Step 1: Understand slowness vector.
The slowness vector is defined as \( \nabla T(x, y, z) \), i.e., the gradient of the travel time.
Step 2: Analyze wavefront properties.
Wavefronts represent surfaces of constant travel time, i.e., \( T(x, y, z) = {constant} \). Rays are perpendicular to wavefronts, so the slowness vector (being the gradient) is normal to the wavefront.
Step 3: Evaluate options.
(A) Incorrect: Slowness is normal, not tangential.
(B) Correct: Slowness vector \( = \nabla T \).
(C) Correct: \( T(x, y, z) \) is constant on a wavefront.
(D) Incorrect: \( T \) increases along a ray path.
Consider a medium of uniform resistivity with a pair of source and sink electrodes separated by a distance \( L \), as shown in the figure. The fraction of the input current \( (I) \) that flows horizontally \( (I_x) \) across the median plane between depths \( z_1 = \frac{L}{2} \) and \( z_2 = \frac{L\sqrt{3}}{2} \), is given by \( \frac{I_x}{I} = \frac{L}{\pi} \int_{z_1}^{z_2} \frac{dz}{(L^2/4 + z^2)} \). The value of \( \frac{I_x}{I} \) is equal to 
Suppose a mountain at location A is in isostatic equilibrium with a column at location B, which is at sea-level, as shown in the figure. The height of the mountain is 4 km and the thickness of the crust at B is 1 km. Given that the densities of crust and mantle are 2700 kg/m\(^3\) and 3300 kg/m\(^3\), respectively, the thickness of the mountain root (r1) is km. (Answer in integer)