the slower something evaporates the larger the crystals
It is true that lava cools quickly and forms minerals with small crystals.
Granite cools slowly underground, allowing for the formation of larger crystals. This slow cooling process contributes to its coarse-grained texture and characteristic patterns.
Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.
It depends on the cooling rate of the magma. If the magma cools slowly underground, large crystals can form, creating intrusive igneous rocks. If the magma cools rapidly on the Earth's surface, small crystals or glassy textures can result in extrusive igneous rocks.
Generally, large crystals represent slow cooling rates and small crystals represent fast cooling rates. Crystals need time to form and since extrusive rocks cool very quickly, they have very tiny crystals and some don't even have crystals because the rate of cooling was so fast that crystals didn't have time to nucleate. On the other hand, intrusive rocks cool rather slowly allowing crystals to grow.
Evaporating a copper sulphate solution you can obtain anhydrous crystals of CuSO4. Increasing the temperature CuSO4 will be thermally dissociated.
No. Intrusive igneous rocks have large crystals because they cool slowly.
If the lava cools quickly the crystals will be smaller than if it cooled slowly.
Porphyry cooled slowly, allowing large crystals to form within a fine-grained matrix. This slow cooling process gives porphyry its characteristic appearance of large crystals embedded in a finer grained groundmass.
It is true that lava cools quickly and forms minerals with small crystals.
Granite cools slowly underground, allowing for the formation of larger crystals. This slow cooling process contributes to its coarse-grained texture and characteristic patterns.
Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.
When liquid rock cools slowly, crystals will be bigger because there is more time for the crystals to grow and develop before the rock solidifies. In contrast, when liquid rock cools quickly, crystals are smaller because there is less time for them to form and grow.
As a rule of thumb, oils that evaporate quickly are considered emotionally uplifting, while slowly-evaporating oils are thought to have a calming effect.
Igneous rocks that cool slowly have larger crystals because there is more time for the crystals to grow and develop before the rock solidifies. In contrast, rocks that cool quickly have smaller crystals due to limited time for crystal growth during the rapid cooling process.
Borax crystals grow better in a refrigerator because the lower temperature slows down the rate of evaporation, allowing the crystals to form more slowly and evenly. This helps to prevent impurities from forming in the crystals and results in larger, more well-defined crystals.
Crystals can grow at different speeds depending on various factors such as temperature, pressure, and chemical composition. Some crystals may form quickly under ideal conditions, while others may take a longer time to grow. Overall, the growth rate of crystals can vary widely from fast to slow.