'Oceanic plate collides' diaporamas de présentation

Geology and Nonrenewable Minerals

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Geology and Nonrenewable Minerals

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Volcanoes

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Jeopardy

Jeopardy. Parts of the Earth. Lava and Pyroclastic Materials. Continental Drift. Explosive vs. Nonexplosive. Boundaries. Q $100. Q $100. Q $100. Q $100. Q $100. Q $200. Q $200. Q $200. Q $200. Q $200. Q $300. Q $300. Q $300. Q $300. Q $300. Q $400. Q $400. Q $400. Q $400.

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Ch. 9 Study Guide Answers

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8.9(A) Describe the historical development of evidence that supports plate tectonic theory.

Earth & Space. 8.9(A) Describe the historical development of evidence that supports plate tectonic theory. Evidence for plate tectonics

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Volcanoes

Volcanoes. Chapter 7. Volcanoes. A volcano is a weak spot in the crust where molten material, or magma, comes to the surface Magma is the molten mixture of rock-forming substances, gases, and water from the mantle Once it has reached the surface= lava Solid rock forms once lava cools.

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Constructive Force 1

Constructive Force 1. A Plate Tectonics 1)Alfred Wegener hypothesized that all of the continents were once connected to form one large land mass called Pangaea. Evidence of Continental drift 2. a) As a student, and scholar he saw the globe as a broken jigsaw puzzle.

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Chapter 9 Volcanoes

Chapter 9 Volcanoes. 9.1 How and Where Volcanoes Form. How and Where Volcanoes Form. The term volcano refers to both the opening that the lava escapes from and the landform that develops around this opening. Magma Formation. A volcanic eruption occurs when magma rises to the surface.

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DO NOW! HAPPY THURSDAY!!! September 27, 2012

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Plate Tectonics

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Volcanoes

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To the teacher:

To the teacher:. This CPO Science PowerPoint presentation is designed to guide you through the process of presenting the lesson to your students. The presentation uses a 5-E teaching model: Engage, Explore, Explain, Elaborate, and Evaluate.

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Tectonic Processes: Plate Tectonics

Tectonic Processes: Plate Tectonics. November 16 th , 2011. Plate Tectonics. Seven Large and Many small plates. 80km thick Move a few cm a year. Types of movement. Convergent Divergent Transform-Fault ( ie . Slip and slide). Subduction. Oceanic plate collides with continental plate

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