magma
pressure from under the surface forces the magma up!
A volcanic vent or conduit is an opening that leads from the crater of a volcano down to pools of magma below the surface. This conduit allows magma to travel from the magma chamber to the surface during an eruption.
When magma comes up to Earth's surface and hardens, it is called lava.
Magma moves up Earth's surface in a pipe.
Magma travels through the Earth's crust via magma chambers and magma reservoirs, typically moving upwards towards the surface due to its lower density compared to the surrounding rocks. The movement of magma is influenced by factors such as temperature, pressure, and the presence of cracks or fractures in the crust.
As magma rises, it carves a tube-shaped structure called a "magma conduit" or "volcanic conduit." This structure allows the magma to travel from the magma chamber beneath the Earth's surface to the surface during a volcanic eruption. The conduit can solidify into igneous rock once the magma cools and crystallizes.
The magma starts cooling and crystallizing. The crystallization cause the magma to change composition. This is referred to as magma evolution.
Magma is liquid rock before it reaches the surface magma which reaches the surface is called lava.
The part of a volcano that connects the vent with the magma chamber is called the "conduit" or "volcanic conduit." This cylindrical passage allows magma to travel from the magma chamber, located beneath the surface, up to the vent, where it can erupt. The conduit plays a crucial role in determining the characteristics of volcanic eruptions.
Pressure in magma builds up as it rises toward the surface because the weight of the overlying rock increases, causing the magma to be squeezed and pressurized. This pressure can eventually lead to volcanic eruptions.
magma moves up earth suface
The channel that magma uses to travel toward the vent in a volcano is called a "conduit." It is a narrow passage within the volcano that allows molten rock to move from the magma chamber to the surface during an eruption.