Yes, marble can have large crystals because it is a metamorphic rock that forms from the recrystallization of limestone. The size of the crystals in marble can vary depending on the specific conditions under which it formed.
When limestone is heated under pressure, it forms marble. This process, known as metamorphism, occurs when the mineral calcite in the limestone recrystallizes into the interlocking calcite crystals that compose marble.
Heat and pressure turn limestone into marble through the process of metamorphism, where the mineral composition and texture of the rock are changed. This transformation occurs as a result of high temperature and pressure altering the original calcium carbonate minerals of limestone into the interlocking crystals that characterize marble.
Large crystals in a mineral specimen typically form when the mineral has enough time and space to grow without being obstructed by nearby crystals. This often occurs in environments with slow cooling rates or low levels of impurities, allowing the crystals to grow to a considerable size.
Crystals formed from slow cooling typically have larger crystal sizes due to more time for the atoms to arrange in an ordered structure. This results in minerals with well-defined crystal faces and clearer textures, as seen in intrusive igneous rocks like granite and gabbro.
The cost of crystals can vary widely based on their type, quality, and rarity. On average, common crystals like amethyst or quartz can range from $10 to $50 per pound. However, rare or precious crystals such as diamonds or emeralds can cost thousands or even millions of dollars per pound.
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Large mineral crystals are commonly found in igneous rocks, such as granite and pegmatite, where slow cooling allows minerals to grow large. Certain metamorphic rocks, like marble and schist, can also contain large mineral crystals due to high pressures and temperatures. Veins and pockets within rocks can sometimes host large crystals as well.
Marble (with the chemical formula CaCO3) is a crystalline material.
The crystals in marble can vary in size, but they are typically small to medium in size, typically ranging from a few millimeters to a few centimeters. Marble is a metamorphic rock primarily composed of calcite or dolomite crystals that give it its characteristic appearance.
Marble has visible interlocking crystals on a freshly fractured surface, and will fizz when strong vinegar is applied.
Marble is composed of small particles of calcite or dolomite minerals, which are crystalline forms of calcium carbonate. These particles give marble its unique texture and appearance.
When magma coos slowly, it allows large crystals to form. The process of evaporation helps to form crystals.
Limestone can be metamorphosed into marble through the process of recrystallization under high pressure and temperature conditions. The calcite crystals in limestone are transformed into interlocking crystals of calcite or dolomite in marble, resulting in increased hardness and a distinctive pattern and coloration.
Extreme heat and pressure.
Igneous rocks can have both small and large crystals, depending on how quickly they cool. If an igneous rock cools slowly beneath the Earth's surface, it can form large crystals, while rapid cooling at the Earth's surface or in an eruption can result in small or no visible crystals.
When limestone is heated under pressure, it forms marble. This process, known as metamorphism, occurs when the mineral calcite in the limestone recrystallizes into the interlocking calcite crystals that compose marble.