Difference between Lava and Magma

The difference between lava and Magma relates to their location. Well, before discussing this difference, let’s see what each word means. Most of us don’t know that we are raising the temperature below the Earth’s surface as we go down. The temperature of the center or core, it is said, is so high that it is formed in addition to molten rock and other solid objects due to extremely high temperatures. This mixture of molten rock is called Magma. This Magma lives in particular places called chambers, which lead to volcanoes. When the volcano erupts, this Magma is constantly eaten up in the volcano. When this Magma comes out of the volcano, it is known as lava. Although technically saying there is no difference between Magma and lava because it is Magma known as lava, many are confused about their difference. This article tries to find out the difference between Magma and lava, if any.

As we discussed earlier, Magma is the molten rock we stand on in the cold Earth and cannot feel or imagine how hot it is below the Earth’s center. One thorn travels down and enters the methyl, the temperature gradually rises, and there are metal pockets where an animal can get rocks. This molten rock, which is called Magma, is brittle and cracks through and underground groundwater.

The Earth’s underground plates depend on each other for collisions. Usually, these plates fit the bird pieces together in a giant jug, but they release friction and a lot of energy when they are removed. When the plate collides, the one-second slide pushes the other, and the bottom pushes one down. Causes molten rock or Magma to fall between these plates. Those who feel like the rage of volcanic nature are substantial safety valves that create pressure due to the high temperature of the Earth. The Magma that reaches the mouth of the volcano is about 700-1300 degrees Celsius.

According to their chemical composition, there are three types of Magma. They are basaltic Magma, andesitic Magma, and rheological Magma. Basaltic Magma is low in K and Na and high in Fe, Mg, and Ca. Andesitic Magma mediates Fe, MG, CA, K, and Na. Finally, rhyolitic Magma is high in K and Na and low in Fe, Mg, and Ca.

Lava is also molten rock. When subterranean Magma comes out of a volcano, it is called lava. Different types of benefits are classified according to their fairness or viscosity. Saliva can flow to the bottom for thin kilometers and makes a gentle flow or slope. Thick lava finds it challenging to wash, and most lava does not even flow and plug up a volcanic mouth, causing significant eruptions in the future.

Let’s see what the different types of lava are. There are three main types of lava: 

1. A’a, 2. Pahoiyo, and 3. Pilo lava.

A’A is the first type of lava, and it is pronounced as’ ah-ah. ‘Such lava does not flow very fast. It will look like a slow-moving mass of lava with a solid surface. Once this lava is hard, it is challenging for anyone to walk on that surface. Then, there is lava in Pahoa too. This name is pronounced as PO-ho-o. This type of lava can easily flow down slopes because the viscosity is lower than A’A lava. Finally, we have sand lava—this type of lava you see when an underwater volcano erupts. Like hot water, when this hot lava fills with cold water, it cools automatically and forms a solid shell. When more lava comes from the volcano’s mouth, more pillows like shell cracks and hard surfaces are created.

What is the difference between Lava and Magma?

• Magma is molten rock material inside the Earth’s crust. Meanwhile, when it finds its way to the volcano through sculptures and cracks and comes from the volcano’s mouth, the same Magma is called lava.
• Magma is deep underground when a hot mixture of lava gas and molten rock emerges from a volcano.
• Three types of lava such as ‘A,’ Pahooio, and Pilo Lao. Depending on their chemical composition, there are three types of Magma as well. They are basaltic Magma, andesitic Magma, and realistic Magma.