A vent or opening that expels molten rock or magma from the interior of Earth
Shield Volcano
Mountain with broad, gently sloping sides and nearly circular base, formed when layers of basaltic lava accumulate during nonexplosive eruptions
Hotspots are regions in Earth's mantle due to high-temperature mantle plumes that rise toward the surface, melting rock and forcing magma towards the crust. The magma then flows upward to Earth's surface as lava
Fissure Volcano
Volcanic vent through which lava erupts without explosive activity, lava spreads to form huge pools which then cool and solidify
Majority of volcanoes in the world form along the boundaries of Earth's tectonic plates, which are massive expanses of our planet's lithosphere that continually shift, bumping into one another
Calderas are formed when the summit or the side of the volcano collapses into magma chambers, resulting in collapsed walls and cliffs above the surface of water
Cinder Cone Volcano
Steep conical hill of volcanic debris with a bowl-shaped center, eruptions from a single opening expel rock fragments called scoria or cinders
Type of Volcano according to appearance
Fissure Volcano
Cinder Cone Volcano
Composite Volcanoes
Shield Volcano
Composite Volcanoes
Majestic volcano with tall symmetry, formed when layers of volcanic fragments alternate with lava, also known as strato volcano
Formation of Volcanoes
Occurs along the boundaries of Earth's tectonic plates where one plate often plunges deep down below the other in a subduction zone
Shield Volcano
A mountain with broad, gently sloping sides and a nearly circular base, formed when layers of basaltic lava accumulate during nonexplosive eruptions
Types of volcanic fragments
Volcanic ash
Cinders
Lava
Scoria
Ash flow deposits
Dormant Volcanoes may have the capacity to erupt later on, with long intervals between their last eruption and the latest one
Lapillus
Volcanic fragments with sizes ranging from 2mm to 64 mm, come in different shapes like teardrop, dumbbell, or spheroid, made up of molten or semi-molten lava ejected from a volcanic eruption
Volcanic Ash
Very fine-grained fragments of pulverized rocks, minerals, and volcanic glass, formed when dissolved gases in magma expand and escape violently into the atmosphere
Formation of layers in stratovolcanoes
Stratification
Inactive Volcanoes are those that have not erupted in history but still have the potential to do so
Lahar
Also known as mud flow or debris flow, mixtures of volcanic debris and water, classified into primary or hot lahars from volcanic eruption and secondary or cold lahars due to heavy rainfall
Volcanic Bombs
Masses of molten rocks larger than 65 mm, formed when a volcano ejects viscous fragments of lava with a hard outer rock shell and liquid inside
Stratovolcano
Also known as strato volcano, formed by layers of volcanic fragments such as volcanic ash and cinders alternating with lava
Active Volcanoes are presently erupting or have erupted in the last 10,000 years, expected to erupt sooner rather than later
Pyroclastic materials
Volcanic ashes
Volcanic bombs
Volcanic blocks
Lapillus
Lahar
Volcanic Blocks
Solidified fragments greater than 64 mm in diameter, ejected from explosive volcanic eruptions, consisting of broken pieces of the volcano's edifice
Composite Volcano, also known as stratovolcano, is tall and symmetrically shaped, formed by layers of volcanic fragments alternating with lava
Volcanoes on Earth are not randomly distributed. Around 80% of volcanoes are located along convergent plate boundaries, 15% along divergent plate boundaries, and about 5% far from plate boundaries. Volcanoes far from plate boundaries form as a result of hotspots
Calderas formed
Calderas are formed when the summit or the side of the volcano collapses into the magma chamber, creating cliffs that stand several meters above the surface of water
Cinder cone Volcano has a steep conical hill of volcanic debris and a bowl-shaped crater, created by eruptions from a single opening, with rock fragments called scoria or cinders being expelled
How does volcano form?
The majority of volcanoes in the world form along the boundaries of Earth’s tectonic plates, which continually shift and bump into one another. When tectonic plates collide, one often plunges deep below the other in a subduction zone
Types of Volcanoes According to Activity
Active volcanoes
Dormant volcanoes
Inactive volcanoes
Active volcanoes are presently erupting or have erupted in the last 10,000 years, expected to erupt sooner rather than later. Dormant volcanoes may erupt later on with long intervals between eruptions. Inactive volcanoes are not currently erupting
Vulcan
The God of Fire in Roman mythology
Fissure Volcano erupts lava without explosive activity, forming cracks in the ground and expelling vast quantities of lava
Types of Volcano According to Appearance
Fissure Volcano
Cinder cone Volcano
Composite Volcano
Shield Volcano
Volcano
A volcanic island in the Aeolian Islands of Italy, vents or openings that expel molten rock or magma from the interior of Earth
Anatomy of Volcanoes
Flank
Summit
Magma reservoir
Conduit
Dikes
Vent
Crater
Base
Silt
Ash cloud
Parasitic Cone
Shield Volcano is a mountain with broad, gently sloping sides and a nearly circular base, formed by basaltic lava accumulating during nonexplosive eruptions
Hotspots are hot regions in Earth’s mantle due to high-temperature mantle plumes that rise toward the surface, melting rock and forcing it toward the crust as magma, which then flows upward to Earth’s surface as lava
Inactive volcanoes
Those that have not erupted in history but still have the potential to do so
Those that have not erupted in the past 10,000 years
Dormant Volcanoes in the Philippines
Apo, Cuernos de Negros, Gorra, Maripipi, Mariveles, Negron, Angeles City, Olongapo City
Volcanic Ashes
Very fine-grained fragment of pulverized rocks, minerals, and volcanic glass formed during volcanic eruptions