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By Savita S. More

TN Board Class 6 Social Science Unit 1 The Universe and the Solar System

 

The velocity of the Earth’s rotation is zero at poles.

The velocity of the Earth’s rotation is zero at the poles because of the nature of rotational motion. At the poles, the rotational axis intersects the surface, so there is no lateral movement as the Earth spins. All points at the poles essentially stay in the same position while the Earth rotates around its axis. Conversely, at the equator, points on the surface travel the longest distance in a day, leading to the highest rotational velocity.

 

Answer in detail

 

Distinguish between inner and outer planets.

Inner Planets (Terrestrial Planets) Outer Planets (Jovian Planets)
Mercury, Venus, Earth, Mars Jupiter, Saturn, Uranus, Neptune
Closer to the Sun Farther from the Sun
Primarily composed of rock and metal Primarily composed of gases and ices
Smaller in size Larger in size
Solid, rocky surfaces Gaseous with no well-defined solid surface
Thinner atmospheres Thick atmospheres composed mainly of hydrogen and helium
Few or no natural satellites Many natural satellites
No ring systems Prominent ring systems (especially Saturn)
Higher temperatures due to proximity to the Sun Lower temperatures due to distance from the Sun
Slower rotation Faster rotation

 

What are the effects of rotation and revolution?

  Rotation:

Day and Night: The Earth’s rotation on its axis causes day and night. As the Earth rotates, different parts of its surface move into and out of the sunlight, creating a cycle of daylight and darkness approximately every 24 hours.

Coriolis Effect: The rotation of the Earth affects the movement of air and water masses, causing them to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This is known as the Coriolis effect and influences weather patterns and ocean currents.

Time Zones: The Earth’s rotation is divided into 24 time zones, each one roughly corresponding to 15 degrees of longitude. This system helps standardize time across different regions of the world.

  Revolution:

Seasons: The Earth’s revolution around the Sun, combined with the tilt of its axis, causes the changing seasons. As the Earth orbits the Sun, different parts of the Earth receive varying amounts of sunlight throughout the year, resulting in seasonal changes.

Varying Day Lengths: The tilt of the Earth’s axis also causes variations in the length of day and night throughout the year. During summer, days are longer, and nights are shorter, while during winter, days are shorter, and nights are longer.

Equinoxes and Solstices: The Earth’s revolution leads to specific points in the year known as equinoxes (when day and night are equal) and solstices (the longest and shortest days of the year). These occur due to the tilt and position of the Earth in its orbit.

 

Explain the characteristics of the various spheres of the Earth.

  Lithosphere:

The lithosphere is the solid, outermost layer of the Earth. It includes the crust and the upper part of the mantle.

It consists of various types of rocks and minerals and forms the continents and ocean floors.

The lithosphere is broken into tectonic plates that float on the semi-fluid asthenosphere below. The movement of these plates causes earthquakes, volcanic activity, and the formation of mountains.

  Hydrosphere:

The hydrosphere encompasses all the water on Earth, including oceans, seas, rivers, lakes, glaciers, and water vapor in the atmosphere.

It covers about 71% of the Earth’s surface, with the vast majority of this water found in the oceans.

The hydrosphere plays a crucial role in regulating the Earth’s climate and weather patterns through the water cycle, which includes processes such as evaporation, condensation, precipitation, and runoff.

  Atmosphere:

The atmosphere is the layer of gases surrounding the Earth. It is composed primarily of nitrogen (78%) and oxygen (21%), with traces of other gases like carbon dioxide, argon, and water vapor.

The atmosphere is divided into several layers based on temperature and composition: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere.

It protects life on Earth by absorbing harmful solar radiation, reducing temperature extremes between day and night, and providing essential gases for respiration and photosynthesis.

  Biosphere:

The biosphere is the zone of life on Earth, where living organisms interact with the lithosphere, hydrosphere, and atmosphere.

It includes all ecosystems, from the deepest ocean trenches to the highest mountains, where life is possible.

The biosphere is characterized by the presence of life forms, including plants, animals, and microorganisms, which depend on and contribute to the cycling of nutrients and energy within their environments.

 

 

 

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