A caldera forms by
A. flooding of rivers by lahars to produce a lake.
B. overflow of a lava lake.
C. draining of a magma chamber beneath a volcano during an eruption.
D. the accumulation of tephra around a vent.

Answers

Answer 1

The correct answer is C. A caldera is a large, basin-shaped depression that forms when a volcano partially or completely collapses following the draining of a magma chamber during an eruption.

When a magma chamber beneath a volcano is emptied during an eruption, the roof of the chamber can no longer support the weight of the overlying rock and collapses. The collapse creates a large, circular depression, which can be several kilometers in diameter and several hundred meters deep. This depression is known as a caldera. Calderas are often associated with large, explosive eruptions that release enormous amounts of ash, pumice, and other volcanic debris. These eruptions can be so powerful that they can trigger earthquakes and tsunamis, and can even have global climate effects.

In contrast, options A, B, and D describe other volcanic phenomena. Option A describes the formation of a lake by flooding from lahars, which are fast-moving, mudflows that can occur during volcanic eruptions. Option B describes the overflow of a lava lake, which can occur when the volume of lava being supplied to the lake exceeds the capacity of the lake to hold it. Option D describes the accumulation of tephra (volcanic ash and other volcanic material) around a vent, which can lead to the formation of a volcanic cone.

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Related Questions

the term urban sprawl describes the expansion of cities into rural areas. this phenomen has ccured around the world and has had economic, health, and environmental consequences

Answers

Yes, the term "urban sprawl" generally refers to the outward expansion of cities into previously rural or undeveloped areas, often resulting in low-density, automobile-dependent development patterns.

Urban sprawl has occurred in many regions around the world and has had a range of economic, health, and environmental consequences.

(a) Two causes of urban sprawl are population growth and the desire for larger living spaces. As populations increase, cities expand to accommodate more people, and as people become more affluent, they often seek larger homes with more land, which can only be found outside of cities in rural areas.

(b) Two human health effects associated with urban sprawl are increased air pollution and decreased physical activity. As more people move into suburban areas, there is an increase in traffic and emissions from cars, which can contribute to respiratory problems and other health issues.

Additionally, suburban areas often lack sidewalks and public transportation, making it difficult for residents to engage in physical activity and maintain a healthy lifestyle.

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Which of the following would not be a feature of coastal erosion?
a. Sea cave.
b. Baymouth barrier.
c. Sea stack.
d. Headland.

Answers

Baymouth barrier is not a coastal erosion it represents a depositions feature and occurs during longshore drift

The feature that would not be a result of coastal erosion is Baymouth barrier. The correct option is b.

Coastal erosion refers to the process by which waves, currents, and other natural forces gradually remove and wear away the shoreline. A sea cave (a), sea stack (c), and headland (d) are all features created by coastal erosion.

Sea caves form when waves erode softer rock along the coastline, sea stacks are formed when erosion isolates a section of harder rock from the mainland, and headlands occur when softer rocks are eroded away, leaving a protruding section of harder rock.

On the other hand, a baymouth barrier is formed by sediment deposition and is typically associated with coastal deposition, not coastal erosion. Hence the correct option is b.

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describe the series of processes involved in transforming an igneous rock into a sedimentary rock. please be sure to include all the processes and steps depicted on the diagram.

Answers

Process involved in transforming an igneous rock into a sedimentary rock.

Here are the steps:

1. Weathering: This is the first step, where the igneous rock is exposed to the elements, such as wind, water, and temperature changes, causing it to break down physically and chemically.

2. Erosion: After weathering, the smaller rock fragments and mineral particles are transported by natural agents like wind, water, or ice.

3. Deposition: The eroded rock fragments and mineral particles eventually settle out and accumulate in a new location, such as a riverbed, lakebed, or ocean floor. This process is called deposition.

4. Sedimentation: Over time, more and more layers of sediments accumulate, increasing the pressure on the lower layers. This process of sediment accumulation is called sedimentation.

5. Compaction: As the pressure on the sediments increases, the spaces between the particles are reduced, causing them to pack together tightly. This process is known as compaction.

6. Cementation: During compaction, dissolved minerals in the groundwater precipitate and act as a glue, binding the sediment particles together. This process is called cementation.

7. Lithification: Compaction and cementation together transform the loose sediment into a solid sedimentary rock. This process is known as lithification.

In summary, the transformation of an igneous rock into a sedimentary rock involves weathering, erosion, deposition, sedimentation, compaction, cementation, and lithification.

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Volcanism at divergent plate boundaries is most often associated with which magma type? What causes rocks to melt in these settings?

Answers

Volcanism at divergent plate boundaries is most often associated with basaltic magma. This type of magma is characterized by low viscosity and high fluidity, which allows it to flow easily to the surface and form lava flows.

The tectonic plates of the Earth migrate apart at divergent plate borders, leaving a void in the crust. This opening enables magma to fill the void by rising from the mantle.

A middle-ocean ridge is then formed as the magma solidifies and produces new crust. When magma interacts with seawater as it rises, it may result in explosive eruptions and the formation of hydrothermal vents.

In these conditions, decompression melting is the primary contributor to rock melting. The strain on the underlying mantle lessens when the plates separate.

The mantle rock partially melts and forms magma as a result of the pressure drop, which lowers the melting point of the rock. Then, as the magma rises to the surface, lava pours outward.

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