Metamorphic Rocks
metamorphic
You can't alter it. A triple point is ONE set of pressure (p) end temperature (T), a physical property for each pure compound or element in all three phases together (s, l, g).
The group that is not altered in an experiment is the control group, because all conditions are kept the same.
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.
igneous rocks
metamorphic
Metamorphic rocks.
Metamorphic rocks.
metamorphic
It becomes a metamorphic rock, altered by heat, pressure, or hot fluids.
It becomes a metamorphic rock, altered by heat, pressure, or hot fluids.
It becomes a metamorphic rock, altered by heat, pressure, or hot fluids.
It becomes a metamorphic rock, altered by heat, pressure, or hot fluids.
Metamorphic rock is formed by high pressure and temperature acting on existing rock. This process can be likened to "pressure cooking," as the rock is altered and compacted into a new form without melting. Examples of metamorphic rocks include marble, schist, and gneiss.
You can't alter it. A triple point is ONE set of pressure (p) end temperature (T), a physical property for each pure compound or element in all three phases together (s, l, g).
The group that is not altered in an experiment is the control group, because all conditions are kept the same.
Limestone.