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In general, minerals can form in two ways: through the crystallization of melted materials, and through the crystallization of materials dissolved in water.
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Five different ways in which minerals are used are1.electronics,2.jewelry,3.coins,4.in construction,5.in foods
They are divided into puddingstone and somipone. Puddingstone is made of tiny minerals but somipone is made up of HUGE minerals.
All minerals in the silicate group share a common structural feature: they contain silicon (Si) and oxygen (O) in varying ratios, forming the silicate tetrahedron (SiO₄). This tetrahedron can link together in different ways, resulting in various silicate structures, such as chains, sheets, or three-dimensional frameworks. Additionally, silicate minerals are typically found in igneous, metamorphic, and sedimentary rocks, making them the most abundant group of minerals in the Earth's crust.
You can tell if a mineral is a mineral by its characteristics: *color *luster *streak *hardness *cleavage/fracture *crystalline structure
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Minerals break in three main ways: cleavage, fracture, and splintery fracture. Cleavage occurs when minerals break along flat planes defined by their crystal structure. Fracture happens when minerals break irregularly without any specific pattern. Splintery fracture is a type of fracture where the broken piece has sharp edges or splinters.
The most common way is when water that got into cracks freezes and expands, breaking apart the rock. Other simple ways include minerals dissolving in moving water (especially with soluble minerals like calcium carbonate = limestone.)
minerals differ in appearance and texture
Feel their pulse, listen for breathing, and look for their chest moving.
In general, minerals can form in two ways: through the crystallization of melted materials, and through the crystallization of materials dissolved in water.