Composed of the crust and upper mantle, in constant but very slow motion
Plate Tectonics Theory
The entire lithosphere of the Earth is broken into numerous segments called Plates, continuously moving
Major Plates
Pacific Plate
North American Plate
South American Plate
Eurasian Plate
African Plate
Antarctic Plate
Indo-Australian Plate
Minor Plates
Philippine Plate
Nazca Plate
Scotia Plate
Cocos Plate
Caribbean Plate
Arabian Plate
Anatolian Plate
Continental crust
Thicker but less dense
Oceanic crust
Thinner but denser
Epicenter
Location on the Earth's surface directly above the focus of an earthquake
Focus
Exact site of the origin of an earthquake below the epicenter
Seismic waves
Primary (P-waves)
Secondary (S-waves)
Long Surface Waves (L-waves)
waves and S-waves travel into the Earth's interior while L-waves travel on the surface
The farther the recording instrument is from the focus, the greater the difference in arrival times of the first P-wave compared to the first S-wave
The difference in the arrival time will tell us the distance of the earthquake's focus from the seismic recording station, but not the direction
Triangulation Method
Use distance information from three seismic stations to locate the earthquake's epicenter
Pacific Ring of Fire
A long chain of volcanoes and other tectonically active structures that surround the Pacific Ocean, one of the most geologically active areas on Earth
The Philippines is situated along the Pacific Ring of Fire
Disaster & Emergency Preparedness
Make a plan
Build a kit
Be informed
Plate Boundaries
The lines at the edges of the different pieces of lithosphere
Convergent Plate Boundary
Two plates move toward each other, also known as "destructive boundary"
Types of Convergent Plate Boundary
Continental-Oceanic Convergence
Oceanic-Oceanic Convergence
Continental-Continental Convergence
Continental-Oceanic Convergence
Oceanic crust bends down into the mantle through Subduction, leading edge melts forming a continental volcanic arc parallel to the trench
Oceanic-Oceanic Convergence
Older oceanic plate subducts, leading edge melts forming a volcanic island arc parallel to the trench
Continental-Continental Convergence
Two continental plates collide and buckle up forming mountain ranges, no subduction or trench formation
Many parts of the Philippines originated from oceanic-oceanic convergence
About 40-50 million years ago, India and Eurasia collided to begin the formation of Himalayas
Divergent Plate Boundary
Plates separate and move apart in opposite directions, also known as "constructive boundary"
Divergent Plate Boundary
Molten rocks (magma) rise from the Earth's mantle to the surface, solidifying to create new oceanic crust or seafloor
The Mid-Atlantic Ridge is the longest mountain chain on Earth, running along the Atlantic Ocean floor
The Red Sea contains some of the world's hottest and saltiest seawater, connected to the Mediterranean Sea via the Suez Canal
Transform Fault Boundary
Plates slide past or slip past each other, creating a crack or undersea canyon/linear fault valley
The San Andreas Fault is a continental transform fault that forms the tectonic boundary between the Pacific Plate and the North American Plate
Hot Spot
Concentration of heat in the mantle capable of creating magma
As the Pacific Plate moves, different parts of it will be on top of the mantle plume, creating a trail of volcanic islands and seamounts across the Pacific Ocean floor
Convection Current
Heat-transfer process that involves the movement of energy from one place to another, causing hot fluid to rise and less hot fluid to sink
Convection currents happen in the mantle, due to the heat generated by the core from the decay of radioactive elements
Volcano growth and death
1. Repeated over many millions of years
2. Leaves a long trail of volcanic islands and seamounts across the Pacific Ocean floor
Convection current
A heat-transfer process that involves the movement of energy from one place to another
Convection currents
Move a fluid, gas particles, or molten rocks
Due to differences in the densities and the temperature of a specific gas or fluid
Hot fluid tends to rise as it expands, less hot fluid tends to sink as it contracts
Convection
One of the kinds of heat transfer, the other two are radiation and conduction
Convection current in the mantle
1. Mantle is the second inner layer of Earth, made up of mostly hot rocks and magma
2. Heat generated by the core due to the decay or breakdown of radioactive elements