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adfadfname the five major geological paleofeatures related to earthquakes we have talked about in class |
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scarps are cliff faces that come from vertical displacement |
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those are coastal platform sequences. each step up from platform to platform relates to a tectonic uplift event |
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draw how a subduction zone will generate a tsunami |
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tsunamis in the sediment record |
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tsunamis can leave a large layer of marine sediment they wash up as they move onshore. this marine sediment is often quite distinct from the terrestial sediment |
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what is an event horizon? |
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an event horizon refers to stratigraphic interpretation. The event horizon is the ground layer at the time of a quake |
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the important thing to notice here is a scarp and two beheaded streams |
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lake sediment records as a paleoseismology tool |
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lake sediment records can be used to look at the timing of past landslides. when landslides occur, they dump non-organic material onto lake bed. this is distinct from the organic material that is deposited the rest of the time. Landslides are related to earthquakes, date the landslides and you can date the earthquakes |
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