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The Physical World Chapter 2.

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Presentation on theme: "The Physical World Chapter 2."— Presentation transcript:

1 The Physical World Chapter 2

2 THE SUN The planets: (at least 8) and each is in it’s own orbit around the sun Mercury, Venus, Earth and Mars= inner planets Jupiter, Saturn, Uranus, Neptune= outer planets Largest= Jupiter Earth= 5th in size Smallest= Mercury All the planets except Mercury and Venus have moons. Planet Earth

3 Our solar system

4 Our Solar System Ceres and Pluto are dwarf planets
Terrestrial planets and gas planets T= Mercury, venus, Earth and Mars G= Jupiter, Saturn, Uranus, and Neptune Asteroids: small, irregular shaped, planet-like objects (Between Mars and Jupiter) Asteroid Belt Comets: made of icy dust particles and frozen gases look like bright balls with long, feathery tails Meteoroids: pieces of earth debris- chunks of rock and iron. Our Solar System

5 Hydrosphere: 70% of our planet’s surface is water
Hydrosphere: 70% of our planet’s surface is water. Made up of Rivers, Oceans, Lakes, and other bodies of water. Lithosphere: 30% of the Earths surface is land. Made up of continents and islands. Atmosphere: The air we breathe. Made up of 78% nitrogen, 21 % oxygen and small amounts of argon and other gases Biosphere: all people, animals and plants live on or close to the Earth’s surface. Getting to know Earth

6 Earth’s Height and Depths
Highest point: Mount Everest 29,028 feet Lowest dry point: Dead Sea at feet below sea level Underwater canyon: Mariana Trench- 35,827 feet Earth’s Height and Depths

7 Core: Very center of the planet is a super-hot but solid inner core (iron and nickel). Outer core has iron and nickel melted. Mantle: thick layer of hot dense rock, consisting of silicon, aluminum, iron, magnesium, oxygen and other elements. Crust: a rocky shell forming the Earth’s surface 2 miles thick under oceans, 75 miles thick under mountains. Crust is broken up into more than a dozen great slabs of rock called plates that float on a partially melted layer in the upper portion of the mantle. The plates carry the Earth’s oceans and continents. Earth’s Structure

8 Earth’s Structure

9 Pangaea: continentals together before continental drift.

10 Plates

11 Continental drift: the theory that the continents were once joined and then slowly drifted apart.
Plate Tectonics: the term scientist use to describe the activities of continental drift and magma flow, which create many of Earth’s physical feature. Magma: molted rock that is located below Earth’s surface Vocabulary

12 Plates Continental plates: granite, lighter, less dense material
Oceanic plates: basalt, darker, more dense Plates

13 How plates move Oceanic----continental (volcano, magma melts)
Continental >---< continental (mountains) Continental -- continental (rift) Spreading Oceanic -- Oceanic (islands, volcanoes) Oceanic ---- sea floor spreading How plates move

14 Fold: a Bend in layers of rock, sometimes caused by plate movement
Fault: a crack or break in Earth’s crust Faulting: process of cracking that occurs when the folded land cannot be bent any further. Convention currents: magma heating and cooling like a lava lamp Hot spots: magma comes closer to the crust Vocabulary


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