Source: The Earth: Our Habitat β Textbook of Social Science (Geography), Class VI, Pages 10β17 Class: VI
Section 1. The Globe π
π Globe = A true model (miniature form) of the earth.
- Earth is slightly flattened at the North and South Poles and bulges in the middle.
- The globe is not fixed β it can be rotated (like a top spin or potter's wheel).
- Countries, continents and oceans are shown in their correct size on the globe.
Section 2. Key Reference Lines and Points π
| Term | Definition | Key Fact |
|---|
| Axis | Needle fixed through the globe in a tilted manner | Imaginary line on the real earth β no actual needle |
| North Pole / South Pole | Two points through which the axis passes | Globe moves west to east around this axis |
| Equator | Imaginary line dividing the globe into two equal halves | 0Β° latitude β most important reference point |
| Northern Hemisphere | Northern half of the earth (above equator) | One of two equal halves |
| Southern Hemisphere | Southern half of the earth (below equator) | One of two equal halves |
Section 3. Latitudes β Parallels of Latitude π
π Parallels of Latitudes = All parallel circles from the equator up to the poles. Measured in degrees.
| Fact | Detail |
|---|
| Equator | 0Β° latitude |
| North Pole | 90Β°N latitude |
| South Pole | 90Β°S latitude |
| North of equator | Called north latitudes β marked N |
| South of equator | Called south latitudes β marked S |
| Size of parallels | Decreases as we move away from equator |
Example: Chandrapur (India) = 20Β°N | Belo Horizonte (Brazil) = 20Β°S β same parallel number, opposite hemispheres.
π― By measuring the angle of the Pole Star from your place, you can know the latitude of your place.
Section 4. Important Parallels of Latitudes π
| Parallel | Value | Hemisphere |
|---|
| Tropic of Cancer | 23Β½Β°N | Northern |
| Tropic of Capricorn | 23Β½Β°S | Southern |
| Arctic Circle | 66Β½Β°N | Northern |
| Antarctic Circle | 66Β½Β°S | Southern |
Section 5. Heat Zones of the Earth π
| Heat Zone | Boundaries | Temperature | Reason |
|---|
| Torrid Zone | Tropic of Cancer to Tropic of Capricorn | Maximum heat | Mid-day sun overhead at least once a year |
| Temperate Zones (N + S) | Tropic of Cancer to Arctic Circle (N); Tropic of Capricorn to Antarctic Circle (S) | Moderate | Sun never overhead; rays increasingly slanted |
| Frigid Zones (N + S) | Arctic Circle to North Pole (N); Antarctic Circle to South Pole (S) | Very cold | Sun never rises much above horizon; rays always slanting |
βοΈ Slanted rays spread over a larger area β less heat per unit area. Direct rays concentrate heat on smaller area β more heat. (Source: Torch-light analogy, Figures 2.4a/b)
Section 6. Longitudes β Meridians of Longitude π
π Meridians of Longitude = Semi-circles running from North Pole to South Pole. Measured in degrees (further divided into minutes and seconds).
- Distance between meridians decreases towards the poles β becomes zero where all meridians meet.
- All meridians are of equal length (unlike parallels).
- Counting begins from the Prime Meridian (0Β°) β passes through Greenwich, British Royal Observatory.
- Count goes 180Β° eastward and 180Β° westward from Prime Meridian.
- 180Β°E and 180Β°W are the same line.
- Prime Meridian + 180Β° meridian divide earth into Eastern Hemisphere (E) and Western Hemisphere (W).
Section 7. The Grid π
π Grid = Network of parallels of latitudes and meridians of longitudes. Used to locate any point on the globe.
Example: Dhubri (Assam) = 26Β°N, 90Β°E β find where these two lines intersect on the globe.
Section 8. Longitude and Time π
- Sun is the best natural time-keeper. Local time = reckoned by shadow cast by the sun (shortest at noon).
- Earth rotates 360Β° in 24 hours β 15Β° per hour β 1Β° per 4 minutes.
- Places east of Greenwich = ahead; places west = behind.
| Position | Time when it is 12 noon at Greenwich |
|---|
| 15Β°E | 1:00 p.m. (1 hour ahead) |
| 15Β°W | 11:00 a.m. (1 hour behind) |
| 180Β° | Midnight |
- All places on the same meridian share the same local time.
Section 9. Standard Time π
π Standard Time = Local time of a country's central meridian, adopted as uniform time for the whole country.
Need: Local times differ on different meridians β impractical for train timetables and daily life.
| Detail | Value |
|---|
| India's Standard Meridian | 82Β½Β°E (82Β°30'E) |
| India's Standard Time | Indian Standard Time (IST) |
| IST ahead of GMT | 5 hours 30 minutes |
- Earth divided into 24 time zones of 1 hour each β each zone covers 15Β° of longitude.
- Russia has eleven standard times (largest longitudinal extent example).
Common Confusions β οΈ
| Confusion | Clarification |
|---|
| Latitude vs Longitude | Latitudes = horizontal circles (N/S of equator). Longitudes = vertical semi-circles (E/W of Prime Meridian). |
| Parallels vs Meridians | Parallels decrease in size towards poles. Meridians are all equal length, meeting at poles. |
| Equator vs Prime Meridian | Equator (0Β° lat) β N/S Hemispheres. Prime Meridian (0Β° long) β E/W Hemispheres. |
| Prime Meridian value | Always 0Β° β not 90Β°. North Pole = 90Β°N. These are different things. |
| 180Β°E and 180Β°W | Same line β not two separate meridians. |
Memory Aids π‘
| What to Remember | Mnemonic / Trick |
|---|
| Latitude lines run eastβwest | π‘ LAT = LATeral β flat rungs across the globe like a ladder |
| Longitude lines run northβsouth | π‘ LONG = LONG drop β fall from North Pole to South Pole |
| Cancer = North, Capricorn = South | π‘ C before Ca β Cancer comes first in alphabet, sits above equator (North) |
| Earth rotates 15Β° per hour | π‘ 15 Γ 24 = 360 β one full circle in one full day |
| IST = GMT + 5Β½ hours | π‘ India is "5Β½ steps ahead" β add 5 hours 30 minutes to London time |
Exam Corner π―
Directly from The Earth: Our Habitat Exercise, Pages 16β17:
| Question | Topic | Reference |
|---|
| Q1(a) β True shape of the earth? | Shape of earth | Page 10 |
| Q1(b) β What is a globe? | Globe definition | Page 10 |
| Q1(c) β Latitudinal value of Tropic of Cancer? | Important parallels | Page 11 |
| Q1(d) β Three heat zones of the Earth? | Heat zones | Pages 12β13 |
| Q1(e) β Parallels of latitude and meridians of longitude? | Definitions | Pages 11β13 |
| Q1(f) β Why does torrid zone receive maximum heat? | Heat zones β reason | Page 12 |
| Q1(g) β Why 5:30 p.m. in India when noon in London? | IST / Standard time | Page 15 |
| Q2(a) β Value of Prime Meridian β (ii) 0Β° | Prime Meridian | Page 13 |
| Q2(b) β Frigid zone lies near β (i) the Poles | Frigid zone | Page 13 |
| Q2(c) β Total number of longitudes β (i) 360 | Longitudes | Page 13 |
| Q2(d) β Antarctic Circle located in β (ii) Southern hemisphere | Antarctic Circle | Page 11 |
| Q2(e) β Grid is a network of β (i) parallels of latitudes and meridians of longitudes | Grid | Page 13 |
| Q3(a) β Tropic of Capricorn located at | 23Β½Β°S | Page 11 |
| Q3(b) β Standard Meridian of India | 82Β½Β°E (82Β°30'E) | Page 15 |
| Q3(c) β 0Β° Meridian also known as | Prime Meridian | Page 13 |
| Q3(d) β Distance between longitudes decreases towards | The poles | Page 13 |
| Q3(e) β Arctic Circle located in the __ hemisphere | Northern | Page 11 |
Abbreviation Legend
| Abbreviation | Full Form |
|---|
| IST | Indian Standard Time |
| GMT | Greenwich Mean Time |
| N / S / E / W | North / South / East / West |