Download presentation
Presentation is loading. Please wait.
Published byDeborah Cameron Modified over 9 years ago
1
Earth’s Interior and Plate Tectonics Integrated Science Ch 12
2
This is how the continents formed…. http://www.youtube.com/watch?v=TzzGPf Vx32M&list=PLABDC7B24FAFE33FDhttp://www.youtube.com/watch?v=TzzGPf Vx32M&list=PLABDC7B24FAFE33FD
3
The Earth is like a parfait, it has layers If you cut the earth in half, it would look very much like a parfait, with different layers and compositions based on density The earth has three main layers, the crust, the mantle, and the core
4
The Crust We live on this layer Its is cool, and made of solid rock Oceanic crust is thinner and denser than continental crust. The crust is the least dense portion of the earth and only about 12-25 miles thick
5
The Mantle Layer of rock that is denser than the crust About 1800 miles thick Outer mantle is solid rock Inner mantle the rocks are extremely hot and bendable like gum (plastic)
6
The Core The center of the earth Made mostly of iron and nickel The inner core is solid metal while the outer core is liquid metal
7
The Earth heats up with depth At only 2 miles down the temperature increase to 120 F The core is much hotter than the mantle In the core, temperatures reach over 10,000 F
8
The earth heats up with depth The earth gets warmer towards the core because it contains so many radioactive isotopes These unstable isotopes are constantly breaking down, releasing huge amounts of energy, which in turn heat the earth
9
How do plates move? http://www.youtube.com/watch?v=ryrXAGY1dmE
10
Evidence #1: The Pangea Puzzle In the 20 th century, Alfred Wegener noticed that eastern S.America fits into western Africa He also noticed that several of the other continents fit together like puzzle pieces He also found that fossil evidence showed that several of the same organisms are found on continents now separated by oceans He theorized that 250 million years ago all the continents combined to form the giant land mass he named pangea
11
How did this happen? The earth’s outer shell, called the lithosphere is made of the crust and upper portion of the mantle. This lithosphere is very rigid and consists of 7 large pieces and a few small ones that fit together like a puzzle These large pieces are called tectonic plates
12
Plate Tectonics These plates fit together like puzzle pieces and move in relation to each other these plates move away, towards, or alongside each other Tectonic plates move about 6 inches per year
13
Divergent Plate Boundaries In some areas, the plates move away from each other When this occurs, hot liquid rock called magma rises and cools, forming new lithospheric rock
14
Convergent Plate Boundaries Less dense continental plate floats over more dense oceanic plate This process is called subduction As this more dense rock goes down into the mantle, it heats up and melts The magma rises and pushes up the crust, forming volcanic mountains also earthquakes
15
Subduction - two plates meet, the more dense plate (oceanic crust), dives beneath the less dense plate (continental crust)
16
Continental vs. Continetal Same density so no subduction Builds non- volcanic mts. Earthquakes
17
Oceanic vs. Oceanic Similar density, but subduction anyway Earthquakes, trenches, volcanic island arcs
18
Transform Fault Boundaries These are areas where plates move along side one another As plates move, they can cause cracks in the lithosphere called faults As plates move along side each other at these faults, the plates cause a great deal of force and create earthquakes
19
RECAP RECAP Divergent Plate Boundaries –Divergent means plates MOVE AWAY from each other Convergent Plate Boundaries –Convergent means plates MOVE TOWARD each other Transform Fault Boundaries –areas where plates move along side one another like this or this
20
Earth is made of 3 main layers –Crust- cool, thin, made of rock, 10-25 miles thick –Mantle, denser than crust, 2500 miles thick, 80% of earth’s volume: inner mantle solid rock, outer mantle bendable gummy rock –Core- center of earth, made of iron and nickel, made of 2 layers: inner solid metal, outer liquid metal
21
Pangea- 250 million years ago all the continents combined to form the giant land mass called Pangea Lithosphere (earth’s outer shell) is made of the crust and upper portion of the mantle. lithosphere -very rigid and consists of 7 large pieces (called tectonic plates) and a few small ones that fit together like a puzzle
22
Plate Tectonics These plates fit together like puzzle pieces and move in relation to each other these plates move away, towards, or alongside each other Tectonic plates move 6 inches per year
23
Evidence 2: Biogeographical
24
Final views http://www.youtube.com/watch?v=QrQDX nnXOo4&feature=player_embedded#!http://www.youtube.com/watch?v=QrQDX nnXOo4&feature=player_embedded#!
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.