The absolute pressure is the sum of the atmospheric pressure and the pressure due to the water column. The pressure due to the water column is:
\[
P_{\text{water}} = \rho g H,
\]
where:
- \(\rho = 1050 \, \text{kg/m}^3\) (density of sea water),
- \(g = 9.8 \, \text{m/s}^2\) (acceleration due to gravity),
- \(H\) is the depth in meters.
The total pressure at depth \(H\) is the atmospheric pressure plus the pressure due to the water:
\[
P_{\text{total}} = P_{\text{atm}} + \rho g H.
\]
Substituting the values:
\[
4.2 \, \text{MPa} = 0.101 \, \text{MPa} + (1050 \times 9.8) \times H.
\]
\[
4.2 \times 10^6 = 101 \times 10^3 + (1050 \times 9.8) \times H.
\]
Solving for \(H\):
\[
4.2 \times 10^6 - 101 \times 10^3 = (1050 \times 9.8) \times H,
\]
\[
4.099 \times 10^6 = 10290 \times H,
\]
\[
H = \frac{4.099 \times 10^6}{10290} \approx 398.5.
\]
Thus, the depth is approximately:
\[
\boxed{397 \, \text{to} \, 399 \, \text{m}}.
\]