Conclusion correctly identifying a mineral or rock is

Conclusion: Correctly identifying minerals and rocks is important for understanding terrain around the world. For example, if there is a large amount of igneous rocks somewhere, it can be concluded that there is certainly a certain type of volcanic activity in part of the history. We can not reach this conclusion unless we know how to correctly identify rocks and minerals. First, by discriminating between color and gloss, we will judge the physical appearance of each rock and mineral. Next, we calculated hardness, mass and volume of each mineral. Once I know the quantity and quality, I started calculating the density. But my figures are not accurate. My gauge does not represent an accurate weight, it gives a rounded weight, so all calculations are slightly off. After finding the density I dropped a small amount of vinegar on each rock to see how they responded. All of my accurate findings are listed under "Data". That is, my understanding of minerals and rocks grew exponentially. With each property you can identify each mineral and rock. Once you complete this lab, you will change the quality of each mineral obtained. Because I find a better ratio, my calculation may be accurate. Minerals use the collected data to identify each mineral sample. They are quartz, feldspar, plaster, galena and iron ore.

2. Which characteristics are most useful and not practical for mineral identification? Description The most useful properties for identifying minerals are stripes, cleavage / cracking, and hardness. Since some minerals have almost the same physical properties as other minerals, it is difficult to judge what minerals are, by observing minerals. Streaks, stiffness and cleavage / bone fractures help identify distinguishable things in the eyes.

All rocks except obsidian and coal are made of minerals. (Obsidian is a glass volcanic rock and is made of organic carbon.) Most rocks contain various minerals which are mixtures of certain kinds of rocks. When specifying a rock, you first need to identify the various minerals that make up the rock. Minerals are natural inorganic solids with defined chemical composition and lattice structure. Thousands of minerals have been confirmed on the earth, but only 10 kinds of minerals, such as plagioclase, quartz, feldspar, amphibolite, pyroxene, peridot, calcite, biotite and garnet, constitute the crust. Most of the clay.

Conclusion: Correctly identifying minerals and rocks is important for understanding terrain around the world. For example, if there is a large amount of igneous rocks somewhere, it can be concluded that there is certainly a certain type of volcanic activity in part of the history. We can not reach this conclusion unless we know how to correctly identify rocks and minerals. First, by discriminating between color and gloss, we will judge the physical appearance of each rock and mineral. Next, we calculated hardness, mass and volume of each mineral. Once I know the quantity and quality, I started calculating the density. But my figures are not accurate. My gauge does not represent an accurate weight, it gives a rounded weight, so all calculations are slightly off. After finding the density I dropped a small amount of vinegar on each rock to see how they responded. All of my accurate findings are listed under "Data". Mineral 1