Stature Trend of Korean Male Adults in the Colonial Period －Focusing on Police Records in the South Sakhalin Area－

2021 ◽  
Vol 41 ◽  
pp. 47-82
Author(s):  
Young-Jun Cho
Keyword(s):  
Colonial Period ◽  
The South ◽  
South Sakhalin ◽  
Police Records

The source rocks in the southwestern part of the South Sakhalin Basin

2017 ◽  
Vol 72 (1) ◽  
pp. 63-74
Author(s):  
T. A. Kiryukhina ◽  
S. I. Bordunov ◽  
A. A. Solov’eva
Keyword(s):  
Source Rocks ◽  
The South ◽  
Southwestern Part ◽  
South Sakhalin

Quechua’s Southern Boundary: The Case of Santiago del Estero, Argentina

2012 ◽  
Author(s):  
ELIZABETH DeMARRAIS
Keyword(s):  
Colonial Period ◽  
Archaeological Record ◽  
The South ◽  
Population Movements ◽  
Southern Boundary ◽  
North West ◽  
Documentary Sources ◽  
The Andes ◽  
Continued Use

This chapter examines the far southern boundary of Quechua's spread throughout the Andes. It argues that Quechua reached north-west Argentina in Inka times and that it was widely used during the colonial period as well. The rationale for this argument is based primarily on evidence for (1) the extent of Inka resettlements in Argentina; (2) the nature of Inka relations with local peoples in the far south; and (3) continued use of Quechua under the Spaniards, as described in the documentary sources. Less clear are the precise population movements that brought Quechua speakers initially to Santiago del Estero, as the archaeological record suggests that the Inka frontier lay higher up the slopes in the provinces of Salta, Jujuy, Tucumán, and Catamarca, where the majority of Inka installations are found. The documents reveal that activities of the Spaniards had further, far-reaching consequences for Quechua's presence in the south Andes, and that ultimately Quechua was replaced in most of north-west Argentina by Spanish.

The Legacy of European Colonialism

2007 ◽  
Author(s):  
Gregory Knapp
Keyword(s):  
Eighteenth Century ◽  
Fifteenth Century ◽  
New Technologies ◽  
Colonial Period ◽  
Resource Extraction ◽  
South American ◽  
The South ◽  
European Colonialism ◽  
The Impact ◽  
The Guianas

South America was first “encountered” by Europeans during Columbus’ third voyage in 1498. This marked the end of the pre-Columbian period of the continent, and the beginning of the colonial period that lasted until the end of the wars of independence in the early nineteenth century. Total liberation of the continent from Spain was finally achieved at the Battle of Ayacucho in 1824. Brazilian independence from Portugal was achieved more peacefully in 1822, when Dom Pedro became constitutional emperor. The Guianas remained colonies far longer; indeed Guyane (French Guiana) is still an overseas department of France, while Suriname (Dutch Guiana) became independent in 1975, and Guyana (originally a Dutch colony, later British) became independent in 1966. It could be suggested that dependency remained after the end of formal colonial rule, owing to the continued influence of global economic powers on the continent. However, for the purposes of this chapter, the colonial period can be considered as lasting for 326 years from 1498 to 1824. If recent research has tended to enhance our appreciation of the impact of pre-Columbian peoples on the South American environment, it has also corrected some stereotypes concerning European colonial impacts. Europeans were not the first to substantially impact the South American environment. The colonial period was generally marked by depopulation and agricultural disintensification, with the result that many environments were more “pristine” at the end of the eighteenth century than at the end of the fifteenth century. Migrations, cultural hybridities, and new local, regional, and global economic linkages led to changes in demands on agriculture and resource extraction. New technologies, crops, and social structures also had an impact. These impacts were not always as negative as sometimes portrayed, and local populations often had a substantial say in the outcome. Many of the most noticeable impacts resulting from the encounter with Europeans did not become widespread until after independence (McAlister, 1984; Bethell, 1987; Hoberman, 1996; Hoberman et al., 1996; Mörner, 1985; Newson, 1995; Robinson, 1990; Butzer and Butzer, 1995).

scholarly journals The New Avalanche-Like Stochastic Model for Parameterization of Seismicity and Its Application to the South Sakhalin Island Seismicity

2012 ◽  
Vol 2012 ◽  
pp. 1-12 ◽  
Author(s):  
M. V. Rodkin ◽  
I. N. Tikhonov
Keyword(s):  
Stochastic Model ◽  
Hierarchical Structure ◽  
Strong Earthquake ◽  
Sakhalin Island ◽  
Seismic Process ◽  
The South ◽  
Anomalous Increase ◽  
Seismic Regime ◽  
South Sakhalin ◽  
Two Parameters

Seismic process is usually considered as an example of occurrence of the regime of self-organizing criticality (SOC). A model of seismic regime as an assemblage of randomly developing episodes of avalanche-like relaxation, occurring at a set of metastable subsystems, can be the alternative of such consideration. The model is defined by two parameters characterizing the scaling hierarchical structure of the geophysical medium and the degree of metastability of subsystems of this medium. In the assemblage, these two parameters define a modelb-value. An advantage of such approach consists in a clear physical sense of parameters of the model. The application of the model for parameterization of the seismic regime of the south part of Sakhalin Island is considered. The models of space changeability of the scaling parameter and of temporal changeability of the parameter of metastability are constructed. The anomalous increase of the parameter of metastability was found in connection with the Gornozavodsk and Nevelsk earthquakes. At the present time, high values of this parameter occur in the area of the Poyasok Isthmus. This finding is examined in comparison with other indications of an increase in probability of occurrence of a strong earthquake in the South Sakhalin region.

scholarly journals Laboratory research of geomechanical parameters of sedimentary rocks massifs in the South Sakhalin

2017 ◽  
Vol 1 (1) ◽  
pp. 30-36 ◽  
Author(s):  
P.A. Kamenev ◽  
◽  
O.M. Usoltseva ◽  
P.A. Tsoi ◽  
V.N. Semenov ◽  
...  
Keyword(s):  
Sedimentary Rocks ◽  
Laboratory Research ◽  
The South ◽  
Geomechanical Parameters ◽  
South Sakhalin

scholarly journals Analysis and revision of the Miocene boreal faunae of bivalve mollusks of the South Sakhalin

2020 ◽  
Author(s):  
В.Д. ХУДИК ◽  
Ю.Д. ЗАХАРОВ
Keyword(s):  
Japan Sea ◽  
Climatic Conditions ◽  
Bivalve Mollusks ◽  
The South ◽  
The North ◽  
Initial Stage ◽  
The Japan Sea ◽  
South Sakhalin ◽  
Early Neogene ◽  
Climatic Cooling

Приведены результаты изучения остатков фаун двустворчатых моллюсков из миоценовых отложений Южного Сахалина. Их анализ позволил выделить три бореальных комплекса моллюсков: невельский, раннечеховский и курасийский, фиксирующие периоды похолодания климата в миоцене региона. Изучение неогеновых представителей родов Lucinoma и Mya позволило обозначить среди них ряд таксонов, имеющих стратиграфическое значение. Установленное присутствие тепловодных двустворок в фаунах позднечеховского времени Южного Сахалина, очевидно, отражает собой начальный этап тенденции нарастающего потепления климата в миоцене региона с климатическим оптимумом в верхнедуйско-сертунайское время. Высказывается следующее мнение: неустойчивые климатические условия в позднем палеогене – раннем неогене северной части Япономорского региона могли быть основной причиной возникновения здесь одного из мощных центров эволюции морских малакофаун бореальных районов северной Пацифики. The results on the studying of the faunae of bivalve mollusks remains from miocene deposits of the South Sakhalin are presented. The analysis of the last ones allowed distinguishing the following three boreal assemblages of mollusks: Nevelskiy, early Chekhovskiy and Kurasiiskiy, recording the period of climatic cooling in miocene of the region. Studying of Neogene representatives of Lucinoma and Mya generas allowed identifying some taxa among them which have stratigraphic significance. The detected presence of warm water bivalves in the faunae of the late Chekhovsky time of the South Sakhalin appears to reflect the initial stage of the tendency of the intensifying climate warming happened during miocene, with climatic optimum during the Verkhneduysky – Sertunaysky times. An opinion is expressed that the unstable climatic conditions in the northern part of the Japan Sea region during late Paleogene – early Neogene could have been the main reason for originating of one of the high-potential centers of evolution of the marine malacofaunae of boreal regions of the North Pacific.

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