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chapter 12
chapter 12

Planet Earth - Wayne State University Physics and Astronomy
Planet Earth - Wayne State University Physics and Astronomy

... does not move up and down within it Temperatures here increase with elevation Near the top of the stratosphere, one finds a layer of ozone (O3) Ozone is a good absorber of ultraviolet light It thus protects the surface from the sun's ultraviolet radiation and makes it possible for life to exist on t ...
tectonics2a
tectonics2a

... There are several large tectonic plates and a number of much smaller plates. The Earth’s continents sit on plates composed of both oceanic and continental crust. The huge Pacific plate is composed almost entirely of oceanic crust, and is being subducted around almost its entire western ...
Lesson 2 | Shaping Earth`s Surface
Lesson 2 | Shaping Earth`s Surface

... The Mid-Atlantic ridge is part of an interconnected ocean ridge system that is the largest topographic feature on Earth’s surface, more than 70,000 km (43,000 miles) in length. This ocean ridge system winds through all the oceans something like the seam on a basketball. The ridges are from 3,000 to ...
Plate Tectonics 2015
Plate Tectonics 2015

... core flows around the solid inner core ...
EIPG_11e_Lecture_Ch13
EIPG_11e_Lecture_Ch13

... Continental rift usually occurs along two of the arms ...
The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics

Hydrothermal Vents
Hydrothermal Vents

... (Ecuador) ...
In this lecture we will discuss the Lithosphere, the solid part of the
In this lecture we will discuss the Lithosphere, the solid part of the

Background Information
Background Information

... Continental + Continental – When two pieces of continental crust come together at a convergent plate boundary, neither one of them will subduct. Their light density makes them too buoyant to subduct into the asthenosphere, so instead, they rise up to create a mountain ...
high-res
high-res

... •  3) Experiments test if hypothesis is valid –  Can hypothesis predict the results for related phenomena? •  Too little known about the ocean floor and Earth’s interior. •  Hypothesis incomplete because it doesn’t address the oceans themselves. •  BUT - from 1930’s through 1950’s much was learned a ...
FCAT Review Test - Rock Cycle Multiple Choice Identify the choice
FCAT Review Test - Rock Cycle Multiple Choice Identify the choice

... 1. Which of the following is true about rocks? a. Rocks are composed of only one mineral. c. Coal is not considered a true rock. b. Rocks do not contain any mineral matter. d. Most rocks are a mixture of minerals. ...
Plate Tectonics 2
Plate Tectonics 2

... USGS Natl. Earthquake Center, Public Domain Star shows location of magnitude 8.3 Kurile Eq, 11/15/2006 ...
Crust
Crust

... - dense (sinks under continental crust) - young ...
Deep Ocean Basins
Deep Ocean Basins

... move, they create different landforms. The mountain ranges of the mid-ocean ridge, trenches, and underwater volcanoes are all formed by interactions of Earth's plates. At the mid-ocean ridge, plates are diverging or moving apart. Magma squeezes up though cracks between the plates and hardens to form ...
Plate Tectonics
Plate Tectonics

... In a divergent plate boundary, molten rock rises to the surface and cools to become new crust. This newly formed crust is continually being replaced by new molten rock. Older crust diverges and is forced to move away from the area where new molten rock will form into new crust. ...
6.1 Earthquakes and
6.1 Earthquakes and

... A fault zone is an area where several plates are touching  The San Andreas Fault is actually several faults that all connect to form one long fault zone ...
plate boundaries
plate boundaries

... – Downward plunge of cold rocks gives rise to oceanic trenches ...
Plate Tectonics Power Point
Plate Tectonics Power Point

... Ocean-floor spreading helps to explain how continents drift. As a piece of the ocean floor moves, it takes its continent (if it has one) with it. Individual sections of midocean ridges are straight but the ridges as a whole curve.This is because the straight sections are offset by thin cracks known ...
Earth`s Composition
Earth`s Composition

... The core is the innermost layer of the Earth. It is about 7,000km thick and goes all the way to the center of the earth. This layer is the most difficult to study since it cannot be reached. Scientists believe that the core is composed of mostly iron and nickel. They have used the data from how seis ...
C1a
C1a

... The Answer: 1) Scientists discovered 50 years later that the Earth generates massive amounts of heat through radioactive decay in the core. This heat generated convection currents in the mantle causing the crust to move 2) We also now know that the sea floor is spreading outwards from ...
Practice09o
Practice09o

... h. tipped past vertical ...
Document
Document

... • Does the core exchange material with the mantle? (Do plumes come from the CMB?) • What are the characteristics of mantle convection in terms of its ability to stir and homogenize heterogeneous ...
Interactive Plate Tectonics - Fredericksburg City Schools
Interactive Plate Tectonics - Fredericksburg City Schools

... accepted since the 1960s, states that the earth's outer layer, or lithosphere, is broken into several large slabs called___________. These plates, which hold the continents and oceans, are __________ but constantly _____________around the planet. The movement of the plates not only supports our unde ...
Folding and Faulting
Folding and Faulting

... syncline, but was compressed with a greater force causing the angle to be much smaller. • Folds such as these occur to form steep mountain slopes like those in Whistler, British Columbia. • To the left is a photo of a tight fold formed by extreme pressure on these rocks. ...
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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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