A Japanese word pronounced as "soo-nah-me" which means "wave in the harbor"
Tsunamis are sometimes misnamed as "tidal waves"
Tsunami
A massive ocean wave triggered by underwater earthquakes or volcanic activity, posing a serious threat by flooding coastal areas with powerful and destructive force
How a tsunami is formed
1. Faults are seen not solely on land but also under the ocean
2. When a fault at the ground of the ocean swiftly moves, the water over it can be stirred
3. An abrupt force from an underwater fault can create a wave named a tsunami
Earthquakes
If the earthquake occurs in the ocean, it can push up powerful waves, known as tsunamis
The sudden upward or downward movement of the seafloor during an earthquake creates large tsunami waves
Notallfault movement underneath the sea will create a tsunami
Faults that move during a horizontal direction or sideways will not result in tsunami
Causes of tsunami
Earthquake
Icefalls
Volcaniceruptions
Heavyrainfall
Cosmicimpacts
Landslides
Earthquake as a cause of tsunami
The sea floor abruptly deforms and displaces the sea water lying above
Large vertical movements of earth's crust can occur at plate boundaries which are called "faults"
Volcaniceruptions as a cause of tsunami
Volcanic eruptions create disturbance undersea by creating great force and thus generate tsunami
Icefalls as a cause of tsunami
If their heightislargerthantheirwidth, they can be unstable following break off and roll over, potentially creating a giant wave
Heavy rainfall as a cause of tsunami
Heavy rainfall cause overflow of water and generate tsunamis
Cosmic impacts as a cause of tsunami
When a meteorite or an alien force impact the ocean area disturbing the water from above, tsunami is caused
Landslides as a cause of tsunami
When there is large landslide in mountains in the sea, the tsunami is caused and effect fell at bays
72% of tsunamis are generated by earthquakes
A disturbance that displaces a large water mass from its equilibrium position can cause a tsunami
Our continent for the past many years has been only one continent called Pangaea
The continents are above the tectonic plates that are moving
Layers of the Earth
Crust (thinnest layer)
Mantle (thickest layer)
Core (innermost layer, made up of solid, liquid, iron, and nickel, classified into inner core and outer core)
Tectonic plates
Massive, irregularly shaped slabs of solid rock, generally composed of both continental and oceanic lithosphere
Plate boundary
A three-dimensional surface or zone across which there is a significant change in the velocity (speed or direction) of motion of one lithospheric plate relative to the adjacent lithospheric plate
Earthquake
The shaking of the surface of Earth due to the sudden release of energy in the Earth's crust
Fault
Cracks in Earth's crust between two huge plates, a fracture or zone of fractures between two block of rocks, allowing the blocks to move relative to each other
Parts of a fault
Footwall (block positioned under the fault plane)
Hanging wall (block above the fault plane)
Fault plane (planar surface along which there is slip during an earthquake)
Dip-slip fault
Inclined fractures where the blocks have mostly shifted vertically, if the rock mass above an inclined fault moves down it is a normal fault, if the rock above the fault moves up it is a reverse fault
Normal fault
Develops in areas where the land is pulling apart or stretching, one block of land slips downward in relation to the other block
Reverse fault
Occurs in areas undergoing compression
Strike-slip fault
Fault plane is usually vertical, with lateral or horizontal forces carrying the sides past each other
Oblique-slip fault
Caused by a combination of shearing and tension or compressional forces, has both dip-slip (normal or reverse) and strike-slip components
Active fault
Known to have recently generated earthquakes within the last 10,000 years, and may still continue to generate earthquakes
List of active faults
Marikina Valley Fault
Western Philippine Fault
Eastern Philippine Fault
Southern of Mindanao Fault
Central Philippine Fault
Inactive fault
Do not show signs of ever having generated an earthquake in the last 10,000 years, but may possibly still generate an earthquake in the future