Report and Opinion
(Rep Opinion)
ISSN 1553-9873 (print); ISSN 2375-7205 (online),
doi prefix:
10.7537, Monthly
Volume
16 - Issue 12, Cumulated 186, December 25, 2024
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CONTENTS
No.
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Titles /
Authors /Abstracts
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Full Text
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No.
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1
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Study On Geology
And Geomorphology
*Akoijam Linthoi
Devi And **Dr. Bhuvnesh Kumari
*Research Scholar,
Department of Earth Science, SunRise University, Alwar,
Rajasthan (India)
**Associate
Professor, Department of Earth Science, SunRise University,
Alwar, Rajasthan (India)
Email:
Linthoiakoijam2014@gmail.com
Abstract:
The greater part of the study area is covered with metamorphic
crystalline rocks of Archaean age belonging to the
Charnockite-Khondalite group. Overlying the Archaeans are the
fossiliferous Upper Cretaceous formations mainly occurring
around 10 km N.W of Vridhachalam and between the Red hills of
Pondicherry and the high ground of Tiruvakkarai. Overlying the
Cretaceous rocks are the Cuddalore formations of MioPliocene
age. These comprise sandstone of often-ferruginous pebble bed,
sand and clay with lignite seams at places and silicified wood
at other places. These in turn, are overlain by the rocks of the
Coromandal formation of Holocene age occurring as long linear
bands along the northeastern coast around Marakkanam. During sub
recent to recent times, there has been the deposition of
alluvium, coastal sands and lateritic soil.
[Devi,
A.L. and Kumari, B. STUDY ON GEOLOGY AND GEOMORPHOLOGY.
Rep Opinion
2024;16(12):1-4].
ISSN 1553-9873 (print); ISSN 2375-7205 (online).
http://www.sciencepub.net/report.
01. doi:10.7537/marsroj161224.01
Keywords:
Geomorphology;
Geology; Silica Sands |
Full Text |
1
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2
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Study On
Self-Efficacy Of Teachers In Teaching
*Amila Huidrom and
**Dr. Vivek Upadhyay
*Research Scholar,
Department of Education, SunRise University, Alwar, Rajasthan
(India)
**Assistant
Professor, Department of Education, SunRise University, Alwar,
Rajasthan (India)
Email:
amilahuidrom@gmail.com
Abstract:
Teachers’
effectiveness depends on various things and self-efficacy is one
of them. The construct of self-efficacy was coined by
psychologist Albert Bandura in his social cognitive theory.
Self-efficacy refers to one’s belief about his/her capabilities
to accomplish specific tasks. Teachers who have a high sense of
belief in their teaching capabilities will achieve higher goals
while teachers who have a low sense of belief in their
capabilities will be under the shadow of fear of failures. Over
the last four decades, researchers have thrown the light on
teachers’ self-efficacy in teaching and learning and established
it as one of the important effective constructs. Self-efficacy
plays a vital role for teachers to accomplish their goals,
tasks, and how they approach instructional challenges. Teachers
with a low self-efficacy evade challenging activities, take
creative activities and situations as difficult to do, take most
of the things negative and lose confidence in their abilities
while teachers with a high self efficacy welcome challenging
activities as to be mastered, create deeper interest in their
activities, develops a high sense of commitments and mend
swiftly from failures. The purpose of this study is to review
the construct of teachers’ self-efficacy and its importance in
teachers’ effectiveness.
[Huidrom,
A. and Upadhyay, V. STUDY ON SELF-EFFICACY OF TEACHERS IN
TEACHING.
Rep Opinion
2024;16(12):5-8]. ISSN 1553-9873 (print); ISSN 2375-7205 (online).
http://www.sciencepub.net/report.
02. doi:10.7537/marsroj161224.02
Key Words:
Self-efficacy; Teacher Self-efficacy; Measurement of Teacher
Self-efficacy |
Full Text |
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3
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Assessment of
Tree Canopy Cover on Urban Heat Island Effect in Owerri
Metropolis, Nigeria
*Japheth, H.D.,
Azubuike, N.O. and Nwanoli, M.S. 1
Department of
Forestry and Wildlife Technology, The Federal University of
Technology, Owerri-Nigeria.
* Corresponding:
daujaph@gmail.com;
+234 8068347777
ABSTRACT:
Cities are
facing rising temperatures due to global warming and fast urban
growth. This study focused on the Owerri metropolis in Imo
state, Nigeria, seeking to examine the influence of tree canopy
cover on urban heat island effects and to comprehend the local
community's perception of tree canopy cover. Two hundred fifty
semi-structured questionnaires were administered to participants
in sampled locations within the Owerri urban area through
purposive and random sampling techniques. The results of the
research indicate that planting trees (42.3%) strategically,
including various species such as native (34.5%)), exotic
(12.8%), fruit (42.6%), and ornamental species, helps reduce
high temperatures to levels of comfort as perceived by 23.6% of
the respondents. Trees are vital for providing shade, which
helps lower Urban Heat Island effects, decrease energy usage,
improve air quality, and aid evapotranspiration to cool the
surrounding air. To increase tree canopy coverage in residential
areas across the state, it is recommended that governmental
entities, NGOs, and key stakeholders create and execute tree
planting policies, as indicated by 80.4% of survey participants.
Establishing precise yearly goals for tree planting projects can
be a successful tactic to increase tree coverage, ultimately
leading to a better quality of life for city residents.
[Japheth, H.D.,
Azubuike, N.O., and Nwanoli, M.S.
Assessment of Tree
Canopy Cover on Urban Heat Island Effect in Owerri Metropolis,
Nigeria.
Rep Opinion
2024;16(12):9-18]. ISSN 1553-9873 (print); ISSN 2375-7205
(online).
http://www.sciencepub.net/report.
03. doi:10.7537/marsroj161224.03
Keywords:
Environmental; Heat; Population; Tree-cover;
Urbanization. |
Full Text |
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4
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Milankovitch
cycles — Basics of Monsoon Time Scales: Formulation of New
Mexican Monsoon Time Scale
Gangadhara Rao
Irlapati
H.No.5-30-4/1,
Saibabanagar, Jeedimetla, Hyderabad, India-500055
E-mail:
gangadhar19582058@gmail.com
Introduction:
According to the Milankovitch cycle, the angle of the Earth's
axial tilt (obliquity) regarding the orbital plane (the
obliquity of the ecliptic) varies between 22.1° and 24.5°, over
a cycle of about 41,000 years. The current tilt is 23.44°,
roughly halfway between its extreme values. Milankovitch cycles
are a series of periodic changes in the Earth's orbit around the
Sun that affect the amount of solar radiation the Earth
receives, which in turn influences climate change. This tilt
does not remain constant at 23.44°. It oscillates up and down
and slowly moves to 24.5°. The oscillation of up and down will
be about 85 years, according to the Monsoon Time Scales. That
is, about 60 years up, 25 years down, in total oscillating once
every about 85 years. When it moves up to 22.1°, droughts and
famines occur, and when it moves up to 24.5°, heavy rains and
floods occur. Oscillating in this way, it slowly moves forward.
All this can be clearly observed in the Monsoon Time Scales. If
this is true, then we are close to reaching 24.5°, So, are there
going to be more climate changes in the coming centuries? What
are the Milankovitch Cycles? What is their importance in the
study of climate changes? How they determine the scientific
accuracy of Global Monsoon Time Scales? What is the
relationship between Milankovitch cycles and Global Monsoon Time
Scales? What are the new things that can be learned by Global
Monsoon Time Scales? What is the need to establish the New
Mexican Monsoon Time Scale to unravel the mysteries of the New
Mexican Monsoon? Let's discuss in this paper. I call on world
scientists to establish the New Mexican Monsoon Time Scale
following the Basics of Monsoon Time Scales outlined below,
based on the India Monsoon Time Scale which is successfully
proved out in practice and break down the mysteries of the New
Mexican monsoon.
[Gangadhara Rao
Irlapati. Milankovitch cycles — Basics of Monsoon Time Scales
: Formulation of New Mexican Monsoon Time Scale. Rep
Opinion 2024;16(12):19-73]. ISSN 1553-9873 (print); ISSN
2375-7205 (online).
http://www.sciencepub.net/report.
04. doi:10.7537/marsroj161224.04
Keywords:
Bioforecast(1965-70), A New Hypothetical Model of Cosmology
(1970-77), Inquisition(1977-79), Basics of Geoscope (1980-87),
Basics of Monsoon Time Scales (1987-91), Indian Monsoon Time
Scale(1991), Researches on Earth and space related
issues(1991-2000), Numerical Weather Periodic Tables (2000-10),
Designs of Geoscope projects (2010-20), Designs of Global
Monsoon Time Scales (2020-). |
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