Gutenburg Discontinuity
Gutenburg Discontinuity
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
He didnt just discover 'a boundary' between mantle and outer core. He provided the first reasonable accounting of Earths interior (proved the thought that the earth was in layers and not just a homogenous planet). He was also the first to estimate the temperature and physical properties of the earths core, which is why the boundary is called after him. He first discovered the layers through seismic waves from earthquakes, realising they had different magnitudes and intensity because they must have had to go through layers before reaching the surface as well as depending where the epicentre is.
The boundary between the mantle and core is known as the core-mantle boundary. It lies approximately 2,900 kilometers below the Earth's surface. This boundary separates the molten iron-nickel outer core from the solid iron-nickel inner core.
90 degrees
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
It is 500 to 900 Celsius at the upper boundary and 4000 Celsius at the boundary near the outer core. A2. The values range between 500 deg C at the crust boundary, to over 4 000 deg C at the outer Core boundary.A1. between 100 to 1600 Celsius. The Mantle temperature varies to about 1600-4000 degrees.The average temperature of the mantle is is 5400 ºF (3000ºC).
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
Gutenburg Discontinuity
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
The boundary between the mantle and core is called the core-mantle boundary. This region is marked by a significant change in density and composition, representing the transition from the solid mantle to the liquid outer core of the Earth.
The Earth's interior is made up of four layers, the crust, mantle, outer core and the inner core. In the mantle, temperatures range between 500 to 900 degrees Celsius at the upper boundary with the crust; to over 4,000 degrees Celsius at the boundary with the outer core.
yes!
Gutenburg Discontinuity
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
boundary between the lower mantle and the outer core