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Magma traps in gases which create a buildup of pressure like air bubbles do

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14y ago

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What happens to the gases in it as magma rises toward the surface?

As magma rises, the gases contained within expand due to the decrease in pressure on them as they rise. This creates bubbles that float through the magma, Like the sudden decrease in pressure on the gas in a carbonated beverage when opening, it's container releases a mass of rising bubbles.


What happens to the dissolved gases in magma as the magma ascends towards the surface of earth?

As magma rises, the gases contained within expand due to the decrease in pressure on them as they rise. This creates bubbles that float through the magma, Like the sudden decrease in pressure on the gas in a carbonated beverage when opening, it's container releases a mass of rising bubbles.


What are the spherical or elongated openings seen in many aphanitic rocks left by escaping gas bubbles as magma solidifies?

These are called vesicles, which are voids left by gas bubbles escaping from magma as it solidifies. They are commonly seen in aphanitic rocks like basalt and andesite.


Why do Jews behave like Jews?

Perhaps you care to elaborate...if not, then ask yourself: Why do Frenchmen behave like Frenchmen Why do Germans behave like Germans Why do Gambians behave like Gambians Why do Norwegians behave like Norwegians Why do Nepalese behave like Nepalese Why do Venezuelans behave like Venezuelans. Get the point?


Why do holes form in some extrusive rock?

the holes in extrusive igneous rocks (lava) are called vesicles. They are formed by gas escaping from the rock when molten, leaving bubbles in the melt which which may be preserved when the lava solidifies


Why is magma stiffer than lava?

Magma is typically stiffer than lava because it contains more gas bubbles and crystal structures that can restrict flow. When magma rises to the surface and cools, the gas bubbles escape and the crystal structures align, allowing lava to flow more easily.


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What is the texture of cooling magma?

Cooling magma can have a variety of textures, depending on factors like mineral content, cooling rate, and the specific type of magma. Common textures include aphanitic (fine-grained), phaneritic (coarse-grained), porphyritic (mixed grain sizes), glassy (amorphous), or vesicular (with gas bubbles). Each texture provides clues about the conditions under which the magma cooled and solidified.


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They behave like very fierce and very angry.


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Which set of magma conditions produces the most explosive eruptions?

Magma that is high in silica content and gas bubbles is most likely to produce the most explosive eruptions. This type of magma creates high viscosity, which traps gas bubbles and builds up pressure until it violently explodes. These eruptions typically occur at stratovolcanoes like Mount St. Helens.


What state of matter is magma?

slime is a liquid. it has a definite volume but not a definite shape. and when you leave it on a flat surface, it spreads like a puddle. specifically, slime is a non newtonian fluid. non newtonian means that it doesn't behave like we think it should behave.