Lab 17 2 earthquakes and subduction zones 2025

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  1. Click ‘Get Form’ to open the lab 17.2 document in the editor.
  2. Begin by entering your name, date, and period at the top of the form. This personalizes your submission and helps keep track of your work.
  3. In the 'Hypothesis' section, formulate a hypothesis regarding the relative ages of crust at the convergent boundaries. Use insights from Figure 1 to guide your thoughts.
  4. Proceed to the 'Data and Observations' section. Here, you will plot earthquake data for both the Peru-Chile Trench and Tonga Trench on separate graphs. Utilize our platform's drawing tools for accuracy.
  5. After plotting, draw best-fit lines for each graph to illustrate trends in your data clearly.
  6. Complete the analysis questions by providing detailed answers based on your observations from the graphs you created.
  7. Finally, review all sections for completeness before saving or sharing your document directly through our platform.

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sub​duc​tion (ˌ)səb-ˈdək-shən. : the action or process in plate tectonics of the edge of one crustal plate descending below the edge of another.
An example of a series of islands that formed from a genuine subduction zone is the Aleutian Islands, positioned near the border between two oceanic plates. Another example of a subduction zone would be the one that formed the Cascade Volcanoes in Oregon, Washington, and Western Canada.
The most powerful earthquakes, tsunamis, volcanic eruptions, and landslides occur in subduction zones where tectonic plates collide and one plate is thrust beneath another.
When tectonic plates move, they are either pulled apart or come together. Subduction occurs in a subduction zone when two tectonic plates are pulled together. In subduction, oceanic plates always subduct under continental plates because they are denser. The mantle below melts the plate due to the high temperature.
The type of plate boundary that is known to create the most powerful and deep earthquakes are the convergent plate boundaries. Additionally, these type of earthquakes occur due to plate collisions at the subduction zones.
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Subduction occurs when an oceanic plate runs into a continental plate and slides beneath it.

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