Rocks Form By Crystallization And Consolidation Of Molten Magma - Web for instance, a rock called pegmatite is formed by the crystallization of magma enriched with water in the veins of other rocks, and may contain beryl, tourmaline and topaz. This explains why a cooling magma can have some crystals within it and yet remain predominantly liquid. Web magma is the term used to describe molten material within the earth; Web 3.3 crystallization of magma. Web 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. The sequence in which minerals crystallize from a magma is known as the bowen reaction series (figure 3.3.1 and figure 3.3.3). The minerals that make up igneous rocks crystallize at a range of different temperatures. But the molten rock usually contains some suspended crystals or dissolved gases. All magma develops underground, in the lower crust or upper mantle, because of the intense heat there. Igneous rocks form through the crystallization of magma.
Web magma is the term used to describe molten material within the earth; Web for instance, a rock called pegmatite is formed by the crystallization of magma enriched with water in the veins of other rocks, and may contain beryl, tourmaline and topaz. Web 3.3 crystallization of magma. Igneous rocks form through the crystallization of magma. This explains why a cooling magma can have some crystals within it and yet remain predominantly liquid. All magma develops underground, in the lower crust or upper mantle, because of the intense heat there. But the molten rock usually contains some suspended crystals or dissolved gases. The sequence in which minerals crystallize from a magma is known as the bowen reaction series (figure 3.3.1 and figure 3.3.3). The minerals that make up igneous rocks crystallize at a range of different temperatures. Web 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.