scholarly journals Geo-Strategic Imperative of North-Western Border: Triangular Region Kalapani - Lipulekh and Limpiadhura of Nepal

Unity Journal ◽  
2021 ◽  
Vol 2 ◽  
pp. 29-40
Author(s):  
Bharat Khanal
Keyword(s):  
Strategic Competition ◽  
The North ◽  
Maximum Benefit ◽  
Special Relations ◽  
Western Border ◽  
Strategic Imperative ◽  
Extreme North ◽  
Article 5 ◽  
North Western ◽  
India And China

The extreme north western region of Nepal is bordered with India and China and separated by Mahakali River. As per Article 5 of Sugauli treaty and various other evidences like, historical facts, ancient maps, river science, government correspondence and other documents proves that the river originating from Limpiadhura form the international boundary between Nepal and China. However, the certain parts of Nepalese territory have been under the control of India from seven decades. Owing to the historical and geographical proximity, Nepal has maintained special relations with her immediate neighbors, India and China, despite several complex situations. Remaining away from strategic competition and rivalry; and gaining maximum benefit from India and China as they are global and regional players would best serve the national interest of Nepal. Underdeveloped nature of physical infrastructures, nascent institutional structures and poor presence of government machinery in the North western border of Nepal has complicated the problem. Our neighbors should be sensitive and respectful to our concerns and interests. Delicate handling of border issues is in our interest. Nepal has become the center of geopolitical interest in the present world. Sands of geopolitics are constantly shifting in South Asia and Nepal cannot remain aloof from it. Influence in Nepal from competition and cooperation is rising. There is a need of cooperation for transit economy and trilateral cooperation. Nepal should use her diplomatic expertise and regain our territory by maintaining friendly and harmonious relations with her neighbors. Nepal and India shouldn’t delay in resolving such outstanding disputes. Both countries should bring their evidences and carefully examine that evidence by creating a favorable negotiating environment. Above all, national consensus on such sensitive issue is important.

scholarly journals Reproductive health among Venezuelan migrant women at the north western border of Brazil: A qualitative study

2021 ◽  
pp. 100060
Author(s):  
Maria Y. Makuch ◽  
Maria Jose D. Osis ◽  
Cinthia Brasil ◽  
Helder S.F. de Amorim ◽  
Luis Bahamondes
Keyword(s):  
Reproductive Health ◽  
Qualitative Study ◽  
Migrant Women ◽  
The North ◽  
Western Border ◽  
North Western

scholarly journals Three generations of stars: a possible case of triggered star formation

2020 ◽  
Vol 496 (1) ◽  
pp. 870-874
Author(s):  
M B Areal ◽  
A Buccino ◽  
S Paron ◽  
C Fariña ◽  
M E Ortega
Keyword(s):  
Star Formation ◽  
Young Stellar Objects ◽  
H Ii Regions ◽  
Stellar Objects ◽  
Three Generations ◽  
The North ◽  
Western Border ◽  
H Ii Region ◽  
New Generation ◽  
North Western

ABSTRACT Evidence for triggered star formation linking three generations of stars is difficult to assemble, as it requires convincingly associating evolved massive stars with H ii regions that, in turn, would need to present signs of active star formation. We present observational evidence for triggered star formation relating three generations of stars in the neighbourhood of the star LS II +26 8. We carried out new spectroscopic observations of LS II +26 8, revealing that it is a B0 III-type star. We note that LS II +26 8 is located exactly at the geometric centre of a semi-shell-like H ii region complex. The most conspicuous component of this complex is the H ii region Sh2-90, which is probably triggering a new generation of stars. The distances to LS II +26 8 and to Sh2-90 are in agreement (between 2.6 and 3 kpc). Analysis of the interstellar medium on a larger spatial scale shows that the H ii region complex lies on the north-western border of an extended H2 shell. The radius of this molecular shell is about 13 pc, which is in agreement with what an O9 V star (the probable initial spectral type of LS II +26 8 as inferred from evolutive tracks) can generate through its winds in the molecular environment. In conclusion, the spatial and temporal correspondences derived in our analysis enable us to propose a probable triggered star formation scenario initiated by the evolved massive star LS II +26 8 during its main-sequence stage, followed by stars exciting the H ii region complex formed in the molecular shell, and culminating in the birth of young stellar objects around Sh2-90.

Aeolian Environments

2005 ◽  
Author(s):  
Eduard Koster
Keyword(s):  
Sand Dunes ◽  
Ural Mountain ◽  
Aeolian Processes ◽  
The North ◽  
Aeolian Deposits ◽  
The World ◽  
Western Border ◽  
Late Weichselian ◽  
The Baltic ◽  
North Western

The literature on aeolian processes and on aeolian morphological and sedimentological features has shown a dramatic increase during the last decade. A variety of textbooks, extensive reviews, and special issues of journal volumes devoted to aeolian research have been published (Nordstrom et al. 1990; Pye and Tsoar 1990; Kozarski 1991; Pye 1993; Pye and Lancaster 1993; Cooke et al. 1993; Lancaster 1995; Tchakerian 1995; Livingstone and Warren 1996; Goudie et al. 1999). However, not surprisingly the majority of these studies discuss aeolian processes and phenomena in the extensive warm arid regions of the world. The results of aeolian research in the less extensive, but still impressive, cold arid environments of the world are only available in a diversity of articles. At best they are only briefly mentioned in textbooks on aeolian geomorphology (Koster 1988, 1995; McKenna-Neuman 1993). Likewise, the literature with respect to wind-driven deposits in western Europe is scattered and not easily accessible. The aeolian geological record for Europe, as reflected in the ‘European sand belt’ in the north-western and central European Lowlands, which extends from Britain to the Polish–Russian border, is known in great detail (Koster 1988; van Geel et al. 1989; Böse 1991). Zeeberg (1998) showed that extensive aeolian deposits progress with two separate arms into the Baltic Region, and into Belorussia and northernmost Ukraine. Recently, Mangerud et al. (1999) concluded that the sand belt extends even to the Pechora lowlands close to the north-western border of the Ural mountain range in Russia. Sand dunes and cover sands are widespread and well developed in this easternmost extension of the European sand belt. The northerly edges of this sand belt more or less coincide with the maximal position of the Late Weichselian (Devensian, Vistulian) ice sheet, while the southern edges grade into coverloams or sandy loess and loess (Mücher 1986; Siebertz 1988; Antoine et al. 1999). However, along these southern edges the dune fields and sand sheets regionally are derived from different sources, such as the sands of the Keuper Formation or the floodplains of the Rhine and Main rivers.

scholarly journals New evidence of Lindenia tetraphylla (Vander Linden, 1825) (Odonata, Gomphidae) reproduction at the north-western border of its distribution

2016 ◽  
Vol 25 (2) ◽  
pp. 287-294 ◽  
Author(s):  
Marina Vilenica ◽  
◽  
Antun Alegro ◽  
Nikola Koletić ◽  
Zlatko Mihaljević ◽  
...  
Keyword(s):  
The North ◽  
Western Border ◽  
New Evidence ◽  
North Western

scholarly journals A PRELIMINARY LIST OF ACRIDIIDÆ OF ONTARIO

1902 ◽  
Vol 34 (10) ◽  
pp. 251-258 ◽  
Author(s):  
E. M. Walker
Keyword(s):  
Native Species ◽  
The South ◽  
Full List ◽  
The North ◽  
South West ◽  
Extreme North ◽  
North Western ◽  
Unrecorded Species

Since the last of my “Notes on Some Ontalio Acridiidæ” were printed, five species have been added to the list, and the number of localities for those already recorded has been considerably increased. I think,therefore, that it will make the notes more complete to conclude them with a full list of the species of this family known to occur in the Province, with their distribution as hitherto recorded.Only a small portion of the territory included in the Province of Ontario has been at all thoroughly explored by entomologists, but I do not believe there are very many native species of Acridiidæ not included in the present list. Doubtless, horvever, some of the Manitoba and Minnesota forms extend into the north-western part of Ontario, while it is extremely probable that there are unrecorded species in the south-west, and possibly a few in the east and extreme north.

scholarly journals The Khaung Daing hot spring (Inle lake, Southern Shan State, Myanmar): development opportunities and challenges

2019 ◽  
Vol 98 ◽  
pp. 09027
Author(s):  
Elisa Sacchi ◽  
Sergio Comizzoli ◽  
Eloisa Di Sipio ◽  
Viviana Re ◽  
Marco Rotiroti ◽  
...  
Keyword(s):  
Isotopic Exchange ◽  
Environmental And Health Effects ◽  
Hot Spring ◽  
Lake Basin ◽  
Geothermal Resource ◽  
The North ◽  
The Matrix ◽  
Western Border ◽  
High Concentrations ◽  
North Western

Located on the north-western border of the Inle lake basin, the Khaung Daing hot spring outflows at ca. 70°C. Temperature at depth, calculated with chemical geothermometers is probably less than 150°C, therefore classifying it as a medium-low enthalpy geothermal resource. Geochemical and isotopic results also demonstrate that the hot spring is fed by local groundwater, equilibrated with the carbonate rocks but without isotopic exchange with the matrix. Trace elements, particularly As (119 µg/L), display high concentrations, raising some concern about potential environmental and health effects.

Genesis of Graphite in Metapelites in the North-Western Border of the Lypniazhka Massif (the Inhul Domain of the Ukrainian Shield)

2021 ◽  
Vol 43 (2) ◽  
pp. 12-28
Author(s):  
N.M. LYZHACHENKО ◽  
S.I. KURYLО ◽  
S.M. BONDARENKO ◽  
R. MILOVSKY ◽  
S. MILOVSKA
Keyword(s):  
Carbon Isotope ◽  
Raman Spectra ◽  
Ukrainian Shield ◽  
Metamorphic Rocks ◽  
Biogenic Origin ◽  
Raman Spectroscopic ◽  
The North ◽  
Western Border ◽  
Graphite Structure ◽  
North Western

This study presents results of an investigation of metamorphic rocks of the Inhul-Inhulets series located in the northwestern border of the Lypniazhka granite-migmatite massif (Inhul domain, the Ukrainian Shield). The rocks were studied petrographically and mineralogically and carbon isotope, Raman spectroscopic and microprobe measurements were made. Graphite and calcite were given special attention. Metapelites and quartz-rich graphite-biotite-garnet rocks were investigated. The former consist of biotite, graphite-biotite, amphibole-bearing graphite-biotite gneisses. Graphite in them is evenly distributed through the rock groundmass. The δС13 values of graphite lie between -39.4‰ and -33.6‰ (relative to PDB). The graphite is considered to be of biogenic origin. Quartz-rich graphite-biotite-garnet rocks are less common, but they also contain graphite. The latter occurs as inclusions in the major minerals either forming clusters. Its δС13 values fall between -28.45‰ and -22.2‰ (relative to PDB). Based on the Raman spectra, carbon from the gneisses has an ordered graphite structure. The temperature of graphite crystallization was estimated to be between 554 and 630°С and corresponds to the amphibolite facies.

scholarly journals The Mammals of Suffolk

Oryx ◽  
1956 ◽  
Vol 3 (5) ◽  
pp. 266-270
Keyword(s):  
Nineteenth Century ◽  
East Coast ◽  
Private Ownership ◽  
Wild Mammals ◽  
The North ◽  
Deciduous Woodland ◽  
Forestry Commission ◽  
Western Border ◽  
Coniferous Plantations ◽  
North Western

Suffolk is probably better known for its famous domestic “trinity of breeds”, the Suffolk Horse, the Red Poll Cow and the Suffolk Sheep, than for its wild mammals, though some of these last are interesting as being apparently at the extreme end of their geographical range. Everywhere it is one of the most highly keepered and over most of its area one of the most highly cultivated of all English counties, though there is a considerable acreage of light sandy heaths along the east coast and in the Breckland on the north western border, heaths now largely covered by the coniferous plantations of the Forestry Commission. Even on the better land there is a fairly considerable acreage of mixed deciduous woodland in private ownership, most of it planted during the first half of the nineteenth century as pheasant coverts.

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