Test - Scioly.org
... Dynamic Planet – Test Written by: Araneesh Pratap (Chattahoochee High School) ...
... Dynamic Planet – Test Written by: Araneesh Pratap (Chattahoochee High School) ...
Test - Scioly.org
... Dynamic Planet – Test Written by: Araneesh Pratap (Chattahoochee High School) ...
... Dynamic Planet – Test Written by: Araneesh Pratap (Chattahoochee High School) ...
Untitled - Studentportalen
... The layered structure, core mantle and crust, was formed due to internal melting in the very early history. A cool rocky planet was heated. Heat was produced by impact energy, decaying radioactive elements (at least 7 times more abundant than today) and gravitational energy converted to heat. Melti ...
... The layered structure, core mantle and crust, was formed due to internal melting in the very early history. A cool rocky planet was heated. Heat was produced by impact energy, decaying radioactive elements (at least 7 times more abundant than today) and gravitational energy converted to heat. Melti ...
Slideshow
... (molten rock) gets closer to the crust it begins to lose heat and sink back down towards the core. This creates convections currents which cause the plates to move. ...
... (molten rock) gets closer to the crust it begins to lose heat and sink back down towards the core. This creates convections currents which cause the plates to move. ...
How Earth*s Plates Move
... hundreds of feet over millions of years as the plates separated. This formed the Great Rift Valley. ...
... hundreds of feet over millions of years as the plates separated. This formed the Great Rift Valley. ...
Tectonic Plate Movement - Ms. Gravette and the Mad Scientists
... Ridge Push • New rock formed at the oceanic ridges rests on top of the old rock due to its density ...
... Ridge Push • New rock formed at the oceanic ridges rests on top of the old rock due to its density ...
plate tectonics
... • The theory of plate tectonics states that Earth’s lithosphere is broken into many pieces—tectonic plates—that move slowly over the asthenosphere. Scientists can detect this motion only by using special equipment, such as global positioning systems (GPS). Tectonic plates can collide, separate or sl ...
... • The theory of plate tectonics states that Earth’s lithosphere is broken into many pieces—tectonic plates—that move slowly over the asthenosphere. Scientists can detect this motion only by using special equipment, such as global positioning systems (GPS). Tectonic plates can collide, separate or sl ...
Tectonic Lithospheric Plate Boundaries
... You have learned that lithospheric plates move due to convection, slab pulling and ridge pushing –basically gravity and heat. You have also categorized many different mountains according to their shape. Let’s find out how these shapes came to be. Interact with pages 100 and 101. Use the outline prov ...
... You have learned that lithospheric plates move due to convection, slab pulling and ridge pushing –basically gravity and heat. You have also categorized many different mountains according to their shape. Let’s find out how these shapes came to be. Interact with pages 100 and 101. Use the outline prov ...
FREE Sample Here
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
FREE Sample Here
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
6. Along which type(s) of lithospheric plate
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
... c. Anthropologists have found human carvings in Africa that match those in Brazil. d. Glaciers near the mouth of the Amazon River in Brazil carried distinctive rocks into South Africa, demonstrating that those countries were once connected. e. Ages of bedrock formations match across the Atlantic Oce ...
Plate Tectonic
... The crust that is more dense dives (“sinks”) under the other one and returns to the mantle (this is called subduction). ...
... The crust that is more dense dives (“sinks”) under the other one and returns to the mantle (this is called subduction). ...
Sea floor spreading and the effects it has on the world In partnership
... but the Mid-Atlantic ridge? The Mid- Atlantic ridge runs along the entire Atlantic ocean and is very visible in maps of seafloor bathymetry. This mountainous ridge is also a major divergent plate and one of the main sources for the world’s new oceanic crust. This ridge isn’t the only ridge in the wo ...
... but the Mid-Atlantic ridge? The Mid- Atlantic ridge runs along the entire Atlantic ocean and is very visible in maps of seafloor bathymetry. This mountainous ridge is also a major divergent plate and one of the main sources for the world’s new oceanic crust. This ridge isn’t the only ridge in the wo ...
1 - Lyndhurst School District
... What determines which plate will be on top? ____________________________________ The plate that is more dense will (sink/rise). What is more dense, oceanic or continental crust? ____________________________________ Which one will sink? ____________________________________ What happens to the mantle ...
... What determines which plate will be on top? ____________________________________ The plate that is more dense will (sink/rise). What is more dense, oceanic or continental crust? ____________________________________ Which one will sink? ____________________________________ What happens to the mantle ...
Topo. Tubs
... an ocean ridge is a “mountain range” deep under the ocean’s surface, and a trench is a deep gorge in the ocean floor and includes the deepest spots on Earth. Maps of the ocean floor are created by instruments on or towed behind ships. A major advance in ocean-floor mapping is called sonar. This tech ...
... an ocean ridge is a “mountain range” deep under the ocean’s surface, and a trench is a deep gorge in the ocean floor and includes the deepest spots on Earth. Maps of the ocean floor are created by instruments on or towed behind ships. A major advance in ocean-floor mapping is called sonar. This tech ...
air mass large body of air that has the same characteristics of
... sediment; especially silt and sand, deposited at the mouth of a river. ...
... sediment; especially silt and sand, deposited at the mouth of a river. ...
Document
... – Flat, featureless, sediment-covered ocean floor • Trenches – Arc-shaped depression in the deep seafloor – a converging oceanic plate is subducted ...
... – Flat, featureless, sediment-covered ocean floor • Trenches – Arc-shaped depression in the deep seafloor – a converging oceanic plate is subducted ...
Earth`s Layers FOLDABLE© Question Sheet
... Reproduction for educational purposes is encouraged. ...
... Reproduction for educational purposes is encouraged. ...
Earth`s Internal Structure Earth`s Layered Structure In the preceding
... Earth’s Internal Structure Earth’s Layered Structure In the preceding section, you learned that the segregation of material that began early inEarth’s history resulted in the formation of three layers defined by their chemical composition—the crust, mantle, and core. In addition to these composition ...
... Earth’s Internal Structure Earth’s Layered Structure In the preceding section, you learned that the segregation of material that began early inEarth’s history resulted in the formation of three layers defined by their chemical composition—the crust, mantle, and core. In addition to these composition ...
ES Ch 3 Quiz Review `13
... C. Ocean-Floor Spreading (pages 60-63 of Section 3-2 of text, “Chapter 3 Notes continued…pp. 60-63”, “Earth’s Magnetism” Lab to be returned, “Finding Ages of Rocks” to be done) • Know the meaning of the theory of sea floor spreading and how it relates to features of the oceans and to continental dri ...
... C. Ocean-Floor Spreading (pages 60-63 of Section 3-2 of text, “Chapter 3 Notes continued…pp. 60-63”, “Earth’s Magnetism” Lab to be returned, “Finding Ages of Rocks” to be done) • Know the meaning of the theory of sea floor spreading and how it relates to features of the oceans and to continental dri ...
The Theory of Plate Tectonics
... Plate Tectonics • The Earth’s lithosphere is divided into plates that move on top of the asthenosphere. Lithosphere ...
... Plate Tectonics • The Earth’s lithosphere is divided into plates that move on top of the asthenosphere. Lithosphere ...
Tectonics and Stratigraphy
... Divergent Boundaries • Continental to continental: Rift valleys are produced by tensional tectonic forces which occur at divergent plate boundaries. Rift valleys typically appear as a downdropped Graben between a pair of faults, or vertical Earth movements. Rift valleys are often associated with an ...
... Divergent Boundaries • Continental to continental: Rift valleys are produced by tensional tectonic forces which occur at divergent plate boundaries. Rift valleys typically appear as a downdropped Graben between a pair of faults, or vertical Earth movements. Rift valleys are often associated with an ...
plates - edl.io
... Ocean / Ocean Convergence Oceanic crust collides with another oceanic crust and one plate subducts. – This has been known to produce a chain of islands from the resulting molten rock rising to the surface to create volcanic ...
... Ocean / Ocean Convergence Oceanic crust collides with another oceanic crust and one plate subducts. – This has been known to produce a chain of islands from the resulting molten rock rising to the surface to create volcanic ...
ES Practice quiz part 2 sect 3
... D. The following diagram shows how island arcs form. Label the type(s) of crust (include the word “crust” in each answer), and trench. Then, answer the questions that follow. Magma ...
... D. The following diagram shows how island arcs form. Label the type(s) of crust (include the word “crust” in each answer), and trench. Then, answer the questions that follow. Magma ...
Part 2…Plate Tectonics
... Developing the Theory 1. How much of the earth’s surface is beneath the water? 2. What was the ocean bottom thought to be like in early times/ 3. What technologic advances greatly improved our ability to envision the ocean bottom? 4. What is the mid ocean ridge system? What are its dimensions? 5. Wh ...
... Developing the Theory 1. How much of the earth’s surface is beneath the water? 2. What was the ocean bottom thought to be like in early times/ 3. What technologic advances greatly improved our ability to envision the ocean bottom? 4. What is the mid ocean ridge system? What are its dimensions? 5. Wh ...
Abyssal plain
An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3000 and 6000 m. Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains cover more than 50% of the Earth’s surface. They are among the flattest, smoothest and least explored regions on Earth. Abyssal plains are key geologic elements of oceanic basins (the other elements being an elevated mid-ocean ridge and flanking abyssal hills). In addition to these elements, active oceanic basins (those that are associated with a moving plate tectonic boundary) also typically include an oceanic trench and a subduction zone.Abyssal plains were not recognized as distinct physiographic features of the sea floor until the late 1940s and, until very recently, none had been studied on a systematic basis. They are poorly preserved in the sedimentary record, because they tend to be consumed by the subduction process. The creation of the abyssal plain is the end result of spreading of the seafloor (plate tectonics) and melting of the lower oceanic crust. Magma rises from above the asthenosphere (a layer of the upper mantle) and as this basaltic material reaches the surface at mid-ocean ridges it forms new oceanic crust. This is constantly pulled sideways by spreading of the seafloor. Abyssal plains result from the blanketing of an originally uneven surface of oceanic crust by fine-grained sediments, mainly clay and silt. Much of this sediment is deposited by turbidity currents that have been channelled from the continental margins along submarine canyons down into deeper water. The remainder of the sediment is composed chiefly of pelagic sediments. Metallic nodules are common in some areas of the plains, with varying concentrations of metals, including manganese, iron, nickel, cobalt, and copper. These nodules may provide a significant resource for future mining ventures.Owing in part to their vast size, abyssal plains are currently believed to be a major reservoir of biodiversity. The abyss also exerts significant influence upon ocean carbon cycling, dissolution of calcium carbonate, and atmospheric CO2 concentrations over timescales of 100–1000 years. The structure and function of abyssal ecosystems are strongly influenced by the rate of flux of food to the seafloor and the composition of the material that settles. Factors such as climate change, fishing practices, and ocean fertilization are expected to have a substantial effect on patterns of primary production in the euphotic zone. This will undoubtedly impact the flux of organic material to the abyss in a similar manner and thus have a profound effect on the structure, function and diversity of abyssal ecosystems.