Intrusive or granite.
Igneous rocks can have both small and large crystals, depending on how quickly they cool. If an igneous rock cools slowly beneath the Earth's surface, it can form large crystals, while rapid cooling at the Earth's surface or in an eruption can result in small or no visible crystals.
Igneous rocks will develop large crystals is they cool slowly underground.
No, melted rock that cools quickly result in igneous rock with large minerals because large crystals take time to form and the rocks that usually have them are the ones that were formed inside the earth.
Igneous rocks will develop large crystals is they cool slowly underground.
It depends on the cooling rate of the magma. If the magma cools slowly underground, large crystals can form, creating intrusive igneous rocks. If the magma cools rapidly on the Earth's surface, small crystals or glassy textures can result in extrusive igneous rocks.
sedimantry
Large mineral crystals are commonly found in igneous rocks, such as granite and pegmatite, where slow cooling allows minerals to grow large. Certain metamorphic rocks, like marble and schist, can also contain large mineral crystals due to high pressures and temperatures. Veins and pockets within rocks can sometimes host large crystals as well.
Igneous rocks can contain both small and large crystals, depending on how quickly they cooled from molten material. If they cooled slowly beneath the Earth's surface, they tend to form large crystals, as seen in rocks like granite. Conversely, if they cooled rapidly on the surface, such as in volcanic eruptions, they typically have small crystals or a glassy texture, as seen in rocks like basalt.
granite
Porphyrite of any composition, granite, gabbro, diorite. Most intrusive igneous rocks have crystals large enough to see with the naked eye. Another term used to define an igneous rock with large crystals is coarse-grained.
Igneous rocks such as granite can contain large crystals due to slow cooling and solidification of magma beneath the Earth's surface. This slow cooling allows for the formation of large mineral crystals such as feldspar, quartz, and mica. These crystals are typically visible to the naked eye and contribute to the distinctive appearance of granite.
Large crystals in igneous rocks usually form when the magma cools slowly underground, allowing the crystals more time to grow. The composition of the magma, the cooling rate, and the amount of available space for crystal growth all play a role in determining the size of crystals in the rock. Rapid cooling at the Earth's surface typically results in the formation of fine-grained rocks.