The asthenosphere is the invisible layer of the earth’s atmosphere that has an outer layer of ozone, a layer of water vapor, and a layer of carbon dioxide. A good example of this is the atmosphere of the earth’s North Pole. If you look up the word “asthenosphere” in a dictionary, you will see that the word simply refers to the outer layer of the atmosphere.
I don’t know if there is a direct relationship between the mantle and the asthenosphere, but the mantle does appear to be a buffer between the outer layer and the atmosphere, so I would imagine that the mantle is a part of the asthenosphere.
I think that the mantle is a buffer between the outer layer and the atmosphere. We have an idea of a layer of air above the surface of the earth. That air is moving around at a constant speed. The mantle is a buffer between the layer above the surface and the layer below the surface.
If the mantle is the buffer between the layer above the surface and the layer below the surface, then the mantle is a layer of the earth and it is the equivalent of the atmosphere above the surface of the earth. The mantle is the layer that is between the surface of the earth and the core. The mantle is also very thin at the top of the mantle and thicker at the bottom, so it protects the earth from the powerful forces that are generated at the core of the earth.
The mantle is a very thin layer at the very top and very thick at the very bottom. In fact, it is only about 3,000 feet thick at the very top of the mantle. It is an extremely thin layer compared to the top layers of the earth, which are about 10,000 feet thick. It is extremely thin compared to the layers of the earth that are the ocean depths.
The mantle is one of the most dense layers in the earth’s crust and its presence is responsible for a lot of the earth’s atmosphere. It’s also responsible for the formation of deep ocean trenches which is where we are in our Earth’s mantle. This is like the top layer of the earth but is not as dense as the mantle.
The mantle is the outermost layer of the earth and the densest layer of the earth. It is the first layer to be laid down, before the layers of the earth. It is thought to be less dense than the mantle and that it is the lowest layer of the earth. The mantle has been found to be roughly 30-34 miles deep and contains the largest amount of iron and cobalt. The mantle is created by the fusion and subduction of the oceanic crust to the mantle.
The concept of the mantle and the core is fairly well understood. The mantle is the outermost layer of the earth and is thought to be less dense than the crust. The mantle is built up by the fusion and subduction of the oceanic crust to the mantle. The mantle is thought to be 30-34 miles deep and contains the largest amount of iron and cobalt. The mantle is created by the fusion and subduction of the oceanic crust to the mantle.
A better way to think about this is that the mantle is the crust that we know and love, and the core is the part that we don’t know and love. This, of course, is only one way to think about it–the mantle is also the core, and a large portion of the mantle may be the crust.
Since the core is just an oceanic mantle, there are two ways to think of a mantle: the continental and subcontinental. The continental mantle is thought to be up to 60 miles deep and is thought to contain all the iron that you can find. The subcontinental mantle is thought to be less than 60 miles deep and contains almost all the cobalt and other metals.