They would differ in temperature, mineralogy, density, and pressure.
Temperature: The upper mantle is cooler than the lower mantle. Composition: The upper mantle is more silicate-rich and less dense compared to the lower mantle. Physical properties: The upper mantle is more rigid and brittle, while the lower mantle is more ductile and capable of flow.
The main difference between the upper and lower mantle is their depth within the Earth. The upper mantle is located closer to the Earth's surface, extending from the crust to a depth of about 410-660 km, while the lower mantle lies beneath the upper mantle, extending from around 660-2,891 km deep. Additionally, the upper mantle is more rigid and composed of mainly solid rock, while the lower mantle experiences higher pressures and temperatures, leading to more plastic behavior.
The three sub layers of the mantle are the lithosphere, asthenosphere, and mesosphere. The lithosphere is the rigid outer layer consisting of the crust and upper part of the mantle. The asthenosphere is a partially molten layer beneath the lithosphere that allows for the movement of tectonic plates. The mesosphere is the lowermost and solid part of the mantle.
The principal divisions of the solid Earth based on compositional differences are the crust, mantle, and core. The crust is the outermost layer and is composed mainly of lighter elements like silicon and oxygen. The mantle lies beneath the crust and consists of denser silicate minerals. The Earth's core is located at the center and is primarily made up of iron and nickel.
The three layers of the geosphere are the crust, mantle, and core. The crust is the outermost layer and is divided into continental and oceanic crust. The mantle lies beneath the crust and is divided into the upper and lower mantle. The core is the innermost layer and is further divided into the outer core and inner core.
Temperature: The upper mantle is cooler than the lower mantle. Composition: The upper mantle is more silicate-rich and less dense compared to the lower mantle. Physical properties: The upper mantle is more rigid and brittle, while the lower mantle is more ductile and capable of flow.
The three main spheres in the Earth's mantle are the upper mantle, the transition zone, and the lower mantle. The upper mantle extends from the Moho (the boundary between the crust and the mantle) to about 410 kilometers deep, while the transition zone lies between 410 and 660 kilometers. The lower mantle extends from 660 kilometers to the outer core, reaching depths of around 2,900 kilometers. Each of these layers has distinct physical and chemical properties that influence geological processes.
The main difference between the upper and lower mantle is their depth within the Earth. The upper mantle is located closer to the Earth's surface, extending from the crust to a depth of about 410-660 km, while the lower mantle lies beneath the upper mantle, extending from around 660-2,891 km deep. Additionally, the upper mantle is more rigid and composed of mainly solid rock, while the lower mantle experiences higher pressures and temperatures, leading to more plastic behavior.
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The 3 main layers of earth (crust, mantle, core) are divided into crust, upper mantle, lower mantle, outer core, and inner core.
The three major subdivisions of the Earth are the crust (including the continents and ocean floor), the mantle (made up of the upper mantle and lower mantle), and the core (which consists of the outer core and inner core). These subdivisions are based on differences in composition, density, and physical properties.
Technically, the most interior is the inner core, then the outer core, then the lower mantle
The three parts that make up the Earths mantle are the crust, core, and mantle.
That depends on what three 'economies' you are talking about.
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It recognizes fundamental differences in prokaryotes.