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    examBoard: Cambridge
    examType: IGCSE
    lessonTitle: Volcanic Features
    
Geography - Physical Geography - Tectonic Hazards - Volcanic Features - BrainyLemons
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Tectonic Hazards » Volcanic Features

What you'll learn this session

Study time: 30 minutes

  • Different types of volcanoes and their features
  • Formation processes of volcanic landforms
  • Key volcanic features including craters, calderas and lava domes
  • Types of volcanic materials (lava, ash, pyroclastic flows)
  • Case studies of significant volcanic eruptions
  • How volcanic features affect human settlements

Introduction to Volcanic Features

Volcanoes are one of Earth's most dramatic and powerful natural features. They form when magma from the Earth's mantle rises to the surface, creating various landforms depending on the type of eruption, magma composition and local geological conditions.

Key Definitions:

  • Volcano: An opening in the Earth's crust through which molten rock, ash and gases erupt.
  • Magma: Molten rock beneath the Earth's surface.
  • Lava: Magma that has reached the Earth's surface.
  • Pyroclastic material: Rock fragments and ash ejected during explosive eruptions.

Types of Volcanoes

Volcanoes come in different shapes and sizes, each with unique characteristics and formation processes.

🌋 Shield Volcanoes

Shield volcanoes have gently sloping sides and form from fluid basaltic lava flows. They're the largest volcanoes on Earth.

Example: Mauna Loa in Hawaii rises 9 km from the sea floor and is the world's largest active volcano.

Features: Broad, dome-like shape with gentle slopes (usually less than 10°).

🔥 Composite Volcanoes

Also called stratovolcanoes, these have steep sides and are made up of alternating layers of lava and ash.

Example: Mount Fuji in Japan and Mount St. Helens in the USA.

Features: Steep sides (30-35°), conical shape and often have a summit crater.

🚬 Cinder Cones

Small, steep-sided volcanoes formed from ejected lava fragments that build up around the vent.

Example: Paricutin in Mexico, which famously grew in a farmer's field in 1943.

Features: Simple cone shape, steep sides (30-40°) and a circular crater at the summit.

💧 Lava Domes

Formed when thick, viscous lava piles up near the volcanic vent rather than flowing away.

Example: Lassen Peak in California.

Features: Steep-sided, rounded mounds that form when lava is too thick to flow far from its source.

Key Volcanic Features

Volcanoes create distinctive landforms both during and after eruptions. Understanding these features helps geographers analyse volcanic activity and potential hazards.

Craters

Bowl-shaped depressions at the summit of a volcano, formed by explosive eruptions or collapse.

Most active volcanoes have a main crater at their summit where eruptions occur.

💥 Calderas

Large, basin-shaped depressions formed when a volcano collapses into its empty magma chamber after a major eruption.

Calderas are much larger than craters and can be several kilometres wide.

📝 Volcanic Plugs

Formed when magma solidifies in a volcano's vent, creating a resistant rock formation that remains after erosion removes surrounding material.

Edinburgh Castle in Scotland sits atop an ancient volcanic plug.

Volcanic Materials and Deposits

The materials ejected from volcanoes create various features and landforms that shape the surrounding landscape.

🔥 Lava Flows

Streams of molten rock that flow from a volcanic vent during an eruption. The type of lava affects the resulting landforms:

  • Aa lava: Thick, slow-moving with a rough, blocky surface.
  • Pahoehoe lava: Thin, fast-flowing with a smooth, rope-like surface.

Lava flows create features like lava plateaus, lava tubes and pillow lavas (when erupted underwater).

💣 Pyroclastic Deposits

Material ejected explosively from a volcano, including:

  • Ash: Fine particles that can travel thousands of kilometres.
  • Lapilli: Pea to walnut-sized fragments.
  • Volcanic bombs: Larger fragments that are partly molten when ejected.
  • Pyroclastic flows: Fast-moving currents of hot gas and volcanic matter that can reach speeds of 700 km/h.

Secondary Volcanic Features

Volcanic activity creates additional features beyond the main volcano structure:

  • Fumaroles: Openings where volcanic gases escape from beneath the surface.
  • Hot springs: Areas where groundwater is heated by magma and rises to the surface.
  • Geysers: Hot springs that periodically eject water and steam into the air.
  • Mudpots: Acidic hot springs with limited water that mix with surrounding soil to create bubbling mud.

Case Study Focus: Mount Pinatubo Eruption (1991)

Mount Pinatubo in the Philippines erupted in June 1991 after being dormant for 600 years. It was one of the largest eruptions of the 20th century.

Key features formed:

  • A 2.5 km wide caldera formed at the summit after the eruption.
  • Pyroclastic flows travelled up to 16 km from the volcano, filling valleys with volcanic deposits up to 200m thick.
  • A crater lake formed in the caldera, which continues to change colour due to chemical reactions, rainfall and volcanic activity.

Impact: The eruption ejected 10 billion tonnes of magma and 20 million tonnes of sulfur dioxide, causing global temperatures to drop by 0.5°C for two years.

Volcanic Features and Human Settlements

Despite the hazards, people often live near volcanoes for several reasons related to the features they create:

🌾 Benefits

  • Fertile soils: Volcanic ash weathers quickly to form nutrient-rich soils excellent for agriculture.
  • Geothermal energy: Volcanic areas provide renewable energy through hot springs and steam vents.
  • Tourism: Volcanic features attract visitors, supporting local economies.
  • Building materials: Volcanic rocks like pumice and basalt are used in construction.

Challenges

  • Eruption hazards: Lava flows, pyroclastic flows and ash falls threaten settlements.
  • Lahars: Volcanic mudflows can travel long distances, burying communities.
  • Gas emissions: Toxic gases like sulfur dioxide can cause health problems.
  • Infrastructure damage: Ash can collapse roofs, contaminate water supplies and disrupt transport.

Case Study Focus: Heimaey, Iceland (1973)

When the Eldfell volcano erupted on Heimaey island in 1973, it demonstrated how volcanic features can be both destructive and beneficial:

  • The eruption created a new volcanic cone and threatened to close the island's vital fishing harbour.
  • Residents used seawater to cool advancing lava flows, successfully diverting them away from the town.
  • The harbour was actually improved by the new lava formations, which provided better protection from the sea.
  • Homes buried in ash were excavated and the volcanic heat was harnessed for a district heating system.

This case shows how understanding volcanic features can help communities adapt to and even benefit from volcanic activity.

Monitoring Volcanic Features

Scientists monitor changes in volcanic features to predict eruptions and reduce risk:

  • Ground deformation: Swelling or bulging of a volcano can indicate rising magma.
  • Gas emissions: Changes in the amount or composition of gases released from fumaroles.
  • Seismic activity: Earthquakes often precede volcanic eruptions.
  • Temperature changes: Increasing heat in crater lakes or around volcanic vents.

Understanding volcanic features is essential for hazard management, as different volcano types produce different hazards. Shield volcanoes typically have less explosive eruptions with lava flows as the main hazard, while composite volcanoes can produce devastating pyroclastic flows and widespread ash deposits.

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