To determine the true angle of dip \( \theta \) in relation to the apparent angles of dip \( \theta_1 \) and \( \theta_2 \), we start by understanding that these are observed in two vertical planes that are perpendicular to each other. The relationship is derived from the vector components of the Earth's magnetic field.
Given:
The true angle of dip \( \theta \) can be expressed in terms of the apparent angles observed in each plane. The formula relating these angles is:
\(\cot^2 \theta = \cot^2 \theta_1 + \cot^2 \theta_2\)
Let's understand why this formula holds:
Therefore, substituting the values of the apparent angles of dip into the cotangent form gives the true angle of dip. The correct option is:
cot2θ = cot2θ1 + cot2θ2
This conclusion rules out the other options which suggest subtraction or the use of tangent, as these do not hold under the conditions given.