chapter 11 -- plate tectonics
... • The theory states that hot, less dense material in the mantle is forced upward to the surface at the ______-________ ridges. • As magma is forced upward at mid-ocean ridges, it flows in ________ directions away from the ridge. • As it moves away from the ridge, the magma cools, solidifies, gets __ ...
... • The theory states that hot, less dense material in the mantle is forced upward to the surface at the ______-________ ridges. • As magma is forced upward at mid-ocean ridges, it flows in ________ directions away from the ridge. • As it moves away from the ridge, the magma cools, solidifies, gets __ ...
Name_____________ Plate tectonics review 1 State the latitude
... Base your answers to questions 17 through 21 on the map and the modified Mercalli intensity scale below. The map shows modified Mercalli intensity scale damage zones resulting from a large earthquake that occurred in 1964. The earthquake’s epicenter was near Anchorage, Alaska. The cities Kodiak and ...
... Base your answers to questions 17 through 21 on the map and the modified Mercalli intensity scale below. The map shows modified Mercalli intensity scale damage zones resulting from a large earthquake that occurred in 1964. The earthquake’s epicenter was near Anchorage, Alaska. The cities Kodiak and ...
Atmospheric - Penicuik High School
... The ocean currents are also pushed along by the wind cells (Hadley, Ferrell etc). The coriolis effect (the spin of the earth) deflects ocean currents and winds so they rotate clockwise in the northern hemisphere and anticlockwise in the southern hemisphere. Only in the Pacific and Atlantic do Ocean ...
... The ocean currents are also pushed along by the wind cells (Hadley, Ferrell etc). The coriolis effect (the spin of the earth) deflects ocean currents and winds so they rotate clockwise in the northern hemisphere and anticlockwise in the southern hemisphere. Only in the Pacific and Atlantic do Ocean ...
Carbon cycle dice game
... relative to the rocks around it. It hits the base of the overlying continental crust and pools there, transferring heat to the overlying felsic rock material. This heat transfer causes crystallization of the basalt and partial melting of the overlying crust, producing an intermediate-composition mag ...
... relative to the rocks around it. It hits the base of the overlying continental crust and pools there, transferring heat to the overlying felsic rock material. This heat transfer causes crystallization of the basalt and partial melting of the overlying crust, producing an intermediate-composition mag ...
Types of Plate Boundaries
... boundary between two plates: the Nubian plate to the west and the Somalian plate to the east. The rift valley is a classic example of a divergent plate boundary. Rift Valley-view video ...
... boundary between two plates: the Nubian plate to the west and the Somalian plate to the east. The rift valley is a classic example of a divergent plate boundary. Rift Valley-view video ...
Inside Edition
... The interaction of the crust and mantle gives rise to tectonic activity and crustal movement The crust and mantle are broken down into three different zones Lithosphere – cool, rigid upper layer of earth Asthenosphere – softer layer of the earth under the lithosphere Mesosphere – very slowly flowing ...
... The interaction of the crust and mantle gives rise to tectonic activity and crustal movement The crust and mantle are broken down into three different zones Lithosphere – cool, rigid upper layer of earth Asthenosphere – softer layer of the earth under the lithosphere Mesosphere – very slowly flowing ...
Table 1. Plate Boundaries of an Unkn
... To complete this worksheet, see the instructions in the textbook (Chapter 3 Investigation). Table 1. Plate Boundaries of an Unknown Ocean and Continents This perspective view shows two continents, labeled A and B, separated by an ocean. • Use the topography to identify possible plate boundaries and ...
... To complete this worksheet, see the instructions in the textbook (Chapter 3 Investigation). Table 1. Plate Boundaries of an Unknown Ocean and Continents This perspective view shows two continents, labeled A and B, separated by an ocean. • Use the topography to identify possible plate boundaries and ...
designed by the 2007 NASA Ames Academy for Space Exploration
... answers to key questions about mass extinction events, genomic dispersal and evolution, and pathogen dispersal in the atmosphere. Also, microbial resistance to radiation, pressure, and temperature extremes can be studied with organisms that can exist in the atmosphere. ...
... answers to key questions about mass extinction events, genomic dispersal and evolution, and pathogen dispersal in the atmosphere. Also, microbial resistance to radiation, pressure, and temperature extremes can be studied with organisms that can exist in the atmosphere. ...
Unit 1 Test Review
... Which is the largest, thickest layer of the Earth? a. Crust b. Inner Core c. Outer Core ...
... Which is the largest, thickest layer of the Earth? a. Crust b. Inner Core c. Outer Core ...
Plate Tectonics - Asheboro High School
... come together at convergent boundariescreates a subduction zone plate descends into the mantle and melts into magmacomes back up through the boundaryforms volcanoes when it reaches the surface. ...
... come together at convergent boundariescreates a subduction zone plate descends into the mantle and melts into magmacomes back up through the boundaryforms volcanoes when it reaches the surface. ...
Lecture 1
... (UTC) = time scale all weather observations are reported in…represents local time on Prime Meridian – Ranges from 0-24 hrs – Eastern Time Zone is 5 hrs behind UTC, 4 hours behind during Daylight Savings Time E.g. 12Z = 7:00am EST or 8:00 am EDT ...
... (UTC) = time scale all weather observations are reported in…represents local time on Prime Meridian – Ranges from 0-24 hrs – Eastern Time Zone is 5 hrs behind UTC, 4 hours behind during Daylight Savings Time E.g. 12Z = 7:00am EST or 8:00 am EDT ...
1 - kleung
... 18. Many scientists believe that the movement of lithospheric plates is caused by ____________________________. 19. One example of a continental-continental plate convergence is the ____________________________ mountains. 20. If there is a crack, or break, in rock but the rocks are not moving, the b ...
... 18. Many scientists believe that the movement of lithospheric plates is caused by ____________________________. 19. One example of a continental-continental plate convergence is the ____________________________ mountains. 20. If there is a crack, or break, in rock but the rocks are not moving, the b ...
Study Guide: Plate Tectonics
... 36. The main points of evidence for _____ are fossils, rocks, and climate. ...
... 36. The main points of evidence for _____ are fossils, rocks, and climate. ...
Picture
... 2. Explain how soil forms. 3. Identify the factors that affect soil development, including living things. Explain how these factors affect the development of soil. 4. Define humus. Identify where it is found. 5. Explain the difference between a soil horizon and soil profile. 6. Describe the physical ...
... 2. Explain how soil forms. 3. Identify the factors that affect soil development, including living things. Explain how these factors affect the development of soil. 4. Define humus. Identify where it is found. 5. Explain the difference between a soil horizon and soil profile. 6. Describe the physical ...
Teaching Geoscience with Data, Models, and Visualizations
... Where do the volcanoes go as the plate moves away from the ridge? ...
... Where do the volcanoes go as the plate moves away from the ridge? ...
Slide 1
... Evidence: hot spots As plates move, the volcanoes are carried away from the hot spot Only volcanoes near the hot spot are are active Can determine direction and speed of the plate motion ...
... Evidence: hot spots As plates move, the volcanoes are carried away from the hot spot Only volcanoes near the hot spot are are active Can determine direction and speed of the plate motion ...
Evolution of the Earth`s atmosphere - Beck-Shop
... atoms are oxidized in respiration or in the decay of organic matter, which is the reverse of Reaction (1.1). However, for every few tens of thousands of molecular carbons formed by photosynthesis, one escapes oxidation by being buried or “fossilized.” Most of the Earth’s unoxidized carbon is contain ...
... atoms are oxidized in respiration or in the decay of organic matter, which is the reverse of Reaction (1.1). However, for every few tens of thousands of molecular carbons formed by photosynthesis, one escapes oxidation by being buried or “fossilized.” Most of the Earth’s unoxidized carbon is contain ...
Tectonic–climatic interaction
Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.