Magma that solidifies in a bubble shape under the crust is called a "laccolith." Laccoliths form when magma intrudes between layers of rock and causes the overlying strata to bulge upward, creating a dome-like structure. These formations can vary in size and are often found in volcanic regions.
Magma that solidifies in a bubble shape under the crust is called "vesicular" or "vesicular basalt" if it forms from basaltic magma. The bubbles, or vesicles, are created by gas bubbles escaping from the magma as it cools and solidifies. This texture indicates that the magma was rapidly cooled, often during volcanic eruptions or near the surface.
Ocean crust is formed through a process called seafloor spreading, where magma rises up at mid-ocean ridges, cools, and solidifies to create new crust. This process is part of plate tectonics, where oceanic plates move away from each other, allowing new crust to form at the ridges.
The process of new crust forming at mid-ocean ridges is called seafloor spreading. Magma rises up from the mantle, solidifies at the ridges, and creates new crust as tectonic plates move apart.
The molten material moving upward within the Earth's crust is called magma. Magma is formed from the melting of rocks in the Earth's mantle and can rise to the surface through volcanic activity. As magma cools and solidifies, it forms igneous rocks.
the break in the inner crust that is not filled with magma is called
Intrusion of magma that solidifies in a bubble shape under the Earth's crust is called a pluton. This forms when magma is trapped in a pocket underground and slowly cools and solidifies, creating distinct bubble-shaped structures.
Ocean crust is formed through a process called seafloor spreading, where magma rises up at mid-ocean ridges, cools, and solidifies to create new crust. This process is part of plate tectonics, where oceanic plates move away from each other, allowing new crust to form at the ridges.
Magma that hardens within the Earth's crust is called intrusive igneous rock. This type of rock forms when magma cools and solidifies beneath the Earth's surface, resulting in the formation of intrusive features like batholiths, dikes, and sills.
The process of new crust forming at mid-ocean ridges is called seafloor spreading. Magma rises up from the mantle, solidifies at the ridges, and creates new crust as tectonic plates move apart.
The molten material moving upward within the Earth's crust is called magma. Magma is formed from the melting of rocks in the Earth's mantle and can rise to the surface through volcanic activity. As magma cools and solidifies, it forms igneous rocks.
Igneous, the world magma really gives away the answer. Magma = Ignite Ignite is to do with fire, heat and flame etc.
When magma reaches the earth's surface, it is called lava. when it solidifies, it forms new crust, or rock.
the break in the inner crust that is not filled with magma is called
The sequence of rock strips at oceanic ridges is called "oceanic crust." It is formed through the process of seafloor spreading where magma rises through the Earth's crust, solidifies, and creates new crust. This process helps drive the movement of tectonic plates.
Molten rock deep beneath the Earth's crust is called magma.
Igneous rock is formed from the crystallization of molten magma or lava. Intrusive igneous rock is formed beneath Earth's crust from magma. Extrusive igneous rock is formed above Earth's crust from the crystallization of lava.
A crust is not destroyed at a divergent boundary, where tectonic plates move away from each other. This movement creates new crust as magma rises to the surface and solidifies.