Types Flashcards

1
Q

Types Based on Structure

A

Cinder Cone
Composite
Shield

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2
Q

Types Based on Activity

A

Active
Inactive
Potentially Active

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3
Q

Types of Eruptions

A

Phreatic or Hydrothermal
Phreatomagmatic
Strombolian
Vulcanian
Plinian

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4
Q

Types Based on Eruption

A

Phreatic or Hydrothermal
Phreatomagmatic
Strombolian Vulcanian
Plinian

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5
Q

are the simplest type of volcano. They are built from particles and blobs of solidified lava ejected from a single vent.

A

Cinder Cone

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6
Q

are large, typically steep-sided, symmetrical cones of large dimension formed from alternating layers of lava flows, volcanic ash, cinders, blocks, and pyroclastic materials.

A

Composite

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7
Q

are large, broad volcanoes that look similar to shields from above - hence the name. These volcanoes are built almost entirely of fluid lava flow thus these volcanoes are not steep.

A

Shield

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8
Q

those volcanoes that have had at least one eruption during the past 10,000 years. They are those that erupted recently and still showing regular activity like emission of gases, lava and ash flows.

A

Active

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9
Q

those that have not erupted for the last 10,000 years and is not expected to erupt again in a comparable time scale of the future. There are no signs of volcanic activity for a long period of time because magma supply is cut off. Also the physical form of the volcano has signs of intensive weathering and erosion

A

Inactive

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10
Q

those that have no records of volcanic activity but are morphologically young-looking.

A

Potentially Active

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11
Q

a stream-driven eruption as the hot rocks come in contact with water. It is short lived, characterized by ash columns but may be a beginning of a larger eruption.

A

Phreatic

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12
Q

violent eruption due to the contact between water and magma. As a result, a large column of very fine ash and high-speed and sideway emission of pyroclastic materials called base surges are observed.

A

Phreatomagmatic

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13
Q

periodic, weak to violent eruption characterized by fountain lava, just like the Irazu Volcano in Costa Rica.

A

Strombolian

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14
Q

characterized by tall eruption columns that reach up to 20 km high with pyroclastic flow and ash fall tephra like that of Paricutin Volcano in Mexico.

A

Vulcanian

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15
Q

excessively explosive type of eruption of gas and pyroclastic materials, like in Pinatubo Volcano in Zambales.

A

Plinian

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