scholarly journals RESEARCH OF BATYRBEK MOUNDS ON NARYN SAND

2021 ◽  
Author(s):  
Marat Kasenov
Keyword(s):  
Iron Age ◽  
Sandy Loam ◽  
Northwestern Part ◽  
The Caspian Sea ◽  
North East ◽  
The North ◽  
West Kazakhstan ◽  
Western Side ◽  
Clay Rocks ◽  
Archaeological Excavations

The article presents the results of archaeological excavations on the Batyrbek Mound on the Naryn sand. The Naryn sands are located in the northwestern part of the Caspian Basin, between the Volga and Ural rivers. Administrative covers Isatai Was Makhambet areas of Atyrau region and the southern part of Bokey Orda, Zhangala and Akzhaiyk parts of the West Kazakhstan region. The area is 40 thousand km 2. The sandy zone is on average 21 m below sea level. The region is formed by deposits of the Khvalyn and Khazar periods of the Caspian Sea. Consists of arrays Batbayar, Botany, Condulet, Manteca Arcticum, Zhamankum Horde. The north-East is occupied by the Kamyshovo-Samara floodplain. Often the wind blows, a dust storm. A river with a constant flow of no streams. Fresh water reserves underground (at a depth of 1.5-2 m) are plentiful. There are many wells and oases. The spring floodplain runoff of Karaozen and Saryozen sometimes irrigates the northern side of the Naryn sand. The soil cover consists mainly of pale brown, sandy loam, and salt-gray soils[1]. In September 2019, excavations were carried out of 2 burial grounds dating back to the Iron Age, located 3.36 km south of the village of Batyrbek, located on the north-western side of the Kurmangazinsky district of Atyrau region. In archaeological excavations, tombs typical of the Iron Age were discovered. 4 graves were discovered, buried in the late period. The article covers the research of these mounds. The mounds are found in the northwestern part of the Naryn sand, in the steppe areas of «takyr», consisting of hard clay rocks. There were hundreds of Iron Age burial mounds in these areas. The mound was excavated for the first time.

Bronze Age Barrows on Charmy Down and Lansdown, Somerset

1950 ◽  
Vol 30 (1-2) ◽  
pp. 34-46 ◽  
Author(s):  
Audrey Williams
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
The South ◽  
Stream Flows ◽  
North East ◽  
The North

Charmy Down is a plateau three miles north-east of Bath (fig. 1, 1), east of the Bath-Tetbury road. About a square mile in extent it has a general height of well over 600 ft. To the north the scarp falls swiftly, on the east more gently, to the wooded valley of St. Catherine's Brook, a tributary of the Bristol Avon and the modern Somerset–Gloucester boundary. At the foot of the steep western scarp a second stream flows south to the Avon. On the south Chilcombe Bottom separates Charmy Down from Solsbury Hill, distinguished by its Iron Age earthwork. The underlying rock is oolite, a southward continuation of the Cotswold formation.

scholarly journals All the Roads to Patavium: Morphology, Genesis and Development of the Roman Road Network Around Padua

2017 ◽  
Vol 3 (1) ◽  
Author(s):  
Michele Matteazzi
Keyword(s):  
Iron Age ◽  
Late Antiquity ◽  
Road Network ◽  
Methodological Approach ◽  
13Th Century ◽  
Urban Centers ◽  
Italian Peninsula ◽  
North East ◽  
The North ◽  
The City

Abstract This paper deals with the analysis of the ancient road network around the city of Padua, attempts to reconstruct its morphology and to define its genesis and development between the second Iron Age and Late Antiquity (6th/5th cent. BC to 6th cent. AD). The study follows a methodological approach that today we define as „archaeomorphological“, first proposed by E. Vion in the late 1980s. By applying this methodology to the Paduan territory, it was possible to identify a series of routes of probable ancient origin radially converging toward the center of Roman Patavium, and linking it to other urban centers in the region and to the minor centers located within its ager. The presence of Iron Age settlements along the path of many of these routes suggests that the development of such a road network likely begins in pre-Roman times, which also highlights the ancient strategic importance of Padua and its territory as a fundamental junction between the center and the North-East of the Italian peninsula. On the other hand, the Roman road network somehow survived into the Late Antiqueand Early Medieval times, always influencing the distribution of settlements and the orientation of churches, until it was for the greater part restored by the Commune of Padua over the 13th century.

scholarly journals STATE OF POPULATION OF PIKE PERCH OF THE LOWER FLOW OF THE URAL RIVER

2018 ◽  
pp. 83-89
Author(s):  
Sergey Vladimirovich Kuzmenko ◽  
Arkadii Fedorovich Sokolsky ◽  
Alexander Nickolaevich Nevalennyy ◽  
Nikolay Nikolayevich Popov
Keyword(s):  
Caspian Sea ◽  
Fishing Ground ◽  
Commercial Fishing ◽  
The Caspian Sea ◽  
Foreign Markets ◽  
North East ◽  
The North ◽  
Pike Perch ◽  
Exploration And Production ◽  
Commercial Species

In domestic and foreign markets a great demand for pike perch is caused by the fact that its meat is a digestible and dietetic product. Due to growing scales of exploration and production of oil, as well as of poaching in the last years pikeperch and other species suffer from anthropogenic load. In 1990 spike perch catches reached 4.49.000 tons and made 1/3 of total catch of semi anadromous and river fish. During the last decade pike perch catches have decreased in the Ural-Caspian region up to 380 t, according to data of 2016. The study of pike perch populations on fishing zones of the Ural (delta, Malaya Dambinskaya fishing ground) covered the data obtained in 2010-2016. There have been studied migrating periods of pike perch to the spawning grounds. Since 2011 there has been stated a drastic decrease of sire number and a much less catch of pike perch per one casting in autumn, which was caused by the permission for fishing in the coastal part of the Caspian Sea. According to the research data, there have been given size-weight parameters of pike-perch producers in the Ural river during 10 years (2006-2016). The tendency to juvenation of spawning pike perch species is stated due to increasing share of the first spawning species, as well as due to decreasing number of male species in the catches as their age increased. Fultin and Clark’s condition coefficients are shown. Importance of pike perch as a commercial species in the ecosystem of the Ural-Caspian fishery zone contributes to define the following recommendations on saving and restoring pike perch population: to reduce commercial catches in the estuarine area of the Ural; to forbid commercial fishing in the coastal area of the north-east part of the Caspian Sea; to intensify fishery inspection in the Urals.

scholarly journals Mapping of S4 Over the Arabian Peninsula During Solar Minimum

2021 ◽  
Author(s):  
Abdollah Darya ◽  
Muhammad Shaikh ◽  
Ilias Fernini ◽  
Hamid AlNaimiy
Keyword(s):  
Solar Minimum ◽  
Arabian Peninsula ◽  
Ionospheric Irregularities ◽  
Scintillation Index ◽  
Study Region ◽  
Amplitude Scintillation ◽  
North East ◽  
The North ◽  
Western Side ◽  
Using Data

In this letter, we study the temporal and spatial variability of ionospheric irregularities by generating high-resolution maps of the observed amplitude scintillation index (S4) using data from a multi-constellation and multi-frequency GNSS receiver. The study region is the Arabian Peninsula, which falls under the northern crest of the equatorial ionization anomaly (EIA). Even though the study was conducted during a solar minimum period, considerable occurrences of pre-sunset scintillation have been observed between 15-17 local time, particularly during the winter solstices. While most scintillation occurrences have been observed at low elevation (15 to 30 degrees), a considerable number of scintillation patches have been observed towards the north, east, and southeast of the receiver location, for elevation angles ranging from 40 to 60 degrees. Our analysis shows that BeiDou geostationary orbit (GEO) and inclined GEO (IGSO) satellites may have been the main contributor to the increased number of scintillation occurrences observed around the eastern side of the receiver as compared to the western side. Out of all the GNSS constellations with MEO satellites, GPS was the most impacted by amplitude scintillation, while BeiDou and Galileo satellites were the least affected. It is anticipated that the patches of ionospheric irregularities reported in this work would be further enhanced as the solar activity increases in the coming years. Therefore, this work can serve as a reference for future studies during periods of increased geomagnetic activity.

scholarly journals Shipping amphorae and shipping sheep? Livestock mobility in the north-east Iberian peninsula during the Iron Age based on strontium isotopic analyses of sheep and goat tooth enamel

PLoS ONE ◽  
2018 ◽  
Vol 13 (10) ◽  
pp. e0205283 ◽  
Author(s):  
Silvia Valenzuela-Lamas ◽  
Hector A. Orengo ◽  
Delphine Bosch ◽  
Maura Pellegrini ◽  
Paul Halstead ◽  
...  
Keyword(s):  
Iberian Peninsula ◽  
Iron Age ◽  
Tooth Enamel ◽  
North East ◽  
The North ◽  
Isotopic Analyses

Economic change after the agricultural revolution in Southeast Asia?

Antiquity ◽  
2014 ◽  
Vol 88 (339) ◽  
pp. 112-125 ◽  
Author(s):  
Charlotte L. King ◽  
R. Alexander Bentley ◽  
Charles Higham ◽  
Nancy Tayles ◽  
Una Strand Viðarsdóttir ◽  
...  
Keyword(s):  
Iron Age ◽  
Regional Differences ◽  
Isotope Analysis ◽  
River Valley ◽  
Seventh Century ◽  
Early States ◽  
North East ◽  
The North ◽  
Agricultural Revolution ◽  
North Eastern

Three prehistoric sites in the Upper Mun River Valley of north-eastern Thailand have provided a detailed chronological succession comprising 12 occupation phases. These represent occupation spanning 2300 years, from initial settlement in the Neolithic (seventeenth century BC) through to the Iron Age, ending in the seventh century AD with the foundation of early states. The precise chronology in place in the Upper Mun River Valley makes it possible to examine changes in social organisation, technology, agriculture and demography against a background of climatic change. In this area the evidence for subsistence has been traditionally drawn from the biological remains recovered from occupation and mortuary contexts. This paper presents the results of carbon isotope analysis to identify and explain changes in subsistence over time and between sites, before comparing the results with two sites of the Sakon Nakhon Basin, located 230km to the north-east, to explore the possibility of regional differences.

scholarly journals Notes on some animal parasites in British Guiana

1916 ◽  
Vol 7 (2) ◽  
pp. 179-190 ◽  
Author(s):  
G. E. Bodkin ◽  
L. D. Cleare
Keyword(s):  
Sea Level ◽  
Sand Dunes ◽  
Coastal Region ◽  
The South ◽  
British Guiana ◽  
North East ◽  
The North ◽  
South West ◽  
Western Side ◽  
River Valleys

British Guiana lies between the latitudes 0·41′ N. (source of the Essequebo River) and 8° 33′ 22″ N. (Punta Playa), has a depth from north to south of about 500 miles, a seaboard of about 270 miles trending in a south-easterly direction, and occupies in the north-east of South America an area approximately equal in extent to Great Britain. It is bounded on the north by the Atlantic Ocean, on the east by Surinam or Dutch Guiana, on the south and south-west by Brazil, and on the west by Venezuela.The Colony may be divided broadly into three belts. The northern one consists of a low-lying flat and swampy belt of marine alluvium—the coastal region. This rises gradually from the seaboard and extends inland for a distance varying from 5 to 49 miles. It is succeeded by a broader and slightly elevated tract of country of sandy and clayey soils. This belt is generally undulating, and is traversed in places by sand-dunes rising from 50 to 180 ft. above sea-level. The more elevated portion of the Colony lies to the southward of the above-mentioned regions. It rises gradually to the south-west, between the river valleys, which are in many parts swampy, and contains three principal mountain ranges, several irregularly distributed smaller ranges, and in the southern and eastern parts numerous isolated hills and mountains. The eastern portion is almost entirely forest-clad, but on the south-western side there is an extensive area of flat grass-clad savannah land elevated about 300 feet above sea-level.

scholarly journals Mapping of S4 Over the Arabian Peninsula During Solar Minimum

2021 ◽  
Author(s):  
Abdollah Darya ◽  
Muhammad Shaikh ◽  
Ilias Fernini ◽  
Hamid AlNaimiy
Keyword(s):  
Solar Minimum ◽  
Arabian Peninsula ◽  
Ionospheric Irregularities ◽  
Scintillation Index ◽  
Study Region ◽  
Amplitude Scintillation ◽  
North East ◽  
The North ◽  
Western Side ◽  
Using Data

In this letter, we study the temporal and spatial variability of ionospheric irregularities by generating high-resolution maps of the observed amplitude scintillation index (S4) using data from a multi-constellation and multi-frequency GNSS receiver. The study region is the Arabian Peninsula, which falls under the northern crest of the equatorial ionization anomaly (EIA). Even though the study was conducted during a solar minimum period, considerable occurrences of pre-sunset scintillation have been observed between 15-17 local time, particularly during the winter solstices. While most scintillation occurrences have been observed at low elevation (15 to 30 degrees), a considerable number of scintillation patches have been observed towards the north, east, and southeast of the receiver location, for elevation angles ranging from 40 to 60 degrees. Our analysis shows that BeiDou geostationary orbit (GEO) and inclined GEO (IGSO) satellites may have been the main contributor to the increased number of scintillation occurrences observed around the eastern side of the receiver as compared to the western side. Out of all the GNSS constellations with MEO satellites, GPS was the most impacted by amplitude scintillation, while BeiDou and Galileo satellites were the least affected. It is anticipated that the patches of ionospheric irregularities reported in this work would be further enhanced as the solar activity increases in the coming years. Therefore, this work can serve as a reference for future studies during periods of increased geomagnetic activity.

scholarly journals Mapping of S4 Over the Arabian Peninsula During Solar Minimum

2021 ◽  
Author(s):  
Abdollah Darya ◽  
Muhammad Shaikh ◽  
Ilias Fernini ◽  
Hamid AlNaimiy
Keyword(s):  
Solar Minimum ◽  
Arabian Peninsula ◽  
Ionospheric Irregularities ◽  
Scintillation Index ◽  
Study Region ◽  
Amplitude Scintillation ◽  
North East ◽  
The North ◽  
Western Side ◽  
Using Data

In this letter, we study the temporal and spatial variability of ionospheric irregularities by generating high-resolution maps of the observed amplitude scintillation index (S4) using data from a multi-constellation and multi-frequency GNSS receiver. The study region is the Arabian Peninsula, which falls under the northern crest of the equatorial ionization anomaly (EIA). Even though the study was conducted during a solar minimum period, considerable occurrences of pre-sunset scintillation have been observed between 15-17 local time, particularly during the winter solstices. While most scintillation occurrences have been observed at low elevation (15 to 30 degrees), a considerable number of scintillation patches have been observed towards the north, east, and southeast of the receiver location, for elevation angles ranging from 40 to 60 degrees. Our analysis shows that BeiDou geostationary orbit (GEO) and inclined GEO (IGSO) satellites may have been the main contributor to the increased number of scintillation occurrences observed around the eastern side of the receiver as compared to the western side. Out of all the GNSS constellations with MEO satellites, GPS was the most impacted by amplitude scintillation, while BeiDou and Galileo satellites were the least affected. It is anticipated that the patches of ionospheric irregularities reported in this work would be further enhanced as the solar activity increases in the coming years. Therefore, this work can serve as a reference for future studies during periods of increased geomagnetic activity.

scholarly journals Excavations of the burial mound near the Yalta village in 2019

2020 ◽  
Vol 10 (28-29) ◽  
pp. 31-51
Author(s):  
Viacheslav Zabavin ◽  
◽  
Serhij Nebrat ◽  
Keyword(s):  
Material Culture ◽  
Bronze Age ◽  
Iron Age ◽  
Early Iron Age ◽  
Burial Mound ◽  
State University ◽  
North East ◽  
The North ◽  
New Research ◽  
Sea Area

The article presents the results of new research of the archeological expedition conducted by Mariupol State University in the North-East Azov Area. Archaeological research was carried out in the South of Donetsk region near the village of Yalta in 2016. In the mound 9 graves of the Bronze Age and 1 burial of the early Iron Age were investigated. The primary embankment was built during the Early Bronze Age by the tribes of the Pit Grave culture. The oldest burials in the mound are 4, 5 and 7. The most interesting was the children's burial 7. The buried child was accompanied by four ceramic vessels. Subsequently, another grave of the Pit Grave culture was built in the mound – burial 8. During the Late Bronze Age the population of the Zrubna / Timber-grave culture continues to use the necropolis. Researched at least three burials of the Zrubna / Timber-grave culture – 1, 2 and 10. Based on the typological analysis of the ritual-inventory complex, they can be attributed to the second (developed) horizon of the Zrubna / Timber-grave culture burial grounds of the North Azov Sea Area. As regards burial 3, presented by the authors, date back to the early Iron Age and precede the sites of the Scythian time. The burial 3 from Yalta are determined as complex of Chernohorivka type / Chernohorivka group of Cimmerian Culture or as late Chernohorivka complex. The authors consider peculiarities of the rite and inventory complex as well as some aspects of cultural and chronological character, spiritual and material culture of the tribes which, in the researchers’ view, are conflated with the historical Cimmerians. The burial in the mound placed near the villag of Yalta demonstrate some certain features of ingenuity. The man buried in the mound was most likely to have something to do with the religious or the hieratic sphere of life. The materials of the investigated burial mound enrich our knowledge about the ancient past of the population of the Azov steppes.

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