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
No
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
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.
with heat and pressure
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.
Heat and pressure
Metaconglomerate.
yes