scholarly journals Типология таштыкских поминов южной части Хакасско-Минусинской котловины

2021 ◽  
Vol 70 (5) ◽  
pp. 155-158
Author(s):  
О.А. Артонова

The article deals with the Tashtyk commemorations that existed in the HunnoXianbian era. Based on the study and systematization of ground, intra-stone structures and the composition of offerings, the typology of Tashtyk commemorations located in the south of the Khakass-Minusinsk basin is performed

Author(s):  
E.V. Vashchenko ◽  
◽  
P.A. Zubritskiy ◽  
A.L. Lelekova ◽  
◽  
...  

The results of research for 2014–2019 for 16 observation wells – indicators of total hardness, iron and manganese content-were processed. On the example of the site located in the area of Ust-Abakan and Chernogorsk, the analysis of factors that determine the increased concentrations of manganese and iron was carried out.


Author(s):  
Peter Fischer ◽  
Teresa Bürge ◽  
Laerke Recht ◽  
Dominika Kofel ◽  
David Kaniewski ◽  
...  

In the seventh season at the Bronze Age city of Hala Sultan Tekke excavations continued in City Quarter 1 (CQ1) where georadar indicated stone structures to the south of the area excavated in 2010–2012. Massive domestic structures, which belong to three phases of occupation (Strata 1–3), were exposed. Both the most recent Stratum 1, and Stratum 2 were destroyed in a conflagration. The three phases are preliminarily dated to the 13th and 12th centuries BC. Excavations were also carried out in Area A, roughly 600 m to the south-east of CQ1. Seven circular anomalies indicated by our geomagnetic survey were excavated. Two were pits of modern date, and three were identified as Late Cypriot wells. Another anomaly turned out to represent a rich Late Cypriot offering pit with figurines and more than 60 ceramic vessels. Amongst the Mycenaean vessels are several “chariot kraters” and a large vessel with the oversized image of a female robed in a splendidly adorned Minoan-style dress. The remaining anomaly probably represents a tomb of a very wealthy family so far containing, inter alia, 80 locally produced and imported vessels, gold jewellery, weapons, scarabs, and seals. The material in the offering pit and the tomb reflects far-reaching intercultural connections in the period from the 16th to the 13th centuries BC.


2007 ◽  
Vol 39 (2) ◽  
pp. 168-169
Author(s):  
Howayda Al-Harithy

After the cease-fire, I visited villages and towns in South Lebanon that suffered terrible destruction during the July 2006 war and that were facing the challenge of reconstruction. When I arrived to the border town of Bint Jbeil, I saw bulldozers demolishing beautiful, old stone structures. I stopped to inquire why; who authorized such actions and on what bases? With these questions, I approached the workers, the Council of the South (the government agency in charge of damage assessment and rubble removal), local residents, and the municipality. The answers varied: the structures were too damaged to save, we needed to widen the street, to build a better building, to erase the scars of war, to get full compensation, and so forth.


Antiquity ◽  
1942 ◽  
Vol 16 (64) ◽  
pp. 307-319
Author(s):  
Cyril Fox

In 1937 the writer described in ANTIQUITY a series of cottages—the dwellings of crofters—in Llanychaer and adjacent parishes of northern Pembrokeshire. These were two-roomed stone structures with a central doorway on one side: the door opened into the living room where the most striking sight was the great open fireplace at the gable end, the chimney structure of which projected into the room. A number of such dwellings has recently been examined in a coastal district of the same county to the south of Milford Haven, in Castle-martin parish. These show variations in the character and plan of the open fireplace, which are of interest, and probably also of cultural significance; they also provide fresh evidence of the hearth-dairy association manifested at Llanychaer.


2018 ◽  
Vol 7 (2) ◽  
pp. 44-49
Author(s):  
Tamara Viktorovna Zlotnikova

This paper deals with the species and ecological structure of ornithological complexes on the territories of quarry excavations. The research was carried out in the left-bank part of the South Minusinsk basin. 6 quarries were researched all the year round, 4 quarries were researched incidentally. The quarries were of various purposes (extraction of sand, clay, rubble, storage of domestic garbage), age (from 1 to 15 years) and size (from 1 to 20 hectares). 39 species of birds have been identified, which is more than 15% of the avifauna of the basin. The largest numbers of species (from 4 to 6 each) are the Fringillidae, Corvidae, Sylviidae, Muscicapidae families. The nature of the species stay on the territory has been established. Nesting species have been recorded to be 19, visitors - 20. Only in summer there are 25 species, only in winter there are 7 species, 7 species more are marked on sites both in summer and winter. Dendrophilic and petrophilic species are mainly nested. The nesting of Passer montanus (L.) and Oenanthe oenanthe (L.) was marked on all sites, the nesting of Riparia riparia (L.) was marked on the majority sites. Most species are synanthropic. The species richness of birds is shown to be determined, first of all, by the habitat structure: the presence of vertical soil breaks, stone structures, trees, shrubs, grass cover, reservoirs. The presence of food waste and the nature of the surrounding biotopes are also of particular importance.


1962 ◽  
Vol 24 (2) ◽  
pp. 303-322 ◽  
Author(s):  
Bernard Cosman
Keyword(s):  

2000 ◽  
Vol 179 ◽  
pp. 201-204
Author(s):  
Vojtech Rušin ◽  
Milan Minarovjech ◽  
Milan Rybanský

AbstractLong-term cyclic variations in the distribution of prominences and intensities of green (530.3 nm) and red (637.4 nm) coronal emission lines over solar cycles 18–23 are presented. Polar prominence branches will reach the poles at different epochs in cycle 23: the north branch at the beginning in 2002 and the south branch a year later (2003), respectively. The local maxima of intensities in the green line show both poleward- and equatorward-migrating branches. The poleward branches will reach the poles around cycle maxima like prominences, while the equatorward branches show a duration of 18 years and will end in cycle minima (2007). The red corona shows mostly equatorward branches. The possibility that these branches begin to develop at high latitudes in the preceding cycles cannot be excluded.


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