The Earth is layered
Major Plates of the World
Mantle Convection
Historical Movement (Past 250mya)
Pangaea
Evidence of Past Plate Movement
Ice Sheets
Magnetic Reversals
Magnetic Reversals
Magnetic Reversals
Magnetic Reversals
Location of Earthquakes
Convergent Boundaries
Transform Boundary
Divergent Boundary
Plate Boundary Review
Plate Boundaries Plate boundaries are seismically active: Earthquakes Volcanoes Mountains
Causes of Earthquakes Eruption of a volcano Collapse of a cavern Impact of a meteor Stress that builds up between two lithospheric plates.
EQ Terminology
EQ’s release energy in the form of waves
P and S waves
EQ waves are recorded using a Seismograph
Earthquake P-Wave and S-Wave Travel Time – For EQ Location
Locating EQ’s
Can you find the Epicenter? Seismic Stations P-wave arrival times: Calculate: 1. distance from seismic station and; 2. epicenter for each case study. Case Study I: Denver 2:40 New Orleans 2:00 Scranton 2:50 Case Study II: Cancun 4:00 Boston 3:20 Juneau 4:50