6.Chapter3.Geo.Locating Places on the Earth
Chapter 3.Geography.
Locating
Places on the Earth
Page 21 We
know that distance and direction help us to locate a place on a map or a
globe. If we are at a new place, we try
to observe certain features of our surroundings. These features, such as a temple, a hill or a
river help us in locating places. These
features are called the reference points or landmarks The earth being spherical
in shape has no edges or corners which can be used as reference points in
locating the places. However, the end
points of the imaginary axis of the earth on which it rotates, provide us two
basic points of reference. These end
points of the earth's axis are called North Pole and South Pole. These are the fixed points on the earth. The South Latitude North Pole lies exactly
below the Pole Star and opposite to it is the South Pole. Using the two Poles as basic reference
points, an imaginary circle is drawn around the earth midway between the two
Poles. This great circle, divides the
earth into two halves, and is known as the Equator. The half portion of the earth to the north of
the Equator is called the Northern Hemisphere.
The southern half is called the Southern Hemisphere. A perpendicular line from any of the Poles to
the Equator makes an angle of 90 °.
Thus, the North Pole is at 90 'N and the South Pole is at 90 ° S. South
Pole LATITUDES Horizontal lines drawn on a globe or a map are called lines of
latitude. Since these lines run parallel
to each other they are called parallels of latitudes. The latitude of a place on the Earth's
surface is its angular distance in the north or in the south of the
equator. It is measured as an angle
subtended at the center of the earth.
The latitudes are always expressed in degrees. They are numbered from 0 to 90 ° North and
South. Equator is located at 0 ".
Each degree of latitude is divided into 60 minutes and a minute is further sub
- divided into 60 seconds. Suppose the latitude of a place is 8 degrees 4
minutes and 25 seconds, we can express it as 8 '. , 4,25
Page
22 The lines of
latitude are the imaginary lines which encircle the earth. All of them are
parallel to the equator, all places having the same value of latitude to the north or the south of the equator lice
on the same latitude For example, 30 * N latitude line joins all places located
at an angular distance of 30% north of the equator. The equator, beling in the
middle Salong the North Pole 90 'N of
the two poles of the earth is the longest line of latitude. Its length is equal
to the circumference of the earth which is about 40,075.16 km As we move away
from the equator, the circumference of equator the circle decreases. The two
poles are, however, only points. While
writing the parallels of latitudes, it is essential to write letter Nor S with
them. Letter 'N' is written with the latitudes of the Northern Hemisphere and
'S' with the latitudes of the Southern Hemisphere. For example, Kerala (in India ) is located 90'S between 8 ° 18'N to 12 48'N
of equator. CED Parallels of Latitude
The Trumber of latitudes, when drawn at 1 'interval, are 90 in the Northern
Hemisphere and 90 in the Southern Hemisphere.
The latitude of the equator is 0 ". Besides the equator and two
poles, other important lines of latitude are: Tropic ol Cancer 1. The Tropic of
Cancer (23% 'N) - It lies north of the equator in the Northen Hemisphere. 234 2. The Tropic of Capricorn (23 / S) - It
is located south of the equator in the Southern Hemisphere. Tropic of Capricom
3. The Arctic Circle (66) N) - This important line of latitude is above the
Tropic of Cancer in the Northern
Hemisphere, 4. The Antarctic Circle (66% 'S) - It is below the Tropic of
Capricorn in the Southern Hemisphere. Important Lines of Latitude HEAT ZONES
North Pole 90'N 66% N Arctic Circle 23H'N 56%
09 Equator 23'S Antarctic Circle 66Y'S South Pole 90'S Some parts of the
earth receive more heat than other parts because of the variation in the angle
of the rays of the sun. Depending on the heat received, the zones are named
differently these are - Torrid Zone ,
Temperate Zone and Frigid Zone. Let us discuss them one by one . The
Torrid Zone The Tropic of Cancer and the Tropic of Capricorn mark the limits of
this zone. In this zone, the rays of the
sun are exactly overhead once a year except on the equator, where the mid-day
sun is overhead twice a year. Hence, it
receives maximum heat from the sun and is very hot.
Page 23
The Temperate Zone The zone between the Tropic of Cancer and
the Arctic Circle is called the North Temperate Zone. The zone between the Tropic of Capricorn and
the Antarctic Circle is called the South Temperate Zone. The sun rays in both these zones are never
directly overhead. The angle of the sun
rays decreases as we go ww towards the poles.
That is way these zones are neither very hot nor very cold. They have moderate temperature. The Frigid Zone The Heat Zones It lies from
Arctic Circle to the North Pole and from Antarctic Circle to the South
Pole. This zor remains covered with ice
and snow for the most part of the year because the rays of the sun a always
slanting. Hence, it is the coldest zone
of the earth. LONGITUDES 5 The meridians
of longitude are a set of imaginary vertical lines. They are in the form of semi-circles which
converge towards the two poles and are the widest at the equator. Unlike the parallels of latitudes, they are
all equal in length. West The lines of
longitudes are drawn all around the globe at an interval of an angle of 1
'. As all these lines of longitudes are
equal, one particular line of longitude was to be selected SAL for numbering
them. The line of longitude passing
through the British Royal Observatory at Greenwich, London, has been adopted as
the Prime Meridian or Longitude There are 180 ° longitudes each drawn on both
sides of Longitudes the Prime Meridian.
The value of the meridians of longitude starts from 19 to 180 ° towards
the e as well as towards the west side of the Prime Meridian. The half part of the earth on the east to
Prime Meridian is called Eastern Hemisphere and the other half to the west is
called the West Hemisphere. Thus, in
each hemisphere there are 180 longitudes.
The total number of longitude thus, 360. Meridians to the east of Prime
Meridian are marked as 'E', whereas to the west of Pri Meridian as 'W'. However, 180 ° is a common line and form
International date line in the Pa Ocean.
Page 24
GRID
SYSTEM A network of the lines of latitude and North Pole longitude intersecting
each other is called a Grid. Each place
on the globe is intersected by vertical and horizontal lines. Thus, with the help equator of these two sets
of lines or the grid system the location of any place can be determined. For Primo Meridian example, Nasik in
Maharashtra is located at an intersection of 20'N parallel of latitude and 74'E
South Pole line of longitude Grid of Parallels and Meridians
LONGITUDE AND TIME In ancient times, changing seasohs, day and night and position of the sun were some of the means to
estimate time. People observed the path
of the sun in DE the sky to estimate the time.
The earth, as we know, rotates from west to east and completes one
rotation in 24 hours. This also means
that 360 longitudes face V the mid - day sun one after the other in 24 hours,
thus, (15 longitudes pass before the sun in a period of one hour or 60 minutes.
Further, it takes 4 minutes for one Sundial with time longitude to cross before the sun. All
the places located on the same meridian have the same local time. The local
time of one meridian differs from the other. If it is noon or 12.00 o'clock at
Greenwich,
Do You Know?
the local time
of all places at 30 ° E longitude will be In Latin am means ante meridian 30 x
4 (minutes) = 120 minutes or 2 hours ahead. It means and pm means post
meridian. the time on 30º E will be 12 + 2
= 2.00 pm On the other hand, the local time of all places at 30 ° W
longitude will be 2 hours behind the Greenwich time. It will be 12 - 2 = 10.00
am Thus, the local time will be ahead at all the places in the east of a given meridian and it will be
behind at all places in the west of a given meridian.
STANDARD TIME We know that places located on different
meridians have different local time. It
would create a lot of difficulties, if all countries would adopt different
local time. The railway time - table and
the
Page 25
schedules of the air flights would be difficult to
prepare. People crossing the longitudes
would have to adjust their watches.
India lies between 68% E and 97'25 'E longitudes. Think about the problems, the people of India
would face if they follow the different local times. (In order to avoid this problem and maintain
its uniformity all over a country, it was decided to adopt the local time of a
central meridian of a country as the Standard Time of India mostly the meridian
selected, is divisible by 7 ° 30 'so
that the difference Jantar Mantar Jaipur between its standard time and
the Greenwich Mean Time (GMT) is expressed in the multiple half an hour '. The
meridian, selected for a country, is called the Standard Meridian.
Do you know?
Some countries have a vast longitudinal
extent. That is why countries like Russia has nin and USA has four time zones.
(India, spanning roughly over 30 "longitudes, has
selected 82 ° 30 'E longitude as its Standard Meridian. It passes through a
place near Mirzapur. Its local time is taken as the Indian Standard Time (IST).
The Greenwich Mean Time ( GMT) is 5%
hours behind the Indian Standard Time. Greenwich Mean Time is followed by all
countries for the international airlines and ship fleets,
Do you know? Although,
about 30 longitudes pass over India, yet it has only one standard meridian
and one standard time for the whole
country for convenience. This is called Indian Standard Time (IST). Keywords
schedule: it is a plan for carrying out a process or procedure. subtended: form
an angle at a particular point. variation: it is a slight difference in condition or amount in
certain limits.
Sir I am ASHWANI RAJ from class -6 C sir you send the Q ans of this chapter
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