Amphibole is a group of inosilicate minerals characterized by their double-chain silicate structure, which gives them a complex composition often including iron, magnesium, calcium, and aluminum. They typically exhibit a prismatic crystal habit and can be found in a range of colors, including dark green, black, and brown. Amphiboles are known for their cleavage at angles of about 124 and 56 degrees, and they are commonly found in metamorphic and igneous rocks. These minerals are important in geology as they can provide information about the conditions under which rocks formed.
One physical property that can be used to distinguish quartz from amphibole is hardness. Quartz has a hardness of 7 on the Mohs scale, while amphibole minerals like hornblende have a hardness ranging from 5 to 6. Additionally, quartz typically has a glassy luster, while amphibole minerals have a dull to vitreous luster.
The rock can be classified as a basalt if it is dark-colored and has a fine-grained texture, given its high plagioclase feldspar content and the presence of amphibole and biotite. Alternatively, if it has a lighter color, it could be classified as a diorite or andesite, depending on the specific proportions of minerals and its overall composition. The significant presence of amphibole and biotite suggests a more intermediate composition, potentially placing it in the andesite category. Overall, further details about its color and specific mineral characteristics would aid in precise classification.
Fluorite is a mineral that is hard enough to scratch calcite, which has a hardness of 3 on the Mohs scale, as fluorite has a hardness of 4. However, fluorite cannot scratch amphibole, which typically has a hardness ranging from 5 to 6. Thus, fluorite fits the criteria of being harder than calcite but softer than amphibole.
Granite and diorite contain both.
Amphiboles are minerals containing mostly silicon, oxygen, iron, and magnesium.
Granite is a rock containing both amphibole and potassium feldspar.
The individual minerals in the Amphibole group are between 5-6 on the Mohs scale.
The Amphibole chemical formula is Mg,Fe,Ca,Na)2-3(Mg,Fe,Al)5(Si,Al)8O22OH2.
One physical property that can be used to distinguish quartz from amphibole is hardness. Quartz has a hardness of 7 on the Mohs scale, while amphibole minerals like hornblende have a hardness ranging from 5 to 6. Additionally, quartz typically has a glassy luster, while amphibole minerals have a dull to vitreous luster.
An Amphibole (eg asbestos).
An arfvedsonite is a rare sodium amphibole mineral.
plagioclase feldspar, pyroxene, horneblende (amphibole)
No, amphibole minerals typically have a hardness of around 5 to 6 on the Mohs scale, while glass has a hardness of about 5.5. This means that amphibole is not hard enough to scratch glass.
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Amphibole is a group of inosilicate minerals that are typically dark-colored and composed of double-chain silicate structures. They are commonly found in metamorphic and igneous rocks, and some types of amphibole, such as hornblende, can also be present in hydrothermal veins. Amphiboles have a variety of physical properties and are known for their long, prismatic crystal shapes.
amphibole
The rock can be classified as a basalt if it is dark-colored and has a fine-grained texture, given its high plagioclase feldspar content and the presence of amphibole and biotite. Alternatively, if it has a lighter color, it could be classified as a diorite or andesite, depending on the specific proportions of minerals and its overall composition. The significant presence of amphibole and biotite suggests a more intermediate composition, potentially placing it in the andesite category. Overall, further details about its color and specific mineral characteristics would aid in precise classification.