scholarly journals Geological model of the Achimov clinoform series within the south-eastern slope of the Srednemessoyakhsky Swell

2018 ◽  
pp. 17-25
Author(s):  
E.A. Potapova ◽  
◽  
Keyword(s):  
Geological Model ◽  
Eastern Slope ◽  
The South ◽  
South Eastern

scholarly journals Population Settlement in the South-Eastern Slope of the Great Caucasus and Evaluation of Anthropogenic Impacts (on the Example of the Shamakhi-Ismayilli zone)

2020 ◽  
Vol 6 (3) ◽  
pp. 198-207
Author(s):  
H. Shakiliyeva
Keyword(s):  
Anthropogenic Impacts ◽  
Main Direction ◽  
Eastern Slope ◽  
The South ◽  
Change Dynamics ◽  
South Eastern ◽  
Settlement Areas

Population settlement on the South–Eastern slope of the Great Caucasus and evaluation of anthropogenic impacts are one of the main direction, that’s why this problem was pain attention in the research of the Shamakhi-Ismayilli zone. Change dynamics of the population, their settlement areas were determined; the problems which the means activity creates problems in the nature were investigated in the article.

scholarly journals FEATURES OF ECOLOGY AND BIOTOPIC DISTRIBUTION OF RODENTS ON THE SOUTH-EASTERN SLOPE OF THE BOGOS RIDG

2020 ◽  
pp. 18-22
Author(s):  
Kamil Zubairovich OMAROV
Keyword(s):  
Species Composition ◽  
Relative Abundance ◽  
Eastern Slope ◽  
The South ◽  
Biotopic Distribution ◽  
South Eastern ◽  
Wide Range

As part of the inventory work in the Kosobsko-Keleb Reserve in 2017–2019, the species composition was identified and the relative abundance of rodents on the south-eastern slope of the Bogos ridge was estimated. It is shown that rodents inhabit a fairly wide range of biotopes on the south-eastern slope of the Bogos ridge, which is largely predetermined by the peculiarities of their ecology and the nature of their specialization.

scholarly journals ROLE OF RELIEF MORPHOMETRIC PARAMETERS ON THE AGRICULTURAL DEVELOPMENT IN THE MOUNTAIN GEOSYSTEMS OF THE SOUTH-EASTERN SLOPE OF THE GREATER CAUCASUS

2017 ◽  
Vol 2017 (4) ◽  
pp. 26-31
Author(s):  
Гюльнар Гаджиева ◽  
Gyulnar Gadzhieva ◽  
Зулейха Эюбова ◽  
Zuleikha Eyubova
Keyword(s):  
Agricultural Development ◽  
Structural Changes ◽  
Lower Layer ◽  
Decisive Role ◽  
Morphometric Parameters ◽  
Eastern Slope ◽  
The South ◽  
Mountain Areas ◽  
Greater Caucasus ◽  
South Eastern

<p>Natural geosystems of the south-eastern slope of the Greater Caucasus are genetically related to the large morphostructural units that constitute the territory, as well as to the aerodynamic condition of the lower layer of the troposphere. The study revealed that there are contradictions in the geosystems formation of various local morphostructures. Thus, the differentiation of geosystems may either be intensifi or weakened, depending on the height of mountain areas and ridges. The slope and direction of visibility of the area are the basic elements that play a decisive role in the shaping of structural and genetic features of the area in question. The article features the structural changes that are observed in natural geosystems based on the slope and direction of visibility maps and charts of the contemporary geosystems in the south-eastern slope of the Greater Caucasus. The research also features the infl of morphometric parameters of the relief on the agriculture development in the mountain geosystems of the south-eastern slope of the Greater Caucasus in GIS.<strong></strong></p>

Brachypterous ground beetles of the Trichotichnus subgenus Bottchrus Jedlička (Coleoptera, Carabidae) from the Himalaya, with description of fifteen new species

Zootaxa ◽  
2017 ◽  
Vol 4323 (3) ◽  
pp. 301
Author(s):  
BORIS M. KATAEV ◽  
JOACHIM SCHMIDT
Keyword(s):  
New Species ◽  
Western Slope ◽  
Mountain Range ◽  
Southern Slope ◽  
Eastern Slope ◽  
The South ◽  
South Eastern ◽  
New Synonyms ◽  
Central Nepal ◽  
The Himalaya

The paper deals with the taxonomy of brachypterous species of the subgenus Bottchrus Jedlička, 1935 of the genus Trichotichnus Morawitz, 1863 occurring in the Himalayan region. The following new species are described: T. (B.) baglungensis sp. n. from the Baglung Lekh mountain range, Baglung District, western Central Nepal; T. (B.) parvulus sp. n. from Mt. Panchhase and the Krapa Danda mountain range, Kaski District, western Central Nepal; T. (B.) bubsaensis sp. n. from the eastern slope of the middle Dudh Koshi Valley near Bubsa, Solu Khumbu District, eastern Central Nepal; T. (B.) schawalleri sp. n. from the western slope of the Arun Valley, Bhojpur District, East Nepal; T. (B.) obliquebasalis sp. n. from the Khimti Khola Valley near Shivalaya, Dolakha District, eastern Central Nepal; T. (B.) panchhaseensis sp. n. from Mt. Panchhase, Kaski District, western Central Nepal; T. (B.) siklesensis sp. n. from the Sikles mountain range on the southern slope of Annapurna Peak II, western Central Nepal; T. (B.) pusillus sp. n. from the south-western slopes of Manaslu Himal (Bara Pokhari Lekh and Dudh Pokhari Lekh mountain ranges), and from the south-eastern slope of Annapurna Himal (Telbrung Danda mountain range), Lamjung District, western Central Nepal; T. (B.) ganeshensis sp. n. from the south-western slope of Ganesh Himal, Nuwakot District, Central Nepal; T. (B.) minutus sp. n. from the mountains surrounding the Kathmandu Valley (Shivapuri Lekh, Mt. Phulchoki), Central Nepal; T. (B.) gupchiensis sp. n. from the Gupchi Danda mountain range on the south-eastern slope of Manaslu Himal, Gorkha District, western Central Nepal; T. (B.) brancuccii sp. n. from the southern slope of the Helambu mountain range, Sindhupalchok District, Central Nepal; T. (B.) manasluensis sp. n. from the Bara Pokhari Lekh mountain range on the south-western slope of Manaslu Himal, Lamjung District, western Central Nepal; T. (B.) sikkimensis sp. n. from Pelling near Geyzing, West Sikkim, India; T. (B.) martensi sp. n. from the western slopes of the Singalila mountain range, Taplejung District, East Nepal. The following four species are redescribed: brachypterous T. (B.) holzschuhi Kirschenhofer, 1992; T. (B.) cyanescens Ito, 1998; T. (B.) hingstoni Andrewes, 1930; and dimorphic T. (B.) birmanicus Bates, 1892; and new data on their distribution are provided. The lectotype is designated for T. hingstoni Andrewes, 1930. The following two new synonyms are proposed: Trichotichnus birmanicus Bates, 1892 = T. (Bellogenus) probsti Kirschenhofer, 1992, syn. n., and T. hingstoni Andrewes, 1930 = T. (Pseudotrichotichnus) curvatus Ito, 1996, syn. n. The brachypterous and dimorphic species of Bottchrus known from the Himalaya are divided into eight informal groups based mostly on the degree of reduction of hindwings and the configuration of the median lobe of the aedeagus, and their relationships are briefly discussed. The distributional data of all these species are mapped. 

Rodingite from the Girvan-Ballantrae complex, Ayrshire

1954 ◽  
Vol 30 (227) ◽  
pp. 525-528 ◽  
Author(s):  
T. W. Bloxam
Keyword(s):  
Eastern Slope ◽  
The South ◽  
Precise Form ◽  
South Eastern ◽  
South West ◽  
Lower South

Occurrence and relationships. Altered and garnetized gabbros occur in association with serpentinite occupying the lower south-eastern slope of Byne Hill, one mile to the south of Girvan. The rocks crop out above Balaclava Wood near the footpath from Bynehill Bridge to Craiglea. Although the precise form of the altered gabbros is not very well revealed, they appear to be dikes intrusive into the surrounding serpentinized harzburgite. Contacts with the serpentinite are exposed in two places but are evidently lines of later movement. The relationships of these altered gabbros to the main gabbro mass of Byne Hill are obscure. They are, however, probably contemporaneous, since sporadic garnetization of the main gabbro occurs along its contact with serpentinite farther to the south-west.

scholarly journals The geological structure of the left part of Big Polya river (Prepolar Urals) on the results of geological training surveying practice in 2015

2015 ◽  
Vol 11 (3) ◽  
pp. 62-66
Author(s):  
Konstantin Yu Kudrin
Keyword(s):  
Geological Structure ◽  
Geological Mapping ◽  
Eastern Slope ◽  
The South ◽  
South Eastern ◽  
Left Part ◽  
Platinum Belt ◽  
North Western ◽  
Complex Of Parallel Dikes

Largescale geological mapping of the left part of the valleys of the Big Polya river of (downstream) and Polya river (upstream) on the Eastern slope of the Prepolar Urals is performed. Most (north-western) part of the territory represents a fragment of a large heterogeneous Shchekurinskiy massif, which is the most northern representative in the chain of mafic-ultramafic intrusions of the Uralian platinum belt. The south-eastern part of the area is composed of basalts and dolerites of the complex of parallel dikes.

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