Earthquakes Earthquake describes both sudden slip on a
Earthquakes!
Earthquake describes both sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip. Seismogram showing Shaking from an Earthquake.
Earthquakes happen at Plate Boundaries and Faults
Focus vs. Epicenter Focus: The location where the earthquake begins. At fault line underground. Epicenter: The point on the Earth's surface located directly above the focus of an earthquake
Earthquake Sequence Foreshock: Small shaking before major shaking. Earthquake: Primary Wave, Secondary Wave (also Surface waves such as Rayleigh and Love Waves: cause the most damage). Aftershocks: Smaller shaking after main quake.
Primary Wave (PWave/Compressional Wave) Primary Wave (Pwave): Fastest wave. First to arrive and be felt. Waves are parallel to direction of movement. Feels like an explosion. Move through solids, liquids, gasses.
Secondary Wave (S-Wave) S-Wave: Slower than P -Wave. Arrives and felt second. Wave are perpendicular to direction of movement. (Shear). Can only move through solids.
Seismograms: Shows P and S Waves Which is P-Wave? Which is S-Wave?
P-Wave and S-Wave shadow Zones Moho: Boundary Between crust and Mantle.
Finding the Epicenter: Triangulate Position with at least 3 Seismometers
Richter Scale Used to measure earthquakes. Logarithmic Scale. Each whole number is 10 times more intense. Ex. A Magnitude 3 is 100 times more intense than Magnitude 1.
Occurs when thrust fault under ocean displaces ocean water upward. Tsunami
Liquefaction Loosely packed, water logged sediments can act like a fluid from intense shaking during an earthquake.
Earthquake Damage: Haiti 2010
Earthquake Safe Structures
- Slides: 15