To find the depth of the river, we need to understand the relationship between the velocity gradient, shearing stress, and viscosity. The velocity gradient is given by \(\frac{dv}{dy}\), where \(v\) is the velocity and \(y\) is the distance or depth in this context. The formula relating shearing stress \(\tau\), velocity gradient, and viscosity \(\eta\) is:
\(\tau = \eta \cdot \frac{dv}{dy}\)
Given:
Assuming the bottom layer of the river is stationary, the velocity gradient is given by:
\(\frac{dv}{dy} = \frac{v}{d}\)
Here, \(d\) is the depth we need to find. Substitute the known values into the shearing stress equation:
\(10^{-3} = 10^{-2} \cdot \frac{10}{d}\)
Solving for \(d\):
\(d = \frac{10^{-2} \cdot 10}{10^{-3}} = 100 \ m\)
The calculated depth of the river, \(100 \ m\), fits within the expected range of 100 to 100 meters, indicating a correct solution.


The Young's modulus of a steel wire of length \(6 m\) and cross-sectional area \(3 \,mm ^2\), is \(2 \times 10^{11}\) \(N / m ^2\). The wire is suspended from its support on a given planet A block of mass \(4 kg\) is attached to the free end of the wire. The acceleration due to gravity on the planet is \(\frac{1}{4}\) of its value on the earth The elongation of wire is (Take \(g\) on the earth \(=10\, m / s ^2\)) :