A weak point in the tectonic plate where the pressure inside the crust is released
Focus
The area inside the Earth where an earthquake starts is known as the focal point. It is centered on the portion of the fault that has the greatest movement
Epicenter
The point at the Earth's surface directly above the focus. During an earthquake, the strongest shaking occurs at the epicenter
Magnitude
Measures the energy being released from the origin of the earthquake
Seismograph
Instrument measures the magnitude
Richter Magnitude Scale
Measures the quantity of seismic energy released by an earthquake
Intensity
The strength of the trembling made by the earthquake at a place
Mercalli Scale
Determines the intensity of an earthquake, which varies depending on where you are
Active faults
Areas along which displacement is expected to occur. Since a shallow earthquake produces displacement across a fault, all shallow earthquakes occur on active faults. These are considered to be geologic hazards
Inactive faults
Areas that can be identified but which do not have earthquakes
Earthquake
Shaking off the ground caused by the movement of tectonic plates
Mostly occurs along the fault line
Can cause great damage to properties and life loss
Various Potential Earthquake Hazards
Ground Shaking
Ground Rupture
Liquefaction
Ground Subsidence
Tsunami
Landslide
Ground Shaking
Vibration of the ground; triggers liquefaction & landslides
Ground Rupture
Offset of the ground
Liquefaction
Sand/soil & groundwater mixed
GroundSubsidence
Sinking/settling of the ground surface
Tsunami
Giant sea waves generated by an earthquake w/ a magnitude greater than 7.0
Landslide
Down a slope
Deadliest: Indian Ocean (Sumatra Indonesia); Casualties: 350,000; Year: 2004
Recognizing the Natural Signs of an Impending Tsunami
1. Feel - shaking; magnitude greater than 7.0
2. See - unusual sea-level fluctuation
3. Hear - loud roaring
Earthquake Hazard Map
A special type of map that shows the possible physical & geographical effect of an earthquake w/in a particular area/region; known as ground shaking hazard map
Ground shaking
Caused by the release of stored energy in the lithosphere that was released
Its strength is measured in terms of velocity, acceleration, frequency, and duration
Primary Volcanic Hazards (Direct)
Lava Flow
Pyroclastic Density Current
Tephra Falls
Volcanic Gas
Lava Flow
Molten volcanic rock
Pyroclastic Density Current
Mixed volcanic rock fragments & hot gasses
Pyroclastic flow
Contact with ground
Pyroclastic surge
Move above ground
TephraFalls
A shower of pyroclastic materials
Tephra Falls
Ash - less than 2 mm in diameter
Lapilli - 2-64 mm in diameter
Blocks - greater than 64 mm in diameter
Volcanic Gas
Gas components of volcanic rocks that reacted with other elements in the environment which results to harmful chemicals
Secondary Volcanic Hazards (Indirect)
Lahar
Debris Avalanches
Tsunami
Lahar
Mud flow
Primary (Hot Lahar)
Caused by pyroclastic materials reaching watersheds/eruption of a crater lake
Secondary (Cold Lahar)
Caused by heavy rains
Debris Avalanches
Result from the built up of volcanic debris
Lava Flow
Least dangerous
Speed of 3km/day to 50km/h
Speed is determined by the lava's viscosity (resistance to flow), density, & local area's land features
Effusive eruption
Tephra Fall
Plinian eruption - eruption column
Lapilli & blocks will fall relatively near the volcano
Ashes reaches father places
Large amount of ash is called ash fall
Pyroclastic Density Current
Verydangerousphenomenon
Reach a temperature around 700 C
Travel with a speed of 100 km/h
Cause asphyxiation (death by suffocation) & incineration (death by burning)