What temperature does rock melt?

Fire is one of the most dangerous and unpredictable natural disasters. Rock responds to fire in a number of ways to protect itself and its environment. However, there has been a lot of debate on if rock melts or not. And if rock melts, at what temperature does rock melt?

The most common rock to be melted is granite, which melts at a temperature range of 1,200 degrees to 1,300 degrees Fahrenheit.  Granite is a very hard rock and tends to hold its shape when molten, so it will not flow like sandstone or limestone would in a lava stream.

It is important you know that the rock melt temperature is a measure of the temperature at which rock is subject to melting. The rock’s temperature can be measured using an instrument called a thermal probe or simply by using an ordinary thermometer.

What temperature does rock melt?

What temperature does rock melt

Rock and gravel, which are not set in concrete, can be melted by high temperatures. Some of the common rocks that are used for filling construction sites are sandstone, limestone, granite, and quartz. Generally speaking, most types of rocks melt anywhere from 650 to 2,500 degrees Celsius.

When rock melts, it expands and becomes more fluid. This process is called thermal expansion. The temperature at which rocks melt varies depending on their composition. Hotter rocks melt at lower temperatures, and cooler rocks melt at higher temperatures.

Can hot rock burn the skin?

Hot rocks are used in many places for household purposes, including for cooking and cleaning. While it is true that hot rocks can burn the skin, the sensation of heat may be relatively mild.

Also, hot rock is being used as an exfoliating treatment to remove dead, dry skin from your body. The heat that comes with using this treatment can burn the skin. Please use caution if you choose the hot stone as your exfoliating choice.

What temperature does granite melt at?

Different types of igneous rocks melt at different temperatures. Granite, which is a metamorphic rock formed by the cooling of molten rock or lava, melts at 1200° Fahrenheit, Basalt and gabbro melt at 2,170° to 3,200° Fahrenheit (1,270° to 1,450° Celsius), and Andesite melts at 2,300° (1,360° Celsius).

Also, the melting temperature of granite is determined by its characteristics. If the stone has a uniform grain, then it will be easier to melt. However, if it is an irregularly structured rock, then temperatures of over 1000°C may be needed to achieve complete melting.

What temperature does stone melt?

The stone will melt at a certain temperature, depending on its composition. If you are melting a granite block, you will want to be using either an electric or gas kiln that can reach at least 1,100 to 1,200 degrees Fahrenheit (600 to 700 Celsius).

Stone can easily be damaged by fire and high temperatures. However, when taken care of properly, stone can withstand high temperatures in your fireplace. Therefore, while a stone fireplace may not be practical to use, it is imperative that you bring it inside during cold weather.

Can rocks melt?

As a rock slowly cools down to its solid state, it may become malleable enough to deform when heated. Depending on the composition of the rock and its temperature, it will be divided into two categories: partial melting and complete melting.

Partial melting

Partial melting of rock is the process by which a small percentage of a rock mass becomes molten. The theory behind this process suggests that simply heating up certain basaltic rocks can make them melt more easily.

In geology, the partial melting of some mineral bodies and crustal rocks occurs when the Earth’s surface is exposed to intense geological processes that cause them to melt and become liquid.

Complete melting

Complete melting of rock is the melting of the entire solid rock mass. This can take place in any type of terrestrial or extraterrestrial object in which there are fractures, a surface structure, and a liquid phase present. In some examples, this includes magma or lava flows (such as those observed during volcanic eruptions) where molten material moves through cracks in the ground to form a lava lake.

When the rock has been melted (dissolved), the temperature will rise to a point where the solid rocks are absorbed by what is left behind. This may form magma or an igneous intrusion, which ultimately erupts through volcanoes and mountains.

What is the melting point of rocks?

The temperature at which rock breaks down melts under pressure and generates melting points in this sense is called the melting point of rock. A melting point of rock refers to the temperature at which it loses its crystalline structure but does not become liquid.

Also, the melting point of rocks is determined by their composition and structure. If the rock is composed of minerals that are less dense, it will melt at temperatures lower than the actual melting point. Below are the types of rocks and their melting point.

1. Igneous rocks

Igneous rocks are formed from magma (lava), which erupts onto the surface of the Earth’s crust. Igneous rocks can form in three main ways: Plutonic, Volcanic, and Metamorphic. It is these different source types that make up the vast majority of igneous rock types on Earth.

The melting point of an Igneous rock is the temperature at which the minerals contained in it solidify and lock up their heat. The higher the melting point of a mineral, the greater its specific heat capacity and thermal conductivity are.

The global melting point threshold for igneous rocks is close to 4,000 °C (6,432 °F), above which the chemical bonds in minerals start breaking down because temperatures become too high.

2. Sedimentary rocks

Sedimentary rocks are those that have been formed by the accumulation of material in sedimentary environments. Sedimentation is the process by which loose particles that have the potential to become rock are transported, deposited, and cemented together.

Also, sedimentation serves to put layers of rock on top of each other and adds compaction to a deposit. Sedimentary rock’s melting point is the temperature at which an igneous rock loses its melting point behavior. The melting point depends on the composition of the rock and may be different in different minerals.

The rocks melt at a high temperature, above 1222°C. These rocks are formed when sediments are buried and converted into solid rock. They can contain some minerals, but most have nothing more than the mineral grains that form them.

Also, the temperature ranges in sedimentary rocks can change as the composition of sediments changes or if the rocks are heated from below or from above. They also vary slightly depending on how much water was present at the time of formation.

3. Metamorphic rocks

Metamorphic rocks often form sedimentary and metamorphic rocks are pushed deep within the earth. The result is a rock that has been changed in appearance due to the pressure and heat of its underground journey.

The melting point of metamorphic rocks is about 3000-3300 °C. Metamorphic rocks have very high surface energy, due to which the melting point does not rise above the temperature at which they melt.

How hard is it to melt a rock?

It is very hard, and the melting temperature and time all depend on some factors. To melt a rock, you need to heat it up until it melts. If you want to melt rock in a home, you’ll need to heat the rock in an oven. You can also melt rocks outdoors by setting them on fire or putting them in a fire pit.

If you’re melting rocks for use in construction projects, like building dams and bridges, you’ll need special equipment that can heat the rocks without causing any damage or injury to yourself or others nearby.

Factors that affect the melting temperature of rocks?

What temperature does rock melt

There are a number of factors that affect the melting temperature of rocks. These include the temperature, pressure, and composition of the rock.


Not all rocks melt at the same temperature. The melting point of a rock depends on its composition but also on its temperature. For example, if you heat quartz (silica), it will melt at about 2,800 degrees Fahrenheit (1,600 degrees Celsius).

If you heat feldspar (an igneous rock) or amphibole amphibolites (a sedimentary rock), they will melt at temperatures closer to 2,700 degrees Fahrenheit (1,500 degrees Celsius).


The pressure is a factor that affects the melting temperature of rocks. The higher the pressure, the lower the melting point. This is because high pressure increases the density of any substance and makes it harder to melt.

The melting point of a substance decreases with increasing pressure, but it doesn’t decrease in direct proportion to the increase in pressure.

Water content

Water content is a key factor in the melting temperature of rocks. Rocks with high water content melt at lower temperatures than rocks that have low water content.

When we say “high” and “low,” we mean the ratio of water to total mass, i.e., the ratio of H2O to rocks’ total weight.

So if you had two rocks, each with an equal amount of mass but one with twice as much water as the other, then their melting points would be different: The rock with twice as much water would melt at a higher temperature than the other rock.


The melting temperature of rocks is affected by the time it takes to heat up. The longer it takes for the rock to melt, the more energy is required to do so. Apart from time, there are other factors that contribute to the melting of rocks.

Also, I have shared on this page all you need to know about what temperature does rock melt. I go on to give the information on different types of rocks. You can read them above with their melting point.