Table of Contents
What is the formation of crystals as magma cools?
Igneous rocks form when magma (molten rock) cools and crystallizes, either at volcanoes on the surface of the Earth or while the melted rock is still inside the crust.
What happens when magma cools to form minerals?
2) Intrusive: magma cools under the Earth’s surface. The magma cools very slowly. As magma cools minerals are formed into an interlocking arrangement producing an igneous rock. If the magma cools slowly then the reactions proceed for a longer period of time and the resulting mineral crystals (grains) become large.
How does cooling rate affects crystal size?
As the rate of cooling increases, crystal size decreases. This means that something which cools very quickly will have smaller crystal formations, and something which cools slowly will have larger crystal formations.
What mineral will form first as magma cools down last?
Of the common silicate minerals, olivine normally crystallizes first, at between 1200° and 1300°C. As the temperature drops, and assuming that some silica remains in the magma, the olivine crystals react (combine) with some of the silica in the magma (see Box 3.1) to form pyroxene.
What type of rock is formed when magma enters another formation?
Magma can intrude into a low-density area of another geologic formation, such as a sedimentary rock structure. When it cools to solid rock, this intrusion is often called a pluton. A pluton is an intrusion of magma that wells up from below the surface. Plutons can include dikes and xenoliths.
What happens to kinetic energy as magma cools?
As magma cools, kinetic energy decreases when atoms slow down. Eventually, if magma cools sufficiently, atoms will slow down enough so that some bonds will begin to persist. This is the beginning of the formation of crystals from a melt, and the beginning of the formation of igneous minerals.
What is magma that has cooled into a solid called?
Magma that has cooled into a solid is called igneous rock. Magma is extremely hot—between 700° and 1,300° Celsius (1,292° and 2,372° Fahrenheit). This heat makes magma a very fluid and dynamic substance, able to create new landform s and engage physical and chemical transform ations in a variety of different environment s.
What is the relationship between the formation of bonds and crystallization?
A balance exists between the formation of bonds and the rate at which they break apart. If bonds break as fast as they form there will be no net crystallization. As magma cools, kinetic energy decreases when atoms slow down. Eventually, if magma cools sufficiently, atoms will slow down enough so that some bonds will begin to persist.