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Chapter 6 Plate Tectonics
Chapter 6 Plate Tectonics

... crust is broken into about 19 pieces These plates move on top of the asthenosphere. ...
Section 4 Sea-Floor Spreading
Section 4 Sea-Floor Spreading

...  The Pacific is shrinking. This happens when the deep ...
Mature vs. Immature Sandstone
Mature vs. Immature Sandstone

... sediment grains as well as the types of sandstone present. The compositions of the grains distinguish the source area and rock type. It also correlates with the amount of transport and erosion the sediments encounter. Mature sandstones can be found far from the source area. The amount of transport a ...
8.4 Earth`s Layers
8.4 Earth`s Layers

... Asthenosphere Lithosphere – Earth’s outermost layer that consists of the crust and uppermost mantle. It forms a relatively cool, rigid shell Asthenosphere – located below the lithosphere. Relatively soft, and weaker layer. Warmer than the lithosphere ...
Word format
Word format

... remain a solid at 800°C deep down in the Earth’s crust because: A. there is less water present B. oxygen in the atmosphere affects the melting temperature C. the melting point is different at sea level than higher up D. all minerals remain solid in the Earth’s crust E. the melting temperature rises ...
Growing and Shrinking Oceans
Growing and Shrinking Oceans

... So if new crust is being formed, why doesn’t the Earth grow larger? Well, that’s because even while new rock is being created, older rock is being destroyed at about the same rate. You learned that subduction is when one tectonic plate (usually a thin oceanic plate) gets forced below another tectoni ...
Minerals • Mineral is a substance that is: • Solid • Formed in Nature
Minerals • Mineral is a substance that is: • Solid • Formed in Nature

...  The earth’s surface is constantly changing because of the Rock Cycle  Mountains, valleys, rivers and many other features are created or destroyed due to: o Weathering- breaking down rocks into sediment o Erosion – Moving the sediment from one place to another o Deposition – the sediment stops mov ...
Benchmark Test Study Guide October 2013 Standard: The student
Benchmark Test Study Guide October 2013 Standard: The student

... •Forms from the _compaction__ and/or _cementation_ of rock pieces, _mineral grains_, or shell fragments called sediments_. •Sediments are formed through the processes of _weathering _ and erosion of rocks exposed at Earth’s surface. •_Sedimentary__ rocks can also form from the chemical depositing of ...
Chapter_2_Section_2_NOTES
Chapter_2_Section_2_NOTES

... a) Where a plate of _ocean _______ crust collides with a plate of _continental crust, the ocean crust plunges underneath and melts. The molten rock erupts onto the surface through a _volcano_________________. b) When two plates push together, the crust cracks and splinters from ___the pressure_. The ...
Continental Drift
Continental Drift

Key - Scioly.org
Key - Scioly.org

... 2 points for a correct description of slab pull (must mention that the force from subducting sections affects diverging sections). 1 point for stating that slab pull is stronger. ...
Key - Scioly.org
Key - Scioly.org

Worksheet
Worksheet

... 21. _________This is the name of the super-continent 250 million years ago. 22. _________Molten rock under the surface of the Earth is called. 23. _________The deepest area of the oceans. 24. _________Along crack in the crust is called a 25. _________The idea that the Earth's plates are moving acros ...
UKRIGS Education Project
UKRIGS Education Project

C2 Revision - Purbrook Park School
C2 Revision - Purbrook Park School

... • The reaction conditions of the Haber Process are said to be a compromise. • When you increase the temperature of the reaction, the rate of the reaction increases, and the Haber Process will reach equilibrium quicker. The increase in temperature decreases the yield of the reaction, as the forward r ...
Earth 50 2nd Midterm Exam November 14, 2005 Multiple Choice (2
Earth 50 2nd Midterm Exam November 14, 2005 Multiple Choice (2

Chapter 22.1: Earth’s Structure
Chapter 22.1: Earth’s Structure

... The study of the planet E.’s composition & structure ...
3. Caledonian Orogenesis
3. Caledonian Orogenesis

... Horizontal to gently dipping strata. ...
It`s a Rock`s Life - Tellus Science Museum
It`s a Rock`s Life - Tellus Science Museum

... some new rock as the Earth moves through its normal cycles. A rock’s life can be summed up in one word: CHANGE! We have no control over it either. Like it or not, we just keep on rolling through the Rock Cycle of life… The Rock Cycle is a process that continues over and over and over and has been ch ...
CHAPTER 14
CHAPTER 14

... Tectonic plates have rearranged the earth’s continents and ocean basins over millions of years like pieces of a gigantic jigsaw puzzle. The plates have three types of boundaries. Natural hazards such as earthquakes and volcanoes are likely to be found at plate boundaries. ...
Slide 1
Slide 1

... Mostly happens at Plate Boundaries. ...
Introduction to Rocks
Introduction to Rocks

... related to each other.  These science concepts are like a puzzle: All of the “pieces” work together to make something bigger.  The concepts are also an example of cause & effect. When one process occurs another process will occur in return. ...
Hawaiian Islands - Helena High School
Hawaiian Islands - Helena High School

... ...
Settle-Carlisle leaflet (pdf file)
Settle-Carlisle leaflet (pdf file)

Webelos Activity Badge Geologist
Webelos Activity Badge Geologist

... the past". Hutton advocated that given sufficient time, processes that were now working could account for all of the geologic features we now see. Geologists call this principle the principle of uniformitarianism. Geology includes the study of materials that make the earth, the processes that change ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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