Philippine Institue of Volcanology and Seismology (PHIVOLCS) is the government agency that monitors and studies volcanoes and earthquakes.
magma inside the volcano has high temperature
there are 3 general volcanic types according to the shape of their cones, namely, shield volcano, cinder cones, composite cones
the external parts of a volcano are summit, slope, and base
at the summit, there is an opening which may either be a crater or a caldera
a crater is a funnel-shaped opening at the top of a volcano
a caldera is formed when a part of the wall collapses following an explosive eruption
taal has 47 craters while mayon only has one
viscosity is the property of the material's resistance to flow
the viscosity of magma decreases with temperature
the higher the temperature of a magma is, the lower its viscosity is
magmas with high silica content are more viscious than those with low silica content
the loss of gases makes magma more viscious, forming a dome or a columnar
lava with less silica content has low viscosity that it can travel a great distance, forming a thin sheet of lava
lava with high silica content is too viscious to travel far, and tends to break up as it flows
lava with low amount of gases and high silica content is very viscious and does not flow out at all as it rises, forming a columnar plug in the vent
lava with low amount of gas as it rises has high viscosity that it piles p at a vent resulting in a dome
there are 5 types of volcanic eruptions namely phreatic or hydrothermal, phreatomagmatic, strombolian, vulcanian, and plinian
phreatic or hydrothermal eruption occurs when water from underground reservoirs heats up and turns into steam which causes an explosion
phreatomagmatic eruption happens when hot rock meets groundwater causing an explosive reaction
strombolian eruption is characterized by small fountains of lava ejected intermittently from vents
plinian eruption is characterized by large amounts of ash being thrown into the air
vulcanian eruption is characterized by violent explosions producing dark clouds of ash and smoke
shield volcanoes are formed when magma rises through cracks in the crust and cools
cinder cones are built from ejected fragments, they have a steep slope, wide crater and are the most abundant of the three major volcano types
composite cones or stratovolcanoes are large, neraly perfect sloped structure formed from alternate solidification of both lava and pyroclastic deposits
dearalc, it is a volcanic crater that is formd when a part of the wall of the crater collapses following an explosive eruption
magma are molten rocks inside the earth
lava, magma that has been ejected out of a volcano
mauna loa is an example of shield volcano
paricutin is an example of cinder cone
mayon is an example of composite or stratovolcano
active volcano that has atleast one record of eruption during the past 10,000 years
a dormant volcano is an active volcano that is not erupting but supposed to erupt again
there are 24 active volcanoes
iraya, smith, babuyan claro, didicas, and cagua are examples of an active volcanoes
inactive volcano are also called extinct or sleeping volcanoes. it is one that could erupt but has not erupted for more than 10,000 years
anilao hill, batuan, uruit, tamburok, cabaluyan are examples of inactive volcanoes
plate tectonics is the theory that explains how the continents were formed and moved around the world