When samples of magma are cooled quickly they do not have time to develop any crystal structure. The liquid sample will turn into a glassy solid. Under natural conditions this rapid cooling would result in a material known as obsidian. This is a black to brownish material that has all the characteristics of glass; conchoidal fracture, hardness, light transmission in thin edges, etc. depending on the type of magma.
Obsidian, even though seemingly a solid, is called a super-cooled liquid, just like window glass. There is no crystal structure at first but over a long period of time crystals will start to grow within the obsidian. This is known as "snowflake obsidian" because the crystals are suspended like flakes in ice. It has been said that there is no obsidian older than 10,000 years as it has all crystallized in that time.
very coarse
When magma cools, it can solidify into different types of igneous rock depending on the cooling rate. Slow cooling can form coarse-grained rocks like granite, while rapid cooling can form fine-grained rocks like basalt. If the magma cools very quickly at the Earth's surface, it can solidify into volcanic glass like obsidian.
Intrusive igneous rocks are formed by slow cooling magma below the earth's surface. Extrusive igneous rock is formed by magma cooling quickly, at or near the surface.
No, glassy igneous rocks form when magma cools so quickly that mineral crystals do not have time to form. This rapid cooling prevents the atoms in the magma from arranging themselves into a crystalline structure, resulting in an amorphous, glassy texture.
Komatiite is an extrusive igneous rock that forms from very hot magma erupting onto the surface of the Earth and cooling quickly. It is characterized by its high magnesium content and typically forms where there are high mantle temperatures.
very coarse
When magma cools, it can solidify into different types of igneous rock depending on the cooling rate. Slow cooling can form coarse-grained rocks like granite, while rapid cooling can form fine-grained rocks like basalt. If the magma cools very quickly at the Earth's surface, it can solidify into volcanic glass like obsidian.
Very deep underground.
Intrusive igneous rocks are formed by slow cooling magma below the earth's surface. Extrusive igneous rock is formed by magma cooling quickly, at or near the surface.
If you are asking about how they were formed magma from volcano that are shot in the air of quickly spewed out causing the magma to cool very quickly forming a very smooth surface on obsidian. Becuase the magma cooled so fast it couldn't slowly cool into a rough textured rock.
Yes obsidian is glassy because it cooled very fast.
It forms very small crystals, not visible without magnification.
yes, slowly cooling magma will crystallize (granite). If it cools quickly, the lava will have very small crystals and will contain air pockets (pumice, if it is cooled in chunks) or can even be very thin, like hair, very straight. (Pele's hair)
when magma cools fast you get smaller crystals when it cools slow you get large crystals its very simple
No, glassy igneous rocks form when magma cools so quickly that mineral crystals do not have time to form. This rapid cooling prevents the atoms in the magma from arranging themselves into a crystalline structure, resulting in an amorphous, glassy texture.
Komatiite is an extrusive igneous rock that forms from very hot magma erupting onto the surface of the Earth and cooling quickly. It is characterized by its high magnesium content and typically forms where there are high mantle temperatures.
Yes obsidian is glassy because it cooled very fast.