scholarly journals TERRITORIAL AND ETHNIC EXCLUSION IN THE METROPOLIS OF LYON

Author(s):  
Alina S. Khusainova ◽  
◽  
Darya S. Elmanova ◽  

This study is dedicated to identifying residential areas of the Metropolis of Lyon, which combines territorial and ethnic exclusion. In the framework of this study, territorial exclusion is understood as the territorial isolation of residential areas from the main residential area of the agglomeration due to the presence of various kinds of territorial barriers: water bodies, industrial and commercial areas, parklands, large highways. Ethnic exclusion in this study is understood as a partial exclusion from society (social exclusion) of population groups that are ethnically different from the main part of the population. The share of immigrants in the population of the communes and the share of social housing in the total housing stock of the communes of the Metropolis of Lyon were used as markers of ethnic exclusion. A comparison of territorially isolated residential quarters and data on the share of immigrants and the share of social housing revealed social housing quarters that combine signs of ethnic and territorial exclusion of the population: Mas-du-Taureau in the commune Vaulx-en-Velin in the north-east of the Metropolis of Lyon, Parilly and Terraillon in Bron in the east, Minguettes in Vénissieux in the south of the metropolitan area. During the interview, these social housing complexes were called by experts as the most disadvantaged and criminalized in the Metropolis of Lyon, which confirms the author’s hypothesis about the importance of territorial exclusion in the emergence and development of ethnic exclusion.

2009 ◽  
Vol 28 ◽  
Author(s):  
Tore Høisæter

Based on literature data and my extensive material from along the coast, the distribution of shell bearing marine, benthic gastropods known from Norwegian waters, is outlined. The geographic area covered goes down to c. 1200 m on the continental slope, and extends from the Swedish border<br />in the south to the Russian border in the north-east. On the slope the distribution is restricted to an area east of 0°, and south of 72° N. Neither the North Sea nor the western ‘slope’ of the Norwegian Trench are included. Systematics and nomenclature follow Clemam (Check List of European Marine Mollusca) closely. The emphasis is on the distribution of each species within the designated area, but taxonomic and nomenclaturial problems are discussed wherever considered relevant. Altogether 365 species level taxa are included, of which 326 are considered as definitely belonging to the Norwegian fauna. The rest are recorded as doubtful, either because only empty shells have been found, or their confirmed distribution falls outside the limits here defined. Of the ‘species’ included, I consider at least 18 to be undescribed, while another 16 were described from Norwegian material after Høisæter (1986) was published. The northern distributional limit is extended for 47 species, while 11 species have received a new southern limit. Sixty six species have a generic name diferent from the one used in Høisæter (1986), while 35 species have another specific name. All changes are listed in the main part of the article, and references are given to the sources for the changes. Four faunal components are recognized: a slope component, species mainly found in negative temperatures on the continental slope, between 500 and 1200 m; an Arctic component, species in Norway almost exclusively found in East Finnmark; a group of species in Norway found only or mainly on the Skagerrak coast or in Oslofjorden; and finally the main group found along most of the coast.


Palaeobotany ◽  
2017 ◽  
Vol 8 ◽  
pp. 28-44 ◽  
Author(s):  
L. B. Golovneva ◽  
S. V. Shczepetov ◽  
A. E. Livach

The analysis of the distribution of plant remains in deposits of the Aigur and Toptan formations (Omsukchan district of the Magadan Region) showed that the main part of the species that were included in the Toptan stratoflora (Samylina, 1976), in fact come from the Aigur Formation. Floristic assemblages of the Aigur and Toptan formations are very similar in systematic composition. Increasing the diversity of flowering plants and reduction of typical Cretaceous taxa (cycadophytes and Ginkgoales was not indicated on the boundary between these formation. Thus, there is no evidence of significant changes in the floristic composition at this stratigraphic level and the existence of independent Toptanian stage in the evolution of the mid-Cretaceous flora of the North-East of Russia. Floristic assemblages from the Galimyi, Aigur and Toptan formations are proposed to be merged into a single Sugoi flora, which should be attributed to the Buor-Kemus stage of floral development (lower-middle Albian). The description of the lectostratotype of the Toptan Formation is first published and distribution of this formation is illustrated.


2016 ◽  
Vol 56 (4) ◽  
pp. 511-524 ◽  
Author(s):  
V. M. Lytkin ◽  
A. A. Galanin

The remote map‑making technique and results of field investigations made possible for the first time to reveal a great number of rock glaciers within the area of the Suntar‑Khayata Range (North‑East Asia). A total of 540 formations were identified. Among them, 47 rock glaciers were classified as corrie (cirque) tongue‑shaped formations and 493 ones – as niche lobe‑shaped (single‑ and multi‑lobe) rock glaciers. Occurrence of such formations is 8.4/100 km2, that is the largest in the North‑East Asia. The rock glaciers in this region are found within a range of true altitudes from 1297 up to 2402 m asl. The majority of active features, however, are confined to the interval between 1500 and 1900 m asl. Rock glaciers occur in the altitudinal range of 1297 to 2402 m asl. The majority of active features, however, are confined to the interval between 1500 and 1900 m asl, and the main part of active formations is located within the range of 1500‑2500 m. The frequency analysis of true altitudes of the rock‑glacier occurrence indicates that their formation can be caused by the hypsometry of the region relation to morphoclimatic zonality.


2021 ◽  
Vol 881 (1) ◽  
pp. 012063
Author(s):  
E Wulandari ◽  
Z Zahriah ◽  
Z Fuady ◽  
F Sabila

Abstract Ujung Pancu is on the North coast of Aceh, known as one of three defense areas (Lhee Sagoe) during the Aceh Darussalam Kingdom, in 18-19 centuries guarding against enemy attacks from the sea, and the role of Hamzah Fansury in the 16-17 centuries. This area has destroyed when the tsunami disaster, causing some traces of the old city to be relatively lost but still can be traced. This paper aims to reconstruct and discuss the concept of Ujung Pancu spatial structure, especially Lam PageuVillage in the 18th century. It also will examine the approximate architecture of the Hamzah Fansury cultural site. This paper is considered essential as a historical study to bring back the experience of cultural sites as national personality assets under the UNESCO concept and has the opportunity to be a religious cultural tourism destination around Banda Aceh City, as well as being a location for religious relaxation in the face of the Covid 19 outbreak. This study uses exploration by exploring the potential of the natural environment and reconstructing the regional spatial organization system and spatial patterns. The results show that a) The area organizing system is very considerate of the coastal-bay-hills ecological aspect, with the orientation of the area towards the sea in the North-East, with the hills as natural fortresses in the West-Southern part, the three main spots are important areas with the system integrated location of each other; b) 3 important spots, namely: 1). the location of the cleric Hamzah Fansury’s hermitage on the hills, it is estimated that it also functions as a “reconnaissance” place; 2) Footprints of the harbor fort on the beach are inundated, 3) Coastal residential areas that are still ongoing today. The conclusion of the study, the regional spatial management system shows a spatial hierarchy based on security zones, the closer to the mountain the more private, and the closer to the beach the more common (profane). There is a synergy between the need to maintain regional space and natural character.


2015 ◽  
Vol 78 ◽  
pp. 854-859 ◽  
Author(s):  
Miaomiao He ◽  
Alexander Brownlee ◽  
Timothy Lee ◽  
Jonathan Wright ◽  
Simon Taylor

2010 ◽  
Vol 2 (2) ◽  
pp. 5-10
Author(s):  
Jurgita Alchimovienė ◽  
Neringa Gudienė

Territory planning instructions of residential areas (quarters) are analyzed in this article. In Lithuania there is no validated united normative database for territory planning, which could regulate renovation of residential quarters. Accordingly, it is an actual problem. Modernization of blocks of flats is widely analyzed and it causes a lot of discussions recently. Modernization could be fulfilled more efficiently in quarters or even residential areas. Consequently, territorial spatial planning of areas (quarters) is very important. This article covers analysis of terms of a residential area and a quarter, building intensity and building density, functional zones, regulations of territory management and use, greenery, social infrastructure. Also a quality of life, depreciation of buildings and a priority of renovation of residential areas is examined.


Antiquity ◽  
1976 ◽  
Vol 50 (200) ◽  
pp. 216-222
Author(s):  
Beatrice De Cardi

Ras a1 Khaimah is the most northerly of the seven states comprising the United Arab Emirates and its Ruler, H. H. Sheikh Saqr bin Mohammad al-Qasimi, is keenly interested in the history of the state and its people. Survey carried out there jointly with Dr D. B. Doe in 1968 had focused attention on the site of JuIfar which lies just north of the present town of Ras a1 Khaimah (de Cardi, 1971, 230-2). Julfar was in existence in Abbasid times and its importance as an entrep6t during the sixteenth and seventeenth centuries-the Portuguese Period-is reflected by the quantity and variety of imported wares to be found among the ruins of the city. Most of the sites discovered during the survey dated from that period but a group of cairns near Ghalilah and some long gabled graves in the Shimal area to the north-east of the date-groves behind Ras a1 Khaimah (map, FIG. I) clearly represented a more distant past.


1999 ◽  
Vol 110 (5-6) ◽  
pp. 455-463 ◽  
Author(s):  
S. Güvenç ◽  
Ş Öztürk
Keyword(s):  

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