Exam 3: Earth Structure and Plate Tectonics
What is plate convergence and what types of features are produced from convergence?
Plate convergence happens when lithospheric plates come together. There are three types of convergence and are defined by the composition and density of plates that are coming together: (1) the convergence of oceanic crust toward continental crust, (2) the convergence of oceanic crust and oceanic crust and (3) continental crust towards continental crust. Because of the density differences between oceanic and continental crust, different features are produced. When oceanic crust collides with continental crust, as off the west coast of South America, the oceanic crust slides underneath the continent and the continental crust buckles forming the Peru-Chili trench and the Andes Mountains. In the north Pacific where oceanic crust converges with oceanic crust island arcs are formed. Lastly, when two plates of continental crust collide, spectacular features such as the Himalayan mountains and the Tibetan plateau are formed.
Alfred Wegener was a polar explorer who suggested that at one time, Earth's landmasses were joined into a supercontinent called Pangaea.
True
Density is a measure of relative heaviness and is defined as mass per unit volume.
Which of the following lists represents the main components of the Earth's crust?
There are 2 types of plate divergences: divergent oceanic crust and divergent continental crust.
How has the history of plate movement been captured in residual magnetic fields?
Earlier than 200 million years ago, the continents were joined into one supercontinent called:
Japan is located along the Pacific Ring of Fire and experiences many earthquakes. Almost all of the earthquakes around Japan occur:
Convection in the asthenosphere, in part, facilitates continental drift.
The magnetic striping of the seafloor is considered evidence of seafloor spreading and:
About how many kilometers (miles) is it from the Earth's center to the outer edge of the outer core?
A cross section of Earth reveals a layered structure that has different thicknesses and densities. How do geologists know this?
As early as the 1700s, scientists and explorers notice a remarkable coincidence of shape of the Atlantic coasts of Africa and which continent?
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