between the mantle and the core..
between the mantle and the core..
Gutenburg Discontinuity
No, the Lehmann discontinuity is believed to be located between 220 km and 260 km beneath the Earth's surface. The Gutenberg discontinuity, on the other hand, sits at a depth of around 2,900 km.
The Gutenberg Discontinuity is found beneath the Mohorovičić discontinuity (Moho) in the lithosphere. It is located at a depth of about 70 km to 400 km below the Earth's surface. This boundary separates the upper mantle from the lower mantle.
No, the Gutenberg discontinuity and the Conrad discontinuity are not the same. The Gutenberg discontinuity refers to the boundary between the Earth's crust and the underlying mantle, located at a depth of about 30 to 50 kilometers. In contrast, the Conrad discontinuity is the boundary within the crust, separating the upper crust from the lower crust, typically found at depths of about 10 to 20 kilometers. Both discontinuities are important in understanding the Earth's internal structure, but they occur at different depths and represent different geological layers.
between the mantle and the core..
Wiechert-Gutenburg Discontinuity
The Wiechert-Gutenberg discontinuity is located at a depth of around 2,900 kilometers (1,800 miles) below the Earth's surface, between the outer core and the lower mantle. This boundary marks the transition between the liquid outer core and the solid mantle in the Earth's interior.
The Wiechert-Gutenberg Discontinuity is located within the Earth's mantle, specifically at a depth of approximately 400 to 700 kilometers (about 250 to 430 miles) beneath the Earth's surface. It marks the boundary between the upper mantle and the lower mantle, characterized by a change in seismic wave speeds and material properties. This discontinuity is named after the seismologists Emil Wiechert and Beno Gutenberg, who contributed to our understanding of the Earth's internal structure.
The Gutenberg Discontinuity is a boundary within the Earth's interior that separates the outer core from the lower mantle. It is characterized by a rapid increase in seismic wave velocities, indicating a change in composition and physical properties. The Gutenberg Discontinuity is located at a depth of about 2,900 kilometers (1,800 miles) beneath the Earth's surface.
Gutenburg Discontinuity
Wiechert-Gutenburg Discontinuity
The outermost layer, known as the Earth's crust, indicates a dramatic decrease in material density compared to the denser layers beneath it, such as the mantle and core. This decrease in density is due to the lighter composition of the rocks and minerals that make up the crust compared to the denser materials found deeper within the Earth.
We know the discontinuity exists because of different types of seismic waves; certain waves can penertrate to different depths. Seismic waves are refracted at the Gutenburg discontinuity, which marks the upper boundary of the earth's core
Jason Wiechert's birth name is Jason McCarroll Wiechert.
The Gutenberg Discontinuity, is the boundary, as detected by changes in seismic waves, between the Earth's lower mantle and the outer core about 1800 miles below the surface.It is also called the core-mantle boundary.
Eric Wiechert is 6' 1".