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What type of rock has little to no grain development and has a vesicular texture?
A rock with little to no grain development and a vesicular texture is typically called a vesicular rock. It is formed from a volcanic eruption, where gases trapped in the lava create bubbles or vesicles. The most common example is vesicular basalt.
Is pumice rock vesicular and glassy?
Yes. Pumice is so fine-grained, often times it's crystals are vesicular and glassy.
What type of volcanic rock is extremely vesicular and glassy?
Obsidian is a type of volcanic rock that is extremely vesicular and glassy in appearance. It forms when lava cools quickly with minimal crystal growth, resulting in a smooth texture and shiny appearance.
What structure in the ovary contains the developing oocyte egg?
in the Vesicular (Graafian) follicle
What rock is formed from low silica magma?
Basalt.Vesicular texture describes an aphanitic rock characterized by preservation of cavities (vesicles) originally filled by escaping gases. Highly vesicular basalts (low-silica magma) are called scoria, whereas highly vesicular rhyolite (high-silica magma) is known as pumice
Why vesicular texture is associated with peridotites?
Peridotites are invasive rocks formed underneath the earth's surface and the high pressure conditions Dodge gases from forming and getting away
Why vesicular texture is not associated with peridotites?
Peridotites are invasive rocks formed underneath the earth's surface and the high pressure conditions dodge gases from forming and getting away
An igneous rock with lots of gas bubble voids has a?
It has a vesicular texture.
What type of rock has little to no grain development and has a vesicular texture?
A rock with little to no grain development and a vesicular texture is typically called a vesicular rock. It is formed from a volcanic eruption, where gases trapped in the lava create bubbles or vesicles. The most common example is vesicular basalt.
What is vesicular texture in rock?
* 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.
How is the vesicular texture of an igneous rock formed?
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.
Is pumice rock vesicular and glassy?
Yes. Pumice is so fine-grained, often times it's crystals are vesicular and glassy.
What type of volcanic rock is extremely vesicular and glassy?
Obsidian is a type of volcanic rock that is extremely vesicular and glassy in appearance. It forms when lava cools quickly with minimal crystal growth, resulting in a smooth texture and shiny appearance.
Does lava have gas?
Yes. Gases may be trapped in lava. These may form bubbles on the surfaces of a flow, giving it a vesicular texture when it cools.
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.
Which features are extrusive igneous rocks least likely to have?
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.
Igneous feature would you find rocks with a vesicular texture?
You would typically find rocks with vesicular texture in igneous features such as volcanic necks, lava flows, and volcanic ash deposits. Vesicles are voids or cavities left behind by gas bubbles trapped in the cooling magma.
