Earthquake - is a weak to violent shaking of the ground produced by
the sudden movement of rock materials below the earth’s surface. It is a wave-like movement of the earth’s
surface and may classified as tectonic or volcanic.
tremor : temblor
Volcanic Earthquakes: are produced by movement of magma beneath volcanoes.
Tectonic earthquakes: are produced by sudden movement along faults and plate boundaries.
Focus - actual location beneath the surface where the earthquake begins.
epicenter - point on the earth’s surface located directly above the focus of an earthquake.
fault - refers to a fracture, fissure, or a zone of weakness where movement has occurred.
magnitude - energy released at the source of the earthquake and determined by seismographs.
intensity -strength of shaking produced by the earthquake at a certain location.
seismograph -instrument that records an earthquake
seismometer -sensor that detects ground motion.
seismogram - record of earthquake retrieved from a seismograph.
aftershock -usually weaker earthquakes that follow the main shock of an earthquake’s sequence
ground shaking - disruptive up-down and sideways movement or motion experienced
ground rupture - displacement on the ground due to the movement of fault
liquefication -mixing of sand or soil and water underground during the shaking of a moderate or strong earthquake
tsunami -sea waves resulting from the disturbance of ocean floor by an earthquake.
earthquake induced landslide - failures in steep or hilly slopes triggered by an earthquake
earthquake induced ground subsidence - a gradual setting or sudden sinking of the earth's surface
tsunami - sea waves resulting from the disturbance of ocean floor by an earthquake
earthquake induced lanslide - failures in steep or hilly slopes triggered by an earthquake
earthquake induced ground subsidence -a gradual settling or sudden sinking of the earth’s surface
tsunamis can be detected using our human senses
recognize a tsunami's natural signs through:
feel
hear
see
run
two kinds of tsunami: local tsunami & far field or distant tsunamis
storm surges -are wind generated waves on the surfaces of the sea
local tsunami - confined to coasts within a hundred kilometers of the source usually landslide or a pyroclastic flow.It can reach the shoreline within 2-5 minutes
far field or distant tsunamis -can travel from 1 to 24 hours before reaching the coast of the nearby Countries. These tsunamis mainly coming from the countries bordering Pacific Ocean like Alaska in USA and