Step 1: Understanding geothermal gradient.
The geothermal gradient is the rate of temperature increase with depth. It is calculated by the formula:
\[
\text{Geothermal Gradient} = \frac{\text{Temperature Difference}}{\text{Depth}}
\]
The temperature difference is \( 275°C - 25°C = 250°C \). The depth is calculated using the lithostatic pressure, with the pressure increasing at 0.3 kbar/km. The depth is:
\[
\text{Depth} = \frac{3 \, \text{kbar}}{0.3 \, \text{kbar/km}} = 10 \, \text{km}
\]
Step 2: Calculation.
Now, calculate the geothermal gradient:
\[
\text{Geothermal Gradient} = \frac{250 \, °C}{10 \, \text{km}} = 25.0 \, °C/\text{km}
\]
Step 3: Conclusion.
The geothermal gradient is 25.0°C/km.
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) 
Match the seismic discontinuity in Group I with their occurrence in Earth's interior in Group II.
\[\begin{array}{|l|l|} \hline \textbf{Group I} & \textbf{Group II} \\ \hline \text{P. Conrad} & \text{1. Between lower mantle and outer core} \\ \hline \text{Q. Mohorovičić} & \text{2. Between crust and upper mantle} \\ \hline \text{R. Gutenberg} & \text{3. Between inner and outer core} \\ \hline \text{S. Lehmann} & \text{4. Between lower and upper crust} \\ \hline \end{array}\]
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.) 