Acid (highly siliceous) - much of it andesite if I recall my reading of it correctly.
Krakatoa (or '~tau') is a still-active island-arc volcano above a complex, very active subduction zone.
When magma intrudes parallel to another rock layer, the formation is called a "sill." Sills are typically horizontal or gently inclined and form when magma forces its way between existing rock layers without breaking through to the surface. This process can create distinct mineral compositions and textures within the surrounding rock.
Minerals form in igneous rock as magma or lava cools. The minerals will form from the available chemicals in the magma as their crystallization temperature is reached. The sequence of mineral crystal formation from magma is described in the Bowen's Reaction Series. Metamorphic rock minerals are aligned, altered, or recrystallized from existing rock minerals due to the effects of heat and/or pressure.
No, Magmatic is and adjective meaning of or realting to magma. Magma is not a mineral but molten rock underground.
Quartz can be an igneous rock when it forms from the cooling and solidification of molten rock deep within the Earth's crust. During this process, silica-rich magma cools and crystallizes to form quartz. As the magma cools slowly, quartz crystals have time to grow and develop, leading to the formation of igneous rocks containing quartz, such as granite.
No, magma is molten rock, and it is a semi liquid that exists below the surface (when it's above the surface, it's called lava). When magma cools underground it becomes an intrusive igneous rock which is composed of combinations of various minerals.
Yes, there are two pathways in the rock cycle through which magma can transform into sedimentary rock. The first pathway involves magma cooling and solidifying into igneous rock, which can then be weathered and eroded into sediments that are transported and eventually lithified into sedimentary rock. The second pathway involves the direct alteration of magma through processes like hydrothermal activity, which can lead to the formation of mineral deposits that, over time, may contribute to sedimentary rock formation through erosion and deposition.
When magma cools, it forms igneous rock.
When rock is heated by nearby magma, the process is known as contact metamorphism. In this process, the intense heat from the magma alters the mineral composition and texture of the surrounding rock without causing it to melt. This can lead to the formation of new metamorphic rocks, characterized by changes such as recrystallization or foliation. The degree of metamorphism depends on the temperature of the magma and the duration of exposure.
Obsidian is formed from volcanic lava that cools quickly with minimal crystal growth. It is primarily derived from rhyolitic magma that cools rapidly on the Earth's surface, leading to the formation of a glassy rock without distinct mineral crystals.
Magma is molten rock. A mineral is a naturally occurring inorganic solid, with a definite chemical formula, and a crystalline structure.
Magma is molten rock. A mineral is a naturally occurring inorganic solid, with a definite chemical formula, and a crystalline structure.
Igneous rock is formed when magma rises to the surface of the Earth and cools. This process can lead to the formation of rocks like basalt or granite depending on the cooling rate and mineral composition.