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the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
The Earth has three compositional layers and five structural layers. Both layers have iron, magnesium, aluminum and silica.
One is in the soil and the other is in the atmosphere.
In order to answer this you need to understand the difference between the compositional layers of the earth and the physical layers. The crust and mantle are differing layers of the earth based on chemical composition. The lithosphere is a layer of the earth defined based on it's physical or mechanical properties (how it deforms). The lithosphere is composed of the crust and the portion of the upper mantle which deforms elastically and fails in a brittle manner (fractures can propagate through the material). So in the question where you ask is the crust and lithosphere brittle, the answer is yes as the crust is entirely part of the lithosphere which by definition is brittle. However as described above, a section of the upper mantle is also a brittle solid and so that too is part of the lithosphere. However below this, the mantle behaves as a ductile solid.
foliated rocks are arranged in parallel layers, or bands. Unfoliated rocks are not banded and are not put into parallel layers.
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the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
The Earth has three compositional layers and five structural layers. Both layers have iron, magnesium, aluminum and silica.
Core Crust and Mantle
The crust, mantle, and core. :)
mantle,crust,core
The compositional layers of the earth are the crust, mantle and core. The physical layers are the lithosphere, asthenosphere, mesosphere, outer and inner core.
Mechanical layering of the earth: - Lithosphere (solid/rigid), 0-150km - Asthenosphere (solid/elastic), 150-660km - Mantle (solid/rigid), 660- 2900km - Outer core (liquid), 2900-5730km - Inner core, 5730-6400km Chemical layering of the earth: - Crust (oceanic and continental), 0-40km - Mantle, 40-2900km - Core, 2900-6400km
Crust, mantle, and then core.!(:
Continental crust
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