prepared by: ms. siddhi hegde pawar public school kandivali

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The Four Realms of the Earth Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

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Page 1: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

The Four Realms of the Earth

Prepared by: Ms. Siddhi Hegde Pawar Public SchoolKandivali

Page 2: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

How many planets do we have?

Which planet has life?

Page 3: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

EarthLiving planet.

Only planet that supports life.

Page 4: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Life possible on Earth because-

Page 5: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Biosphere

Atmosphere

Hydrosphere

Lithosphere

Page 6: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Lithosphere• Derived from Greek word for stone –

litho.• Solid outer part of earth.• Thin cover of soil. Helps the plants to

grow.• 29% of earth’s surface.• 7 huge masses – 7 continents.• The edges of the continents and the

ocean floors together form the lithosphere.

Page 7: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Structure of the Earth• The earth’s

interior is based on density of materials and behaviour of seismic waves.

• The crust forms only 1 % of the volume of the earth, 84 % consists of mantle and 15 % makes up the core.

Page 8: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Crust• Outermost and thinnest layer.• Thickness varies.• Two types – continental crust and

oceanic crust.

SIMA

SIMA

Page 9: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Cross section of the Earth

Page 10: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

• Rocks • Minerals

Page 11: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Types of rocks

Igneous

Intrusive

Extrusive

Sedimentary

Metamorphic

Page 12: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali
Page 13: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Atmosphere

• Derived from Greek word for air – atmo.

Page 14: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Vertical change in average global atmospheric temperature. Variations in the way temperature changes with height indicates the atmosphere is composed of a number of

different layers (labeled above). These variations are due to changes in the chemical and physical characteristics of the

atmosphere with altitude.

Page 15: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Most of our planet's weather occurs in the troposphere. This image shows a view of this layer from an airplane's window (Photo © 2004 Edward

Tsang).

Page 16: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Hydrosphere

• Derived from Greek word for water – hydro.

Page 17: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

• The second factor controlling tides on the Earth's surface is the Sun's gravity. The height of the average solar tide is about 50% the average lunar tide. At certain times during the moon's revolution around the Earth, the direction of its gravitational attraction is aligned with the Sun's (Figure 8r-2). During these times the two tide producing bodies act together to create the highest and lowest tides of the year. These spring tides occur every 14-15 days during full and new moons.

Page 18: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Forces involved in the formation of a spring tide

Page 19: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

• When the gravitational pull of the moon and Sun are at right angles to each other, the daily tidal variations on the Earth are at their least (Figure 8r-3). These events are called neap tides and they occur during the first and last quarter of the moon.

Page 20: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Forces involved in the formation of a neap tide.

Page 21: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

The following illustration describes the flow pattern of the major subsurface ocean currents. Near surface warm currents are drawn in

red. Blue depicts the deep cold currents. Note how this system is continuously moving water from the surface to deep within the

oceans and back to the top of the ocean. (Source: Arctic Climate Impact Assessment -ACIA).

Page 22: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Hydrologic Cycle.

Page 23: Prepared by: Ms. Siddhi Hegde Pawar Public School Kandivali

Biosphere

• Derived from .Greek word for life – Bio.