at two poles the lines of latitude are nearly two dotes why
Answers
THE EARTH is nearly a sphere. It is because of the fact that the
equatorial radius and the polar radius of the earth is not the same.
The rotation of the earth over its axis produces bulging at the equator.
Hence, the actual shape resembles that of an oblate spheroid. The
shape of the earth presents some difficulties in positioning its surface
features, as there is no point of reference from which to measure the
relative positions of other points. Hence, a network of imaginary lines
is drawn on a globe or a map to locate various places. Let us find out
what are these lines and how are they drawn.
The spinning of the earth on its axis from west to east provides
two natural points of reference, i.e. North and South Poles. They form
the basis for the geographical grid. A network of intersecting lines is
drawn for the purpose of fixing the locations of different features.
The grid consists of two sets of horizontal and vertical lines, which
are called parallels of latitudes and the meridians of longitudes.
Horizontal lines are drawn parallel to each other in east-west
direction. The line drawn midway between the North Pole and the
South Pole is called the equator. It is the largest circle and divides
the globe into two equal halves. It is also called a great circle. All the
other parallels get smaller in size, in proportion to their distance
from the equator towards the poles and divide the earth into two
unequal halves, also referred to as the small circles. These imaginary
lines running east-west are commonly known as the parallels of
latitude.
The vertical lines running north-south, join the two poles. They
are called the meridians of longitude. They are spaced farthest apart
at the equator and converge at a point at each pole.