Vesicular igneous rocks cool quickly from magma, resulting in pockets of trapped gas or gas bubble imprints that make it appear porous. Pumice and scoria are examples of igneous rock with vesicles.
Pumice
would fit that description well.
Many basalts, pumice, and scoria contain vesicles.
its the earthes crust because back in the days the earth was pure lava there for it causes vesicular texture
At the surface of a lava flow
Pumice
Pumice
pumice
Porphyritic texture is a feature of some igneous rocks, not sedimentary rocks.
A vesicular texture is one where there are small voids within the igneous rock. These tend to form in extrusive igneous rocks due to the loss of confining pressure which causes gasses dissolved in the molten material to come out of solution or exsolve. These gasses form bubbles within the cooling lava and can become trapped if the lava cools rapidly, leaving a permanent gas bubble or void space within the solidified igneous rock.
Scoria and pumice are vesicular igneous rocks.
vesicular rhyolite, rhyolite, granite, and pegmatite!
Vesicles are rounded spaces that appear in igneous rocks from the solidification of the magma around gas bubbles. Pumice, scoria, and vesicular basalt are igneous rocks that contain vesicles.
Porphyritic texture is a feature of some igneous rocks, not sedimentary rocks.
* Vesicular rock texture is generally displayed in extrusive igneous rocks which contain many vesicles of trapped air, such as pumice or scoria. * Igneous rocks containing holes which were produced as gases escaped from the upper part of lava flow.
* Vesicular rock texture is generally displayed in extrusive igneous rocks which contain many vesicles of trapped air, such as pumice or scoria. * Igneous rocks containing holes which were produced as gases escaped from the upper part of lava flow.
Igneous rocks are identified by first looking at the color index. Felsic igneous rocks contain mostly potassium feldspar. Intermediate igneous rocks contain mostly plagioclase feldspar. Mafic igneous rocks contain pyroxene, olivine, and plagioclase feldspar. Ultra mafic igneous rocks contain mostly olivine. Then igneous rocks are identified based on texture. For example, the texture of igneous rocks can be aphanitic, pegmatitic, phaneritic, glassy, vesicular, etc.
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
A)fossils B)small grains C)vesicular texture D) porphyrtic texture Its one of these answers i chose D. because its more likely to have it. Idk if its the right answer.
Scoria and pumice are vesicular igneous rocks.
vesicular rhyolite, rhyolite, granite, and pegmatite!
A vesicular texture is one where there are small voids within the igneous rock. These tend to form in extrusive igneous rocks due to the loss of confining pressure which causes gasses dissolved in the molten material to come out of solution or exsolve. These gasses form bubbles within the cooling lava and can become trapped if the lava cools rapidly, leaving a permanent gas bubble or void space within the solidified igneous rock.
== == Igneous rocks have formed from molten material either above (extrusive) or below (intrusive) ground level. Extrusive igneous rocks include obsidian, basalt, and rhyolite; intrusive igneous rocks include gabbro and granite.
Crystalline texture.
Obsidian