Notes: The Earth System• A system is a group of parts that work together as

a whole. • The constant flow, or cycling, of matter through

the Earth system is driven by energy. • Energy is the ability to do work. • Energy that drives the Earth system has two main

sources:1.) heat from the sun2.) heat flowing out of Earth as it cools

pg. 63

Earth’s System Has 4 Main Spheres:

1.) Atmosphere- Earth’s outermost layer made up of a mixture of gases: mostly nitrogen and oxygen. Contains dust, cloud droplets, water

vapor, rain, snow, earth’s weather

pg. 65

2.) Geosphere- the solid rocks and metals that make up the Earth. Four parts: crust,

mantle, outer core, inner core

pg. 65

3.) Hydrosphere- Contains all of Earth’s water. Water covers about ¾ of Earth’s surface.

97% is salt water 2% is frozen in the polar

ice caps 1% is drinkable (fresh

water)

pg. 65

4.) Biosphere- the parts of Earth that contain

living organisms

pg. 65

Notes: Constructive Vs. Destructive ForcesLands are constantly being created and destroyed by competing forces. Constructive Forces Destructive ForcesForces that construct and shape the land’s surface by building up mountains and other land masses.

Examples:

Forces that destroy and wear away

landmasses.

Examples:

pg. 67

Notes: Earth’s LayersHow do Geologists Learn About Earth’s Layers? A. They use two main types of evidence to learn about Earth’s

interior: 1.) direct evidence from rock samples a. Geologists have drilled holes as deep as 12.3 km into

Earth. b. The drills bring up samples of rock. These rocks give

geologists clues about Earth’s structure and conditions deep inside Earth.

2.) indirect evidence from seismic waves. a. When earthquakes occur, they produce seismic waves . b. Geologists record the seismic waves and study how they

travel through Earth.

pg. 69

What Are the Features of Earth’s Layers? B. The three main layers of Earth are the crust, mantle and core.

1.) The layers vary greatly in size, composition, temperature, and pressure.2.) The deeper down inside Earth, the greater the pressure. 3.) The temperature inside earth increases as depth increases.

C. The Layers of the Earth1.) Crust – a layer of solid rock that includes both dry land and the ocean floor (Earth’s outer skin) a. Oceanic Crust – the crust that lies beneath the ocean;

mostly composed of basalt (a dark, fine-grained rock) b. Continental Crust – the crust that forms the continents;

mostly composed of granite (a rock that is usually light in color and has coarse grains)

2.) Mantle – a layer of rock that is solid, and very hot

a. Lithosphere – made up of the crust and upper mantle; strong, hard and rigid rock

b. Asthenosphere – below the lithosphere; the material is hotter and under more pressure; the material can bend but is still considered a solid

3.) Core – below the mantle; made mostly of the metals iron a nickel; consists of 2 parts a. Outer Core – molten/liquid metals of iron and nickel b. Inner Core – dense ball of solid metals iron and nickel

Draw and Label the Layers of the EarthPg. 68

Mantle

Crust

Outer Core

Inner Core

Asthenosphere

Lithosphere

I. Plate Tectonics A. ___Continental Drift______

1. Many early scientists have noticed that the Earth’s continents seemed to fit together. 2. ___Alfred Wegener____- proposed

the theory of continental drift a. _Permian Period_ - about 225 million years ago 1.) all the continents formed a supercontinent called Pangaea 2.) ____Panthalassa____ was the major ocean b. __Triassic Period____ - Pangaea was split in two 1.) _____Laurasia_____ in the north (North America, Eurasia) and Gondwanaland in the south ( India, Africa, and South America) 2.) Panthalassa broken in two, one part becomes the ____Tethys Sea______

pg. 71

c. Wegner theorized that continents moved horizontally to their present location.

B. Evidence of Continental Drift 1. Fossil and Climate Clues

a. The reptile ___Mesosaurus____ 1.) fossils found in South America

and Africa 2.) lived on land and water but

would have been impossible for this animal to have swam across an entire ocean

b. A fern _____Glossopteris________ 1.) fossils found in Africa, Australia,

India, South America, and Antarctica

2.) found in areas that vary greatly in climate, scientists believe

these regions once were connected and had similar climates

c. Fossils of warm weather plants were found in Arctic Ocean Islands d. Glacial deposits have been found where no glaciers exist today

2. Sea-floor Spreading

a. ___Mid-Ocean Ridge____- 1. using sound waves, scientists discovered a

system of underwater mountain ranges in many oceans

2. The peaks of some of these mountains can form an island

b. 1960’s scientist, _Harry Hess_, suggested a theory of ___sea-floor spreading___

1. Magma gets forced upward through cracks in the ocean floor 2. As new material comes up it pushes sections of the sea floor away from the ridge. 3. The magma solidifies and creates new sea floor c. Evidence for Sea-floor Spreading

1. Youngest rocks are located at the mid- ocean ridge 2. Reversals of Earth’s magnetic field are

recorded by rocks in strips parallel to ridges

Harry Hess

C. Plate Tectonics

1. Earth’s crust and upper mantle are broken into sections called __plates_____

a. The crust and upper mantle are called the ______lithosphere_________ b. Middle layer of the mantle is the _asthenosphere__ - semi-molten rock, very plastic-like

c. __Convection Currents__ inside Earth cause plate tectonics – the cycle of heating, rising, cooling, and sinking of material inside Earth

2. Plate Boundaries

a. Divergent Boundary - two plates move away from one another; ex. Sea-floor spreading

b. Convergent Boundary -two plates move toward each other, there are three types: 1.) subduction zone- dense ocean plate sinks under light continental plate ex: deep sea trench, volcanic mountain chains 2.) two ocean plates collide ex: deep sea trench, volcanic island chain 3.) two continental plates collide ex: mountains, earthquakes common

c. Transform Fault Boundary - two plates slide past each other; they can

move in opposite directions or in the same direction

Types of Heat TransferRADIATION

The transfer of energy that is carried in rays like light

Examples:•Roasting a marshmallow•Heat from a fire•Getting a sunburn

CONDUCTION

Heat transfer between materials that are touching

Examples:•Frying an egg in a pan•Burning your feet on hot sand•Using a heating pad on sore muscles

CONVECTION

Heat transfer by the movement of a fluid

Examples:•Heating a pot of soup on the stove•Warm air from a heater rising to the ceiling•Cold air from freezer sinking to the floor

pg. 73

I. Plate Tectonics A. _________________________

1. Many early scientists have noticed that the Earth’s continents seemed to fit together. 2. _____________________ - proposed

the theory of continental drift a. __________________- about 225 million years ago 1.) all the continents formed a

supercontinent called

__________________ 2.) _____________________ was

the major ocean b. ___________________ - Pangaea was split in two 1.) ____________________ in the

north (North America, Eurasia) and ______________ in the south ( India, Africa, and South America) 2.) Panthalassa broken in two,

one part becomes the _________________________

pg. 59

c. Wegner theorized that continents moved horizontally to their present location.

B. Evidence of Continental Drift 1. Fossil and Climate Clues

a. The reptile ____________________ 1.) fossils found in South America

and Africa 2.) lived on land and water but

would have been impossible for this animal to have swam across an entire ocean

b. A fern ________________________ 1.) fossils found in Africa, Australia,

India, South America, and Antarctica

2.) found in areas that vary greatly in climate, scientists believe

these regions once were connected and had similar climates

c. Fossils of warm weather plants were found in Arctic Ocean Islands d. Glacial deposits have been found where no glaciers exist today

2. Sea-floor Spreading a. _________________________-

1. using sound waves, scientists discovered a system of underwater mountain ranges in

many oceans 2. The peaks of some of these mountains can form an island b. 1960’s scientist, ______________suggested

a theory of _________________________ 1. Magma gets forced upward through cracks in the ocean floor 2. As new material comes up it pushes sections of the sea floor away from the ridge. 3. The magma solidifies and creates new sea floor c. Evidence for Sea-floor Spreading

1. Youngest rocks are located at the mid- ocean ridge 2. Reversals of Earth’s magnetic field are

recorded by rocks in strips parallel to ridges

Harry Hess

C. Plate Tectonics

1. Earth’s crust and upper mantle are broken into sections called ___________________

a. The crust and upper mantle are called the ____________________________ b. Middle layer of the mantle is the _________________- semi-molten rock, very plastic-like c. ______________________ inside Earth cause plate tectonics – the cycle of heating, rising, cooling, and sinking of material inside Earth

2. Plate Boundaries

a. __________________- two plates move away from one another; ex. Sea-floor spreading

b. __________________-two plates move toward each other, there are three types: 1.) subduction zone- dense ocean plate sinks under light continental plate ex: deep sea trench, volcanic mountain chains 2.) two ocean plates collide ex: deep sea trench, volcanic island chain 3.) two continental plates collide ex: mountains, earthquakes common

c. _________________________- two plates slide past each other; they can

move in opposite directions or in the same direction