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Website10-16-07 1.Get a notes packet from the back of the room. 2.Make sure you have colored pencils. 3.Sit down and insert notes packet into your binder.

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Presentation on theme: "Website10-16-07 1.Get a notes packet from the back of the room. 2.Make sure you have colored pencils. 3.Sit down and insert notes packet into your binder."— Presentation transcript:

1 Website10-16-07 1.Get a notes packet from the back of the room. 2.Make sure you have colored pencils. 3.Sit down and insert notes packet into your binder behind your convection current diagram

2 Website Heat flows outward from Earth's interior. The crust insulates us from Earth's interior heat. The mantle is semi-molten, the outer core is liquid and the inner core is solid.

3 Website

4 New crust forms along mid-ocean spreading centers and continental rift zones. When plates meet, one can slide beneath another. Plumes of magma rise from the edges of sinking plates.

5 Website Thinned or fractured crust allows magma to rise to the surface as lava. Most magma doesn't reach the surface but heats large regions of underground rock.

6 Website When the rising hot water and steam is trapped in permeable and porous rocks under a layer of impermeable rock, it can form a geothermal reservoir.

7 Website When hot water and steam reach the surface, they can form fumaroles, hot springs, mud pots and other interesting phenomena.

8 Website Many areas have accessible geothermal resources, especially countries along the circum-Pacific "Ring of Fire," spreading centers, continental rift zones and other hot spots.

9 Website General Animations 1. Sea Floor Spreading Sea Floor Spreading Sea Floor Spreading 2. Plate Tectonics 3. Savage Earth Plate Boundaries Savage Earth Plate Boundaries Savage Earth Plate Boundaries 4. Plate Boundary Map Plate Boundary Map Plate Boundary Map 5. http://www.wwnorton.com/colle ge/geo/egeo/flash/2_1.swf http://www.wwnorton.com/colle ge/geo/egeo/flash/2_1.swf http://www.wwnorton.com/colle ge/geo/egeo/flash/2_1.swf

10 Website Earth's Crust: There are two different types of crust: thin oceanic crust that underlies the ocean basins and thicker continental crust that underlies the continents. Earth's Crust: There are two different types of crust: thin oceanic crust that underlies the ocean basins and thicker continental crust that underlies the continents. Earth's Crust: Earth's Crust:

11 Website Divergent Boundary -- Oceanic Divergent Boundary -- Oceanic Divergent Boundary -- Oceanic Divergent Boundary -- Oceanic Example Example Mid Atlantic Ridge Mid Atlantic Ridge Mid Atlantic Ridge Mid Atlantic Ridge Effects Effects The Ridge is a high area compared to the surrounding seafloor because of the lift from the convection current below. The Ridge is a high area compared to the surrounding seafloor because of the lift from the convection current below. Sea Floor Spreading Sea Floor Spreading Sea Floor Spreading Sea Floor Spreading

12 Website Divergent Plate Boundary – Continental Divergent Plate Boundary – Continental Divergent Plate Boundary – Continental Divergent Plate Boundary – Continental Example Example The East Africa Rift Valley The East Africa Rift Valley The East Africa Rift Valley The East Africa Rift Valley Animation 1 Animation 2 Animation 1 Animation 2 Animation 2 Animation 2 Effect Effect Rift valley sometimes occupied by a long linear lakes or a shallow arm of the ocean. Rift valley sometimes occupied by a long linear lakes or a shallow arm of the ocean.

13 Website Convergent Plate Boundary - Oceanic and Continental Plates Convergent Plate Boundary - Oceanic and Continental Plates Convergent Plate Boundary - Oceanic and Continental Plates Convergent Plate Boundary - Oceanic and Continental Plates Example Example Washington, Oregon Coast Washington, Oregon Coast Effects Effects The overriding continental plate is lifted up and a mountain range is created The overriding continental plate is lifted up and a mountain range is created

14 Website Convergent Plate Boundary – Oceanic- Oceanic Convergent Plate Boundary – Oceanic- Oceanic Convergent Plate Boundary – Oceanic- Oceanic Convergent Plate Boundary – Oceanic- Oceanic Example Example Aleutian islands and the Eastern Caribbean islands of Martinique are examples of islands formed through this type of plate boundary. Aleutian islands and the Eastern Caribbean islands of Martinique are examples of islands formed through this type of plate boundary. Effect Effect Effects that are found at this type of plate boundary include: an oceanic trench, a chain of volcanic islands, and the destruction of oceanic lithosphere Effects that are found at this type of plate boundary include: an oceanic trench, a chain of volcanic islands, and the destruction of oceanic lithosphere

15 Website Convergent Plate Boundary - Continental Convergent Plate Boundary - Continental Convergent Plate Boundary - Continental Convergent Plate Boundary - Continental Example Example The Himalaya Mountain Range The Himalaya Mountain Range The Himalaya Mountain Range The Himalaya Mountain Range Animation Animation Animation Effects Effects Effects found at a convergent boundary between continental plates include: intense folding and faulting, a broad folded mountain range, shallow earthquake activity. Effects found at a convergent boundary between continental plates include: intense folding and faulting, a broad folded mountain range, shallow earthquake activity.

16 Website Transform Plate Boundaries Transform Plate Boundaries Transform Plate Boundaries Transform Plate Boundaries Example Example San Andreas Fault Zone, Alpine Fault of New Zealand San Andreas Fault Zone, Alpine Fault of New Zealand San Andreas Fault Zone, Alpine Fault of New Zealand San Andreas Fault Zone, Alpine Fault of New Zealand Effects Effects Recurring earthquake activity and faulting. Recurring earthquake activity and faulting.

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