You always look to handle your assignment on time. However, it becomes a hassle as you always have many things to do through your studies. Be it attending lectures or extra-curricular activities; you are at times left with very little time to complete your assignments. More so, in the field of mineralogy, you often have a hard time identifying minerals, completing lab reports, or handling their assignments. If you are in this situation, you should contact HelpForHomework for mineralogy help.
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Mineralogy homework is often challenging. If you do not seek expert guidance, mineralogy can be a hassle to understand. For this reason, our company creates custom papers for you so that you get the A+ grade that you need and easily grasp the concepts. When we talk of custom papers, we talk of uniquely and professionally presented solutions free of plagiarism.
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Our mineralogy help specialists are well conversant with the field through studies and experience in academic writing. With their expertise, they are there to help you identify minerals by studying their physical characteristics. While we can use microscopes to identify minerals, it is essential to use physical properties as they are noticeable. I this case, our writers use chemistry and physical characteristics to identify minerals.
The chemistry and bonding of elements influence the physical characteristics of minerals. The most used characteristics in identifying minerals are color and hardness. Color is obvious and noticeable but does not always provide conclusive identification as the other physical properties. When identifying minerals, we observe the following physical properties:
The color of minerals is a vital physical property, but you do not rely on it as some minerals have the same color. For example, Real gold and pyrite have the same color but different chemical compositions. Moreover, some minerals such as quartz have color variations from colorless to orange. The variations are a result of chemical impurities.
The streak of a mineral is the color it produces while in powder form. Observing the streak of a mineral will give reliable information than color. For example, minerals with the same color can have a different streak. However, the property may also be unreliable in identifying minerals as glassy minerals such as obsidian do not have a streak.
Luster is the reflection of light by a mineral on its surface. We use the luster of a mineral to identify whether it is metallic or non-metallic. For example, minerals with shiny opaque surfaces such as gold have a metallic luster. At the same time, minerals that have a glassy, such as quartz, have a non-metallic luster.
There are different types of non-metallic luster, namely:
The specific gravity of a mineral is its density relative to water.
Hardness is the ability of a mineral to resist scratching. We use a standard Mohs Hardness Scale to study the hardness of minerals. The degree of hardness increases from talc (Softest) to Diamond (hardest).
Mohs Hardness Scale
Mineral cleavage is the breakage of minerals along planes of weakness. However, minerals have different cleavages due to differences in chemical bonds.
The chemical bonds do not determine fracture in a mineral. Instead, we describe fracture as a breakage that is not along the planes of weakness. For example, metals fractures are jagged.
Since all minerals are crystalline, they exhibit shapes based on their molecular structure. In this case, mineral shapes reflect the geometry of and symmetry of the internal crystal lattice.
There are other methods of identifying minerals that a vital for every mineralogist. For example, you can use HCL to test for calcite. If you test a mineral and it fizzes, it is evident the mineral might be calcite. Below are some of the methods you can use to identify minerals:
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