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Igneous and metamorphic rocks.

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How are cubic orthorhombic and tetragonal crystals different?

Cubic, orthorhombic, and tetragonal crystals differ primarily in their symmetry and unit cell dimensions. Cubic crystals have equal lengths in all three axes and exhibit three axes of symmetry, while orthorhombic crystals have three unequal axes that are all at right angles to one another. Tetragonal crystals, on the other hand, have two axes of equal length and one that is different, also maintaining right angles between the axes. These differences in dimensional ratios and symmetry lead to distinct physical properties and crystal forms.


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The size of crystals is primarily determined by temperature, concentration of the solute, and the rate of cooling or evaporation. Higher temperatures can increase solubility, allowing larger crystals to form as the solution cools. A higher concentration of solute provides more material for crystal growth, while slower cooling or evaporation rates generally lead to larger crystals, as they allow more time for atoms to arrange into an orderly structure.


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How can the three crystals could be found in all three rocks at different times?

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Is three dimensional order present in liquid crystals?

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