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When lava makes its way through cracks and fissures developed in the ground, it solidifies almost perpendicular to the ground. It cools down in the sa
Question

When lava makes its way through cracks and fissures developed in the ground, it solidifies almost perpendicular to the ground. It cools down in the same position to develop a wall-like structure. What is this structure called?

A.

​Lacolith​

B.

​Dykes​

C.

​Lapolith​

D.

​Phacolith​

Correct option is B

The structure described is called a Dyke.

Here's why:

  • Dykes: These are sheet-like intrusions of igneous rock that cut across the layering of the surrounding rock. They form when magma intrudes into fractures in the rock and solidifies.
  • Lacolith: These are dome-shaped intrusions that uplift the overlying rock layers.
  • Lapolith: These are saucer-shaped intrusions that sag the overlying rock layers.
  • Phacolith: These are lens-shaped intrusions that concordantly intrude along folds in the host rock.

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