The asthenosphere, part of the upper mantle.
The asthenosphere is partially molten due to high temperatures caused by the heat from the Earth's core. The combination of high pressure and temperature in the asthenosphere allows the rock to deform and flow slowly over geological timescales. This partially molten layer allows the lithospheric plates above to move and interact, driving the process of plate tectonics.
The two layers of the Earth that are either partially or totally melted are the asthenosphere and the outer core. The asthenosphere, located beneath the lithosphere, consists of partially molten rock that allows for the movement of tectonic plates. The outer core, which lies beneath the mantle, is entirely molten and composed mainly of liquid iron and nickel, contributing to Earth's magnetic field.
The mantle is the source of molten rock. This molten material can, if the tectonics are right, penetrate up through the solid outer mantle and the crust to deliver lava, which is molten rock (magma) that has reached the surface of the earth.
The molten materials within the Earth are primarily composed of magma, which is a mixture of molten rock, gases, and minerals. This magma forms in the Earth's mantle and can rise to the surface during volcanic eruptions. Additionally, the Earth's outer core contains molten iron and nickel, contributing to the planet's magnetic field. Overall, these molten materials play a crucial role in geological processes and the formation of Earth's crust.
The asthenosphere is a layer in the upper mantle that is partially molten and is responsible for the movement of tectonic plates. The mesosphere is a layer in the Earth's atmosphere above the stratosphere and below the thermosphere where temperatures drop with increasing altitude. The two layers are located in different parts of the Earth - the asthenosphere is within the Earth while the mesosphere is part of the Earth's atmosphere.
The asthenosphere is partially molten. It is about 5% molten.
The asthenosphere is partially molten. It is about 5% molten.
The partially molten layer of Earth is called the asthenosphere. It is located beneath the lithosphere and is responsible for the movement of tectonic plates.
The outer core is the only molten layer of the Earth. == ==
The asthenosphere is partially molten due to high temperatures caused by the heat from the Earth's core. The combination of high pressure and temperature in the asthenosphere allows the rock to deform and flow slowly over geological timescales. This partially molten layer allows the lithospheric plates above to move and interact, driving the process of plate tectonics.
core of the earth contains the molten iron
No, the asthenosphere is a partially molten and ductile region in the upper mantle of the Earth. The Earth's core is a distinct layer found at the center of the Earth, composed mostly of iron and nickel.
The outer core of the Earth contains molten iron and nickel. This layer is located beneath the Earth's mantle and is responsible for generating the planet's magnetic field.
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 two layers of the Earth that are either partially or totally melted are the asthenosphere and the outer core. The asthenosphere, located beneath the lithosphere, consists of partially molten rock that allows for the movement of tectonic plates. The outer core, which lies beneath the mantle, is entirely molten and composed mainly of liquid iron and nickel, contributing to Earth's magnetic field.
The mantle is the source of molten rock. This molten material can, if the tectonics are right, penetrate up through the solid outer mantle and the crust to deliver lava, which is molten rock (magma) that has reached the surface of the earth.
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.