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Oceanic to Continental Plate of Convergence Zone - Homework | SPHY 101, Assignments of Astronomy

Material Type: Assignment; Class: Introduction to Astronomy; Subject: Physics; University: Spelman College; Term: Spring 2009;

Typology: Assignments

Pre 2010

Uploaded on 08/04/2009

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Physics 101 Astronomy
Spring 2009
Homework due 2/27/2009
The extremely high temperature of the Earth’s core causes material in
the surrounding mantle to become hot, expand, and rise toward the
surface. The mantle material cools by transferring heat to the crust,
sinks, and the rising and sinking together produce a circular motion of
material moving beneath the Earth’s surface. This circulation of
mantle material causes the continental and oceanic plates to move
across the Earth’s surface. At various locations, we are able to
observe the plates colliding, separating and moving horizontally.
The drawing below shows a cross section of the Earth’s surface and
its underlying mantle. At this particular location, the dense oceanic
plate is being forced beneath the less dense continental crust. The
dense oceanic plate experiences higher temperatures (and pressures)
as it is forced deeper into the mantle. This interaction between the
two plates causes them to partly melt and some of that molten
material moves upward through the continental plate, forming
volcanoes.
Oceanic to Continental Plate Convergence Zone
1. In the drawing above, which way (right or left) are the oceanic and
continental plates moving? The oceanic plate is moving to the
right and the continental plate to the left. This is indicated by
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Physics 101 Astronomy Spring 2009 Homework due 2/27/ The extremely high temperature of the Earth’s core causes material in the surrounding mantle to become hot, expand, and rise toward the surface. The mantle material cools by transferring heat to the crust, sinks, and the rising and sinking together produce a circular motion of material moving beneath the Earth’s surface. This circulation of mantle material causes the continental and oceanic plates to move across the Earth’s surface. At various locations, we are able to observe the plates colliding, separating and moving horizontally. The drawing below shows a cross section of the Earth’s surface and its underlying mantle. At this particular location, the dense oceanic plate is being forced beneath the less dense continental crust. The dense oceanic plate experiences higher temperatures (and pressures) as it is forced deeper into the mantle. This interaction between the two plates causes them to partly melt and some of that molten material moves upward through the continental plate, forming volcanoes. Oceanic to Continental Plate Convergence Zone

  1. In the drawing above, which way (right or left) are the oceanic and continental plates moving? The oceanic plate is moving to the right and the continental plate to the left. This is indicated by

an arrow on each plate, and also follows from the direction of the mantle convection directly underneath the plate.

  1. Which is hotter, the piece of mantle material at position A or the piece of mantle material at position D? Explain your reasoning. D is hotter. There are two arguments you can make: temperature increases with depth inside the Earth, and D is deeper. Or, in a convection current, hot material rises and the material at D is clearly shown as rising.
  2. What direction are the pieces of mantle material moving (right, left, up or down) at each of positions A, B, C and D? A: to the right, driving the oceanic plate to the right. This material does not sink until it reaches B. B: Down, from material at both A and C that has cooled due to its contact with the crust. C: to the left, driving the continental plate to the left. D: up, rising toward the crust. It does not deflect to the right until it reaches the crust, at A.
  3. A group of students are discussing plate tectonics, and take the following positions: Student 1: The plates are moving because the mantle material that rises to the surface at a rift pushes the plates apart. Student 2: I disagree. The plates are just floating on the mantle material. They started moving a long time ago, when they Earth initially formed, and the plates’ momentum keeps them moving toward each other. Student 3: I disagree with both of you. The plates are moving because the mantle material is constantly moving and the plates are dragged along by that motion. Do you agree or disagree with any or all of these students? Why? Only student 3 is correct. Student one is incorrect because rifts are a result of plates moving apart, not a cause of that motion. The plates drift along in the direction of mantle convection, and where they spread apart a gap is created. Mantle material rises to fill the gap but does NOT push the plates apart. Student 2 has neglected to consider that when rocks move around, there is a lot of friction and that would have long ago caused any initial movement to die away.

As in the previous question, significant amounts of volcanic activity will quickly cover up craters. Lots of craters implies no activity for a very long time. Therefore the Moon is probably not currently active.

  1. If a new planet were discovered, what evidence would you look for to determine whether or not it has an active, hot and molten interior? Why? State as many features as you can think of that would make your case. Any geologic feature we have studied that is related to plate tectonics would be an indicator of activity: rifts, faults, shield or pyroclastic volcanoes, subduction zones (i.e. trenches). Note that you cannot look under the surface so looking for convection or at the core is not allowed. Crater density is an indirect indicator. Tectonic activity covers up craters so lots of craters implies not a lot of activity. If you cannot see the surface, overall size is a plausible indicator. As we have seen, internal temperature increases with the size of the planet – larger planets are hotter.