Magma traps in gases which create a buildup of pressure like air bubbles do
No
Biological molecules were trapped in molecular bubbles. Cell like structures formed from molecular bubbles-apexx
Water vapor (steam) is inside the bubbles that form inside boiling water. The bubbles that form prior to boiling are mostly dissolved gases escaping from the water.
following are the three factors affecting volcanic eruption or volcanic activity 1. temperature rise in interior which will cause rocks to melt 2. reduction in pressure which has already increased the melting temperature of rocks. 3. addition of fluids like water which helps in decreasing melting temperature of rocks
Molten rock in any of Earth's layers is called magma. The mantle is actually composed of solid, but very hot and plastic-like rock.
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.
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.
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.
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?
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
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.
they behave like idiots
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.
They behave like very fierce and very angry.
ducks behave like kid
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.
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.