Answer :
Rocks with a vesicular texture are characterized by the presence of vesicles, which are small cavities or bubbles that formed as gas was trapped in molten lava during volcanic eruptions.
These rocks are commonly found in volcanic or extrusive igneous features, such as lava flows, cinder cones, and volcanic necks.Lava flows are large, sheet-like formations of solidified lava that can extend for many miles from a volcanic vent. When lava flows rapidly cool and solidify, gases that were trapped in the lava can escape and leave behind vesicles. As a result, rocks with a vesicular texture can be found in the upper portion of lava flows where cooling was most rapid.
Cinder cones are small, steep-sided volcanic cones that are formed from explosive eruptions of gas-rich magma. As the magma is ejected into the air, it cools and solidifies, forming small, pyroclastic fragments known as cinders. These cinders can contain vesicles, resulting in a vesicular texture.
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