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What is an ingenous rock?
an ingenous rock is type of rock formed when lava or magma cools and hardensIt's igneous rock, not ingenious rock. Igneous rock is lava that has hardened into stone. Two examples are obsidian and pumice.
What are two processes a rock must undergo before it can become in an igneous rock?
Two processes a rock must undergo before becoming an igneous rock are melting, where the rock is heated to a point where it turns into magma, and cooling, where the magma solidifies to form an igneous rock.
What is the name of igeneos rock?
There are many varieties of igneous rock. Igneous means it formed as a result of volcanic activity (the word igneous comes from the same root word as ignite) which produces extreme heat. Two main types of igneous rocks are intrusive (cooled gradually underground) and extrusive (cooled more rapidly at or near the surface.) Common examples of igneous rocks include granite, pumice, obsidian, basalt, diorite, andesite.
What is an igeous rock?
Igneous rock is a type of rock that forms from the cooling and solidification of magma or lava. It can be classified into two main types: intrusive igneous rocks, which form below the Earth's surface, and extrusive igneous rocks, which form on the Earth's surface. Some common examples include granite, basalt, and obsidian.
A lava flow is an example of an igneous rock one of the two main igneous rock groups?
It is an example of extrusive igneous rock.
What are two examples of igneous rock?
Granite and Basalt.
What is an ingenous rock?
an ingenous rock is type of rock formed when lava or magma cools and hardensIt's igneous rock, not ingenious rock. Igneous rock is lava that has hardened into stone. Two examples are obsidian and pumice.
What is igneous rock?
Igneous rock is one of the three main rock types based on the method of its formation. It is also referred to as plutonic or volcanic rock depending on where it formed. In a nutshell, to be classified as igneous, a rock must have crystallized and solidified from molten rock (magma) either below ground (intrusive igneous rock) or at or near the surface (extrusive igneous rock).
What type of igneous rocks are there?
There are two main types of igneous rocks: intrusive (plutonic) rocks which form beneath the Earth's surface through slow cooling of magma, and extrusive (volcanic) rocks which form on or above the Earth's surface through rapid cooling of lava. Examples of intrusive igneous rocks include granite and diorite, while examples of extrusive igneous rocks include basalt and rhyolite.
What are two examples of fined grained igneous rocks?
Basalt and rhyolite are examples of fine-grained igneous rocks.
What are two examples of fine-grained igneous rocks?
Basalt and rhyolite are examples of fine-grained igneous rocks.
Where do igneous rock c?
TWO rock get mixed togather
A laccolith is an example of a(n) igneous rock (one of the two main igneous rock groups).?
intrusive
What are two processes a rock must undergo before it can become in an igneous rock?
Two processes a rock must undergo before becoming an igneous rock are melting, where the rock is heated to a point where it turns into magma, and cooling, where the magma solidifies to form an igneous rock.
What are two main classifications of igneous rocks?
The two types of igneous rock are are intrusive and extrusive, depending on where they form. Intrusive igneous rock forms underground from slow cooling magma. Extrusive igneous rock forms at or near the surface from quick cooling lava.
Which two rocks could be cut into building blocks to make walls of buildings?
Igneous rock and Meta-igneous rock.
What is the name of igeneos rock?
There are many varieties of igneous rock. Igneous means it formed as a result of volcanic activity (the word igneous comes from the same root word as ignite) which produces extreme heat. Two main types of igneous rocks are intrusive (cooled gradually underground) and extrusive (cooled more rapidly at or near the surface.) Common examples of igneous rocks include granite, pumice, obsidian, basalt, diorite, andesite.
