Magma consists mainly of molten rock with some dissolved gasses and sometimes crystallized minerals.
Magma (molten rock) rises from feeders or volcanic necks beneath the surface of the crust and flows from volcanic openings onto the surface. When magma reaches the surface, it is called lava.When lava reaches the surface, it immediately begins to cool. During this cooling phase, the liquid lava solidifies much as liquid water would freeze if cooled sufficiently. The solidification occurs because of the crystallization of minerals from chemical components (iron, magnesium, silicon, oxygen) in the lava. The lava will transition from a liquid to either a form of natural glass, or to a rock, depending on the speed at which it cools. Obsidian, a natural glass, and basalt, an extrusive igneous rock, are both formed from cooling lava.
When molten rock cools slowly, it will have a lot of time to form crystals, so the crystal size will be quite big. Take granite, for example. With the naked eye, you can see the individual crystals. The grain size is quite large. The kind of mineral that forms is dependent on the composition of the magma.
An igneous rock is formed when magma cools and hardens. Some examples of igneous rocks are pumice and obsidian.
It can. As lava cools, some of it starts to cool while the rest remains liquid. If it erupts at this point it will result in a porphyritic rock.
'fraid not. some minerals form from magma, which is hot, liquid rock material INSIDE Earth's surface. Not on Earth's surface.
Several minerals form in slow cooling magma. Some of those minerals are quartz, plagioclase feldspar, and potassium feldspar. These are the same minerals that are found in granite.
There are 3 main types of rocks:Igneous RocksForms when molten rock cools.2 types of molten rock: magma, and lava.Intrusion: Forms when magma cools. Intrusion rocks take longer to form because magma takes longer to cool. Magma is under the Earth's surface, and it is very hot there. Imagine how long it would take for magma to cool down somewhere a thousand degrees!Extrusion: Forms when lava cools. Extrusion don't take as long to form, because lava cools much faster than magma does. Lava is at the surface, and the surface is WAY cooler than underground.Sedimentary RockForms when rocks/minerals/remains of plants or animals settle and accumulate.Forms in layers.3 types of sedimentary rock:Clastic - forms from accumulation of rock fragments and minerals.Biologic - forms from plant or animal remains.Chemical - forms when minerals precipitate out of a solution.MetamorphicPreexisting rocks that have changed form by heat and pressure.If you are looking for specific types, here are some brief examples:Igneous RocksBasaltPegmatiteGraniteTuffSedimentary RocksLimestoneCoalShaleSiltstoneMetamorphic RocksSlateGneissSchistMarble
Several minerals form in slow cooling magma. Some of those minerals are quartz, plagioclase feldspar, and potassium feldspar. These are the same minerals that are found in granite.
yes, slowly cooling magma will crystallize (granite). If it cools quickly, the lava will have very small crystals and will contain air pockets (pumice, if it is cooled in chunks) or can even be very thin, like hair, very straight. (Pele's hair)
The faster the rate of cooling the smoother the rock will be. The slower the rate the more rough the texture. The faster it cools the finer the texture of the rock. Slower cooling magmas tend to form courser grained igneous rocks. The more time a magma has too cool, the larger the crystals will be If all the minerals in the magma cools at about the same rate you will have roughly equal sized grains in the rock, in which case the rock will be of phaneritic texture. However you will have conditions in which some of the minerals will solidify while other minerals remain liquid, meaning those that have more time to solidify will have larger crystals . The minerals that solidify will have more time to grow as crystals while the other minerals in that magma will have less time and space to grow as crystals meaning those minerals will have smaller crystals. These rocks with crystals of various sizes are called porphoritic rocks (or porphory)
Magma is essentially molten rock inside earth, possibly with some trapped gasses. To become rock the magma simply cools and solidifies, essentially freezing.
Magma is essentially molten rock inside earth, possibly with some trapped gasses. To become rock the magma simply cools and solidifies, essentially freezing.
Magma consists mainly of molten rock with some dissolved gasses and sometimes crystallized minerals.
The temperature of the magma will affect its viscosity depending on its chemistry. Some minerals crystallize at higher temperatures than others, meaning that portions of the magma may have already solidified. At lower temperatures, the majority of the constituent minerals will have crystallized and solidified, leaving the magma highly viscous.
Magma (molten rock) rises from feeders or volcanic necks beneath the surface of the crust and flows from volcanic openings onto the surface. When magma reaches the surface, it is called lava.When lava reaches the surface, it immediately begins to cool. During this cooling phase, the liquid lava solidifies much as liquid water would freeze if cooled sufficiently. The solidification occurs because of the crystallization of minerals from chemical components (iron, magnesium, silicon, oxygen) in the lava. The lava will transition from a liquid to either a form of natural glass, or to a rock, depending on the speed at which it cools. Obsidian, a natural glass, and basalt, an extrusive igneous rock, are both formed from cooling lava.
Plutonic rocks are intrusive (they solidify before they reach the surface) and have larger crystals because the crystals have had a longer time to accumulate in the heat under the surface. Volcanic rocks are extrusive (they solidify on or near the surface) and have smaller crystals because the element has less time to accumulate when they cool quickly.