Chapter 1 – Locating Places on Earth

Chapter 1 – Locating Places on Earth

 

  1. Globe
  •  The globe  is a true model of the earth.
  • It helps us to understand the position of the shape of the earth, continents, oceans, and countries.
  • Globes can be of different sizes and types – some large and some small, some pocket-sized.
  • We can rotate the globe in the same way that a potter’s wheel or top spins.
  1. Axis
  • A needle is placed in an inclined position on the globe, which  is called  the axis.
  • It is an  imaginary line around which the earth revolves.
  •  The North Pole and the South Pole are the two points through which the axis passes.
  • The Earth does not actually tilt, it is only shown as a model on the globe.
  1. Equator
  • In addition to the axis, there is another imaginary line on the globe that divides the globe into two equal halves. This is  called the  equator.
  • The equator is an important reference point on Earth.
  • The north half of the equator  is called  the Northern Hemisphere and the southern half  is called the  Southern Hemisphere.
  • These two are equal halves.
  1. Latitudes
  • All parallel circles from the equator to the poles  are called  parallels of latitudes.
  • These  are measured in degrees.
  • The latitude of the equator is  0°.
  •  The   value of latitude increases as we move from the equator towards the poles.
  • The North Pole is at 90° North latitude, and  the South Pole is at  90° South latitude.
  • Important Parallels of Latitudes:
    • Tropic of Cancer: 23.5° North latitude (in the Northern Hemisphere)
    •  Tropic of Capricorn: 23.5° South latitude (in the Southern Hemisphere)
    •  Arctic Circle: 66.5° North latitude (near the North Pole)
    •  Antarctic Circle: 66.5° south latitude (near the South Pole)
  1. Heat Zones

Latitude lines define the different  heat zones  on Earth:

  1. Torrid Zone:
    • This is  the area between the Tropic of Cancer and the Tropic of Capricorn.
    • In this region, the sun’s rays fall right above the head at least once a year, which  provides maximum heat  here.
    • It is the warmest tropic.
  1. Temperate Zones:
    • Northern Temperate: The region between the Tropic of Cancer and the Arctic Circle.
    • Southern Temperate: The area between the Tropic of Capricorn and the Antarctic Circle.
    • In these areas, the sun’s rays never fall directly on the head.
    • The temperature here  is moderate.

iii.  Frigid Zones:

    • Northern Cold Zone: The region between the Arctic Circle and the North Pole.
    • Southern Cold Zone: The region between the Antarctic Circle and the South Pole.
    • Here the sun’s rays fall very obliquely and do not rise above the horizon, so  it is very cold  here.

 

 

  1. Longitudes
  • In addition to the lines of latitude,  meridians of longitude  are required to accurately locate locations on Earth.
  • These are semi-circular lines connecting the North Pole with the South Pole.
  • All longitudes have the same length.
  •  Prime Meridian:
    • It is longitude, passing through the Royal Observatory located in Greenwich, near London.
    • It is  also known as Greenwich Meridian.
    • It divides the Earth into the  Eastern Hemisphere and the Western Hemisphere.

 

  1. Grid
  • When latitude lines and longitude lines intersect each other, they form a  grid.
  • Using this grid we can accurately locate any place on Earth.
  • To tell the position of any place, we should know both its latitude and longitude.
  • Example: Delhi is located at  28.7° north latitude and 77.2° east longitude.

 

  1. Measuring Time and Longitude
  • The earth rotates on its axis from west to east.
  • It takes  4  minutes for the earth to travel from one longitude to another. (It takes  24 hours to rotate  360° longitude, then 24 hours/hour to rotate 1°.) 360° = 1440 min/min 360° = 4 min).
  •  Greenwich Mean Time (GMT):  The time at the prime meridian in Greenwich is called  GMT.
  •  Local Time: The local time of a place is determined by the position of the sun at noon.
  •  Standard Time:
    • In order to maintain the uniformity of time within a country, the local time of a central longitude is considered as the standard time of the entire country.
    • Standard meridian of India: 82.5° east longitude is considered as the standard meridian of India.
    • This is because the longitude in India is about 30°  , which can cause a difference of about 2 hours in local time.
    •  Indian Standard Time (IST): 82.5° East Longitude Local Time, which is  5 hours and 30  minutes ahead of  GMT.

Leave a Comment

Your email address will not be published. Required fields are marked *

Scroll to Top