ITO NA YON Flashcards
(24 cards)
The perceptible shaking of the surface of the Earth, resulting from sudden release of energy in the Earth’s crust that creates seismic waves
Earthquake
Is the outermost layer of the Earth is broken into pieces, which are in continuous motion.
Plates
How do plates move?
plates at the Earth’s surface move because of the intense heat in the Earth’s core that causes molten rock in the mantle layer to move in a convection cell pattern. As the warm material rises, cools, and sinks down, it warms up again and rises, pushing the plates and causing them to move.
Types of Natural Earthquakes
Tectonic Earthquakes
Volcanic Earthquakes
Earthquake produced by sudden movement along faults and plate boundaries.
Tectonic Earthquakes
Earthquakes produced by movement of magma beneath volcanoes.
Volcanic Earthquake
WHAT IS THE DIFFERENCE BETWEEN INTENSITY AND MAGNITUDE?
intensity focuses on the strength or force of something at a specific point, while magnitude looks at the overall size or scale of that thing.
it refers to the disruptive up and down and sideways motion experienced during an earthquake.
Ground Shaking
HOW EARTHQUAKE VIBRATIONS GENERATED?
Most natural earthquakes are caused by sudden slip along fault zone.
is a fracture on which one body of rock slides past another.
Fault
TYPES OF FAULT
Normal Fault
Reverse Fault
Right-Lateral Strike-Slip Fault
Left-Lateral Strike-Slip Fault
Types of Seismic Waves (Body Waves)
Primary waves
Secondary Waves
Types of Seismic Waves (Surface Waves)
Love Waves
Rayleigh Waves
The fastest seismic waves that can travel through solids, liquids, and gases.
Primary Waves
Travel through Earth’s interior at about half the speed of primary waves, can travel through solids but not liquids of gases.
Secondary Waves
seismic waves that move along Earth’s surface, cause the largest ground movements and the most damage
Surface Waves
How is Ground Shaking Measured?
Velocity
Acceleration
Frequency
Duration (how long the shaking continues)
The creation of new or the renewed movement of old fractures, oftentimes with two blocks on both side moving in opposite direction
Ground Ruptures
Loosely packed/water-logged sediments at/or near the ground surface lose their strength in response to strong ground shaking
Liquefaction
Types of Liquefaction Features
Flow Failure
Lateral Speed
Ground Oscillation
Loss of bearing strength
Considered the most dangerous types of ground failure due to liquefaction
Flow Failure
Blocks or broken pieces of the flat or very gentle grounds above liquefied zone move laterally.
Lateral Speed
Due to the flat or nearly flat slope, the ground is unable to spreads and instead oscillates like a wave. Water and wet sand are ejected through the fissures that form conical-shape mounds of sand at the surface.
Ground Oscillation
Loss of strength of sediments resulting in tilting of houses and floating of buoyant that are anchored on the liquefied structures zone.
Loss of bearing strength