Explanation:
Talc is the softest mineral that can be measured using the Mohs scale (a one). The maximum score is 10, which is represented by the diamond. At the same time, the scores for fluorite and gypsum are two and four, respectively. Minerals may always scrape other minerals with a lower Mohs rating.
Explanation:
Minerals are categorized according to their chemical makeup and physical characteristics, whereas rocks are classified according to their formation and their minerals.
Explanation:
Mineral-like compounds without a crystalline structure are known as mineraloids. They are frequently discovered in rocks. Polymorphs are inorganic solids that contain two or more minerals with dissimilar crystalline structures.
Explanation:
Chemical composition is not a physical characteristic that is used to categorize minerals. Luster, hardness, cleavage, streak, and shape are the five main physical characteristics used to classify minerals. The chemical makeup of minerals has led to a different classification scheme.
Explanation:
An unglazed porcelain tile is used for a streak test to determine a mineral's natural color. The paper does not have suitable physical characteristics for the streak test. Since streak tests can show a color different from the substance's exterior hue, external observation (examining the mineral's outer surface) is not enough to determine accurate color. Finally, color is not determined by the shine test.
Explanation:
Petrology does not include the field of mineralogical petrology. The different types of rocks, such as metamorphic, igneous, and sedimentary, are studied by petrologists. The geochemistry of materials exposed to high temperatures and pressures is also reviewed by some petrologists, known as experimental petrologists. Petrologists do not look at minerals; mineralogists do.
Explanation:
Minerals with a metallic sheen include galena, pyrite, and magnetite. A mineral having a greasy luster is an opal, while diamonds have an adamantine brilliance. Minerals with a pearly sheen include muscovite and stilbite. There are additionally dull, smooth, waxy, and sub-metallic lusters.
