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.
Amphiboles are minerals containing mostly silicon, oxygen, iron, and magnesium.
Granite and diorite contain both.
A rock containing a moderate amount of biotite, amphibole, and pyroxene could be a diorite. Diorite is an intermediate intrusive igneous rock with a composition between that of granite and gabbro, which typically contains these minerals in varying amounts.
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.