Weak to violent shaking or trembling ground caused by the sudden movement of rocks below
Earthquakeorigin
Originate from tectonicplateboundary
Crust
Composed of solid materials
Crust
Made from plates (tectonic plates)
There are about 20 plates along the surface of earth that move slowly
Movement is brought about by the mantle
Crust together with the upper mantle from the lithosphere
Plates under the ocean are called oceanic plates and the rest are continental plates
Earthquakeoccurrence
1. When two adjacent tectonic plates bump, slide, or slip
2. When pressure slowly builds up and the force is strong enough, these rocks underground will suddenly break or slip
Faults
Lines or cracks in earth surface that are caused by the movement of the plates
Types of faults
Normal
Reverse
Strike-slip
Types of earthquakes
Tectonic
Volcanic
Collapse
Explosion
Tectonic earthquake
Caused by suddenmovements along the tectonic faults and plate boundaries
Volcanicearthquake
Caused by volcanicearthquakes such as rising lava etc.
Collapseearthquake
Smallearthquakes that occur in caves
Explosionearthquake
Caused by nuclearexplosions or chemical materials
Seismology
Study of seismic waves or energy waves
Seismologists
Scientists that study earthquakes
Seismologists
Use seismograph to detect and record earthquakes
Seismogram
Tells how large the seismic waves are
Types of seismic waves
Primary waves (fastest)
Secondary waves (only move through solids)
Surface waves (last to reach the seismograph)
Magnitude
Refers to the size of the seismic waves, measured using the moment magnitude scale (MMS also called Richter scale) represented by Hindu numerals (0-9)
Intensity
Strength of the earthquake based on the observed effect, represented by roman numerals (e.g, I,II,IV,IX)
Aftershock
Smaller earthquakes within one or two lengths
Foreshock
Cannot be called a foreshock unless a larger earthquake in the same location happens
July272019 - Batanes struck by a 5.9 magnitude earthquake with a 5.4 foreshock
PHIVOLCS - Philippine institute of volcanology and seismology - operates 101 seismic monitoring stations all over the country
DRC - data receiving center - determines the earthquake's magnitude
Volcaniceruption
A phenomenon
Volcano
Opening in a earth's crust, erupts when pressure builds up, can be a hill or a mountain where hot molten rocks with gaseous materials are ejected
Philippines is situated on the boundaries of two tectonic plates - Philippine sea plate and Eurasian plate
Types of volcanoes
Cinderconevolcanoes
Compositevolcanoes
Shieldvolcanoes
Lavadomevolcanoes
Cinderconevolcanoes
Have circular or oval cones made up of fragments or particles, cannot get more tall than 300 meters
Compositevolcanoes
Have steepsides although they are shaped like cones, can be as tall as 2.4kilometers
Shieldvolcanoes
Look like a bowl or a shield with long gentle slopes made from lava, lava that flows from these volcanoes is called flood basalts
Lavadomevolcanoes
Formed by thick lava which makes a steep-sided mound as lava piles up near the vent
Activevolcano
Recently erupted or has had at least one eruption for the last 10,000 years
Active volcanoes in the Philippines
Mt.Kanlaon in Negrosislands
Mt.Pinatubo in Zambales
Taal volcano in Batangas
Mt. Mayon in Albay Bicol (erupted 48 times, first recorded in 1616, worst eruption on Feb 1 1814 killed 1,200 people and destroyed Cagsawa Church)
Dormant or inactive volcano
Once an active volcano that has not erupted for 10,000 years but still has the potential to erupt again
Extinct volcano
Volcano is no longer expected to erupt again
PHIVOLCS has been monitoring 23 active volcanoes in the Philippines which may increase in numbers because the country is positioned at the Pacific Ring of Fire which is a 40,000-circle of interconnected fault lines around the Pacific Ocean
Earthquakes and Volcanic eruptions happen frequently in the Pacific Ring of Fire area, which has 452 volcanoes, making up 50% of the world's active and dormant volcanoes, and 90% of the world's earthquakes happen along this area
Volcanologist
Scientists who study volcanoes and their activities, the name of their study is volcanology
Platetectonictheory
Explains the phenomena of volcanoes and earthquakes, convection in the mantle causes the movement of the plates, when the continents collide, with one plate going under the other, it may form a volcano or a mountain range