There are several chemistry websites online with some helpful and resourceful information about crystal structures.You can also locate information on this in specific magazines at your local bookstore.
Yes, the way a mineral cleaves is related to its crystal structure. Cleavage is the way a mineral breaks along planes of weakness due to structural arrangements of atoms within the crystal lattice. Different mineral crystal structures exhibit specific cleavage patterns that can help identify the mineral.
It is a box shape. Here is some more info on the subject matter pertaining to your specific circumstances:Space group: P63/mmc (Space group number: 194)Structure: hcp (hexagonal close-packed)Cell parameters: a: 266.49 pm
Two examples of cubic crystal systems are the face-centered cubic (FCC) structure, found in metals such as copper and aluminum, and the body-centered cubic (BCC) structure, found in metals such as iron and chromium.
Crystals can have a variety of textures depending on their structure and composition. Some common crystal textures include smooth, rough, jagged, and glassy. The texture of a crystal is determined by factors such as how quickly it formed, its internal arrangement of atoms, and any external factors that may have influenced its growth.
Diamonds are clear because they are composed of carbon atoms arranged in a crystal lattice structure that allows light to pass through without significant interference. This crystal structure is highly ordered and uniform, which results in the transparency and brilliance of diamonds.
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
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Size is a factor of habit, crystal structure, and temperature.
The crystal system of rubies is trigonal, which means that the crystal has three equal axes that are all at 60 degrees to each other. This crystal structure is responsible for some of the unique optical properties of rubies, such as the way they reflect and refract light.
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Yes, the way a mineral cleaves is related to its crystal structure. Cleavage is the way a mineral breaks along planes of weakness due to structural arrangements of atoms within the crystal lattice. Different mineral crystal structures exhibit specific cleavage patterns that can help identify the mineral.
Coal does not have a crystalline structure, crystalline structures are only caused when and untainted sample solidifies from another state, coal is caused by pressure and heat applied over thousands of years to dead animals, as a result it contains high levels of impurities and has a very unpredictable and random structure.
Cleavage: The way a mineral breaks along certain planes is determined by its crystal structure. Twinning: Some minerals form twinned crystals due to specific arrangements of atoms in the crystal lattice. Color: The arrangement of atoms in a crystal lattice can contribute to the absorption and reflection of light, affecting the color of the mineral.
Amorphous minerals lack an ordered atomic arrangement or crystal structure. These minerals are generally formed through rapid cooling or in environments where there is little time for crystal growth to occur, resulting in a disordered arrangement of atoms. Examples include obsidian, opal, and some forms of glass.
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No, all igneous rocks have a crystal structure because they form from the cooling and solidification of molten rock material. The size of the crystals can vary depending on the rate of cooling, but some crystals will always form in igneous rocks.
Yeah, you can melt anything if you get it hot enough. Be sure not to confuse the terms crystal and mineral. A crystal is made of a mineral, the fact that it is a crystal, simply means that it's atoms are arranged in a periodical and static way, in the crystal structure. This structure falls apart as soon as the mineral melts, so a molten mineral can not be called a crystal.