Step 1: Recall the Phanerozoic Eon divisions. The Phanerozoic Eon (541 Ma to present) is divided into Paleozoic, Mesozoic, and Cenozoic eras, each containing multiple periods.
Step 2: Approximate durations. - Cambrian: ~541–485 Ma → about 56 million years. - Devonian: ~419–359 Ma → about 60 million years. - Cretaceous: ~145–66 Ma → about 79 million years. - Silurian: ~443–419 Ma → about 24 million years.
Step 3: Compare durations. The Silurian Period is clearly the shortest, lasting only about 24 million years.
Final Answer: \[ \boxed{\text{Silurian}} \]
While doing Bayesian inference, consider estimating the posterior distribution of the model parameter (m), given data (d). Assume that Prior and Likelihood are proportional to Gaussian functions given by \[ {Prior} \propto \exp(-0.5(m - 1)^2) \] \[ {Likelihood} \propto \exp(-0.5(m - 3)^2) \] 
The mean of the posterior distribution is (Answer in integer)
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)