Observablefacts arising due to volcanicactivity such as eruption, with potentialthreat and directimpact on humans, animals, properties, infrastructure, tourism, and political stability
Types of volcanoes
Cindercone volcano
Compositecone volcano
Shield volcano
Volcanic eruption
Leads to different hazards such as Ballistic projectiles, Ash fall, Pyroclastic flows, Lava flows, Volcanic gases, Debris Avalanche or Volcanic landslide, and Tsunami
Cinder cone volcano
Simplest and most common type
Built from ejectedlavafragments
Steep slope, widecrater
Most abundant of the three major volcano types
Ballisticprojectiles
Rock fragments ejected from volcano'smouth, comparable to cannonballs, reaching up to 5 km or 3mi
Cinder cone volcanoes
Paricutin Volcano of Mexico
Mauna Kea of Hawaii
Ashfall or tephrafall
Minute volcanic particles such as pulverizedrock, minerals and silicon, formed during explosive volcanic eruption
Composite cone volcano
Tall, symmetricallyshaped, with steepsides
Large, nearly perfect sloped structure
Formed and built up by many layers of alternating solidification of lava and pyroclasticdeposits
Pyroclastic flows
Highly-densitymix of hot lavablocks, pumice, ash and volcanicgases, moving at very highspeed down volcanic slopes
Composite cone volcanoes
MountFuji of Japan
Mt. Mayon Volcano of Philippines
Lavaflows
Streams of moltenrocks poured or oozed from an erupting vent
Shield volcano
Broad volcano with sloping sides
Formed mainly out of runny lava
Formed by the accumulation of lava that oozes out from the volcano
Broad, slightlydomed structure that resembles a warrior'sshield
Volcanic gases
Gases dissolved in magma that provide the driving force for volcanic eruptions, released into the atmosphere as pressure decreases
Shield volcanoes
Mauna Loa of Hawaii
Erta Ale of Ethiopia
Debris avalanche or volcanic landslide
Massive collapse of a volcano, usually triggered by an earthquake or volcanic eruption
Classifications of volcanoes
Active
Inactive
Tsunami
Seawaves or wave trains generated by sudden displacement of water, such as during undersea eruptions or debrisavalanches
Lahar
Mixtures of volcanicwater and rockfragments that rush down volcano slopes and into surrounding valleys, often triggered by heavy rains or earthquakes
Active volcano
Has a record of eruption within the last 600 years or erupted 10,000 years ago
Volcano which is either erupting or is likely to erupt in the future
Active volcanoes
Kilauea
Mauna Loa
Mauna Kea
Lightning strikes
Occur during volcanic eruptions due to friction between ash, rockfragments, steam and gases in the eruptioncloud
Inactive volcano
Otherwise known as "dormant" volcanoes
Have not erupted for the last 10,000 years
Physical form is being changed by weathering and erosion
Expected to erupt again in the future
Potential volcanic hazards are harmful because they directly affect humans, animals, properties, infrastructure, tourism, and political stability
Inactive volcanoes
MountFuji of Japan
MountKilimanjaro of Tanzania, Africa
Volcanichazards threaten human health through impacts, respiratory issues, contamination, and destruction
Factors affecting volcano eruption
Magma'stemperature
Magma'schemicalcomposition
Amountofdissolvedgasesinmagma
Viscosity
Property of a material's resistancetoflow
Described as the liquid's thickness and stickiness
The more viscous and thicker the material, the greater its resistance to flow
Temperature of magma
Viscosity decreases as temperature increases
Composition of magma
Magmas with high silica content are more viscous than those with low silica content
Magma with less silica content is relatively fluid and travels far before solidifying
Lava with less silica content can travel a great distance and forms a thin sheet of lava
Composition of magma
Lava with low amount of gas and highsilica content is veryviscous and does not flow out as it rises, forming a columnarplug in the vent
Lava with low amount of gas as it rises has high viscosity that it piles up at a vent resulting in a dome
Types of volcanic eruption
Magmaticeruption
Phreatomagmaticeruption
Phreaticeruption
Magmatic eruption
Produces juvenileclasts during explosive decompression from gas release
Includes the ejection of lava or tephra from a magma source within the earth
Generally described as being effusive or explosive
Phreatomagmaticeruption
Violenteruption due to the contact between water and magma
Results in a large column of very fine ash and high-speed and sideways emission of pyroclastics called base surges
Driven by the thermal contraction of magma when it comes in contact with water
Phreatic eruption
Stream-driven eruption as hot rocks come in contact with water
Short lived, characterized by ash columns but may be an onset of a larger eruption
Driven by the expansion of steam
The Philippines ranks second in the world's production of geothermalenergy
14.4% of the Philippines' total power generation is produced from geothermalenergy