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Unit 5: Plate Tectonics

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Tuesday 3/26��BW: Where does Earth get its energy from? Give an example of how it gets energy from this source.

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Energy in Earth’s Four Spheres

  1. Geosphere
  2. Hydrosphere
  3. Atmosphere
  4. Biosphere

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Where does the energy in all four spheres come from?

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Key Idea: The vast majority of ALL energy in the four spheres comes from the SUN

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Hydrosphere: All the water on Earth (oceans, lakes, ponds, water in soil, etc.)

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Energy in the Hydrosphere

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Energy in the Hydrosphere

  • The properties and motion of the hydrosphere are important in MAINTAINING DIVERSE CLIMATES that exist worldwide
  • The Ocean (97% of water on Earth) serves as a reservoir which contributes to how much SOLAR RADIATION (ENERGY) is absorbed.
  • The ocean serves to REDISTRIBUTE ENERGY AND HEAT around the globe, contributing to the different average temperatures that exist over the globe

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Atmosphere: All the gases surrounding Earth (oxygen, nitrogen, methane, etc.)

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Energy in the Atmosphere

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Wednesday 4/3

BW: What are the four spheres of earth? Describe the transport of energy within the sphere that accounts for all of earth’s water.

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Energy in the Atmosphere

  • The atmosphere ABSORBS ENERGY FROM THE SUN in different ways to support life on Earth:
    • Protects life on Earth by SHIELDING IT FROM INCOMING ULTRAVIOLET RADIATION
    • Keeps planet warm THROUGH INSULATION
    • Preventing extremes between day and night temperatures
  • The sun heats layers of the atmosphere causing it to convect DRIVING AIR MOVEMENT and WEATHER PATTERNS around the world.

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Biosphere: All the living things surrounding Earth (plants, animals, and humans)

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Energy in the Biosphere

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Energy in the Biosphere

  • Energy flows from the sun to PRODUCERS (ex: plants) which are the source of all energy in an ecosystem
  • DECOMPOSERS return the energy from dead animals to the soil for producers to use

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Geosphere: All the rock on Earth (all the way down to the core)

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The Layers of the Geosphere

  • The CRUST is Earth’s thin, cool, and rigid outermost rock layer
  • The MANTLE is Earth’s hot, middle rock layer, located between the crust and core
  • The CORE is Earth’s hot, dense, innermost rock layer, located below the mantle

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Energy Transfers Through Convection

  • CONVECTION causes the heated, less dense rock in the mantle near the core to RISE UPWARD, toward the crust
  • As it cools, the colder denser rock SINKS DEEPER into the mantle toward the core due to gravity

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Brainstorm some changes that have happened to the Earth since the beginning of time

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Small Scale Changes

  • Weathering is the breakdown of rock on Earth’s surface
  • Erosion is the removal of rock material by wind, water, ice, or gravity.
  • Deposition is the accumulation of eroded rock material that has been transported from another location

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Many Small Changes Lead to Big Changes

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Key Idea: Many SMALL changes add up to a LARGE change over time

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Slow Changes and Fast Changes

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Do you think these changes we talk about occur similarly to how they did in the distant past? Why or why not?

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Key Concept: Uniformitarianism

Uniformitarianism: the idea that any natural processes we can observe today happened in the same way in the past and will also happen in the same way in the future

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Key Idea: Earth is a DYNAMIC planet, always changing in BIG, SMALL, QUICK, and SLOW ways!

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Tuesday 4/9

BW: How does energy pass through the biosphere?

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Wednesday 4/10

BW: Name an example of a quick change that has happened to earth’s geology. Name an example of a slow change.

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Monday 4/22

BW: What are the three pieces of evidence for Continental Drift Theory? Give an example within each.

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Continental Drift Theory Skit

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Tuesday 4/23

BW: Why did people dismiss Wegener’s theory of Continental Drift?

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Tuesday 4/30

BW: How do you think the continents split apart? Don’t just say plate tectonics; be specific.

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Seafloor Spreading

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Seafloor Spreading: Process by which rocks on either side of the mid-ocean ridge slowly pull away from each other, allowing molten rock to rise and solidify, forming new seafloor

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What evidence would be useful in proving seafloor spreading? (Hint: Think back to rock strata)

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If seafloor spreading were occurring, then the seafloor closest to the mid-ocean ridge would be the youngest, and the seafloor farthest away from the mid-ocean ridge would be the oldest.

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What is causing the seafloor to rise/spread?

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Earth as a terrestrial planet has three distinct layers. What are the names of these three layers?

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  • Convection causes the HEATED, LESS DENSE rock in the mantle to RISE UPWARD, toward the crust
  • Gravity causes the COOLER, MORE DENSE rock to SINK DEEPER into the mantle
  • This circular pattern of movement within the mantle of the Earth based on density is called a CONVECTION CYCLE

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Friday 5/3

BW: What causes seafloor spreading?

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If seafloor spreading is happening, what might you expect to be happening to the size of Earth?

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In other parts of the seafloor, scientists discovered deep valleys called TRENCHES

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What happens when two things collide and neither stops moving?

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Subduction

  • Old seafloor moves back down under the trench through a process called SUBDUCTION
  • Subduction occurs when the collision between two tectonic plates forces the MORE DENSE plate under the LESS DENSE plate

What happens to the old sea floor during subduction?

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  • Scientists often refer to the crust/upper mantle layer as the lithosphere
  • This is made up of separate slabs called tectonic plates
  • These plates are 100 to 120 km thick and include the crust and a small part of the upper mantle

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Monday 5/6

BW: What is the process of subduction and what causes it? (include words plates and dense)

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Seafloor Spreading Model

  • You will create your own diagram of seafloor spreading. Be sure to show the following in your model and include captions that describe what is happening
    • Convection, subduction, mid-ocean ridge, trench, old rock, new rock
    • Also include the DIRECTION that the new rock and old rock follow using arrows

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Tuesday 5/7

BW: What makes up a plate? If the continents drifted apart from one another, what must that mean about how the earth is structured?

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Plate Tectonic Theory

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  • Scientists often refer to the crust/upper mantle layer as the lithosphere
  • This is made up of separate slabs called tectonic plates
  • These plates are 100 to 120 km thick and include the crust and a small part of the upper mantle

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If parts of the Earth’s lithosphere are moving in different directions, what must that mean about how it is structured?

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Plate Tectonic Theory

  • PLATE TECTONICS: the theory that the lithosphere is made up of rigid pieces, called tectonic plates, that move across Earth’s surface
  • Tectonic plates carry the land or water on top of them and fit together like the PIECES OF A PUZZLE
  • There are 15 MAJOR PLATES and several smaller ones not shown

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If plate tectonics is what has caused continental drift, how fast do you think the plates move?

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What causes the plates to move?

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  1. Mantle Convection: Convection in the mantle pushes new rock upward at the ridge
  2. Seafloor Spreading: this new rock solidifies and pushes old rock further and further away
  3. Subduction: the denser plate sinks into and becomes part of the mantle and the rock is recycled

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Three Types of Boundaries

Tectonic Plates interact in THREE ways and form:

  • Convergent Boundaries
  • Divergent Boundaries
  • Transform Boundaries

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Convergent Boundaries

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Convergent Boundaries

  • A convergent boundary occurs where two plates move TOWARD EACH OTHER
  • When this happens, the MORE DENSE plate is subducted under the LESS DENSE plate
  • Subduction causes a TRENCH to form on the seafloor
  • The other plate rises toward the surface and results in VOLCANOES or MOUNTAINS

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Divergent Boundaries

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Divergent Boundaries

  • A divergent boundary occurs where two plates MOVE AWAY FROM each other
  • This process causes seafloor spreading, which causes OCEANS AND SEAS TO BECOME WIDER

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Transform Boundaries

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Transform Boundaries

  • A transform boundary occurs where two plates SLIDE HORIZONTALLY PAST EACH OTHER
  • The tectonic forces push on the plates in OPPOSITE DIRECTIONS, stress builds up along the transform boundary

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Add the three types of boundaries to your guided notes

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Wednesday 5/8

BW: What are the three types of boundaries? Choose one to describe in detail

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What do you think happens when the tension of a transform boundary gets too great?

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So where do volcanoes form and earthquakes happen?

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Thursday 5/9

BW: Why are there so many volcanoes and hurricanes in the ring of fire?

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Rock Cycle

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What is a rock?

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Not this rock…

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What makes up a rock?

  • Rocks are composed of MINERALS

  • Minerals are composed of CRYSTALS

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How do scientists classify different rocks?

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How do you differentiate between rocks?

  1. Composition: What they are made of

  • Texture: Way it looks and feels

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Three Types of Rocks

  • Igneous
  • Metamorphic
  • Sedimentary

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Igneous Processes

  • Igneous rock forms when magma COOLS AND HARDENS
  • The TEXTURE of the rock is determined by how QUICKLY the magma cools
  • When magma starts to cool, its minerals begin to CRYSTALLIZE
  • The SLOWER the cooling, the LARGER the crystals will become

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Intrusive Rock (Igneous)

INTRUSIVE ROCK is igneous rock that forms when magma slowly hardens BELOW Earth’s surface

Examples: Granite / Gabbro

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Extrusive Rock (Igneous)

EXTRUSIVE ROCK is igneous rock that forms when magma cools quickly ON EARTH’S SURFACE (usually from volcanic eruption)

Examples: Pumice / Basalt

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Friday 5/10

BW: What are the two types of igneous rocks? Describe both.

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Metamorphic Processes

  • Metamorphic rock forms from when existing rocks are transformed by HEAT OR PRESSURE
  • They can be grouped into TWO categories based on how they FORM
    • Deformation
    • Recrystallization

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Recrystallization - Changes the actual chemical makeup of the rock just like a cookie baking.

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Brainstorm some ideas about how rocks might break down

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Sedimentary Processes

  • Sedimentary rocks form from the COLLECTION AND CEMENTATION of dissolved minerals, rock fragments, or the remains of organisms
  • Preexisting rocks are broken down through a process called WEATHERING

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Two Types of Weathering

Physical Weathering

  • The breakdown of rock by physical processes (rain, water, wind, etc.) is called PHYSICAL WEATHERING
  • Only changes the SIZE OR SHAPE of the rock!

Chemical Weathering

  • Rock can react chemically when exposed to air, water, soil, and organisms through CHEMICAL WEATHERING
  • Changes the COMPOSITION of the rock!

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Key Idea: All weathering eventually leads to sediment (small pieces of broken-down rock) which then form sedimentary rocks

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Forming of Sedimentary Rock: Erosion vs. Deposition

EROSION is the action of surface processes that REMOVES weathered soil, rock, or dissolved material from one location and then TRANSPORTS IT TO ANOTHER LOCATION

This is a DESTRUCTIVE process

DEPOSITION is when sediments, soil, or rocks are ADDED to the land. Eventually, these rocks form layers through a process called CEMENTATION

This is a CONSTRUCTIVE process

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Key Idea: The Rock Cycle is a continuous set of processes by which any type of rock can CHANGE into any other type.

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What Drives the Rock Cycle?

  • SOLAR ENERGY from the SUN which causes weathering and erosion by wind and water
  • INTERNAL ENERGY from the Earth’s CORE which causes magma

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