Layers _______ of the Earth ayers.

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Presentation transcript:

Layers _______ of the Earth ayers

Today’s Objectives Describe and Explain how and why tectonic plates can move Be able to label and describe Earth’s layers Inner core Outer Core Lower Mantle Upper Mantle Asthenosphere Crust ( including the tectonic plates) Be able to define and describe the term lithosphere, asthenosphere

Regions of the Earth The Earth is made up of three major regions, like an apple: Crust (like the skin) Mantle (like the flesh of the fruit) Core (like the core and seeds)

Earth can be further divided into more layers!

A.The Crust (0-35km) The crust is the top, solid surface layer of the Earth Oceanic crust is the crust under oceans, and continental crust is the crust under the continents It can range from 10km thick (oceanic) to 70km thick (continental)

LITHOS= STONE Plate Tectonics Below the crust is where we find the plates. The crust is attached to the plates The crust and the plates are both solid, rigid and hard We can give the Crust and the Plates a special name= LITHOSPHERE LITHOS= STONE

CRUST PLATES

Tectonic PLATES PLATES Tectonic plates make up the upper most region of a layer called the MANTLE. PLATES

The Mantle: (35-2900km) The mantle is the semi-solid layer directly below the crust. It contains 70% of the Earth’s volume It can itself be broken into 2 distinct parts: The Upper Mantle (35- 670 km) Rigid plates at top part of Upper Mantle Flowing transition zone at bottom part of Upper Mantle called the Asthenosphere The Lower Mantle (670- 2900km)

The Upper Mantle:(35 - 670 km) 660 km think Separated into 2 layers The layer closest to the crust is the solid rock layer that makes up the tectonic plates The layer below the plates is the semi-solid molten layer called the ASTHENOSPHERE

ASTHENOS= WEAK The Asthenosphere The molten rock layer, with a consistency of thick toothpaste Convection Currents in the asthenosphere are partly responsible for the movement of the plates The majority of the heat comes from radioactive decay within the mantle ASTHENOS= WEAK

The Lower Mantle: (670 - 2900km) The lower mantle comprises nearly 50 percent of the Earth’s Interior It is made of solid rock, but has plumes of liquid magma that convect heat from the core to the plates.

The Outer Core: (2900 - 5200km) The outer core consists of flowing, liquid metal. This movement creates the Earth’s main magnetic field. It is composed of Iron and Nickel It is somewhere between 3700- 5500 K

The Inner Core: (5200-6371km) While most of the core is liquid, the inner core is solid Nickel and Iron The inner core is 6000 K!!!

How can we remember... Make a mnemonic (5 minutes) Layers from the crust inward Letters CRUST C UPPER MANTLE U LOWER MANTLE L OUTER CORE O INNER CORE I

Summary: Plate

Earth’s Layers and Plate Movement We care about the layers of the Earth because they can help us to explain how the Earth’s tectonic plates move Convection Currents in the mantle (asthenosphere), thermal heat from the core, gravity and plate interaction all affect plate movement!

Review Quiz! Which layer(s) are part of the lithosphere? Crust, Tectonic plates (uppermost Mantle) Why is it called the lithosphere? Lithos=rock, these layers are rigid (hard) Which layer(s) are part of the asthenosphere? Bottom part of Upper Mantle (flowing) Why is it called the asthenosphere? Asthenos=weak, this layer is flowing (like toothpaste) Which layer is most responsible for movement of the tectonic plates? Asthenosphere What causes this movement? Convection currents in the asthenosphere. Heat from near the core rises and then cools down creating a convection current

Homework Define the following terms in your vocabulary book (you should know these words for next class): plate tectonics, plate boundary, earthquake, trench, volcano, spreading ridge, subduction zone, hot spot Make a cross-section drawing of the earth that shows all the layers, and label them Include approximate depths, consistency (solid? Liquid?), elements (what is made of), etc. DUE: Monday, start of class! Workbook: pg. 218