Geography Tectonic Plates

Types of Volcanoes

Volcanoes are classified into different types based on their shape, eruptive behavior, and magma composition. Here are some of the main types of volcanoes:

1. Shield Volcanoes:
  • Shape: Broad, gently sloping sides forming a shield-like structure.
  • Eruptive Behavior: Effusive eruptions with low-viscosity lava flows.
  • Magma Composition: Basaltic, with low silica content.
  • Examples: Mauna Loa and Kilauea in Hawaii.
2. Cinder Cones:
  • Shape: Steep-sided, conical shape built from cinders (fragments of lava).
  • Eruptive Behavior: Strombolian eruptions with moderate explosivity.
  • Magma Composition: Basaltic to andesitic.
  • Examples: Paricutin in Mexico and Sunset Crater in Arizona.
3. Composite Volcanoes (Stratovolcanoes):
  • Shape: Steep-sided, symmetrical cone shape with alternating layers of lava and pyroclastic material.
  • Eruptive Behavior: Both effusive and explosive eruptions, including lava flows, ash clouds, and pyroclastic flows.
  • Magma Composition: Andesitic to rhyolitic, with higher silica content.
  • Examples: Mount Fuji in Japan, Mount St. Helens in the United States, and Mount Vesuvius in Italy.
4. Caldera Volcanoes:
  • Shape: Large, basin-shaped depressions formed by the collapse of a volcano’s summit.
  • Eruptive Behavior: Can have both effusive and explosive eruptions, often associated with large-scale pyroclastic flows.
  • Magma Composition: Variable, ranging from basaltic to rhyolitic.
  • Examples: Yellowstone Caldera in the United States and Crater Lake in Oregon.
5. Lava Domes:
  • Shape: Rounded, steep-sided mounds formed by the slow extrusion of viscous lava.
  • Eruptive Behavior: Effusive eruptions with slow-moving, viscous lava flows.
  • Magma Composition: Rhyolitic to dacitic, with high silica content.
  • Examples: Mont Pelée in Martinique and Lassen Peak in California.
6. Submarine Volcanoes:
  • Shape: Can vary, but often form seamounts or volcanic islands.
  • Eruptive Behavior: Effusive or explosive eruptions, depending on magma composition and water depth.
  • Magma Composition: Variable, ranging from basaltic to rhyolitic.
  • Examples: Loihi Seamount in Hawaii and the volcanic islands of Iceland.

It’s important to note that volcanoes can exhibit complex behavior and may not always fit neatly into a single category. Some volcanoes may have characteristics of multiple types, and their behavior can change over time.

List Of Important Volcanoes As Per UPSC:

Volcanoes are geological formations that occur when molten rock, known as magma, rises to the surface of the Earth. They can be classified into different types based on their shape, size, and eruptive behavior. Some of the most important volcanoes as per the Union Public Service Commission (UPSC) syllabus are:

1. Mount Everest

  • Located in the Himalayas, on the border between Nepal and China.
  • World’s highest mountain, with a peak elevation of 8,848.86 meters (29,031.7 feet).
  • Formed by the collision of the Indian and Eurasian tectonic plates.
  • Has a complex geological structure, with various rock types and formations.
  • Home to diverse flora and fauna, including rare and endangered species.
  • Considered a sacred mountain in many cultures and religions.

2. K2 (Mount Godwin Austen)

  • Located in the Karakoram mountain range, on the border between Pakistan and China.
  • World’s second-highest mountain, with a peak elevation of 8,611 meters (28,251 feet).
  • Known for its extreme difficulty and high risk of climbing, earning it the nickname “Savage Mountain.”
  • Has a steep and rugged terrain, with glaciers and ice fields.
  • Considered one of the most challenging mountains to climb in the world.

3. Mount Kilimanjaro

  • Located in Tanzania, Africa.
  • Africa’s highest mountain, with a peak elevation of 5,895 meters (19,341 feet).
  • Consists of three volcanic cones: Kibo, Mawenzi, and Shira.
  • Kibo is the highest cone and contains the dormant Kibo caldera, which is 2.5 kilometers (1.6 miles) in diameter.
  • Home to various ecosystems, including rainforests, alpine meadows, and glaciers.
  • A popular destination for登山 and wildlife safaris.

4. Mount Fuji

  • Located on Honshu Island, Japan.
  • Japan’s highest mountain, with a peak elevation of 3,776 meters (12,388 feet).
  • An active stratovolcano, with its last eruption occurring in 1707.
  • Has a symmetrical cone shape and is considered a sacred mountain in Japanese culture.
  • A popular destination for登山 and a symbol of Japan.

5. Mount Vesuvius

  • Located in the Campania region of Italy, near Naples.
  • One of the most dangerous volcanoes in the world due to its proximity to densely populated areas.
  • Has a history of violent eruptions, including the famous eruption in 79 AD that buried the Roman cities of Pompeii and Herculaneum.
  • Currently classified as dormant, but still closely monitored due to its potential for future eruptions.

6. Mount Etna

  • Located on the island of Sicily, Italy.
  • Europe’s largest active volcano, with a peak elevation of 3,329 meters (10,922 feet).
  • Has a complex volcanic structure, with multiple craters and vents.
  • Known for its frequent eruptions, which can be both explosive and effusive.
  • A popular tourist destination, offering stunning views of the surrounding landscape.

7. Yellowstone Supervolcano

  • Located in the western United States, primarily in Wyoming.
  • A large volcanic caldera, measuring approximately 55 by 72 kilometers (34 by 45 miles).
  • Considered a supervolcano due to its potential for producing extremely large volcanic eruptions.
  • Has a history of major eruptions, with the most recent one occurring about 640,000 years ago.
  • Closely monitored by scientists due to its potential impact on global climate and ecosystems.

These are just a few examples of important volcanoes that are relevant to the UPSC syllabus. Understanding their locations, characteristics, and significance is essential for candidates preparing for the UPSC examinations.

Different Types of Volcanic Eruption:

Volcanic eruptions are classified into several types based on their characteristics, such as the explosiveness, lava flow, and eruption style. Here are some common types of volcanic eruptions:

1. Hawaiian Eruption:
  • Characteristics:
  • Low viscosity lava flows
  • Gentle and non-explosive
  • Lava fountains and flows
  • Example: Kilauea volcano in Hawaii
2. Strombolian Eruption:
  • Characteristics:
  • Moderate viscosity lava
  • Mild explosions with lava bombs
  • Strombolian cones are formed
  • Example: Stromboli volcano in Italy
3. Vulcanian Eruption:
  • Characteristics:
  • High viscosity lava
  • Violent explosions with ash clouds
  • Pyroclastic flows and ash falls
  • Example: Vulcano volcano in Italy
4. Plinian Eruption:
  • Characteristics:
  • Highly explosive and powerful
  • Large ash clouds reaching the stratosphere
  • Pyroclastic flows and ash falls
  • Example: Mount Pinatubo eruption in the Philippines (1991)
5. Peléan Eruption:
  • Characteristics:
  • Formation of a lava dome
  • Highly viscous lava
  • Explosive eruptions with pyroclastic flows
  • Example: Mount Pelée eruption in Martinique (1902)
6. Phreatomagmatic Eruption:
  • Characteristics:
  • Interaction of magma with water (e.g., lakes, groundwater)
  • Violent steam explosions
  • Ash clouds and pyroclastic flows
  • Example: Surtsey eruption in Iceland (1963)
7. Icelandic Eruption:
  • Characteristics:
  • Fissure-type eruptions
  • Lava flows cover large areas
  • Less explosive compared to other types
  • Example: Laki eruption in Iceland (1783)
8. Subglacial Eruption:
  • Characteristics:
  • Eruptions beneath glaciers or ice sheets
  • Melting of ice and flooding
  • Ash clouds and pyroclastic flows
  • Example: Eyjafjallajökull eruption in Iceland (2010)
9. Caldera-Forming Eruption:
  • Characteristics:
  • Large-scale eruptions leading to caldera collapse
  • Ash clouds and pyroclastic flows
  • Formation of calderas (large volcanic depressions)
  • Example: Yellowstone supervolcano in the United States
10. Lahars:
  • Characteristics:
  • Volcanic mudflows or debris flows
  • Formed when volcanic material mixes with water
  • Destructive and can travel long distances
  • Example: Nevado del Ruiz eruption in Colombia (1985)

It’s important to note that volcanic eruptions can be complex and may exhibit characteristics of multiple types. Scientists closely monitor volcanic activity to understand their behavior, assess risks, and mitigate potential hazards to nearby communities.

Negative Effects of Volcanoes

Volcanoes are powerful natural phenomena that can have both positive and negative impacts on the environment and human societies. While they can provide fertile soil, geothermal energy, and scenic landscapes, they can also cause significant destruction and disruption. Here are some of the negative effects of volcanoes:

1. Volcanic Eruptions:
  • Ashfall: Volcanic eruptions can release enormous amounts of ash into the atmosphere, which can block sunlight, disrupt air travel, and cause respiratory problems in humans and animals.
  • Lava Flows: Lava flows can destroy buildings, infrastructure, and entire communities in their path. They can also cause wildfires and alter landscapes.
  • Lahars: Lahars are destructive mudflows or debris flows that form when volcanic material mixes with water from melted snow, ice, or heavy rainfall. They can travel at high speeds and cause significant damage to infrastructure and settlements.
  • Pyroclastic Flows: Pyroclastic flows are fast-moving clouds of hot gas, ash, and volcanic fragments that can reach temperatures of up to 1,000 degrees Celsius. They can incinerate everything in their path and travel at speeds of up to 700 kilometers per hour.
2. Climate Impact:
  • Global Cooling: Large volcanic eruptions can release sulfur dioxide and other aerosols into the stratosphere, which can reflect sunlight and cause global cooling. This can lead to changes in weather patterns and disruptions in agriculture.
  • Acid Rain: Volcanic emissions can contribute to acid rain, which can damage forests, aquatic ecosystems, and infrastructure.
3. Health Hazards:
  • Respiratory Problems: Volcanic ash and gases can cause respiratory problems such as asthma, bronchitis, and lung damage.
  • Volcanic Gases: Volcanic gases like sulfur dioxide, hydrogen sulfide, and carbon dioxide can be toxic and pose health risks to humans and animals.
4. Economic Impact:
  • Property Damage: Volcanic eruptions can cause extensive damage to property, including homes, businesses, and infrastructure.
  • Loss of Agriculture: Ashfall and lava flows can destroy crops and livestock, leading to food shortages and economic losses.
  • Tourism Disruption: Volcanic activity can disrupt tourism in affected areas, impacting local economies that rely on tourism revenue.
5. Social Impact:
  • Displacement: Volcanic eruptions can force people to evacuate their homes and communities, leading to displacement and social disruption.
  • Loss of Cultural Heritage: Volcanic eruptions can destroy cultural heritage sites and artifacts, resulting in the loss of cultural identity and historical significance.
Conclusion:

Volcanoes are powerful natural forces that can have both positive and negative impacts on the environment and human societies. While they can provide benefits such as fertile soil and geothermal energy, their destructive potential can cause significant loss of life, property, and disruption to ecosystems and economies. It is important to understand and monitor volcanic activity to mitigate risks and prepare for potential eruptions.

Positive Effects of Volcanoes:

Volcanoes are often associated with destruction and danger, but they can also have several positive effects on the environment and human societies. Here are some of the benefits of volcanoes:

1. Soil Fertility:

Volcanic eruptions release ash and other minerals that enrich the soil, making it more fertile. This can lead to increased agricultural productivity in the surrounding areas. The volcanic ash contains essential nutrients like nitrogen, phosphorus, and potassium, which are vital for plant growth.

2. Geothermal Energy:

Volcanic regions often have high levels of geothermal energy, which can be harnessed to generate electricity. Geothermal power plants use the heat from the Earth’s interior to produce steam that drives turbines, generating clean and renewable energy.

3. Tourism:

Volcanoes can attract tourists from around the world, boosting the local economy. Many people are fascinated by the power and beauty of volcanoes and are willing to travel to see them. This can create jobs and opportunities for businesses in the tourism industry.

4. Biodiversity:

Volcanic eruptions can create new habitats and ecosystems, leading to increased biodiversity. The unique conditions created by volcanic activity, such as lava flows and ash deposits, can support specialized plant and animal species.

5. Mineral Resources:

Volcanic regions are often rich in mineral resources, such as gold, silver, copper, and zinc. These minerals can be extracted and used for various industrial purposes, contributing to economic development.

6. Climate Regulation:

Volcanic eruptions can release aerosols and gases into the atmosphere, which can influence climate patterns. Some volcanic eruptions can cause temporary cooling effects by reflecting sunlight back into space, while others can contribute to global warming by releasing greenhouse gases.

7. Natural Hazards Mitigation:

Volcanic activity can help mitigate other natural hazards. For example, volcanic eruptions can release pressure from tectonic plates, reducing the risk of earthquakes. Additionally, volcanic ash can help absorb and disperse the energy of tsunamis, reducing their impact on coastal areas.

8. Scientific Research:

Volcanoes provide valuable opportunities for scientific research. Studying volcanic processes can help us better understand the Earth’s interior, climate dynamics, and the evolution of life.

Conclusion:

While volcanoes can be destructive, they also offer numerous positive benefits to the environment and human societies. By understanding and managing volcanic activity, we can harness their potential for sustainable development and scientific advancement.

Volcanoes NCERT Notes FAQs
What is a volcano?

A volcano is a vent or fissure in the Earth’s crust through which molten rock, ash, and gases are expelled.

What causes volcanoes to erupt?

Volcanoes erupt when magma, or molten rock, rises to the surface of the Earth. This can happen when the Earth’s tectonic plates move apart, allowing magma to escape from the mantle, or when pressure builds up inside a volcano.

What are the different types of volcanoes?

There are three main types of volcanoes:

  • Shield volcanoes are broad, gently sloping volcanoes that are formed by the eruption of low-viscosity lava.
  • Composite volcanoes, also known as stratovolcanoes, are steep-sided volcanoes that are formed by the eruption of both lava and ash.
  • Cinder cones are small, steep-sided volcanoes that are formed by the eruption of cinders, or small fragments of lava.
What are the dangers of volcanoes?

Volcanoes can pose a number of dangers, including:

  • Lava flows can destroy buildings and infrastructure, and can also cause wildfires.
  • Ash clouds can block out the sun, causing cooling and darkness.
  • Volcanic gases can be toxic, and can cause respiratory problems and even death.
  • Lahars, or mudflows, can be triggered by volcanic eruptions and can travel at high speeds, destroying everything in their path.
How can we predict volcanic eruptions?

Volcanologists use a variety of methods to predict volcanic eruptions, including:

  • Monitoring seismic activity: Earthquakes can be a sign that magma is moving beneath the surface of the Earth.
  • Measuring ground deformation: Bulges in the Earth’s surface can indicate that magma is accumulating beneath the surface.
  • Monitoring gas emissions: Changes in the composition of volcanic gases can indicate that an eruption is imminent.
What can we do to mitigate the effects of volcanic eruptions?

There are a number of things that can be done to mitigate the effects of volcanic eruptions, including:

  • Educating people about the risks of volcanoes: It is important to educate people who live near volcanoes about the risks of volcanic eruptions and how to prepare for them.
  • Developing early warning systems: Early warning systems can help people to evacuate to safety before an eruption occurs.
  • Constructing protective structures: Protective structures, such as lava domes and ash shelters, can help to protect people and property from the effects of volcanic eruptions.
Conclusion

Volcanoes are a powerful force of nature, but they can also be a source of beauty and wonder. By understanding the risks of volcanoes and taking steps to mitigate their effects, we can help to protect ourselves and our communities from the dangers of volcanic eruptions.