Layers of the Earth Using a laser pointer, briefly highlight and describe the layers of the earth’s interior. Also highlight the fact that the earth has.

Slides:



Advertisements
Similar presentations
Plate Tectonics.
Advertisements

Plate Tectonics 1.1 Earth has several layers. 1.2
Plate Tectonics.
Plate Tectonics The Earth’s Crust in Motion…. The Theory In 1910 Alfred begins to wonder… What’s the relationship? Perhaps all these pieces used to be.
STRUCTURE OF THE EARTH Noadswood Science, 2011.
Plate Tectonics.
PLATE TECTONICS Why the Earth is Like It Is. Earth Layers Earth is made up of 5 layers: 1.Inner Core 2.Outer Core 3.Mantle 4.Asthenosphere (Lower and.
Plate Tectonics. Plate Tectonics What is Plate Tectonics The Earth’s crust and upper mantle are broken into sections called plates Plates move around.
Chapter 10 Plate Tectonics. Alfred Wegener Proposed they hypothesis of continental drift Proposed they hypothesis of continental drift CONTINENTAL DRIFT-
Earth’s Layered Structure (Ch. 8.4 in the Text)
Plate Tectonics.
.. Plate Tectonics Theory that the Earth’s crust is made of rigid plates that float on the molten layer of the mantle. Comes from the Greek word meaning.
 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material.
Bellringer: Looking at the world map, what do you notice about the shape of the continents? -Write a 1 paragraph response about what you notice.
The Earth’s Interior & Plate Tectonics Physical Science Chapter 17 Section 1.
Continental Drift Chapter 10. Wegener’s Hypothesis  Once a single supercontinent  Started breaking up about 200 mya  Continents drifted to current.
Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class 2013
Warm-up #43 Mar. 26  Brainstorming: Will California eventually slide into the ocean? Have continents really drifted apart over the centuries?
Africa The Red Sea between Africa and the Arabian peninsula in Asia marks a region where two pieces of the lithosphere are slowly moving apart. Over the.
List 1 fact about Earth. Agenda for Monday Nov 22 nd 1.Finish Movie 2.Layers of the Earth notes.
INSIDE THE EARTH REVIEW COMPLIMENTS OF MS. SINGLETON.
The Lithosphere Mr. Norris. Day 1 Objective: Objective: – I can explain how the Earth is structured – I can explain how the material of earth is changed.
Chapter 7. What are the 3 Major Zones of the Earth?
Plate Tectonics.
Unit 4 Lesson 6 Plate Tectonics
PLATE TECTONICS.
Section 1: Earth’s Interior and Plate Tectonics
Chapter 7 Review Game Plate tectonics
Cause, Effect and Evidence
“Continental Drift” I. Early Evidence of Continental Movement:
What was Wegener’s hypothesis called?
Chapter 9 Plate Tectonics.
Plate Tectonics Evolution of the Earth.
Unit 8 C: Plate Tectonics
Plate Tectonics Jeopardy
Plate Tectonics.
Unit 6 Lesson 4 Plate Tectonics
DO NOW Pick up notes sheet..
Plate Tectonics 1: Continental Drift -Evidence of continental drift
Chapter 10 Plate Tectonics.
Plate Tectonics Evolution of the Earth.
Looking for Patterns in Data
The Earth’s Crust in Motion…
The Earth’s Crust in Motion…
Earth’s Layers Three main layers Crust, Mantle, and Core
Chapter 9.
Features on Earth’s Surface
Warm-Up: March 18, 2016 Write down everything you know about plate tectonics.
Chapter 10 Plate Tectonics.
Early Finisher Tasks If you finish your work early, you may select one of the two books from the basket. 1.) Earth: The Inside Story 2.) The Shaping of.
Plate Tectonics Structure of the Earth Plate Boundaries
Can you explain this map?
The Earth’s Crust in Motion…
Earth’s Structure and Pangaea
Layers of the Earth Using a laser pointer, briefly highlight and describe the layers of the earth’s interior. Also highlight the fact that the earth has.
Plate Tectonics Test.
Chapter 10 Plate Tectonics.
Earth’s Structure and Pangaea
Theory of Plate Tectonics (Part 1)
The Earth’s Crust in Motion…
Theory of Plate Tectonics (Part 1)
Earth’s Structure and Pangaea
Earth’s Structure and Pangaea
Welcome to (insert name) class.
Earth’s Structure and Pangaea
Plate Tectonics Geo Science.
Plate Tectonics Notes.
Continental Drift and Plate Tectonics
Earth’s Structure and Pangaea
Earth’s Structure and Pangaea
Presentation transcript:

Layers of the Earth Using a laser pointer, briefly highlight and describe the layers of the earth’s interior. Also highlight the fact that the earth has oceanic and continental crust.

CRUST/LITHOSPHERE _________ layer __________ on mantle is cool and ________ between ______ km thick __________ on mantle Oceanic Crust: ________ thick Continental Crust ~ ________ thick

Mantle/Athenosphere average thickness is about _________km solid but ________ behaves like ________, flowing and circulating slowly without breaking

Core radius ~ ________ km half of the Earth’s diameter metallic - made of _____ and ________ outer core - ________ inner core -________

Supercontinent Pangea – _______ Similar _____ and ______ _____ forests _____ deposits Discuss the theory of Pangea and show animation (click on link). Tens of Millions of years ago!

Pangaea ___________ revived the early idea of _____________, contending that all of the present-day continents were connected, side-by-side, as long ago as the Carboniferous (~300 Myr). He called the supercontinental mass ___________, Greek for ‘all lands’.

Today’s Continents As soon as maps of the globe became available, people wondered about the arrangement of the continents and oceans. Hundreds of years later, valid explanations were constructed.

The crust and lithosphere are broken up into 25 ________ USGS

Movement of the Plates: _________________ Evidence How it works

Continental Drift: Fossil Evidence Mesosaurus: _________________ Glossopteris: _______________________________________

Continental Drift: Rock Ages Rock ages showed strong correlation across the ___________, as did mountain ranges of similar age.

Continental Drift: Geometry evidence shape of the continents eg. the shape of the west coast of _________ and the east coast of ______________ are remarkably similar and were perhaps once joined

More Evidence:Mantle Convection Materials that can flow tend to lose _____________ by the convection process. This explains circulation in a pot of water that is being heated from below in the same way it describes the ________________ in the Earth’s mantle.

Where convection rises ________________ takes place. Mantle Convection Giant convection cells within the upper mantle drag the plates along laterally. Where convection rises ________________ takes place. Where the convection cells descend they drag crust down, causing ______________

How does it work? _________ – pieces of the lithosphere Plates fit closely together along cracks called _______________ Convection Currents  ______________ Explain that the lithosphere is broken into pieces called plates. The place where the pieces fit together are the boundaries. Using a laser pointer, explain the theory that plate movement is caused by convection currents in the mantle.

Here is another version of the Rock Cycle http://www.volcanoworld.org/vwdocs/vwlessons/lessons/Metrocks/Metrocks2.html

Mechanisms of Plate Tectonics:

Mechanisms of Plate Tectonics: 2 Ridge-Push 1 Mantle 3 drag convective flow of mantle

Sea Floor Spreading Hot material rose at the ______________, thus explaining the high heat flow and volcanic activity, and why the ocean floor is bulged up at the ridges. The logical next step is that where continent and ocean meet, at the __________, ocean crust is being returned to the mantle at the same rate it is being generated at the ridges.

Types of Boundaries __________ Define each term. Have the students as a class mimic the movement of divergent, convergent, and transform boundaries using their hands. Use the hyperlinks as visuals while discussing each type of plate boundary.

To summarize……

C Sliding B Convergent A Divergent plates are __________ new crust is created ______ is coming to the surface plates are ___________ crust is returning to the __________ plates are __________ each other crust is not ________ or __________

C Sliding B Convergent A Divergent Plates move against each other Stress builds up Stress is released ____________ 2 continental plates  __________________ Continental crust  ___________ Oceanic crust  ___________________ C Sliding B Convergent A Divergent 2 oceanic plates or oceanic + continental _________

DIVERGENCE: Sea Floor Spreading Sea floor spreading, leads to _________________ *This hypothesis makes a number of testable predictions.*

* Taking magnetic stratigraphy back in time is paleomagnetism. * Magnetic Reversals Interestingly, the polarity of the magnetic field shifts every 0.5 - 1.0 Myr. That means rocks formed over time will record either ‘_________’ magnetic orientation (like today), or ‘_________’. This leads to alternating bands of normal and reversed magnetism. We are apparently headed into a polarity reversal, to be complete in ~3000 yr. * Taking magnetic stratigraphy back in time is paleomagnetism. *

Paleomagnetism and Sea Floor Spreading The _____________ as products of steady creation of ____ ocean crust over geologic time.

Oceanic Ridges

The ridge is a ___________ Plate Margin and divergence takes place by __________________. From http://www.uwsp.edu/geo/faculty/ritter/glossary/s_u/sea_flr_spread.html New crust is added from upwelling __________ (molten rock) from the upper ___________. Older crust is pushed laterally away from the ridge axis – so that the sea floor spreads away from the ridge axis.

CONVERGENCE: Oceanic Crust – Continental Crust The __________ oceanic crust descends beneath lighter continental crust. __________________ develop due to compressive forces and volcanics (e.g., the Andes of South America). Magma material rises from descending slab and builds _____________ in the rising mountains.

CONVERGENCE: Oceanic Crust-Oceanic Crust The ________, _________ crust normally descends beneath the younger crust. ______________ develop at the surface of the over-riding crust (forming Island Arcs) - e.g ___________

Continental Crust-Continental Crust CONVERGENCE: Continental Crust-Continental Crust Neither plate __________ (both too light). Compressive forces driving plates fold and thrust the continental margins forming an _______________________ belt (e.g., the Himalayan Mountains).

SLIDING: Slip-Strike Faults Plate __________ along which the plates slip by each other. Termed: Slip-Strike Faults/Transform Faults On either side of a fault plate motions are in __________ directions.

The Big Picture Remind students to look for their assigned boundaries and write down information to describe them.