Plate Tectonics Bingo - Western Reserve Public Media
... something down (as by particles washing over it) Eruption: When ash and lava flows and gases are ejected from deep within the earth Fault: An area of stress in the earth where broken rocks slide past each other, causing a crack in the Earth’s surface Igneous rock: Rock that is formed when magma cool ...
... something down (as by particles washing over it) Eruption: When ash and lava flows and gases are ejected from deep within the earth Fault: An area of stress in the earth where broken rocks slide past each other, causing a crack in the Earth’s surface Igneous rock: Rock that is formed when magma cool ...
Chapter 8 Test Review Notes
... had been joined at one time. Strong evidence that two continents were once joined might include similarities in similar coastal rock formations. Wegener’s continental drift hypothesis was not widely accepted because Wegener could not explain how the continents moved. ...
... had been joined at one time. Strong evidence that two continents were once joined might include similarities in similar coastal rock formations. Wegener’s continental drift hypothesis was not widely accepted because Wegener could not explain how the continents moved. ...
Earth’s Sub-Surface Processes
... CRUST: outer surface; can be oceanic or continental LITHOSPHERE: rigid interior of crust ...
... CRUST: outer surface; can be oceanic or continental LITHOSPHERE: rigid interior of crust ...
Metamorphic Rocks
... the rock have changed. All three types of rock can be changed by heat, pressure, or a combination of both. A rock’s texture or mineral composition can change when its surroundings change. If the temperature of pressure of the new environment is different from the one in which the rock formed, the ...
... the rock have changed. All three types of rock can be changed by heat, pressure, or a combination of both. A rock’s texture or mineral composition can change when its surroundings change. If the temperature of pressure of the new environment is different from the one in which the rock formed, the ...
File - Native Expeditions
... 1596 cartographers noticed how continents seemed to fit together like a puzzle 1858 this first rendition was produced ...
... 1596 cartographers noticed how continents seemed to fit together like a puzzle 1858 this first rendition was produced ...
Constructive and Destructive Landforms
... Destructive Landform Processes Break down Earth’s surface causing the land to become ...
... Destructive Landform Processes Break down Earth’s surface causing the land to become ...
Inner Structure of the Earth 3. Mantle
... other and form a spreading zone. These areas are likely to have earthquakes, volcanoes, and rift valleys (a large split along the crest of a mountain). ...
... other and form a spreading zone. These areas are likely to have earthquakes, volcanoes, and rift valleys (a large split along the crest of a mountain). ...
Meg Anderson Earth Unit Test SOL: 5.7 Read each question
... c. an oceanic rock d. a metamorphic rock 5. A student is hiking through a forest taking pictures for science class. Which picture would most likely be used as an example of human impact on Earth? a. a trail built by cutting down trees b. a river eroding away the riverbank c. a bird nest made of dead ...
... c. an oceanic rock d. a metamorphic rock 5. A student is hiking through a forest taking pictures for science class. Which picture would most likely be used as an example of human impact on Earth? a. a trail built by cutting down trees b. a river eroding away the riverbank c. a bird nest made of dead ...
the Earth`s interior must be much greater than 2.8 g/cm3 for the
... the Earth’s interior must be much greater than 2.8 g/cm3 for the entire Earth to average 5.5 g/cm3.This is partly due to the effect of compression, but also partly because the material in the Earth’s core is mostly iron, which is much more dense than rocks, even when it is not under great pressure. ...
... the Earth’s interior must be much greater than 2.8 g/cm3 for the entire Earth to average 5.5 g/cm3.This is partly due to the effect of compression, but also partly because the material in the Earth’s core is mostly iron, which is much more dense than rocks, even when it is not under great pressure. ...
Archean - University of Hawaii at Hilo
... formation of the Core (0-40 km [up to 70], Mantle (40-2890 km), and Crust (outer 2890-5150, inner 5150-6370 km). Moon Maria (younger, recratering and basalt flows from melting) and Highlands (oldest) No water-expelled during collision and melting-not kept in atmosphere due to small size and lack of ...
... formation of the Core (0-40 km [up to 70], Mantle (40-2890 km), and Crust (outer 2890-5150, inner 5150-6370 km). Moon Maria (younger, recratering and basalt flows from melting) and Highlands (oldest) No water-expelled during collision and melting-not kept in atmosphere due to small size and lack of ...
Intrusive Activity Earth Science Notes Chapter 18.3
... ________________________ intrusive igneous rock bodies ________________________ irregularly shaped plutons that are similar to batholiths but smaller ________________________a pluton that forms when magma intrudes parallel to layers of rock ________________________ the larges plutons _______________ ...
... ________________________ intrusive igneous rock bodies ________________________ irregularly shaped plutons that are similar to batholiths but smaller ________________________a pluton that forms when magma intrudes parallel to layers of rock ________________________ the larges plutons _______________ ...
Even More Landform Changes
... B. Weathering is the breaking down of rock into smaller particles. C. Plate tectonics is a theory that explains the movements of the Earth’s plates. D. Deposition is the process of depositing sediment in a new location. ...
... B. Weathering is the breaking down of rock into smaller particles. C. Plate tectonics is a theory that explains the movements of the Earth’s plates. D. Deposition is the process of depositing sediment in a new location. ...
Science Framework
... INNER CORE slowly on top of the mantle - remember, they float. It takes millions of years for plates to move miles, but even over a short period of time, plates are moving. ...
... INNER CORE slowly on top of the mantle - remember, they float. It takes millions of years for plates to move miles, but even over a short period of time, plates are moving. ...
Continental Drift
... • Mapping of the ocean floor revealed a long mountain range running down the middle of the Atlantic Ocean. • It is called the “Mid- ...
... • Mapping of the ocean floor revealed a long mountain range running down the middle of the Atlantic Ocean. • It is called the “Mid- ...
study-guide-test-on-plate
... The plates of the lithosphere float on the asthenosphere The results of plate movements can be seen at plate boundaries The Himalaya mountains are the result of a collision between the indo-Australian plate and Eurasian plate The presence of the same fossils and same rocks found on different contine ...
... The plates of the lithosphere float on the asthenosphere The results of plate movements can be seen at plate boundaries The Himalaya mountains are the result of a collision between the indo-Australian plate and Eurasian plate The presence of the same fossils and same rocks found on different contine ...
Ancient rocks yield clues about Earth`s earliest crust
... Continents today form when one tectonic plate shifts beneath another into the Earth's mantle and cause magma to rise to the surface, a process called subduction. It's unclear whether plate tectonics existed 2.5 billion to four billion years ago Fortunately, a few rocks—which the research team or if ...
... Continents today form when one tectonic plate shifts beneath another into the Earth's mantle and cause magma to rise to the surface, a process called subduction. It's unclear whether plate tectonics existed 2.5 billion to four billion years ago Fortunately, a few rocks—which the research team or if ...
Study Guide: Earth`s Layer, Pangaea, Plate Tectonics, Minerals and
... A. Softer than itself B. As hard or harder than itself 22. Name 3 characteristics all rocks have. They are a solid ...
... A. Softer than itself B. As hard or harder than itself 22. Name 3 characteristics all rocks have. They are a solid ...
Earth Outline
... a. A volcano is any opening in the Earth’s ___________ that allows hot __________, _____________ , and _________ __________to pass through ...
... a. A volcano is any opening in the Earth’s ___________ that allows hot __________, _____________ , and _________ __________to pass through ...
Inside Earth Worksheet
... c. layer of rock that forms Earth’s outer surface d. the “middle” part of the Earth e. layer that is composed of both the crust and the upper part of the mantle that behaves like a brittle, rigid solid f. the layer made up of liquid iron and nickel g. hot, ultramafic rock layer that makes up 68% of ...
... c. layer of rock that forms Earth’s outer surface d. the “middle” part of the Earth e. layer that is composed of both the crust and the upper part of the mantle that behaves like a brittle, rigid solid f. the layer made up of liquid iron and nickel g. hot, ultramafic rock layer that makes up 68% of ...
Plate Tectonics - Paul J. Goodenough
... the further the rock is from the mid-ocean ridge. 2. Magnetism: Changes in the magnetic alignment of the Earth are found in alternating bands in the seafloor rock. III. Theory of Plate Tectonics A. Theory o Combined theory of Continental Drift & Seafloor Spreading. o Earth’s crust & upper mantle (li ...
... the further the rock is from the mid-ocean ridge. 2. Magnetism: Changes in the magnetic alignment of the Earth are found in alternating bands in the seafloor rock. III. Theory of Plate Tectonics A. Theory o Combined theory of Continental Drift & Seafloor Spreading. o Earth’s crust & upper mantle (li ...
weathering_and_erosion
... tectonic plates" coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust (called "non-hotspot intraplate volcanism"), such as in the African Rift Valley, the ...
... tectonic plates" coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust (called "non-hotspot intraplate volcanism"), such as in the African Rift Valley, the ...
Review Mid-Term Exam
... In time EARTH’S interior accumulated heat New atmosphere created by volcanic outgassing and delivery of gases and water by ice-covered comets. ...
... In time EARTH’S interior accumulated heat New atmosphere created by volcanic outgassing and delivery of gases and water by ice-covered comets. ...
Geology
Geology (from the Greek γῆ, gē, i.e. ""earth"" and -λoγία, -logia, i.e. ""study of, discourse"") is an earth science comprising the study of solid Earth, the rocks of which it is composed, and the processes by which they change. Geology can also refer generally to the study of the solid features of any celestial body (such as the geology of the Moon or Mars).Geology gives insight into the history of the Earth by providing the primary evidence for plate tectonics, the evolutionary history of life, and past climates. Geology is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources, understanding of natural hazards, the remediation of environmental problems, and for providing insights into past climate change. Geology also plays a role in geotechnical engineering and is a major academic discipline.