
Differentiate between metallic and non-metallic minerals with examples.
Answer
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Hint:
The terms metallic minerals and non-metallic itself defines the presence of metals inside the elements. It also differs in terms of the formation of new products after melting them.
Complete solution:
The metallic minerals can be defined as the minerals that contain the metals in raw form. They also lead to the formation of a new product or element when they are melted to a certain melting point. The metallic minerals are generally found in the igneous or metamorphic rocks. Some of the examples of igneous rocks are andesite, basalt, pumice, and dacite. Some of the examples of metamorphic rocks include Quartzite, marble, Gneiss, and phyllite. The metallic minerals are also the good conductor of heat and electricity. They are highly ductile and malleable in nature. They are also very lustrous. On the other hand, nonmetallic minerals do not lead to the formation of any other product when they are melted. And they are usually found in the fold mountains and sedimentary rocks. They are also bad conductors of heat and electricity. When the non-metallic minerals are molded into a particular shape, they break down and are not ductile.
Additional Information – When the organic particles are collected or deposited at a particular surface of the earth, they lead to the formation of sedimentary rocks. Some of the examples of sedimentary rocks are sandstone, shale, and limestone.
Note:
Due to the collision of two or more tectonic plates, the fold mountains are formed. Some of the important examples of the fold mountains are the Alps mountains, the Himalayas, and Andes mountains.
The terms metallic minerals and non-metallic itself defines the presence of metals inside the elements. It also differs in terms of the formation of new products after melting them.
Complete solution:
The metallic minerals can be defined as the minerals that contain the metals in raw form. They also lead to the formation of a new product or element when they are melted to a certain melting point. The metallic minerals are generally found in the igneous or metamorphic rocks. Some of the examples of igneous rocks are andesite, basalt, pumice, and dacite. Some of the examples of metamorphic rocks include Quartzite, marble, Gneiss, and phyllite. The metallic minerals are also the good conductor of heat and electricity. They are highly ductile and malleable in nature. They are also very lustrous. On the other hand, nonmetallic minerals do not lead to the formation of any other product when they are melted. And they are usually found in the fold mountains and sedimentary rocks. They are also bad conductors of heat and electricity. When the non-metallic minerals are molded into a particular shape, they break down and are not ductile.
Additional Information – When the organic particles are collected or deposited at a particular surface of the earth, they lead to the formation of sedimentary rocks. Some of the examples of sedimentary rocks are sandstone, shale, and limestone.
Note:
Due to the collision of two or more tectonic plates, the fold mountains are formed. Some of the important examples of the fold mountains are the Alps mountains, the Himalayas, and Andes mountains.
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