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A lava solidifies into nonvesicular basalt instead of vesicular basalt because?
The lack of vesicles in nonvesicular basalt suggests that the lava cooled and solidified quickly, which prevented gas bubbles from forming. This rapid cooling can occur when lava flows over a cold surface or when it is deposited underwater. As a result, the cooling process does not allow enough time for gas bubbles to form and become trapped within the rock, leading to the formation of nonvesicular basalt.
What is the difference between a vesicular igneous rock and a nonvesicular igneous rock?
Vesicular rocks contain lots of small cavities, usually filled with air. Non- vesicular ones don't have these holes. Vesicles are formed when magma suddenly rushes out on to the surface and its dissolved gases come out of solution, blowing bubbles in the liquid rock which are preserved as it cools quickly and sets. An example of a vesicular rock is pumice.
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