Tags & Description
Fissure
elongated fracture or crack on Earth’s crust from which lava erupts
Conduit
passageway through which magma travels to reach Earth’s surface
Vent
opening where volcanic materials are released
Crater
bowl-shaped depression at the top of the volcano where the vent is located
Flank
side of the volcano
Magma chamber or reservoir
underground compartment where the magma is stored
STRATOVOLCANO (COMPOSITE CONE VOLCANO)
The most dangerous volcanoes
SHIELD VOLCANO
Formed by loose and fluid lava that flows over each other. The magma of a shield volcano contains lower amounts of dissolved gases and silica
CINDER CONE
Volcanic eruptions are short-lived and appear like a wild fountain show of fiery lava spewed high in the air
Caldera complex
is a depression formed at the summit of shield volcanoes.
Lava dome
mounds of lava formed after a volcanic eruption.
Submarine volcanoes
these are volcanoes on the ocean floor and are formed through collision of oceanic plates
Glacial volcanoes
are volcanoes that are overlain by glaciers. Examples include the Alaskan volcano.
Blasts
these are hot bursts of trapped gases that push their way through solid barriers and rapidly into the atmosphere
Dome growth
this refers to a mound of lava that grows inside the crater, called a cryptodome. If it grows outside the volcano, it is called an exodome
Gases
water vapor, hydrogen sulfide, sulfur dioxide, hydrogen chloride, hydrogen fluoride, hydrogen and carbon dioxide. Other gases include nitrogen, methane, argon, and helium
Lahar
also called as mudflow or flow of volcanic debris. Can be classified as primary (from the eruption) and secondary (because of heavy rainfall)
Lava flow
refers to the molten rocks that move down the slope of volcanic vents. The viscosity of the lava and the steepness of the volcano slope can influence the rate of lava flow
Pyroclastic flow
this refers to glowing hot material that moves down the slope of an erupting volcano and comes in contact with the surface. Pyro (fire) and clast (broken) are rock fragments spewed during volcanic eruptions
Pyroclastic surges
these are volcanic materials of gases, ash, rock fragments, and water extruded above the ground
Tephra falls
these may consist of combinations of pumice, scoria (basalt), thick rock fragments and crystals with tephra particles
Tsunami
are series of sea waves caused by displacement of large volumes of water because of an underwater earthquake or volcanic eruption
Ash plume
the cloud of ash that comes out of the crater and can travel not just to nearby communities but also to nearby countries
HAWAIIAN
is the least violent type, with highly fluid or runny lava flowing out several vents.
STROMBOLIAN
is violent, featuring continuous ejection of magma and gas.
VULCANIAN
a thick, viscous magma flows around the vent as solid lava and dust are ejected.
PLINIAN
the most violent and explosive type of eruption which is caused by the buildup of viscous magma and dissolved gas.
Geology
is a branch of Science that deals with the study of the physical and historical aspects of Earth.
Geochemistry
chemical composition and changes of materials that make up Earth
Geophysics
behavior of Earth in response to physical forces
Mineralogy
chemical composition and structure of minerals
Petrology
composition and origin of rocks
Paleontology
fossils or remains of organisms
Paleography
geologic maps and location of land masses that may have been lost
Stratigraphy
layers of Earth’s bedrock, which is essentially that of soil, sand, pebbles, stones and rocks
CRUST
the solid rock layer that makes up the outermost portion of the Earth.
MANTLE
below the crust which stretches to a depth of about 2890 km before reaching the core.
CORE
the outer core extends 2266 km while the inner core is 1220 km thick and more than 6200 km below the Earth’s layers.
Tectonic plates:
continental and oceanic
Continental plates
thicker, lighter, and are made up of granitic rocks
Oceanic plates
dense and are made up of basaltic rocks
Convergent boundaries
tectonic plates move against or toward each other.
Oceanic-continental convergence
an oceanic crust may be consumed and brought down through subduction below the continental plate.
Oceanic-oceanic convergence
one oceanic crust is subducted under another oceanic crust to form deep ocean trenches.
Continental-continental convergence
no subduction occurs.
Divergent boundaries
tectonic plates move away from each other.
Transform boundaries
tectonic plates slide horizontally past each other and form faults.
IGNEOUS
are rocks formed out if magma that has cooled down.
SEDIMENTARY
are rocks that consist of previously loose materials, such as sand and soil, which have settled down and are compacted by the weight of overlying sediments and water to make them solid.
METAMORPHIC
are rocks formed when sedimentary rocks or igneous rocks are subjected to enough heat and pressure to change their mineralogical and chemical characteristics
Panning
for gold in a river or a stream is a form of mining.
Smelting
uses heat and chemical agents to chemically separate the desired metal from the other components of the ore
Gold
most valuable metal in the Philippines.
Philippine jade
is not of common variety.
Coal
form of fossil fuel, which refers to organic materials (remains of plants and animals) that have experienced physical and chemical transformations over a long period of time.
Mine tailings
materials that remain after extraction of ore minerals