Extrusive igneous rock is formed from the solidification of lava.Intrusive igneous rock is formed from the solidification of magma.
Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.
Cooling curve of Crystalline solids have breaks, which corresponds to the begining and ends of the crystallisation process. The temperature remains constant during crystallization as the process is accompained by some liberation of energy, which compensates for the loss of heat and causes the temperature to remain constant. -Damodar
It is called an igneous rock.Igneous rock is one of the three main rock types, the others being sedimentary and metamorphic rock. Igneous rock is formed through the cooling and solidification of magma or lava. Igneous rock may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks.
The rate of cooling is the main factor that affects the size of crystals that form as magma cools. Slower cooling allows for larger crystals to develop, while rapid cooling results in smaller crystals or even glassy textures. Other factors such as mineral composition and presence of impurities can also influence crystal size.
minerals form
Crystallization from cooling magma is the process by which minerals solidify from a molten state as magma cools and hardens. As the magma cools, minerals crystallize at different temperatures depending on their chemical composition, leading to the formation of igneous rocks with distinct mineral compositions and textures. This process is a key mechanism driving the formation of various igneous rock types like granite, basalt, and gabbro.
Crystallization and cooling are related processes, but they are not the same. Crystallization is the formation of crystals from a solution, while cooling is one method that can induce crystallization by lowering the temperature of a substance to promote crystal formation. Crystallization can also occur through other methods like evaporation or chemical reactions.
Yes, it is possible for one magma to produce several different igneous rocks with different mineral compositions. This can occur when the magma undergoes different cooling rates or crystallization processes within the Earth's crust, resulting in the formation of various igneous rocks with distinct mineral assemblages.
crystallization above ground and crystallization below ground
Extrusive igneous rock is formed from the solidification of lava.Intrusive igneous rock is formed from the solidification of magma.
Magma moves under the lithosphere because the aesthenosphere (and magma) are ductile - they act as a fluid, although a very viscous one, and they do flow. The viscosity of a magma depends on its mineral composition. Magma will move in convection currents throughout the aesthenosphere due to the heating and cooling of it as it travels throughout the aesthenosphere.
Igneous is one of the three major rock classifications in geology. An igneous rock is a rock formed from the cooling and solidification of magma or lava.
Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.
Cooling curve of Crystalline solids have breaks, which corresponds to the begining and ends of the crystallisation process. The temperature remains constant during crystallization as the process is accompained by some liberation of energy, which compensates for the loss of heat and causes the temperature to remain constant. -Damodar
there are many parts of a volcano. There is the magma chamber: where all of the magma is held. There is the pipe: where the magma comes up and through the volcano. There is the dike, where where a slab forms when magma forces itself across rock layers. There is the crater, where a bowl shaped area forms around a volcanoes central vent. There is the vent: where magms comes out.
The theory of plate tectonics.