If the rock melts the resulting rock type would be igneous rather than metamorphic.
The presence of water can lower the melting temperature of a rock by facilitating the movement of ions and promoting the process of melting. Water reduces the viscosity of molten rock, making it easier for the rock to melt at lower temperatures.
Yes, the Earth's crust has a wide range of melting points depending on the type of rock, but in general, the temperatures required to melt rocks in the crust are higher than the typical surface temperatures of the Earth. The actual temperature of the Earth's crust is generally lower than its melting point.
Water can lower the melting temperature of a mineral by acting as a flux or catalyzing agent, allowing atoms to move more freely and reducing the energy required for melting. This can lead to the formation of new minerals or phases at lower temperatures than would occur without water present.
The two main factors that affect the temperature at which rocks melt are the composition of the rock and the pressure acting on it. Different minerals have different melting points, so the composition of the rock will determine its melting temperature. Additionally, pressure can increase or decrease the melting temperature of rocks, with higher pressure generally increasing melting temperature and lower pressure decreasing it.
To calculate the melting point of an alloy, one must consider the melting points of the individual elements in the alloy and their relative proportions. The melting point of an alloy is usually lower than that of its individual components due to the formation of a new phase. Phase diagrams are often used to predict the melting behavior of alloys.
if rock melts it will form magma, which leads to the formation of igneous rocks
Metamorphic rocks form by rocks being changed while still in the solid state. If the temperature of a rock exceeds its melting point, it will melt and any rock that forms as a result will be considered igneous.
The melting temperature of an alloy is generally lower than the melting temperature of the highest melting temperature of all of its constituents. The eutectic melting temperature is the lowest melting temperature of an alloy system and is in fact sort of defined by that optimal set of percentages of those constituents. The next obvious question is whether there are calculation methods or approximations to determine the melting range of less than "eutectic" percentages.
Solid state
The composition of the magma plays a significant role in determining its melting temperature. Magma with higher silica content tends to have a higher melting temperature. Pressure also affects the melting temperature; higher pressure usually results in a higher melting temperature. Water content can lower the melting temperature of magma by acting as a flux, allowing minerals to melt at lower temperatures.
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upper fixed point is a temperature of stem from water boiling and standards atmospheric pressure lower fixed point is the temperature of pure melting ice.
The presence of water can lower the melting temperature of a rock by facilitating the movement of ions and promoting the process of melting. Water reduces the viscosity of molten rock, making it easier for the rock to melt at lower temperatures.
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energy movement from higher temperature regions
1,763°F melting point of silver 1,984°F melting point of copper the answer is silver