P-waves are longitudinal / compressional waves and so can pass through both solids (rock) and liquids (magma).
The channel through which magma rises within a volcano is called a conduit. This conduit allows magma to move from deep within the Earth up to the surface, where it can eventually erupt as lava.
The channel through which magma rises within a volcano is called the "magma conduit" or "volcanic conduit." This passage allows magma to move from the magma chamber beneath the Earth's surface to the surface, where it can erupt as lava. The size and shape of the conduit can influence the type and intensity of volcanic eruptions.
Magma often moves upward through the Earth's crust along cracks and fractures in the rock, known as magma conduits. These conduits can be created by tectonic activity, such as the movement of tectonic plates, which can provide pathways for magma to reach the surface and form volcanic eruptions.
Molten rock, or magma, rises to the Earth's surface during volcanic eruptions due to increasing pressure in the magma chamber beneath the volcano. This pressure forces the magma to move upwards through cracks and weaknesses in the Earth's crust, eventually erupting onto the surface as lava.
Magma seeps up through the two plates from the mantle and form volcanos.
Because nothing can be still and if more magma forms it has to push the rest away
id say faults the answer is faults
Magma and hydrothermal fluids are hot fluids that can move through small cracks in rock. Magma is molten rock beneath the Earth's surface, while hydrothermal fluids are water heated by volcanic activity that can carry minerals and gases. Both can contribute to the formation of igneous rocks and mineral deposits.
The channel through which magma rises within a volcano is called a conduit. This conduit allows magma to move from deep within the Earth up to the surface, where it can eventually erupt as lava.
The channel through which magma rises within a volcano is called the "magma conduit" or "volcanic conduit." This passage allows magma to move from the magma chamber beneath the Earth's surface to the surface, where it can erupt as lava. The size and shape of the conduit can influence the type and intensity of volcanic eruptions.
Magma often moves upward through the Earth's crust along cracks and fractures in the rock, known as magma conduits. These conduits can be created by tectonic activity, such as the movement of tectonic plates, which can provide pathways for magma to reach the surface and form volcanic eruptions.
it lets you move through walls and on magma etc.
they move because of the magma
Molten rock, or magma, rises to the Earth's surface during volcanic eruptions due to increasing pressure in the magma chamber beneath the volcano. This pressure forces the magma to move upwards through cracks and weaknesses in the Earth's crust, eventually erupting onto the surface as lava.
They are found at a plate boundary. When two plates move apart (divergent) magma rises through the gap.
Magma seeps up through the two plates from the mantle and form volcanos.
When magma rises through the Earth's crust, it forms a tube-shaped structure known as a "magma conduit" or "magma chamber." This conduit serves as a pathway for the magma to move from the mantle or deeper crust to the surface, often leading to volcanic eruptions. As the magma accumulates in the chamber, it can create pressure that eventually results in explosive volcanic activity.