Concept:
The Earth is composed of different layers: crust, mantle, and core. The boundaries separating these layers are called discontinuities, where there is a sudden change in seismic wave velocity due to differences in composition and density.
- Mohorovičić Discontinuity (Moho): Separates crust and mantle
- Gutenberg Discontinuity: Separates mantle and outer core
- Lehmann Discontinuity: Separates outer core and inner core
- Conrad Discontinuity: Separates upper and lower crust (not always distinct)
Step 1:Identify the boundary between crust and mantle.
The boundary where seismic waves suddenly increase in velocity marks the transition from the crust to the mantle.
Step 2:Match with the correct discontinuity name.
This boundary is known as the Mohorovičić Discontinuity, commonly called the Moho.