Sure, here are some examples of rocks that solidified within Earth's crust:

1. Granite: This is a common type of intrusive, felsic, igneous rock which is granular and phaneritic in texture. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy.

2. Diorite: This is an intrusive igneous rock composed principally of the silicate minerals plagioclase feldspar, biotite, hornblende, and/or pyroxene.

3. Gabbro: This is a phaneritic (coarse-grained), mafic intrusive igneous rock. It is the most abundant rock in the deep oceanic crust and can be very diverse in composition.

4. Peridotite: This is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. It is an important rock type because the Earth's mantle is predominantly composed of it.

5. Quartz Diorite: This is an intrusive igneous rock similar to diorite, but containing a larger amount of quartz.

These rocks all solidify within the Earth's crust from magma, which is why they are known as intrusive igneous rocks.

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Sure, here are some examples of rocks that solidified within Earth's crust:

1. Granite: This is a common type of intrusive, felsic, igneous rock which is granular and phaneritic in texture. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy.

2. Diorite: This is an intrusive igneous rock composed principally of the silicate minerals plagioclase feldspar, biotite, hornblende, and/or pyroxene.

3. Gabbro: This is a phaneritic (coarse-grained), mafic intrusive igneous rock. It is the most abundant rock in the deep oceanic crust and can be very diverse in composition.

4. Peridotite: This is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. It is an important rock type because the Earth's mantle is predominantly composed of it.

5. Quartz Diorite: This is an intrusive igneous rock similar to diorite, but containing a larger amount of quartz.

These rocks all solidify within the Earth's crust from magma, which is why they are known as intrusive igneous rocks.

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Sure, here are some examples of rocks that solidified within Earth's crust:

1. Granite: This is a common type of intrusive, felsic, igneous rock which is granular and phaneritic in texture. Granites can be predominantly white, pink, or gray in color, depending on their mineralogy.

2. Diorite: This is an intrusive igneous rock composed principally of the silicate minerals plagioclase feldspar, biotite, hornblende, and/or pyroxene.

3. Gabbro: This is a phaneritic (coarse-grained), mafic intrusive igneous rock. It is the most abundant rock in the deep oceanic crust and can be very diverse in composition.

4. Peridotite: This is a dense, coarse-grained igneous rock, consisting mostly of the minerals olivine and pyroxene. It is an important rock type because the Earth's mantle is predominantly composed of it.

5. Quartz Diorite: This is an intrusive igneous rock similar to diorite, but containing a larger amount of quartz.

These rocks all solidify within the Earth's crust from magma, which is why they are known as intrusive igneous rocks.

example of rocks that solidified within Earth's crust

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