GeologicalHazards are those geologic conditions that present a risk to life (injury or death), of substantial loss or damage to property, or damage to the environment
Natural disasters like earthquakes and tsunamis are linked to platetectonics, the grinding movement of pieces of Earth's crust
With the present state of technology, most geologic events cannot be prevented or even predicted with any precision
Landslides are an exception: they can often be prevented
Areas prone to such events can be identified as earthquakefaultzones, activevolcanoes, and coastalareas susceptible to tsunamis
Geological Hazards
Earthquake Hazards
Volcanic Hazards
Landslide Hazards
Earthquake
also called temblors are weak to violent shaking of the ground produced by the sudden movement of rock materials below the earth's surface
Focus
Point inside the earth where the earthquake started, sometimes called the hypocenter
Epicenter
Point on the surface of the earth directly above the focus
Magnitude
Proportional to the energy released by an earthquake at the focus, calculated from earthquakes recorded by a seismograph, represented by Arabic numbers
Intensity
Strength of an earthquake as perceived and felt by people in a certain locality, a numerical rating based on the relative effects to people, objects, environment, and structures, represented by Roman numerals
In the Philippines, the intensity of an earthquake is determined using the PHIVOLCSEarthquakeIntensityScale (PEIS)
Types of earthquakes
Tectonic earthquakes
Volcanic earthquakes
Tectonic earthquakes
Produced by sudden movement along faults and plate boundaries
Volcanic earthquakes
earthquakes induced by rising lava or magma beneath active volcanoes
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) is a service institute of the Department of Science and Technology (DOST) that is principally mandated to mitigate disasters that may arise from volcanic eruptions, earthquakes, tsunami and other related geotectonic phenomena
Earthquake Hazards
Ground Rupture
Ground Shaking
Liquefaction
Earthquake-induced Landslide
Tsunami
Ground Rupture
Deformation on the ground that marks the intersection of the fault with the earth's surface
Ground Shaking
Disruptive up, down and sideways vibration of the ground during an earthquake, can cause damage or collapse of structures and consequently hazards like liquefaction and landslide
Liquefaction
Phenomenon wherein sediments, especially near bodies of water, behave like liquid similar to a quicksand, causing sinking and/or tilting of structures above it, sandboils, and fissuring
Sand boils
Created in the January 6, 2001Bhuj, India earthquake (moment magnitude 7.6), caused by soil losing its internal cohesion during strong shaking
Earthquake-induced Landslide
Down slope movement of rocks, solid and other debris commonly triggered by strong shaking, causing erosion, burial and blockage of roads and rivers
Tsunami
Series of waves caused commonly by an earthquake under the sea, causing flooding, coastal erosion, and drowning of people and damage to properties
2011Japanearthquake and tsunami
Magnitude 9.0 earthquake struck off Japan's northeastern shore, generating enormous tsunami waves that spread across miles of shoreline, climbing as high as 130 feet (40 meters), tearing apart coastal towns and villages, carrying ships inland, and damaging the Fukushima DaiichiNuclear Power Plant
A vent, hill or mountain from which molten or hot rocks with gaseous material have been ejected, also craters, depressions, hills or mountains formed by removal of pre-existing material or by accumulation of ejected materials
The Philippines sits on a unique tectonic setting ideal to volcanism and earthquake activity, situated at the boundaries of two tectonic plates - the Philippine Sea Plate and the Eurasian plate - both of which subduct or dive beneath
The 2011 earthquake recorded in Japan was the most powerful earthquake recorded to date. Its epicentre was located approximately 72km off the northeast coast of Honshu (the largest island of Japan) and was so powerful it was later estimated that the Earth had been shifted on its axis by between 10 and 25cm, while Honshu was moved 2.4m east.
Geological Hazards
Earthquake Hazards
Volcanic Hazards
Landslide Hazards
Volcano
A vent, hill or mountain from which molten or hot rocks with gaseous material have been ejected
Also craters, depressions, hills or mountains formed by removal of pre-existing material or by accumulation of ejected materials
The Philippines sits on a unique tectonic setting ideal to volcanism and earthquake activity. It is situated at the boundaries of two tectonic plates – the PhilippineSeaPlate and the Eurasian plate – both of which subduct or dive beneath the archipelago along the deep trenches along its east and west seaboard.
RingofFire
also called Circum-Pacific Belt, a path along Pacific Ocean characterized by active volcanoes and frequent earthquakes.
length is approximately 40,000 kilometers (24,900 miles).
traces boundaries between tectonic plates— Pacific, Juan de Fuca, Cocos, Indian-Australian, Nazca, North American, and Philippine Plates.
Seventy-five percent of Earth's volcanoes—more than 450 volcanoes—are located along the Ring of Fire.Ninety percent of Earth's earthquakes occur along its path, including the planet's most violent and dramatic seismic events.
Volcanic hazards directly associated with eruption
Lavaflow
Tephra fall or ashfall and ballisticprojectiles
Pyroclasticdensity currents or PDCs (pyroclastic flow, pyroclastic surge, base surge)
Lateralblast
Volcanicgas
Volcanic hazards indirectly associated with eruption
Lahar, flooding
Debris avalanche, landslide
Volcanic tsunami
Grounddeformation (subsidence, fissuring)
Secondary explosion, PDCs and ashfall
Volcano classification in the Philippines
Active Volcanoes
Potentially Active Volcanoes
Inactive Volcanoes
Landslide
The mass movement of rock, soil, and debris down a slope due to gravity. It occurs when the driving force is greater than the resisting force. It is a natural process that occurs in steep slopes. The movement may range from very slow to rapid. It can affect areas both near and far from the source.