The asthenosphere, part of the upper mantle.
Magma is molten or partially molten rock beneath the earth's surface. A magma chamber is a space, often beneath a volcano, where magma collects.
Partially molten, plastic like, flowing layer located below the solid part of Earth's mantle is the Asthenosphere. The asthenosphere is mechanically weak and ductiley deforming region of the upper mantle.
Because the inner Earth contains molten rock and magma that would kill you in seconds.
line up in the direction of Earth's magnetic field
The molten material that reaches earth's surface is lava :)
The asthenosphere is partially molten. It is about 5% molten.
The asthenosphere is partially molten. It is about 5% molten.
The asthenosphere.
The outer core is the only molten layer of the Earth. == ==
core of the earth contains the molten iron
Its Is the mantle
The most important thing to know is that it's partially solid, and partially molten. Convection occurs there and that's where the lava from volcanoes comes from.
The asthenosphere is partially molten; however, it is an interior layer which is separate from the Earth's inner and outer core. In fact, the asthenosphere is located directly under the lithosphere (the brittle outer shell of Earth), extending only a few hundred miles down from the surface.
The asthenosphere is partially molten; however, it is an interior layer which is separate from the Earth's inner and outer core. In fact, the asthenosphere is located directly under the lithosphere (the brittle outer shell of Earth), extending only a few hundred miles down from the surface.
Magma is molten or partially molten rock beneath the earth's surface and is lighter than the surrounding rock so it tends to rise. As it moves upward, the magma encounters colder rock and begins to cool.
Magma is molten or partially molten rock beneath the earth's surface. A magma chamber is a space, often beneath a volcano, where magma collects.
The Core of the Earth is molten metal, practically all IRON. It contains most of the Earth's Mass.