Educational of the mind is a weapon to a different knowledges which
benefit in ife and developed the mind in many field and practice him in a
regular form in a right thinking and practice sense on exactly recognizing and
conception things which is senses and regulating the memory and providing
with benefit information which fit to minded of person,the present research
aimed at answering the following two questions:
1-Does the concept of mind differ with age?
2-Does the recognition on function of mind developed with development of
age?
The research population consisted of the children in the primary schools
of Baghdad/center,and the students of the Education for woman
college/Baghdad university for the ages(11,18 ,19),the research
sample(22)subjects-was chosen randomly from the statistical population.
Thescale consisted of the(37)questions,first question measured the
cognition of conception of mind, but(36)questions measured the knowing of
function of mind ,this questios depended on number of the previous literatures
its validity and reliability in the Iraqi population.
The following results have been revealed:
1-The age of (19)yars obtain on greatest prons in explaination the concept of
the mind.
2-There are a statistically significant differences are shown to a (19) years in
function of mind in contrary to (11, 18)years.
On the basis of these results,the researcher has made some
recommendations and suggestions.
من نحن ؟ التحديات التي تواجه الهوية الامريكية
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Adopting the concept of urban densification in city planning policies to be more sustainable and livable is of great importance by achieving efficient use of urban land and limiting urban sprawl, as well as reducing the
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Abstract
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This study presents determination of the paleostress magnitudes and orientation of Bekhme Structure in Shaqlawa area northeastern Iraq. Paleostress Analysis of slip-fault measurements is performed using Right dihedral, Lisle diagram and Mohr Circles methods. Depending on Mohr Circles, Bott law and vertical thickness, the magnitudes of the paleostress at the time of the tectonic activity were determined. Firstly, Georient Software was used to estimate the orientation of the paleostresses (σ1, σ2 and σ3). Secondly, using the rupture –friction law, taking into account depth of the overburden and the vertical stress (σv) was calculated to determine the magnitude of the paleostresses (σ1=4500 bars, σ2=1
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