If lava cools too fast, whether it is mafic, felsic, or intermediate crystals fail to develop and volcanic glass forms.
Texture: Aphanitic -- small crystals, invisible without magnification Porphyritic -- visible crystals amid a fine-grained groundmass Phaneritic -- large visible crystals Composition: Felsic -- more than 65% silica Intermediate -- between 55-65% silica Mafic -- between 45-55% silica Ultramafic -- less than 45% silica
When magma coos slowly, it allows large crystals to form. The process of evaporation helps to form crystals.
large mineral crystals are most likely found or have grown in igneous or metamorphic rocks
Igneous rocks will develop large crystals is they cool slowly underground.
Felsic rocks have 0-15% mafic crystals, while mafic rocks have 46-85% mafic crystals.
If lava cools too fast, whether it is mafic, felsic, or intermediate crystals fail to develop and volcanic glass forms.
A mafic rock is composed of mafic minerals such as biotite mica, amphibole, proxene, and olivine. The actual word mafic refers to magnesium and iron; nevertheless, these minerals are called ferromagnesian. Mafic rocks include gabbro, scoria, and basalt. They each have about 46-85% mafic mineral crystals. Periodite, 86-100% mafic minerals, is considered ultramafic because of its olivine composition.
diorite crystals are large and andesite crystals are small
Texture: Aphanitic -- small crystals, invisible without magnification Porphyritic -- visible crystals amid a fine-grained groundmass Phaneritic -- large visible crystals Composition: Felsic -- more than 65% silica Intermediate -- between 55-65% silica Mafic -- between 45-55% silica Ultramafic -- less than 45% silica
It depends on the type of igneous rock. Intrusive igneous rocks such as granite have large crystals, extrusive igneous rocks may have small crystals as in basalt or no crystals as in pumice.
When magma coos slowly, it allows large crystals to form. The process of evaporation helps to form crystals.
Gabbro is a group of dark, coarse-grained, intrusive mafic igneous rocks. They are often found beneath the Earth's surface where they form into crystals.
porphyry
No. Basalt generally has small crystals.
Pumice does not have crystals. It is made of glass.
Igneous rocks will develop large crystals is they cool slowly underground.