CIETRZEW W POLSCE – MOŻLIWOŚCI ZACHOWANIA POPULACJI

2019 ◽  
Vol XII ◽  
pp. 1-1
Author(s):  
Robert Kamieniarz
Keyword(s):  
Environmental Changes ◽  
The Other ◽  
Black Grouse ◽  
Protected Species ◽  
Mountain Areas ◽  
The North ◽  
Other Hand ◽  
North Eastern ◽  
Regional Projects ◽  
North Eastern Part

In 1995 the black grouse was registered in the Polish list of protected species. The national black grouse protection plan has been prepared and a few regional projects of the conservation of grouse and its areas of occurrence have been implemented. Unfortunately, adverse trends have not been turned back in the majority of regions. On the other hand, the population occurrence area has even increased locally in the mountains. The registered changes in the area of black grouse occurrence indicate that this species has the greatest chance of survival in some mountain areas in the southern part of Poland and locally in lowlands in the north-eastern part of the country. However, it is necessary to stop and reverse the unfavourable environmental changes which have been registered in areas of black grouse occurrence.

Salt Trade in Goalpara District During Colonial Period

2019 ◽  
Vol 46 (2) ◽  
pp. 278-291
Author(s):  
Jaysagar Wary
Keyword(s):  
Colonial Period ◽  
The Other ◽  
High Status ◽  
Human Beings ◽  
Salt Production ◽  
The North ◽  
Other Hand ◽  
North Eastern ◽  
Salty Taste ◽  
Salt Trade

Salt is an essential commodity for human beings, and its demand has been increasing in the markets since the early days. There was no information regarding salt production in Assam during the precolonial and colonial periods. On the other hand, small salt brines existed in places like Sadiya, Burhat and Naga hills, but they were unaffordable. At that time, people used Khar, the burn ashes of certain trees which produced a salty taste instead of ready-made salt. The salt became a symbol of wealth which helped people maintain a high status in the society of Assam as well as in the Goalpara district. The salt of Bengal became very famous because of its affordability—its supply was also available at Goalpara in the colonial period. Thus, Goalpara became the centre of salt trade of the north-eastern frontier countries. This article will attempt to highlight the salt trade and its significance in the colonial period.

scholarly journals Between Russian and Belarussian: Dialects of Nevel district, Pskov Oblast

Slovene ◽  
2018 ◽  
Vol 7 (2) ◽  
pp. 303-320
Author(s):  
Anastasia I. Ryko
Keyword(s):  
The State ◽  
Russian Language ◽  
The Other ◽  
Real Situation ◽  
Standard Language ◽  
The Real ◽  
Contemporary State ◽  
The North ◽  
Other Hand ◽  
North Eastern

The article describes the contemporary state of the dialects spoken in the Nevelsky district (Russia, Pskov Province), which is bordering Belarus, in comparison with the north-eastern Belarusian dialects located on the other side of the state border. When establishing the linguistic areas, it was assumed that on one side of this border the dialects would change following the Standard Russian language, while on the other side they would follow Belarusian. However, the real situation is much more complicated: on one hand, some dialectal features disappeared under the influence of the respective standard language; on the other hand, quite often features of both dialects do not correspond to either Standard Russian or Standard Belarusian, and there are existing “Belarusian” features on the territory of Russian dialects.

Lichens of the “Beringia” Nature Park (north-eastern Chukotka Peninsula)

2009 ◽  
Vol 43 ◽  
pp. 172-189 ◽  
Author(s):  
I. I. Makarova ◽  
A. E. Katenin
Keyword(s):  
Wide Distribution ◽  
Lichen Species ◽  
The Other ◽  
The North ◽  
North Eastern ◽  
Nature Park ◽  
North Eastern Part

The list of lichen species includes 231 species found in the lower course of the rivers Chegitun and Utaveem in the north-eastern part of Chukotka Peninsula. The peculiarity of the region is a wide distribution of epiphytic and calcareous lichens in comparison with the other regions of Chukothka Peninsula.

The influence of submesoscale eddies on hydrochemical parameters and structural and functional characteristics of phytoplankton in the north-eastern part of the Black Sea

2019 ◽  
pp. 24-40
Author(s):  
Sergey B. Kuklev ◽  
Vladimir A. Silkin ◽  
Valeriy K. Chasovnikov ◽  
Andrey G. Zatsepin ◽  
Larisa A. Pautova ◽  
...  
Keyword(s):  
Anticyclonic Eddy ◽  
The Black Sea ◽  
Hydrochemical Parameters ◽  
North East ◽  
The North ◽  
Seasonal Thermocline ◽  
North Eastern ◽  
Quantitative Indicators ◽  
The City ◽  
North Eastern Part

On June 7, 2018, a sub-mesoscale anticyclonic eddy induced by the wind (north-east) was registered on the shelf in the area of the city of Gelendzhik. With the help of field multidisciplinary expedition ship surveys, it was shown that this eddy exists in the layer above the seasonal thermocline. At the periphery of the eddy weak variability of hydrochemical parameters and quantitative indicators of phytoplankton were recorded. The result of the formation of such eddy structure was a shift in the structure of phytoplankton – the annual observed coccolithophores bloom was not registered.

Ketilidian structure and the rapakivi suite between Lindenow Fjord and Kap Farvel, South-East Greenland

2000 ◽  
pp. 50-59
Author(s):  
Brian Chadwick ◽  
Adam A. Garde ◽  
John Grocott ◽  
Ken J.W. McCaffrey ◽  
Mike A. Hamilton
Keyword(s):  
Coastal Region ◽  
Field Work ◽  
Natural Environment Research Council ◽  
East Greenland ◽  
The North ◽  
Tectonic Processes ◽  
Field Investigations ◽  
North Eastern ◽  
Bad Weather ◽  
North Eastern Part

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Chadwick, B., Garde, A. A., Grocott, J., McCaffrey, K. J., & Hamilton, M. A. (2000). Ketilidian structure and the rapakivi suite between Lindenow Fjord and Kap Farvel, South-East Greenland. Geology of Greenland Survey Bulletin, 186, 50-59. https://doi.org/10.34194/ggub.v186.5215 _______________ The southern tip of Greenland is underlain by the Palaeoproterozoic Ketilidian orogen (e.g. Chadwick & Garde 1996; Garde et al. 1998a). Field investigations in the summer of 1999 were focused on the structure of migmatites (metatexites) and garnetiferous granites (diatexites) of the Pelite Zone in the coastal region of South-East Greenland between Lindenow Fjord and Kap Farvel (Figs 1, 2). Here, we first address the tectonic evolution in the Pelite Zone in that region and its correlation with that in the Psammite Zone further north. Then, the structure and intrusive relationships of the rapakivi suite in the Pelite Zone are discussed, including particular reference to the interpretation of the controversial outcrop on Qernertoq (Figs 2, 8). Studies of the structure of the north-eastern part of the Julianehåb batholith around Qulleq were continued briefly from 1998 but are not addressed here (Fig. 1; Garde et al. 1999). The field study was keyed to an interpretation of the Ketilidian orogen as a whole, including controls of rates of thermal and tectonic processes in convergent settings. Earlier Survey field work (project SUPRASYD, 1992–1996) had as its principal target an evaluation of the economic potential of the orogen (Nielsen et al. 1993). Ensuing plate-tectonic studies were mainly funded in 1997–1998 by Danish research foundations and in 1999 by the Natural Environment Research Council, UK. The five-week programme in 1999 was seriously disrupted by bad weather, common in this part of Greenland, and our objectives were only just achieved. Telestation Prins Christian Sund was the base for our operations (Fig. 2), which were flown with a small helicopter (Hughes MD-500).

New insights on the north-eastern part of the Ketilidian orogen in South-East Greenland

1999 ◽  
pp. 23-33 ◽  
Author(s):  
Adam A. Garde ◽  
John Grocott ◽  
Ken J.W. McCaffrey
Keyword(s):  
Sea Ice ◽  
Coastal Areas ◽  
East Greenland ◽  
Original Series ◽  
The North ◽  
North Eastern ◽  
North Eastern Part ◽  
Geological Research

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Garde, A. A., Grocott, J., & McCaffrey, K. J. (1999). New insights on the north-eastern part of the Ketilidian orogen in South-East Greenland. Geology of Greenland Survey Bulletin, 183, 23-33. https://doi.org/10.34194/ggub.v183.5201 _______________ During a five week period in August–September 1998 the poorly known north-eastern part of the Palaeoproterozoic (c. 1800 Ma) Ketilidian orogen between Kangerluluk and Mogens Heinesen Fjord in South-East Greenland (Fig. 1) was investigated in continuation of recent geological research in other parts of the orogen. The north-eastern part of the orogen is remote from inhabited areas. It is mountainous and comprises a wide nunatak zone which can only be reached easily by helicopter. Furthermore, access to coastal areas by boat is difficult because many parts of the coast are prone to be ice-bound even during the summer months, due to wind- and current-driven movements of the sea ice.

Colchicum autumnale (Colchicaceae) w okolicach Krakowa – dawne i obecne rozmieszczenie

2019 ◽  
pp. 15-27
Author(s):  
Magdalena Zarzyka-Ryszka
Keyword(s):  
Adjacent Area ◽  
Colchicum Autumnale ◽  
The Past ◽  
The North ◽  
North Eastern ◽  
New Localities ◽  
Present Distribution ◽  
The 19Th Century ◽  
North Eastern Part

The paper describes the past and present distribution of Colchicum autumnale in the vicinity of Cracow, highlights the role of Stanisław Dembosz (who published the first locality of C. autumnale near Igołomia in 1841). Gives information about the occurrence of C. autumnale in Krzeszowice in the 19th century (reported by Bronisław Gustawicz), presents new localities noted in 2012–2014 in meadows in the north-eastern part of the Puszcza Niepołomicka forest and adjacent area (between the Vistula and Raba rivers), and gives a locality found in Cracow in 2005 (no longer extant).

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