The document describes the structure and composition of Earth. It discusses how Earth is made up of four interconnected spheres - the atmosphere, geosphere, hydrosphere, and biosphere. It then focuses on the layers that make up Earth's interior, including the crust, mantle, and core. The crust and mantle are composed mainly of oxygen, silicon, and metals. Heat from the core drives convection currents in the mantle and outer core.
2. System- a group of parts that work together
Energy- the ability to do work. Earth gets
its this ability to work (energy) from the
sun and from the center of the earth as it
cools.
Earth itself is a closed system, but on
earth there are open systems or spheres that
influence one another.
3. The Spheres of the
Earth System:
Atmosphere: the
relatively thin layer of gases that forms
earth’s outermost layer
Mostly Oxygen & Nitrogen
Dust particles
Cloud droplets
Earth’s weather
4. The Spheres of the
Earth System:
Geosphere: nearly all of
earth’s mass
Rocks
Metal & other Minerals
Has three layers
5. The Spheres of the
Earth System:
Hydrosphere: contains all of
Earth’s water
Oceans, glaciers, rivers, lakes, ground
water, & water vapor
Covers ¾ of the Earth
Mostly salt. Only a tiny portion is drinkable.
6. The Spheres of the
Earth System:
Biosphere: the part of
Earth where life exists.
Feedback = the communication between
the spheres
9. GEOLOGISTS are
scientists who study the
processes that create
Earth’s features and
search for clues about
Earth’s HISTORY.
10. What does a geologist do???
They study the CHEMICAL and PHYSICAL
characteristics of rock, the material that forms
Earth’s hard surface.
They map where different types of rocks are
found and describe LANDFORMS, the features
sculptured in rock and soil by water, wind, and
waves.
They study how seismic waves (waves
caused by earthquakes) travel through earth.
11.
12. 2 VERY IMPORTANT
FORCES!
Two forces Change Earth’s Surface:
CONSTRUCTIVE forces – shape the
surface by building up mountains and
landmasses.
Destructive forces are those that slowly
wear away Land masses and, eventually,
every other feature on the surface.
16. THE CRUST
The layer of rock that forms
Earth’s OUTER skin.
Includes dry land and the
OCEAN floor.
Approx. 5 - 40 km thick.
17. More about the CRUST
COMPOSITION – oxygen,
silicon, aluminum, calcium,
iron, sodium, potassium,
magnesium
Temperature VARIES
18. There are 2 types of CRUST
Oceanic crust - the crust beneath the
OCEAN
The THINNEST crust is under the
ocean.
CONTINENTAL crust – the crust that
forms the continents and some major
islands.
19. A Special Note:
The deeper down into Earth, the
greater the pressure and temperature.
(just below earth the rock is cool, but after about
20meters down the temperature
increases nearly 1oC/40m)
20. THE MANTLE
The layer of HOT ROCK below the
crust
Starts 5 – 40 km beneath the
surface
Approx. 3,000 km thick
COMPOSITION – silicon, oxygen,
iron, magnesium
Temperature – 870 °C
21. THREE mantle layers
Lithosphere – brittle rock
Asthenosphere – less rigid rock (metal spoon)
Mesosphere – hot but more rigid due to pressure
22. THE CORE
Makes up 1/3 of Earth’s MASS,
but only 15% of its volume.
Composition – IRON and
NICKEL
23. Outer core – layer of MOLTEN METAL
that surrounds the inner core
The liquid metal causes CURRENTS*
Temperature – 2,200 °C
Approx. 2,250 km thick
24. Inner core – dense ball of solid metal under
extreme pressure.
The solid inner core spins at a slightly
FASTER rate than the spinning of the
whole Earth.
Earth’s MAGNETIC field is created by this
movement
Causes the planet to act like a giant bar
MAGNET
26. BACK TO THOSE CURRENTS. . .
prezi
Heat Transfer (from warm to cool):
Conduction-by touching
Convection – by the movement of fluid
Radiation- by light
27. Density = mass/volume
So. . .
Heat from the core (and the mantle itself)
act like a stove top heating soup. . . this
causes convection currents (hot to cold-rising
& sinking)