Heat and pressure can transform basalt into metamorphic rocks, primarily into types such as amphibolite or greenschist, depending on the specific conditions. The intense heat can cause the minerals within basalt to recrystallize, while pressure can lead to foliation and other structural changes. This process alters the original basalt's texture and mineral composition, resulting in a new metamorphic rock.
Sedimentary rocks
When heat and pressure are applied to basalt, it can transform into a metamorphic rock called greenstone or greenschist. This process can cause minerals in the basalt to recrystallize, resulting in a more compact and foliated texture. Overall, basalt tends to become denser and more resistant to weathering under these conditions.
Sandstone is changed into quartzite and basalt is changed into schist or gneiss through the process of metamorphism.
specific heat of basalt is 0,2
When sandstone is subjected to heat and pressure, it metamorphoses into quartzite, which is a hard, dense rock primarily composed of quartz. Basalt, on the other hand, transforms into metamorphic rocks such as amphibolite or greenstone under similar conditions, depending on the specific minerals present and the intensity of the heat and pressure. These processes are part of the rock cycle, demonstrating the dynamic nature of Earth's geology.
Sedimentary rocks
When heat and pressure are applied to basalt, it can transform into a metamorphic rock called greenstone or greenschist. This process can cause minerals in the basalt to recrystallize, resulting in a more compact and foliated texture. Overall, basalt tends to become denser and more resistant to weathering under these conditions.
Sandstone is changed into quartzite and basalt is changed into schist or gneiss through the process of metamorphism.
specific heat of basalt is 0,2
When sandstone is subjected to heat and pressure, it metamorphoses into quartzite, which is a hard, dense rock primarily composed of quartz. Basalt, on the other hand, transforms into metamorphic rocks such as amphibolite or greenstone under similar conditions, depending on the specific minerals present and the intensity of the heat and pressure. These processes are part of the rock cycle, demonstrating the dynamic nature of Earth's geology.
Yes, basalt is a solid at standard temperature and pressure.
When basalt metamorphoses (changes through heat and/or pressure), it becomes amphibolite. Amphibolite is dark-coloured, and resembles dark, glassy crystals fused together. It is heavy, with a slightly flaked structure.
Heat and pressure change shale into metamorphic rock, specifically slate when exposed to low to moderate levels of heat and pressure, and then further into phyllite, schist, and gneiss as the intensity of heat and pressure increases.
A heat change at constant pressure is called enthalpy change, often denoted as ΔH. It represents the change in total heat content of a system during a process occurring at constant pressure.
with heat and pressure
Heat and pressure
Metaconglomerate.