A caldera is a large, bowl-shaped depression that forms following the evacuation of a magma chamber/reservoir. It is typically caused by the collapse of the ground following a volcanic eruption. Calderas can range in size from a few kilometers to tens of kilometers in diameter, and they are often characterized by steep, inward-sloping walls.
Formation of Calderas
Calderas form in several ways, including:
Explosive Eruptions: When a volcano experiences a massive explosive eruption, the overlying rock and soil can collapse into the emptied magma chamber, forming a caldera.
Subsidence: As magma is erupted from a volcanic vent, the ground above the magma chamber can collapse as the chamber empties, creating a depression.
Collapse of Lava Flows: Large volumes of lava erupted from a volcano can leave a void beneath the surface, leading to the collapse of the overlying rock and the formation of a caldera.
Types of Calderas
There are several types of calderas, including:
Subsidence Calderas: These are formed by the collapse of the ground above an emptied magma chamber.
Explosion Calderas: These result from the explosive eruption of a volcano, which causes the collapse of the overlying rock and soil.
Resurgent Calderas: These calderas experience a resurgence of volcanic activity after the initial collapse, resulting in the uplift of the caldera floor.
Complex Calderas: These calderas exhibit characteristics of both subsidence and explosion calderas, often with multiple collapse events.
Examples of Calderas
Some famous calderas around the world include:
Yellowstone Caldera: Located in Yellowstone National Park, USA, this caldera is one of the largest in the world, measuring approximately 45 kilometers by 75 kilometers.
La Garita Caldera: This caldera, located in Colorado, USA, was formed by a supervolcanic eruption and is associated with the eruption of the Fish Canyon Tuff.
Santorini Caldera: Formed by the massive Minoan eruption around 3,600 years ago, this caldera is located in the Aegean Sea and is a popular tourist destination.
Impact of Calderas
Calderas can have significant impacts on the surrounding environment and communities. Their formation can lead to the release of large amounts of volcanic gases, the deposition of ash and pyroclastic flows, and the destruction of landscapes. Additionally, the collapse of a caldera can lead to the formation of a new volcanic system, which may pose further hazards to the area.
Study Guide
When studying calderas, be sure to focus on the following key points:
The formation mechanisms of calderas, including subsidence, explosive eruptions, and collapse of lava flows.
The differences between various types of calderas, such as subsidence, explosion, resurgent, and complex calderas.
Examples of famous calderas and their locations, as well as their associated volcanic activity.
The potential impacts of caldera formation on the environment and local communities.
Earth/Space Science: Students will use scientific skills and processes to explain the chemical and physical interactions (i.e., natural forces and cycles, transfer of energy) of the environment, Earth, and the universe that occur over time.
Earth History: Explain how sedimentary rock is formed periodically, embedding plant and animal remains and leaving a record of the sequence in which the plants and animals appeared and disappeared.
Explain how sedimentary rock buried deep enough may be reformed by pressure and heat and these reformed rock layers may be forced up again to become land surface and even mountains.
Explain why some fossils found in the top layers of sedimentary rock are older then those found beneath in lower layers: Folding; Breaking; Uplift; Faulting; Tilting.