the escape of gases during cooling
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.
Textures of volcanic rocks include aphantitic (mineral grains are present but microscopic) , porphyritic (some grains are visible to the naked eye), glassy (all or much of the rock lacks a crystalline structure), and vesicular (solidified gas bubbles are present).
Vesicular texture is characterized by the presence of small gas bubbles or vesicles formed during the cooling of magma. Peridotite, being an ultramafic rock primarily composed of olivine and pyroxene, typically forms at greater depths within the Earth's mantle where the pressure is high, preventing the formation of gas bubbles. Consequently, the cooling of peridotite occurs in a solid-state, leading to a dense, granular texture rather than a vesicular one. Thus, vesicular textures are more commonly associated with volcanic rocks that cool rapidly at the surface, allowing gas to escape and form vesicles.
Of or pertaining to vesicles; esp., of or pertaining to the air vesicles, or air cells, of the lungs; as, vesicular breathing, or normal breathing, in which the air enters freely the air vesicles of the lungs., Containing, or composed of, vesicles or vesiclelike structures; covered with vesicles or bladders; vesiculate; as, vesicular coral; vesicular lava; a vesicular leaf., Having the form or structure of a vesicle; as, a vesicular body.
mass production of vesicular and arbuscular mycorrhiza
where did you best hear the vesicular respiratory sounds
in the Vesicular (Graafian) follicle
The tongue can have various textures including smooth, rough, bumpy, and furry. These textures can be influenced by factors such as dehydration, oral health, microbial imbalance, or medical conditions like geographic tongue or oral thrush. It's important to consult a healthcare professional if you notice any unusual textures on your tongue.
Vesicular basalt has small rounded voids called vesicules formed by the molten rock cooling and freezing around pockets of gas. It looks a lot like a rock hard sponge. Non vesicular basalt is a normal solid rock.
Peridotites are invasive rocks formed underneath the earth's surface and the high pressure conditions Dodge gases from forming and getting away
A meteorite can be composed of different materials and so can vesicular basalt, but because of the presence of pores in vesicular basalt a meteorite would likely be heavier, assuming that they have the same volume.
Estrogen