Slide 1 - Duplin County Schools
... http://en.wikipedia.org/wiki/List_of_tectonic_plates http://www.enchantedlearning.com/subjects/astronomy/planets/earth/Continents.shtml http://geography.howstuffworks.com/south-america/the-andes.htm http://www.dailygalaxy.com/my_weblog/2012/03/james-cameron-avatar-directorexplores-mariana-trench-dee ...
... http://en.wikipedia.org/wiki/List_of_tectonic_plates http://www.enchantedlearning.com/subjects/astronomy/planets/earth/Continents.shtml http://geography.howstuffworks.com/south-america/the-andes.htm http://www.dailygalaxy.com/my_weblog/2012/03/james-cameron-avatar-directorexplores-mariana-trench-dee ...
Metamorphic and Igneous
... Why do you think some rocks are heavier than others? Some are denser – less air space between particles ...
... Why do you think some rocks are heavier than others? Some are denser – less air space between particles ...
Plate tectonics and lithosphere architecture: temporal and spatial
... architecture that results from such processes can be greatly disturbed by thermo-tectonic processes. While the Archaean crust of the Kaapvaal and Siberian cratons (> 2500 Ma) is associated with deep (c. 200 km) high velocity anomalies and low heat flow, consistent with the presence of a thick, cold, ...
... architecture that results from such processes can be greatly disturbed by thermo-tectonic processes. While the Archaean crust of the Kaapvaal and Siberian cratons (> 2500 Ma) is associated with deep (c. 200 km) high velocity anomalies and low heat flow, consistent with the presence of a thick, cold, ...
Layers of the Earth - University of Dayton
... At this point in time an ice age ended The glaciers melted and oceans rose causing water to cover what was previously land ...
... At this point in time an ice age ended The glaciers melted and oceans rose causing water to cover what was previously land ...
PPT
... which were previously seemingly unrelated. • Several lines of evidence indicate that the continents as they now exist have moved large distances over the last few hundred million years, both relative to each other and relative to the north and south poles of Earth’s rotation axis. • According to Pla ...
... which were previously seemingly unrelated. • Several lines of evidence indicate that the continents as they now exist have moved large distances over the last few hundred million years, both relative to each other and relative to the north and south poles of Earth’s rotation axis. • According to Pla ...
Class2atxt
... • Seismic waves of energy – P-waves or primary waves (Slinky) – S-waves or secondary waves (up and down) ...
... • Seismic waves of energy – P-waves or primary waves (Slinky) – S-waves or secondary waves (up and down) ...
Test Review Quiz B
... and choked the air with ash clouds. The structure of the volcano was steeply sloping. What type of volcano was this? a. Dome b. Shield c. Composite d. Cinder cone 15. A rift valley is evidence of which kind of plate boundary? a. Uniform c. Divergent b. Convergent d. Transform 16. Which of the follow ...
... and choked the air with ash clouds. The structure of the volcano was steeply sloping. What type of volcano was this? a. Dome b. Shield c. Composite d. Cinder cone 15. A rift valley is evidence of which kind of plate boundary? a. Uniform c. Divergent b. Convergent d. Transform 16. Which of the follow ...
File - Pi Beta Philes!
... forces between the negative and positive nucleons. B. Atoms of two different elements share electrons and protons; the resulting compound is bonded together by the strong, binding energy of shared protons. C. Nuclei of two different atoms share electrons, and the resulting compound is tightly bonded ...
... forces between the negative and positive nucleons. B. Atoms of two different elements share electrons and protons; the resulting compound is bonded together by the strong, binding energy of shared protons. C. Nuclei of two different atoms share electrons, and the resulting compound is tightly bonded ...
Guidelines
... A) Description of the process/problem. This might involve competing models or tectonic histories. If appropriate, use a figure to explain it. B) Your orogen(s) with why this is a good place to study this process/problem. Include a map of the region with some simplified tectonics and geology. C) A pr ...
... A) Description of the process/problem. This might involve competing models or tectonic histories. If appropriate, use a figure to explain it. B) Your orogen(s) with why this is a good place to study this process/problem. Include a map of the region with some simplified tectonics and geology. C) A pr ...
SEA FLOOR SPREADING Mid
... dense, is forced up towards the ocean floor cooling off when it touches water. •When the magma hardens, a small amount of new ocean floor is added to the Earth’s crust. As more magma rises and cools it pushes the new sea floor away from the ridge. This process is called sea floor spreading. ...
... dense, is forced up towards the ocean floor cooling off when it touches water. •When the magma hardens, a small amount of new ocean floor is added to the Earth’s crust. As more magma rises and cools it pushes the new sea floor away from the ridge. This process is called sea floor spreading. ...
Orogenies as records of plate collisions
... colored mdm-grey-brown (labeled continental crust) will be metamorphosed from the regional heat and pressure generated from the collision. Thrust faults flank the metamorphic belt. The diagram does not show the presence of volcanic rocks within the mtn ...
... colored mdm-grey-brown (labeled continental crust) will be metamorphosed from the regional heat and pressure generated from the collision. Thrust faults flank the metamorphic belt. The diagram does not show the presence of volcanic rocks within the mtn ...
Unit 5: Ocean Floor Structure and Plate Tectonics
... The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, plastic mantle which is located below the crust. These plates usually move along smoothly but sometimes they stick and build up pressure. The pressure builds and the rock bends until it snaps. When this ...
... The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, plastic mantle which is located below the crust. These plates usually move along smoothly but sometimes they stick and build up pressure. The pressure builds and the rock bends until it snaps. When this ...
Deforming the Earth`s Crust: Faulting
... Geologic Activity, http://www.nps.gov/pore/naturescience/geologicactivity.htm ...
... Geologic Activity, http://www.nps.gov/pore/naturescience/geologicactivity.htm ...
Deforming the Earth`s Crust: Faulting
... Geologic Activity, http://www.nps.gov/pore/naturescience/geologicactivity.htm ...
... Geologic Activity, http://www.nps.gov/pore/naturescience/geologicactivity.htm ...
Why I choose… (extra credit)
... this unit. Waves are an important part because they cause most of the damage during earthquakes. They also let scientists decode the different layers of our Dynamic Planet. Z-Zone of Subduction Subduction is an important way that our planet gets refreshed and how the plates could move. It can cause ...
... this unit. Waves are an important part because they cause most of the damage during earthquakes. They also let scientists decode the different layers of our Dynamic Planet. Z-Zone of Subduction Subduction is an important way that our planet gets refreshed and how the plates could move. It can cause ...
The Effects of Plate Boundaries
... Both are heavy and neither can be pushed down into the Earth. Can either smush together, or one can go on top of the other, resulting in very tall mountains. Eventually, they come to a stop. Himalayan Mtns. ...
... Both are heavy and neither can be pushed down into the Earth. Can either smush together, or one can go on top of the other, resulting in very tall mountains. Eventually, they come to a stop. Himalayan Mtns. ...
Plate Tectonics
... • The edges of the plates are called boundaries. • There are three types of motion seen at the plate boundaries. ...
... • The edges of the plates are called boundaries. • There are three types of motion seen at the plate boundaries. ...
Igneous Rocks
... In metamorphic rocks, the structure, texture or composition of the rock has changed. ...
... In metamorphic rocks, the structure, texture or composition of the rock has changed. ...
Observing Convection Currents
... address at a major scientific conference on subduction processes in June 1994 that "subduction plays a more fundamental role than seafloor spreading in shaping the earth's surface features" and "running the plate tectonic machinery." The gravity-controlled sinking of a cold, denser oceanic slab into ...
... address at a major scientific conference on subduction processes in June 1994 that "subduction plays a more fundamental role than seafloor spreading in shaping the earth's surface features" and "running the plate tectonic machinery." The gravity-controlled sinking of a cold, denser oceanic slab into ...
File
... Oceanic-continental convergence Ocean plate subducted Continental arc Oceanic trench Deep earthquakes ...
... Oceanic-continental convergence Ocean plate subducted Continental arc Oceanic trench Deep earthquakes ...
6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
... The Great Rift Valley started forming millions of years ago. It slowly continues to deepen and widen, causing many volcanic eruptions and earthquakes in the area. ...
... The Great Rift Valley started forming millions of years ago. It slowly continues to deepen and widen, causing many volcanic eruptions and earthquakes in the area. ...
Rev. 2013 Fast and Slow Changes to Earth`s Surface Volcano – Fast
... Destructive – when they erupt and cover cities, homes, crop land, forest, and all living things that surround them. The lava and ashes cause lose of homes, property, human and animal lives, crops and other food sources. The ash can cover the sky and travel hundreds of miles and cover the sun’s rays ...
... Destructive – when they erupt and cover cities, homes, crop land, forest, and all living things that surround them. The lava and ashes cause lose of homes, property, human and animal lives, crops and other food sources. The ash can cover the sky and travel hundreds of miles and cover the sun’s rays ...
What are the layers of the Earth? What are the characteristics of
... • Approximately 67% of Earth’s mass is found in this layer. • The top boundary, the MOHO, is made up of solid rock. In the center of the mantle, the rock is viscous..it flows like syrup. ...
... • Approximately 67% of Earth’s mass is found in this layer. • The top boundary, the MOHO, is made up of solid rock. In the center of the mantle, the rock is viscous..it flows like syrup. ...
Rock Cycle Who Wants to be a Millionaire PowerPoint
... Deposition is the process of laying down sediments where? ...
... Deposition is the process of laying down sediments where? ...
Large igneous province
A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.