What are the three types of rocks ? Ans: They are three types of rocks are:- * Ingneous rock *Sedimentry rock *Metamorpic rock..
Answers
Answer:
There are three types of rocks:-
Explanation:
- Igneous rocks :- it is formed under the surface of earth.
- Sedimentary rocks:- it is formed outside the surface of earth.
- Metamorphic rocks:- it is formed by igneous and sedimentary rocks.
Answer:
Generally speaking, there are three types of rocks:-
1) Igneous Rocks:- The rocks which are formed when lava cools down, are known as igneous rocks. In terms of origin, there are two types of igneous rocks:
- Plutonic Rocks:- These are igneous rocks, which are formed at some depths in the earth’s crust. For ex- granite, diorite and gabbro.
- Volcanic Rocks:- These are molten rocks which are poured out of volcanoes as lava. They solidify rapidly on the earth’s surface. For ex- basalt.
2) Sedimentary Rocks:- Sedimentary rocks are formed from sediments which accumulated over long periods, usually under water. These rocks may be classified into three major categories with their origin and composition:
- Mechanically Formed:- These rocks have been formed from the accumulation of materials derived from other rocks which have been cemented together. For ex- sandstone, quartz
- Organically Formed:- These rocks are formed from the remains of living organisms such as coral or shellfish, whose fleshy parts have been decomposed. For ex- limestone, chalk, coal
- Chemically Formed:- Such rocks are precipitated chemically from solutions of one kind or another. For ex- gypsum, potash, nitrates
3) Metamorphic Rocks:- When igneous or sedimentary rocks change inside the earth due to immense heat and pressure, they tend to form Metamorphic Rocks. The main examples are:
- Clay changes to slate
- Limestone changes to marble
- Sandstone changes to quartzite
- Granite changes to gneiss
- Shale changes to schist
- Coal changes to graphite
Note:- Coal may also change to diamond but only when the amount of heat and pressure provided is at a very high rate.
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