To determine the correct location of the Gutenberg discontinuity, let's analyze Earth's internal structure and seismic evidence:
1. Understanding Earth's Layers:
Earth's interior is divided into distinct layers separated by seismic discontinuities:
2. Evaluating the Options:
- Crust-mantle boundary: Incorrect (this describes the Moho discontinuity)
- Within the mantle: Incorrect (the discontinuity is a boundary, not within a zone)
- Mantle-core boundary: Correct (separates solid mantle from liquid outer core)
- Within the core: Incorrect (the discontinuity marks the upper core boundary)
3. Key Characteristics:
The Gutenberg discontinuity: Occurs at ~2,900 km depth Marks where P-wave velocities drop sharply (due to liquid outer core) Corresponds to the core-mantle boundary (CMB) Named after seismologist Beno Gutenberg who identified it in 1914
Final Answer:
The Gutenberg discontinuity is located at the boundary between the Earth's mantle and core.