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Types of Sand Dunes

In this Geoshortqa we are going to know about types of Sand Dunes. Types of Sand Dunes, Geoshortqa Sand Dunes Sand dunes are heaps of sand found in deserts . Generally , their heights vary from a few metres to 20m , but in some cases dunes are several hundred metres high and 5 to 8 km long .   The formation of sand dunes requires  • Wind of high velocity  • Abundant sand  • Obstacles such as trees , bushes , forests , rock outcrops , walls against , which dunes may settle  • Ideal places i.e. dune complex , dune colony or dune chain . Dunes formed due to obstacles like hushes , walls etc. are called nebkhas , where dune formed besides desert depressions are called lunettes.   Dunes are classified on the basis of morphology , structure , orientation , location , internal structure , ground pattern and number of slip faces . These are the various types of sand dunes  a) Transverse Dunes are dunes deposited transverse to the prevailing winds direct...
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Isodrosotherm

  In this Geoshortqa we know about Isodrosotherm isodrosotherm, geoshortqa Isodrosotherm A line joining points of the same Dew Point Temperature is called an Isodrosotherm. That means, at every point along a given isodrosotherm, the values of dew point temperature are the same.
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Isoquant

  In this Geoshortqa we know about Isoquant   Isoquant, Geoshortqa Isoquant  In Microeconomics, is a line joining points at which the equal quantity of output is produced.
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Isodose

  In this Geoshortqa we are going to know about i sodose. i sodose, Geoshortqa Isodose  A line Joining points with the same radiation intensity.
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Types of Shock Waves

  In this Geoshortqa we know about  Types of Shock Waves. Shock waves, Geoshortqa Types of Shock Waves (a) Undisturbed materials   At the vary beginning there was no wave action found and all the materials are undisturbed Undisturbed materials, Geoshortqa  There are mainly two types of shock waves are found   1) Body  Waves  These travel through the crust and are of two types  (b) Primary (P) Waves  which cause the crustal rock to move back and forth in the direction of wave movement. Primary (P) Waves , Geoshortqa * click on photo for getting higher resolution  (c) Secondary (S) Waves  which cause the crustal rock to move from side to side i.e. at right angles to the direction of wave movement. Secondary (S) Waves, Geoshortqa 2)  Surface Waves  These travel through the surface rocks and are of two types  (d) Love (L) Waves  which cause the surface rocks to more from side to side, at right angles to th...
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Isochalaz

  In this Geoshortqa we are going to know about Isochalaz. Isochalaz, Geoshortqa Isochalaz An Isochalaz is a line of constant frequency of hail storms .
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Isochasm

  In this Geoshortqa we know about the Isochasm Isochasm, Geoshortqa Isochasm    A line joining points on the Earth's surface that have the same mean frequency of auroras.
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Sustainable development and it's goals

In this Geoshortqa we know about sustainable development and it's goal. Sustainable Development The United Nations Conference on the Human Environment ( Also known as the Stockholm Conference) 1972. Agenda 21 The United Nations Conference on Environment and Development ( UNCED ), 1992 resulted in the formulation of Agenda 21 which is a non-binding action plan of the United Nations with regard to sustainable development. Agenda 21 for Culture 2002 The first world public meeting on culture, held in Porto Alegre, Brazil in 2002, came up with the idea to establish guidelines for local cultural policies, something comparable to what Agenda 21 was for the environment. Sustainable development and it's goals, Geoshortqa Goals of Sustainable Development Agenda 2030, Also known as the Sustainable Development Goals ( SDGs ) were born born at the United Nations Conference on Sustainable Development in Rio de Janeiro in 2012. Sustainable Development Goals ( SDGs ) are :-   No poverty Zero ...
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What is Lahars?

   In this Geoshortqa we know about #Lahars #Lahars, Geoshortqa A volcanic mudflow, also known as Lahars , comprises of a slurry of pyroclastic materials, debris and water which flows down from a Volcano.  #lahar #lahars #halar #lahar    #lahar    #lahar    #lahar  #lahar    #lahar    #lahar    #lahar  #lahar    #lahar  #lahars #halar #lahar #lahar #lahar #lahar  #lahar #lahar #lahar #lahar  #lahar #lahar  #lahars #halar #lahar    #lahar    #lahar    #lahar  #lahar    #lahar    #lahar    #lahar  #lahar    #lahar  #what is lahars #lahars #halar #lahar    #lahar    #lahar    #lahar  #lahar    #lahar    #lahar    #lahar  #lahar    #lahar  #lahars #halar #lahar #lahar #lahar #lahar  #lahar #laha...
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Desert, Wildlife, Air and Water Act.

  In this Geoshortqa we about some important dates related to Desert, Wildlife, Air and Water Act. Desert, Wildlife, Air and Water Act, Geoshortqa
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Famous Theory, Model and Concepts related to geomorphology

 In this Geoshortqa we know about some famous Theory,  Model and Concepts related to geomorphology. Famous Theory, Model and Concepts related to geomorphology, geoshortqa Theory, Model and Concepts   Name                                    Proponent ✓ Complete Cycle Of River Life    -   W.M Davis  ✓ Base Level Of Erosion         -          J.W Powell ✓Karst Cycle Of Erosion   -    Beede and Cvijic ✓ Dynamic Equilibrium Theory      -    J.T Hack ✓Cyclic Nature Of Earth History    -   Hutton  ✓Panplanation               -           C.H Crickmay  ✓Episodic Erosion Model      -      S.A Schumm ✓Graded Stream          ...
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Isoline

In this Geoshortqa , we know about isoline or contour line. Isoline, geoshortqa Contour line or Isoline  : Joins points of the same height above ground.
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Isoquant

  In this Geoshortqa we know about Isoquant   Isoquant, Geoshortqa Isoquant  In Microeconomics, is a line joining points at which the equal quantity of output is produced.
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Isohel

  In this Geoshortqa we know about isohel Isohel An imaginary line joining points on a map having the equal amount of sunshine.
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Types of Shock Waves

  In this Geoshortqa we know about  Types of Shock Waves. Shock waves, Geoshortqa Types of Shock Waves (a) Undisturbed materials   At the vary beginning there was no wave action found and all the materials are undisturbed Undisturbed materials, Geoshortqa  There are mainly two types of shock waves are found   1) Body  Waves  These travel through the crust and are of two types  (b) Primary (P) Waves  which cause the crustal rock to move back and forth in the direction of wave movement. Primary (P) Waves , Geoshortqa * click on photo for getting higher resolution  (c) Secondary (S) Waves  which cause the crustal rock to move from side to side i.e. at right angles to the direction of wave movement. Secondary (S) Waves, Geoshortqa 2)  Surface Waves  These travel through the surface rocks and are of two types  (d) Love (L) Waves  which cause the surface rocks to more from side to side, at right angles to th...
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Internal structure of the Earth

In this Geoshortqa we know about the Internal structure of the Earth Internal structure of the Earth, geoshortqa  
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