How Does a Volcano Form?
What is a volcano?
A volcano is a geological rupture in the Earth's crust triggered by natural forces, such as pressure and temperature in the interior of the Earth. These forces drive gases and hot liquid, known as magma, out through a volcano's orifice known as vent. Once out of the vent, these erupted materials break down, harden or condense around a volcano's vent.
Over thousands or millions of years, the accumulation of magma forms steep-sided cones known as volcanoes. Volcanoes have been erupting molten material, after the formation of the earth, due to the accumulated pressure in the interior of the planet. The formation of volcanoes have contributed to the shaping and configuration of the varied landscapes that make up the planet.
Volcanoes are most commonly formed at the convergence or divergence of tectonic plates. For example in Mid-Ocean Ridges, where tectonic plates spread apart and subduction zones, where one tectonic plate sinks into the earth´s mantle underneath another tectonic plate. Others may form close to or in the middle of tectonic plates, such as Island Arcs and Hotspots. Some others form on the continents, such as in the Continental Rifts.
How a Volcano is Created?
Volcano Formation (Plate Tectonics)
The Earth’s crust is composed of enormous sections of rock called tectonic plates. Tectonic plates resemble puzzle pieces which move constantly against each other. Volcanoes often form in the areas where tectonic plates make contact. The friction created between two plates by the constant movement melts the Earth’s crust, causing the rock underneath the crust to turn into magma due to the great temperatures created by friction.
The now molten hot rock or magma creates great pressure, and over time, it finds its way through the fractures in the plates. Once magma reaches the surface of the Earth, it is called lava. Approximately 1500 volcanoes around the world are considered active, and from these, nearly 90% lie in the Ring of Fire, which is a ring of oceanic volcanoes circling the Pacific Ocean.
Most divergent plate boundaries lie in the bottom of the oceans. That is why most volcanic activity occurs in the oceans. Volcanoes may be formed at subduction zones. A subduction zone is a place where two plates, one oceanic plate and one continental plate, collide. At a subduction zone, an oceanic plate submerges under a continental plate. The friction creates magma. When magma reaches the surface, then, a volcano is formed. A typical example of this type of volcano is Mount Etna on the east coast of Italy.
Where are Volcanoes Located?
What is a Hotspot?
Although most volcanoes are formed in the Ring of Fire under water, there are some that are formed on land. Volcanoes on land, away from tectonic plate boundaries, are known as hotspots. They are formed from rising magma intrusions called mantle plumes. Hotspots are stationary regions of magma chambers under the Earth’s crust. When a mantle plume forms a volcano over hotspot, the movement of the continental plate moves the new formed volcano and exposes new parts of the plate for more volcano formations, creating what is known as volcanic chains. The Hawaiian Islands were formed like this.
Structure of a Volcano
Parts of a Volcano
1. Ash Plume
2. Central Vent
3. Volcanic Ash Rain
4. Layers of Basaltic Lava
5. Earth's Crust
6. Magma Chamber
What is a Volcanic Vent?
Before the formation of a volcano, the Earth's natural forces, such as pressure and temperature, push magma out of the magma chamber, which is a large underground pool of liquid rock, until it erupts as lava on the surface of the Earth or as a boiling gush under the ocean. When molten rock or magma reaches the surface of the Earth either on land or the bottom of the oceans, it cools and hardens.
Much of the Earth's crust is made of basaltic lava, which is the most common igneous rock, and nearly all the ocean floor is made of basalt, as well. Flood lava spreads over flat land, and as it piles up, it forms thick basaltic lava plateaus, known as flood basalts. One of the largest flood basalts, ever created on the surface of the Earth, is the Columbia River Plateau, covering Idaho, Oregon and Washington in the United States.
The cracks or openings through where magma is forced out of the magma chamber are called volcanic vents. Magma gets ejected as lava through these openings. When internal heat and pressure inside the Earth force liquid lava out through a central vent, incandescent jet sprays of molten lava, rock and gases can reach hundreds of meters high into the sky. They may send volcanic material into the sky periodically or incessantly for an extended period of time. Over time, the volcanic fragments build-up around a vent gradually forming layers of volcanic material.
Fractures on the surface of the Earth to Mountains with a Volcanic Vent on its Highest End
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Formations of many Types of Volcanoes
Shield volcanoes are some of the largest volcanoes on Earth with slopes of a few degrees at the further lower end, and medium height slopes of about 10 degrees which flattens at the summit of the volcano. The gentle slope in Shield volcanoes is produced by basaltic lava flows of low viscosity. This type of lava can flow over long distances before it cools down and solidifies. Mauna Loa in Hawaii, 17 km (10.5 miles) high, is a Shield volcano with a gentle slope from the base to the top.
Composite volcanoes, also known as stratovolcanoes, are formed from high viscosity basaltic lava. This type of lava flows slowly due to its high density composition. Over time, high viscosity lava builds up steep-sided conical mountains. During the process of formation of this type of volcanoes, basaltic lava eruptions flow slowly and harden faster than low viscosity lava, providing in each eruption a thick basaltic layer on which successive basaltic lava layers build up. Composite volcanoes are mostly found on the continental plates. Mount Rainier with a height of 4.4 km (2.7 miles) in Washington and Mount Fuji, at 3.7 km (2.3 miles), in Japan are both composite volcanoes.
Hotspots are volcanoes that result from the movement of tectonic plates underneath them. It is believed that during the creation of this type of volcanoes the underlying mantle is extremely hot compared to the mantle in other underground regions. These types of volcanoes are formed from vents that find its way to the surface due to the hot temperature and pressure in the magma chamber. As the overlying layer of the Earth's crust moves due to tectonics, the original volcano moves, as well. With successive tectonic plate movements, more volcanoes are created in a chain. The Hawaiian Islands were formed from a hotspot in the mantle.
Cinder cone volcanoes are the smallest type of volcano. They form from small lava fragments (tephra). As the lava is erupted into the air, it breaks down into its constituent elements that fall down as lapilli and ash, which solidify around the vent, forming a circular cone. Cinder cones normally have a bowl-shaped crater at the top and rarely rise above 300 meters (985 ft.).
Lava domes are formed from high viscosity basaltic lava which barely flows. This type of lava often creates a volcanic dome over and around its vent. When the dome hardens, it can trap gases, creating pressure. When the pressure is big enough, the dome is blown away to pieces in a violent eruption. A lava dome started developing on Mt. St. Helens shortly after the 1980 eruption.
The Ocean Floor
Submarine volcanoes are very common in the ocean floor. Many lie at great ocean depths, unable to reveal their explosive presence due to the extreme weight and cooling effect of ocean water above them. Others, lying at more shallow waters, may reveal their presence by blowing steam and rocky debris above the surface of the sea. Sometimes, submarine volcanoes may form steep pillars over their volcanic vents. Some may grow so large that they reach the ocean surface, forming new islands. The San Juan Islands in the state of Washington may have formed from this type of eruption.
Calderas are huge circular topographic depressions that are formed when a volcanic eruption empties a deep magma chamber, causing the collapse of the overlying land. Calderas can range in size from 4-6 km (2.5-3.7 miles) to up to 50 km (31 miles) wide. Over time, an old magma chamber may fill again with magma, forcing the floor of the caldera to rise. It may remain like this or repeated eruptions may reshape the caldera over and over again in a process known as resurgent caldera. Crater Lake in Oregon, which is an 8 km (5 miles) wide and 600 meters (1970 ft.) caldera, was formed in this way.
Interesting Facts About Volcanoes
- Approximately 90% of all active volcanoes are located in the Pacific Ring of Fire
- The crustsof Mercury, Venus, Earth, Mars and the Moon (the inner planets) are made of basaltic rock.
- More than 95% of the Earth’s first 16 km (10 miles) of crust is made of igneous rock (basalt) formed from lava eruptions.
- Mt. Etna in Italy has been erupting for more than 3,500 years. The first eruption occurred in 1,500 BC.
- Kilaueavolcano in Hawaii is a youngest shield volcano which has been erupting continuously since 1983.
- The Hawaiian islands formed over a hotspot in the middle of the Pacific plate.
Questions & Answers
How is lava formed?
Lava is made underground at around 160 km (100 miles) or more underground where temperatures are hot enough to melt rock. Molten rock underground is called magma, once it is erupted out through a volcano, It´s called lava.
How are volcanoes formed?
The continuous eruption of lava forms volcanoes, and it may take several hundred years for them to develop.
What is a dormant volcano?
Dormant volcanoes are those that may remain inactive for long periods of time, but might erupt suddenly at any moment.
How do volcanoes form on the ocean floor?
They are formed due to the activity of the earth´s lithosphere by plate tectonics. The natural activity of the planet, such as tidal changes, earth´s rotation, gravitational pull cause tectonic plates to shift and collide. This movement of tectonic plates underwater causes underwater volcanoes to form where two tectonic plates meet, most commonly at convergent and divergent boundaries.
© 2012 Jose Juan Gutierrez