List and define the principal physical properties used to identify a mineral. (E)

Short Answer

Expert verified
The principal physical properties used to identify a mineral include: 1. Color: The visible hue of a mineral, although it can be unreliable due to impurities. 2. Luster: The way a mineral reflects light, categorized as metallic or non-metallic. 3. Hardness: The mineral's resistance to scratching, measured using Mohs scale (1-10). 4. Streak: The color of a mineral's powdered form, determined by rubbing it across a streak plate. 5. Crystal Form: The natural shape of a mineral determined by its internal crystalline structure. 6. Cleavage: A mineral's tendency to break along flat, smooth surfaces due to weak crystal structure points. 7. Fracture: How a mineral breaks when it doesn't exhibit cleavage, occurring irregularly. 8. Specific Gravity: A measure of a mineral's density relative to water, comparing the mass of the mineral to the mass of an equal volume of water.

Step by step solution

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1. Color

: Color is one of the simplest physical properties to observe and can be used as a basic characteristic to help identify a mineral. However, it is not always reliable as some minerals can occur in various colors due to impurities.
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2. Luster

: Luster refers to how a mineral reflects light. There are two main categories of luster: metallic and non-metallic. A metallic luster has a shiny, reflective surface, like metal, while non-metallic lusters can be described as glassy, pearly, silky, etc.
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3. Hardness

: Hardness is a measure of how easily a mineral can be scratched. It is determined based on Mohs scale of mineral hardness, which assigns a number from 1 (softest) to 10 (hardest) based on a mineral's ability to scratch another mineral. For example, Talc has a hardness of 1 and Diamond has a hardness of 10.
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4. Streak

: Streak refers to the color of the powdered form of a mineral. It is determined by rubbing the mineral across a streak plate (unglazed porcelain) and observing the color of the residue left behind. Streak is often more reliable than color for identifying minerals, as it is less affected by impurities.
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5. Crystal Form

: Crystal form refers to the mineral's natural shape when it forms in optimal conditions. The arrangement of atoms within a mineral's crystalline structure determines its crystal form. By examining a crystal's form, it is possible to identify the mineral and gain insight into its internal structure.
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6. Cleavage

: Cleavage refers to a mineral's tendency to break along flat, smooth surfaces. When a mineral has good cleavage, it breaks along consistent planes due to weak points in its crystal structure. Cleavage can be described based on how many planes it occurs along and the angles between those planes.
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7. Fracture

: Fracture is a measure of how a mineral breaks when it does not exhibit cleavage. Unlike cleavage, fractures occur in an irregular manner. Types of fracture include conchoidal (shell-like, smooth curves), splintery, and uneven.
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8. Specific Gravity

: Specific gravity is a measure of a mineral's density relative to water. It is determined by dividing the mass of the mineral by the mass of an equal volume of water. Minerals with a higher specific gravity feel heavier for their size compared to those with a lower specific gravity.

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