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
The Earth's compositional layers in order of increasing density are the crust, mantle, outer core, and inner core. The crust is the least dense layer, while the inner core is the most dense layer.
There are generally four main compositional layers in the Earth: the crust, mantle, outer core, and inner core. These layers differ in their composition, temperature, and physical properties, and they play a crucial role in shaping the Earth's structure and dynamics.
The Earth's crust is the thinnest compositional layer, ranging from 5 to 70 kilometers thick beneath the oceanic crust and up to 100 kilometers thick beneath continents.
The Earth is typically divided into four layers: the crust, mantle, outer core, and inner core. These layers have different compositions and physical properties, and they play important roles in shaping the planet's structure and behavior.
the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
Core Crust and Mantle
Earth's compositional layers refer to the different materials that make up the planet (crust, mantle, core), while its structural layers refer to the physical attributes and properties of these layers (lithosphere, asthenosphere, mesosphere, outer core, inner core). The compositional layers focus on the elements and compounds present, while the structural layers focus on how these layers behave and interact.
The crust, mantle, and core. :)
mantle,crust,core
Earth's compositional layers are the crust, mantle, and core, based on the materials they are made of (silicates vs. metals). Structural layers are based on their physical properties and include the lithosphere, asthenosphere, mesosphere, outer core, and inner core. The main difference is that compositional layers are defined by chemical differences, while structural layers are based on physical properties like temperature and behavior.
Compositional layers refer to the different layers of the Earth based on their chemical composition, such as the crust, mantle, and core. Mechanical layers, on the other hand, are based on the physical properties and how they behave under stress, like the lithosphere, asthenosphere, and mesosphere. The crust, mantle, and core are compositional layers, while the lithosphere, asthenosphere, and mesosphere are mechanical layers.
Continental crust
Compositional layers refer to the Earth's division based on the materials that make up each layer (crust, mantle, core), while mechanical layers classify the Earth based on how easily each layer can flow or deform (lithosphere, asthenosphere, mesosphere, outer core, inner core). The compositional layers focus on the materials present, while the mechanical layers focus on the physical properties and behavior of each layer.
The compositional layers refer to the division of the Earth based on the chemical makeup of the layers, such as the crust, mantle, and core. On the other hand, the physical layers are based on the mechanical properties, like the lithosphere (rigid outer layer) and asthenosphere (partially molten layer beneath the lithosphere).
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
The compositional layers of the earth are the crust, mantle and core. The physical layers are the lithosphere, asthenosphere, mesosphere, outer and inner core.