scholarly journals La risa, regulador social de los estados emocionales y la fijación del aprendizaje

TAYACAJA ◽  
2018 ◽  
Vol 1 (2) ◽  
Author(s):  
Edward Enrique Rojas de la Puente
Keyword(s):  
Social Relationship ◽  
Structured Interview ◽  
The Real ◽  
The North ◽  
A Value ◽  
The Social ◽  
North Eastern ◽  
Participative Action Research ◽  
North Eastern Part ◽  
Made In

The following “Theoretic proposal called: the laughter as the real emotional regulator,social and fixing of learnings” this study is conclusive in three fundamental principles: thelaughter is an emotional regulator, the laughter is a social regulator, the laughter is a fixinglearning. This was proved with students from the Toribio Rodríguez de Mendoza NationalUniversity of Amazonas – Peru and groups of people in study.The study was ethnographic-qualitative, with IAP or Participative Action Research. Themethodology was based on the transactional method. We used the qualitative method. Withits own qualitative categorizations of the social science. The technique were the observationand analysis. The data about the effect to arrive to those principles were collected withinstruments as the structured interview, a notebook and films. I can deduce that this is acontribution to the different kinds of socio-educative disciplines and others because we getnew principles mentioned in the first lines; which represents a theoretic contribution inteaching and learning.This study is made with a test and posttest design and with fortuitous groups whoseobjective is appreciate the real effect of laugh. This research with a value to education,sociology and others sciences that study the human being. In conclusion: the laugh moderatethe emotions, the laugh moderate the social relationship and finally the laugh is a fixer ofcomplex learning. The following research project was made in the Awajun ethnic inAmazonas region (out in the north-eastern part of Peru).Keywords: didactic technique, laughter, fixation and retention.

scholarly journals THE LAUGHTER, SOCIAL REGULATOR OF EMOTIONAL STATES AND FIXING OF LEARNING

10.23856/3012 ◽  
2018 ◽  
Vol 30 (5) ◽  
pp. 114-120
Author(s):  
Edward Enrique Rojas de la Puente
Keyword(s):  
Teaching And Learning ◽  
Structured Interview ◽  
Emotional States ◽  
The Real ◽  
The North ◽  
A Value ◽  
The Social ◽  
North Eastern ◽  
National University ◽  
Participative Action Research

The following “Theoretic proposal called: the laughter as the real emotional regulator, social and fixing of learnings” this study is conclusive in three fundamental principles: the laughter is an emotional regulator, the laughter is a social regulator, the laughter is a fixing learning. This was proved with students from the Toribio Rodríguez de Mendoza National University of Amazonas – Peru and groups of people in study. The study was ethnographic-qualitative, with IAP or Participative Action Research. The methodology was based on the transactional method. We used the qualitative method. With its own qualitative categorizations of the social science. The technique were the observation and analysis. The data about the effect to arrive to those principles were collected with instruments as the structured interview, a notebook and films. I can deduce that this is a contribution to the different kinds of socio-educative disciplines and others because we get new principles mentioned in the first lines; which represents a theoretic contribution in teaching and learning. This study is made with a test and posttest design and with fortuitous groups whose objective is appreciate the real effect of laugh. This research with a value to education, sociology and others sciences that study the human being. In conclusion: the laugh moderate the emotions, the laugh moderate the social relationship and finally the laugh is a fixer of complex learning. The following research project was made in the Awajun ethnic in Amazonas region (out in the north-eastern part of Peru).

scholarly journals Itako on screen

2020 ◽  
Vol 21 ◽  
pp. 76
Author(s):  
Ilaria Vecchi
Keyword(s):  
Rural Areas ◽  
Visual Ethnography ◽  
Social Fabric ◽  
The North ◽  
Fieldwork Experience ◽  
The Social ◽  
North Eastern ◽  
Critical Religion ◽  
Visual Methodology ◽  
North Eastern Part

This article is based on my fieldwork with Itako shamans in the north-eastern part of Japan. The progressive modernisation of Japan at the expense of rural areas has also affected Tohoku, resulting in the ageing of the social fabric of its communities. Within this context, this article focusses on traditional and established activities practised by the blind female Itako shamans, who are going through a process of adaptation. Therefore, the article is concerned with this process and, in particular, on the methodology applied before and during my fieldwork experience of spending time, observing, having conversations, and filming these women in their everyday life. In the attempt to understand and document these shamans, I consider the use of visual ethnographic methods for understanding the changing aspects and their implications on the life of these women. While doing this, I also considered their communities and the area in which they live. I analyse this process by blending different methodologies such as visual methodology and digital visual ethnography and the critical religion approach proposed by Fitzgerald (2000). In addition, the paper will describe how I applied this methodology to provide a fresh look at these women and their daily activity.

scholarly journals Hydrological studies in the north-eastern part of the Barents Sea in 2019 and 2020

2021 ◽  
Vol 12 (3-2021) ◽  
pp. 75-81
Author(s):  
T.M. Maksimovskaya ◽  
◽  
G.V. Ilyin ◽  
Keyword(s):  
Barents Sea ◽  
Water Structure ◽  
The North ◽  
The Barents Sea ◽  
North Eastern ◽  
Deep Layers ◽  
Deep Current ◽  
North Eastern Part ◽  
Made In

The article presents the results of hydrological studies of the north-eastern part of the Barents Sea. The observations were made in the oceanographic expeditions R/W “Dalnie Zelentsy” of the MMBI RAS in October–November 2019 and 2020. The analysis of a series of hydrological sections is carried out, which details the vision of the structure of the waters and currents of the studied area. In the water structure, two streams of Atlantic waters are distinguished. The flows are directed opposite to each other and are located in different deep layers. The Atlantic stream emerging from the Barents Sea is identified as a branch of the warm New Earth current. At the beginning of the winter,the current spreads in a layer from the surface to 50–75 m. The Atlantic waters flowing into the Barents Sea are identified as a branch of the deep current of the St. Anna trench. They come from the Polar Basin and pass into the sea from east to west up to 62–60o E.

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.

Examining the Kinships System of the Bodo

Think India ◽  
2019 ◽  
Vol 22 (3) ◽  
pp. 186-192
Author(s):  
Dr. Oinam Ranjit Singh ◽  
Dr. Nushar Bargayary
Keyword(s):  
Social Relationships ◽  
Social Cohesion ◽  
Social Relationship ◽  
Vital Role ◽  
Eastern Region ◽  
The North ◽  
Kinship System ◽  
North Eastern ◽  
The World ◽  
The Relationship

The Bodo of the North Eastern region of India have their own kinship system to maintain social relationship since ancient periods. Kinship is the expression of social relationship. Kinship may be defined as connection or relationships between persons based on marriage or blood. In each and every society of the world, social relationship is considered to be the more important than the biological bond. The relationship is not socially recognized, it fall outside the realm of kinship. Since kinship is considered as universal, it plays a vital role in the socialization of individuals and the maintenance of social cohesion of the group. Thus, kinship is considered to be the study of the sum total of these relations. The kinship of the Bodo is bilateral. The kin related through the father is known as Bahagi in Bodo whereas the kin to the mother is called Kurma. The nature of social relationships, the kinship terms, kinship behaviours and prescriptive and proscriptive rules are the important themes of the present study.

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.

Sign in / Sign up

Export Citation Format

Share Document