Part E - The Geologic History of a Volcanic Neck Cabezon Peak, shown in the phot

Question

Part E - The Geologic History of a Volcanic Neck Cabezon Peak, shown in the photo below, is a classic example of a volcanic neck. This particular eye- catching landform was once a cinder cone. The only remnant left is the harder, more resistant rock of the conduit. Think about the processes (like volcanism and erosion) responsible for the transition of a cinder cone into a volcanic neck Volcanic neck A photo showing a volcanic neck. For this question, focus on the series of geologic events that led to the current expression that we see today. Arrange the following events in order of age.

Explanation / Answer

steps that happen

1.The conduit is exposed at earth's surface to form a volcanic neck

2.The flanks (sides ) of the volcano and the surrounding country rock start to erode away.

conduit :- its a passage for water or any other liquid

3.Magma erupts explosively onto earth surface

4,volcanism ceases and magma crystallizes into rock

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