Concept Review
... _____ 13. What happens when continental and oceanic lithosphere collide? a. Volcanic island arcs are formed. b. Oceanic lithosphere subducts beneath continental lithosphere. c. Large blocks of rock are broken loose. d. Continental lithosphere subducts beneath oceanic lithosphere. _____ 14. What happ ...
... _____ 13. What happens when continental and oceanic lithosphere collide? a. Volcanic island arcs are formed. b. Oceanic lithosphere subducts beneath continental lithosphere. c. Large blocks of rock are broken loose. d. Continental lithosphere subducts beneath oceanic lithosphere. _____ 14. What happ ...
Earth Science Quiz-1 –Main Campus Quiz
... 15. Which of the following statements regarding the scientific method is false? a. A tentative explanation of a body of data is called a hypothesis b. A theory is less likely to be correct than hypotheses. c. A hypothesis is strengthened if it successfully predicts the outcomes of new experiments. d ...
... 15. Which of the following statements regarding the scientific method is false? a. A tentative explanation of a body of data is called a hypothesis b. A theory is less likely to be correct than hypotheses. c. A hypothesis is strengthened if it successfully predicts the outcomes of new experiments. d ...
Jeopardy
... During the rock cycle, a collision between two continental plates could force one plate down toward the heat of the mantle, producing this type of rock. ...
... During the rock cycle, a collision between two continental plates could force one plate down toward the heat of the mantle, producing this type of rock. ...
It`s a Rock`s Life - Tellus Science Museum
... (pronounced ‘nice’) and sedimentary rocks like limestone can change into marble when they are pushed down into the hot pressure-cooker inside the Earth. Some rocks get pushed down so far underground that they melt and become molten rock called magma. Magma also exists in the mantle, the layer betwee ...
... (pronounced ‘nice’) and sedimentary rocks like limestone can change into marble when they are pushed down into the hot pressure-cooker inside the Earth. Some rocks get pushed down so far underground that they melt and become molten rock called magma. Magma also exists in the mantle, the layer betwee ...
Jeopardy 19,21(#3) - Heritage Collegiate
... metals it contains. In fact these minerals are non-metallic. ...
... metals it contains. In fact these minerals are non-metallic. ...
Explain briefly what is Geology, it`s branches and it`s importance and
... Differentiate the different types and origin of sediments that comprise sedimentary rocks. Illustrate the different processes involved in the formation of clastic and non-clastic sedimentary rocks and the depositional environments where these rocks are formed. Illustrate the sub-groups of clas ...
... Differentiate the different types and origin of sediments that comprise sedimentary rocks. Illustrate the different processes involved in the formation of clastic and non-clastic sedimentary rocks and the depositional environments where these rocks are formed. Illustrate the sub-groups of clas ...
sample 7 - msaldrichscience
... segments of the ridge crest. In subduction zones it happens at depths that are very shallow or near the trench. Hot spots originate the boundary between the mantle and the outer core, they are narrow plumes of unusually hot mantle material. Continental accretion is the growth of a continent along it ...
... segments of the ridge crest. In subduction zones it happens at depths that are very shallow or near the trench. Hot spots originate the boundary between the mantle and the outer core, they are narrow plumes of unusually hot mantle material. Continental accretion is the growth of a continent along it ...
the_solid_earth
... The process of compaction and cementation is known as lithication. Some common types of sedimentary rocks are limestone, shale, and sandstone. Gypsum represents a sedimentary rock precipitated from solution. Fossil fuels such as coal and oil shale are sedimentary rocks formed from organic matter. M ...
... The process of compaction and cementation is known as lithication. Some common types of sedimentary rocks are limestone, shale, and sandstone. Gypsum represents a sedimentary rock precipitated from solution. Fossil fuels such as coal and oil shale are sedimentary rocks formed from organic matter. M ...
8-3 Unit Test
... 4. What process can all rocks go through? When rocks go through that process, what do they turn into? All rocks can go through weathering and erosion and when it goes through that process, The rocks are broken down into sediments. ...
... 4. What process can all rocks go through? When rocks go through that process, what do they turn into? All rocks can go through weathering and erosion and when it goes through that process, The rocks are broken down into sediments. ...
The Wonders of Rocks and Minerals
... Answer the following questions to identify minerals that you possess or that are provided by your instructor: (Note: Use the Mineral Identification Key provided for help.) Does the sample have metallic luster? ...
... Answer the following questions to identify minerals that you possess or that are provided by your instructor: (Note: Use the Mineral Identification Key provided for help.) Does the sample have metallic luster? ...
Faults, Fossils, Rocks and Minerals Review:
... What kind of boundary exists where the plates meet at location 10? Convergent ...
... What kind of boundary exists where the plates meet at location 10? Convergent ...
© UKRIGS Education Project: Earth Science On-Site
... Explain why the theory of crustal movement was not generally accepted for many years after it was proposed. Substantive contexts: ...
... Explain why the theory of crustal movement was not generally accepted for many years after it was proposed. Substantive contexts: ...
sea-floor spreading
... The pattern of "stripes" or anomalies is symmetrical around the oceanic ridge. The youngest oceanic rocks are near the ridges with the oceanic rocks becoming older as they move away from the ridge. The black stripes represent rocks that cooled under "normal" conditions and are normally polarized, wh ...
... The pattern of "stripes" or anomalies is symmetrical around the oceanic ridge. The youngest oceanic rocks are near the ridges with the oceanic rocks becoming older as they move away from the ridge. The black stripes represent rocks that cooled under "normal" conditions and are normally polarized, wh ...
The Rock Cycle
... Chemical Sedimentary rock • One of my old friends from the magma chamber is now a chemical sedimentary rock • He formed when minerals in solution became oversaturated and precipitated ...
... Chemical Sedimentary rock • One of my old friends from the magma chamber is now a chemical sedimentary rock • He formed when minerals in solution became oversaturated and precipitated ...
S05_4359_Exam01
... T or F 1. The duration of ground shaking does not affect the numbers of lives lost from earthquakes in populated areas such as large cities. T or F 2. In general, there is an inverse correlation between the frequency and the magnitude of disaster processes such as earthquakes and volcanoes (that is, ...
... T or F 1. The duration of ground shaking does not affect the numbers of lives lost from earthquakes in populated areas such as large cities. T or F 2. In general, there is an inverse correlation between the frequency and the magnitude of disaster processes such as earthquakes and volcanoes (that is, ...
Plate Tectonics
... continent. Gravity pulls it down back into the mantle. • Crust closer to a mid-ocean ridge moves away from the ridge and toward a deep-sea trench. ...
... continent. Gravity pulls it down back into the mantle. • Crust closer to a mid-ocean ridge moves away from the ridge and toward a deep-sea trench. ...
What is Geology?
... that typically contains quartz and feldspar minerals. Welded Tuff is a rock that is composed of materials that were ejected from a volcano, fell to Earth, and then lithified into a rock. It is usually composed mainly of volcanic ash and sometimes contains larger size particles such as cinders. ...
... that typically contains quartz and feldspar minerals. Welded Tuff is a rock that is composed of materials that were ejected from a volcano, fell to Earth, and then lithified into a rock. It is usually composed mainly of volcanic ash and sometimes contains larger size particles such as cinders. ...
Name: Period:___ Date:
... 66- The circulation around a high pressure system is / clockwise, away from the center, where air sinks 67-Air in a high pressure area is / cool & dry Rocks and Minerals: 68-Sedimentary rocks form from / sediments, evaporation of water and organic remains 69-Rocks are identified by their / texture I ...
... 66- The circulation around a high pressure system is / clockwise, away from the center, where air sinks 67-Air in a high pressure area is / cool & dry Rocks and Minerals: 68-Sedimentary rocks form from / sediments, evaporation of water and organic remains 69-Rocks are identified by their / texture I ...
Chapter 17 - Auburn City Schools
... Explain the theory of plate tectonics Compare/contrast the three types of plate boundaries and the features associated with each. ...
... Explain the theory of plate tectonics Compare/contrast the three types of plate boundaries and the features associated with each. ...
Earthquake
... How does the process of a fault-block mountain begin? • Where two plates move away from each other, tension forces create many normal faults • When two of these normal faults form parallel to each other, a block of rock is ...
... How does the process of a fault-block mountain begin? • Where two plates move away from each other, tension forces create many normal faults • When two of these normal faults form parallel to each other, a block of rock is ...
Nonrenewable Resources and Energy
... together by internal forces. At most convergent plate boundaries, the oceanic lithosphere is carried downward under the island or continent. Earthquakes are common here. It also forms an ocean ridge or a mountain range. Convergent ...
... together by internal forces. At most convergent plate boundaries, the oceanic lithosphere is carried downward under the island or continent. Earthquakes are common here. It also forms an ocean ridge or a mountain range. Convergent ...
Earth`s Interior
... The fact that the outer core is molten The fact that rocks and fossils of similar origin show up on different, now separated continents The fact that sedimentary rocks have been laid down in progressive layers The fact that metamorphic rock forms from both igneous and sedimentary rock ...
... The fact that the outer core is molten The fact that rocks and fossils of similar origin show up on different, now separated continents The fact that sedimentary rocks have been laid down in progressive layers The fact that metamorphic rock forms from both igneous and sedimentary rock ...
Algoman orogeny
The Algoman orogeny, known as the Kenoran orogeny in Canada, was an episode of mountain-building (orogeny) during the Late Archean Eon that involved repeated episodes of continental collisions, compressions and subductions. The Superior province and the Minnesota River Valley terrane collided about 2,700 to 2,500 million years ago. The collision folded the Earth's crust and produced enough heat and pressure to metamorphose the rock. Blocks were added to the Superior province along a 1,200 km (750 mi) boundary that stretches from present-day eastern South Dakota into the Lake Huron area. The Algoman orogeny brought the Archaen Eon to a close, about 2,500 million years ago; it lasted less than 100 million years and marks a major change in the development of the earth’s crust.The Canadian shield contains belts of metavolcanic and metasedimentary rocks formed by the action of metamorphism on volcanic and sedimentary rock. The areas between individual belts consist of granites or granitic gneisses that form fault zones. These two types of belts can be seen in the Wabigoon, Quetico and Wawa subprovinces; the Wabigoon and Wawa are of volcanic origin and the Quetico is of sedimentary origin. These three subprovinces lie linearly in southwestern- to northeastern-oriented belts about 140 km (90 mi) wide on the southern portion of the Superior Province.The Slave province and portions of the Nain province were also affected. Between about 2,000 and 1,700 million years ago these combined with the Sask and Wyoming cratons to form the first supercontinent, the Kenorland supercontinent.