is analyzed. Special attention is concentrated on differences in geomorphologic structure of the river Sluch within the Ukrainian shield and Volyn-Podilska plate. Identified and characterized the different parts of the Goryn and Sluch valleys. The conclusions about the role of structural, lithological and other factors in the construction of river valleys are maked. Key words: river valley, terrace, Sluch, Goryn, alluvium, Polissya.

scholarly journals DISCOVERY OF NEW KIMBERLITE FIELDS ON THE SOUTHERN SLOPE OF THE LEONE-LIBERIAN SHIELD (Sierra Leone)

2021 ◽  
pp. 118-126
Author(s):  
Oleksandr BOBROV ◽  
Sergii KLOCHKOV ◽  
Serhiy KAKARANZA ◽  
Oleksandr KAKARANZA ◽  
Yurii FEDORISHIN ◽  
...  
Keyword(s):  
Sierra Leone ◽  
Ultramafic Rocks ◽  
Southern Slope ◽  
Rock Matrix ◽  
Geophysical Research ◽  
Optimal Sequence ◽  
Space Images ◽  
Complex Morphology ◽  
Geomorphological Analysis ◽  
Contact Part

During 2017–2018 not far from Sewafeh town, Kono province (Republic of Sierra Leone), we identified a number of previously unknown manifestations of kimberlite magmatism in the form of a system of individual veins localized at the contact of the migmatite basement and Archean ultrabasic massifs, or in the immediate vicinity of ultramafic massifs, which is part of the rocks of the greenstone belt. The optimal sequence of conducting remote sensing studies, such as interpretation of space images of various resolution, neotectonic and geomorphological analysis, SRTM modeling, and then field geological and geophysical research have facilitated this discovery. According to drilling data, kimberlites in different spots of their occurrence (Punduru 1 area) are represented by subvolcanic phlogopite-olivine (with perovskite), and olivine varieties, as well as veins of numerous intensely metasomatic altered kimberlite breccias (Yomby area). Veins of subvolcanic kimberlites are concentrated in the contact part with ultramafic massifs of magmatic and lava (metakomatiite xenoliths) genesis. Kimberlites are the youngest vein formations in the area, crossing even vein pegmatites, the generation of which was provoked by the intrusion of ultramafic rocks in the basement migmatites (Cederholm effect). Kimberlites are present in the section of wells in the form of separate veins of complex morphology and thickness from a few centimeters to 45 cm. In well P1-2 at a depth of 92 m, these are represented by micro porphyry kimberlites of the basaltoid type with microlithic groundmass, altered by secondary metasomatic processes. Porphyry inclusions are represented by pseudomorphs of carbonate-serpentine composition after olivine and rare phlogopite flakes. Olivine crystals of the second-generation act as micro porphyry inclusions. The rock matrix is carbonate. Carbonate is represented by finely crystalline calcite, or replaced by dolomite. In addition to olivine, the groundmass contains relics or pseudomorphs after phlogopite, as well as magnetite, perovskite (it can be replaced by magnetite), secondary apatite. The kimberlites of the Bambawo area are represented by sub-volcanic porphyry basaltoid kimberlites, autolithic kimberlites and kimberlite xenotuff breccias. 

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