Match the seismic discontinuity in Group I with their occurrence in Earth's interior in Group II.
\[\begin{array}{|l|l|} \hline \textbf{Group I} & \textbf{Group II} \\ \hline \text{P. Conrad} & \text{1. Between lower mantle and outer core} \\ \hline \text{Q. Mohorovičić} & \text{2. Between crust and upper mantle} \\ \hline \text{R. Gutenberg} & \text{3. Between inner and outer core} \\ \hline \text{S. Lehmann} & \text{4. Between lower and upper crust} \\ \hline \end{array}\]
Step 1: Identifying the seismic discontinuities and their occurrences.
- The Conrad discontinuity is located between the lower and upper crust.
- The Mohorovičić (Moho) discontinuity is located between the crust and upper mantle.
- The Gutenberg discontinuity is located between the lower mantle and outer core.
- The Lehmann discontinuity is located between the inner and outer core.
Step 2: Analyzing the options.
(A) P-4, Q-2, R-1, S-3: Correct — This matches the seismic discontinuities with their corresponding locations in the Earth's interior.
(B) P-4, Q-2, R-3, S-1: Incorrect.
(C) P-3, Q-2, R-4, S-1: Incorrect.
(D) P-2, Q-4, R-1, S-3: Incorrect.
Step 3: Conclusion.
The correct answer is (A) P-4, Q-2, R-1, S-3, matching the seismic discontinuities with their corresponding positions in Earth's interior.
A magma having density of 2900 kg m\(^-3\) just reaches the surface through a two-layered crust as shown in the figure below. Assuming isostatic equilibrium, its depth of melting is .......... km. (Round off to one decimal place) 
Refer to the schematic sketch given (not to scale). Assume average saturated density of oceanic crustal rocks = 3200 kg/m3, density of ocean water = 1000 kg/m3, and acceleration due to gravity = 10 m/s2. The overburden pressure at a point (P) located 2 km below seabed and 4 km below the ocean surface is ________ MPa. (Answer in integer.) 