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... 9. Glue the 4 small squares on the paper, next to the corresponding layers. 10. Using a black pen or marker, complete the bracket that connects the two sections of the lithosphere. ASK me if you are not sure where to do this. 11. Label the Diagram using the following terms (asthenosphere, continenta ...
Plate Tectonics - Issaquah Connect
Plate Tectonics - Issaquah Connect

... Folded Mountains Himalayan Mountains ...
Volcanoes - Holy Angels School
Volcanoes - Holy Angels School

... • Composite volcanoes are built from alternating layers of hardened lava flows and ...
How did we get here? Learning Objectives
How did we get here? Learning Objectives

... Understand the processes that are continuously changing Earth’s surface as lithospheric plates move relative to one another. Identify the role of oceanic ridges, transform faults and deep-sea trenches in defining the edges of lithospheric plates. Understand the importance of asthenospheric thermal c ...
Cause of Earthquakes
Cause of Earthquakes

...  Earthquakes occur when energy stored in elastically strained rocks is suddenly released.  This release of energy causes intense ground shaking in the area near the source of the earthquake (Focus) and sends waves of elastic energy, called seismic waves, in all directions throughout Earth.  Earth ...
Continental Drift and Plate Tectonics Part 1 Multiple Choice
Continental Drift and Plate Tectonics Part 1 Multiple Choice

... 24. Which of the following was the biggest problem with Wegener's Theory of Continental Drift? a. He could not explain the mechanism for movement of the continents b. Too many scientists already came up with the same theory c. All of his evidence turned out to be fake 25. Which two mountain ranges a ...
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File

... 18. A ________________________ can also form where two oceanic plates converge. In this case, the colder, older, ________________________ oceanic plate bends and sinks down into the mantle. 19. No subduction occurs when two ________________________ plates collide. 20. Because _______________________ ...
Plate Tectonics
Plate Tectonics

... • Continents that have drifted closer to the equator are warmer because the sun’s rays hit them directly. • Continental drift also changed the flow of ocean currents and wind flows. ...
CE Earthquake Review- 2010 1. How do
CE Earthquake Review- 2010 1. How do

... 34. What happens when two oceanic plates collide? The older, colder, denser plate moves deep into earth creating a trench, or deep valley. 35. What happens when oceanic and continental plates collide? The oceanic plate will dive into the ground and create a subduction zone. 36. What happens when two ...
10.00 points 10.00 points 10.00 points 10.00 points 10.00 points
10.00 points 10.00 points 10.00 points 10.00 points 10.00 points

... The composition of the Earth's atmosphere today is about 78% _____, 21% _____, and much less than 1% _____. Oxygen; nitrogen; carbon dioxide and other gases Nitrogen; carbon dioxide; oxygen and other gases Oxygen; carbon dioxide; nitrogen and other gases Nitrogen; oxygen; carbon dioxide and other ga ...
Continents On The Move
Continents On The Move

... lithosphere and the destruction of old lithosphere. The oldest sea-floor rocks on Earth are only about 200 million years old, because oceanic crust continuously recycles into the mantle at subduction zones (Figure 3). Rocks as old as about 4 billion years are found on continents, because subduction ...
Continental Drift - sciencewithskinner
Continental Drift - sciencewithskinner

... – Magma cools and iron-bearing minerals become magnetized – Orientation becomes permanent pointing north ...
PDF
PDF

... “epigraphs” or map unit labels. An epigraph is a code formed by the combination of alphabetical and/or numerical elements with which a cartographic unit is designated. The formulation informs of the age or of the processes that intervened in their genesis. The epigraph accompanies the cartographic u ...
Plate Boundaries (pp. 160–162)
Plate Boundaries (pp. 160–162)

... _____________________________________________________________________ _____________________________________________________________________ _____________________________________________________________________ 10. Is the following sentence true or false? Crust is neither created nor destroyed along ...
Splash Screen
Splash Screen

... Earth’s Structure (cont.) • Many scientists believe that most of the landmasses forming our present-day continents were once part of one gigantic supercontinent called Pangaea. • Due to continental drift, they slowly separated. • Due to plate tectonics, the physical features of the planet are const ...
Earth`s Structure
Earth`s Structure

...  sea-floor spreading – This occurs under oceans where plates move apart and magma rises to the surface and cools to form new crust. ...
Practice Questions: Plate Tectonics
Practice Questions: Plate Tectonics

... A) Mesosaurus migrated across the ocean from location X to location Y. B) Mesosaurus came into existence on several widely separated continents at different times. C) The continents of South America and Africa were joined when Mesosaurus lived. D) The present climates at locations X and Y are simila ...
3 Causes of Volcanic Eruptions
3 Causes of Volcanic Eruptions

... Magma forms deep in the Earth’s crust and in the upper parts of the mantle. In these areas, the temperature and pressure are very high. Changes in pressure and temperature can cause magma to form. Part of the upper mantle is made of very hot, solid rock. The rock is so hot that it can flow, like sof ...
Seismic Wave
Seismic Wave

... Nonmagmatic volcanism when magma becomes lava—it returns solids, There are less well-known types of volcanism that fluids and gases to the Earth's crust and surface. don't involve magma: mud volcanism is one. Mud volcanoes come in two types. On land, hundreds The solids are igneous rocks, ready to e ...
Question 1:
Question 1:

... pointing north but has reversal, the magnetic strips are one of the proofs that the oceans are created at the ridge. The ocean floor acts as a tape recorder. Once the magma that come out at the ridge cool below the Curie temperature the rocks “remember” the polarity of the magnetic field at the time ...
Earthquakes Presentation
Earthquakes Presentation

... What is an earthquake? An earthquake is a rapid movement of the Earth's surface due to the sudden release of energy accumulated by two plates of the Earth’s crust pushing against each other. The rocks suddenly break along a fault because of all the pressure accumulated inside the Earth in a place c ...
Chapter 5 – Volcanos and other igneous activity
Chapter 5 – Volcanos and other igneous activity

... Chapter 5 Volcanos and other igneous activity The nature of volcanic eruptions  Viscosity is a measure of a material’s resistance to flow  Factors affecting viscosity • Temperature - Hotter magmas are less viscous • Composition - Silica (SiO2) content • Higher silica content = higher viscosity (e. ...
Theory of Plate Tectonics
Theory of Plate Tectonics

... which has become denser as a result of cooling, descends below another plate creating a deepsea trench. – The subducted plate descends into the mantle and melts. – Some of the magma forms new oceanic crust at the ridge or is forced back to the surface, forming an arc of volcanic islands that paralle ...
Unit 7 Lesson 1 Forces that Change the Earth
Unit 7 Lesson 1 Forces that Change the Earth

... divergent plate boundary under the ocean sea-floor spreading: the process by which molten material adds new oceanic crust to the ocean floor deep-ocean trench: a deep valley along the ocean floor beneath which oceanic crust slowly sinks toward the mantle subduction: the process by which oceanic crus ...
Chapter 3- The Dynamic Earth
Chapter 3- The Dynamic Earth

...  Plate Tectonics- rigid layer of the lithosphere is divided into pieces called plates that glide over the underlying athenosphere. – Most geologic activity occurs where these plates meet called plate boundaries. – Colliding plates build mountains. ...
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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.
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