• GG-101-102 | Physical Geography I – II

    F.Y.B.Sc. | Sem I | GG-101-102
    GEOGRAPHY
    PHYSICAL GEOGRAPHY I – II
    GG 101 : INTRODUCTION TO LITHOSPHERE
    GG 102 : MORPHOLOGY OF LANDSCAPE

    Geography is amongst the oldest earth science and much of the geographical work is actually the contribution made by different Greek scholars. The word geography was coined by Eratosthenes, a famous Greek scholar in third century B.C. Geography is actually a combination of two words ‘Geo’ means earth and ‘Graphy’ means to describe, hence if we look at the literal meaning of term geography then it stands for description of the earth surface.
    Lithosphere is solid rocky crust that covers the entire surface of the earth including thebottom of the oceans. Beneath the surface of the Earth there are distinct layers, somewhat comparable to that of an onion. These layers are divided based on various characteristics including density, mineralogy and geochemistry. The outermost layer is known as the ‘lithosphere’ coming from the Ancient Greek ‘lithos’, meaning ‘rocky’. This layer is defined by its mechanical properties; being rigid and non-viscous, it is separated from the underlying layer by a specific rheological boundary
    The earth crust is a habitat to a variety of living organisms in the biosphere ecosystem. Different reliefs like mountains, hills plains etc are created on the earth surface by endogenetic forces which introduce diversity in the habitats. The exogenetic forces originates from the atmosphere in form of carbon, hydrogen, oxygen and nitrogen etc giving rise to different kind of climate’s on earth surface. These forces also help in circulation and exchange of heat between the atmosphere and earth surface and on formation of different landforms by various denudational works on one hand and diversity in the habitats formed by endogenetic forces on the other.
    A landscape is part of the Earth’s surface that can be viewed at one time from one place. It consists of the geographic features that mark, or are characteristic of, a particular area. Landscaping is a complicated endeavor that requires one to be knowledgeable and skilled in various disciplines. The land surrounding a home is the canvas, and it is the landscaper’s job to turn that into something spectacular. A natural landscape is made up of a collection of landforms, such as mountains, hills, plans, and plateaus, Lakes, streams, soils (such as sand or clay), and natural vegetation are other features of natural landscapes. Surface processes comprise the action of water, wind, ice, fire, and living things on the surface of the Earth, along with chemical reactions that form soils and alter material properties, the stability and rate of change of topography under the force of gravity, and other factors, such as (in the very recent past) human alteration of the landscape.
    It is our pleasure to present this book Introduction to Lithosphere to the student of the F.Y.B.Sc. and teachers from different universities especially for KBC, North Maharashtra University, Jalgaon. The teachers will find lot of deficiencies in this book which are made according to new syllabus.

    150.00
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  • GG-103-203 | Practical Geography

    F.Y.B.Sc. | Sem I-II | GG-103-203
    PRACTICAL GEOGRAPHY
    GG-103 : Cartographic Techniques
    GG-203 : Map Projection

    Cartography is a technique that is primary concerned with the reduction of the spatial characteristic of a large area- a portion or all of the earth or another celestial body and putting it in a form that makes it observable. Just the way spoken and written language allows people to communicate beyond the restriction of having to point to everything, a map also allows us to extend the normal range of vision, so to speak and makes it possible for us to see the larger spatial relations that exist over large areas.
    The field cartography has changed enormously during the past four decades, primarily because of the widespread availability of computers. Computers have made for new symbolization, such as dynamic (that is, animated) maps, customized maps for individual users and interactive maps. They have also made possible new methods for scientific visualization and spatial data analysis.
    A graph that uses points and lines to represent change over time is defined as a line graph. In other words, it is the chart that shows a line joining multiple points or a line that shows the link between the points.
    In order that the facts conveyed by a large number of figures may be grasped clearly and quickly, we resort to representing them by geometric figures and curves called diagrams. Thus a diagram is a drawing which expresses the relationship between quantities. Diagrams are used as aids in understanding the facts represented by statistical data clearly and quickly at a glance. The diagrams representing statistical data are known as statistical diagrams.
    Map projection is the method of transferring the graticule of latitude and longitude on a plane surface. It can also be defined as the transformation of spherical network of parallels and meridians on a plane surface. As you know that, the earth on which we live in is not flat. It is geoid in shape like a sphere. A globe is the best model of the earth. Due to this property of the globe, the shape and sizes of the continents and oceans are accurately shown on it. It also shows the directions and distances very accurately.
    It is our pleasure to present this book practical geography to the student of F.Y.B.Sc and teachers from different universities especially for KBC, North Maharashtra University, Jalgaon. The teachers will find lot of deficiencies in this book which are made according to new syllabus.

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  • GG-201-202 | Physical Geography I-II

    F.Y.B.Sc. | Sem II | GG-201-202
    PHYSICAL GEOGRAPHY
    GG – 201 : ATMOSPHERE
    GG – 202 : HDRYOSPHERE

    The atmosphere is of immense importance for the existence of the living organisms of the earth. The atmosphere safeguards the lives of living beings against the effect of harmful rays of the sun. Its gaseous elements like carbon dioxide rear the vegetation and oxygen safeguards the living creatures. The human activities on the surface of the earth helps to bring changes in the structure of the atmosphere, particularly large scale deforestation, industrial smoke, and burning of coal, mineral oil and the natural gas polluting the atmosphere. For the interest of the living beings of the earth, we should refrain ourselves from contaminating the atmosphere. So, we should have an idea about the structure of the atmosphere and how it works.
    According to the theory of hot origin of the earth in the beginning, the earth was a hot gaseous mass and the gases associated with the earth were also hot. Hence, they easily escaped from the earth and lost into the atmosphere. Thereafter, cooling and solidification of hot magma and formation of solid earth crust released several gases namely water vapour, carbon dioxide, hydrogen, methane, ammonia etc. through the process of degassing.
    The Earth system comprises four spheres viz. the lithosphere (solid rocky part of Earth), atmosphere (air surrounding Earth), Hydrosphere (water part of Earth), and biosphere (living things). Thus, hydrosphere is one of the four spheres of Earth system. The water is present in all three phases: solid, liquid and gas. It is distributed among the ocean, glaciers and ice caps, groundwater, surface water and water in the atmosphere in the form of water vapor and clouds. The study of hydrosphere is utmost important for many purposes.
    The primary importance of the hydrosphere is that it contains water, which sustains a variety of life forms and plays an important role in regulating the atmosphere and surrounding ecosystems. The water is not only important for living organisms but also for several natural processes.The oceanic salinity not only affects the marine organisms and plant community but it also affects the physical properties of the oceans such as temperature, density, pressure, waves and currents etc.various aspects of oceanic body is elaborately explained in this book.
    It is our pleasure to present this book Introduction to lithosphere to the student of F.Y.B.Sc and teachers from different universities especially for KBC, North Maharashtra University, Jalgaon. The teachers will find lot of deficiencies in this book which are made according to new syllabus.

    120.00
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  • GG-303-403 | Practical Geography

    S.Y.B.Sc. | Sem IV | GG-303-403
    GEOGRAPHY
    Practical Geography

    The study of Practical Geography has got unprecedential importance in recent times. Though the technical and applied branches like Interpretation of Topographical, Weather Maps and Weather Data Analysis, Surveying and Area Measurement by GPS etc. are in much discussion today, the study of Practical Geography is equally important for obtaining regional information. This book is specially prepared for the students of Second Year B.Sc. Class (C.B.C.S.) of Kaviyatri Bahinabai Chaudhari North Maharashtra University, Jalgaon.
    This book will prove to be useful for the studies of syllabi prescribed in other universities as well as preparations for the new syllabi prescribed for examinations conducted by Union Government and the State Government. Keeping these points in view, present book has been prepared to extend information regarding Practical Geography. This book contains the information regarding Interpretation of Topographical, Weather Maps and Weather Data Analysis, Surveying and Area Measurement by GPS etc.

    85.00
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  • प्राकृतिक भूगोल (शिलावरण, वातावरण व जलावरण)

    सूर्य, चंद्र, तारे, ग्रह हे अवघे विश्व कसे निर्माण झाले, ते कोणी निर्माण केले, विश्वाची व्याप्ती किती आहे आदींसारखे अनेक प्रश्न मानवाला सुरुवातीपासून भेडसावत होते. त्याअनुषंगाने प्राचीन काळापासून ते आजतागायत पुष्कळशा परिकल्पना मांडल्या गेल्या आहेत. अठराव्या शतकापासून पृथ्वीच्या उत्पत्तीविषयी शास्त्रीय दृष्टिकोनातून विचार करण्यास सुरुवात झाली. पृथ्वीचे अंतरंग हे निसर्गातील सर्वात मोठे गुढ आहे. भूकवचात बदल घडवून आणण्याचे कार्य सातत्याने काही शक्ती अथवा प्रेरणा करीत असतात हे स्पष्ट होते.
    प्रस्तुत ग्रंथात काल्पनिक रेषा व पृथ्वीची गती, पृथ्वीच्या उत्पत्तीचा परिचय, पृथ्वीचे अंतरंग, खंड व महासागर यांच्या वितरणाविषयीचे सिद्धांत, खडक आणि विदारण, नदीचे कार्य, वाऱ्याचे कार्य, वातावरण आणि सौरशक्ती, वायुभार आणि वारे, आर्द्रता आणि वृष्टी, सागरतळ, समुद्रप्रवाह इ. विविध मुद्यांचा परामर्ष घेतलेला असून साध्या-सुलभ भाषेत मांडण्याचा प्रयत्न केला आहे.

    Prakurtik Bhugol (Shilavaran, Vatavaran V Jalavaran)

    295.00
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