Step 1: Understand the problem setup.
The Earth can be modeled as a sphere. The core is the inner part of the Earth, and the rest of the Earth is made up of the mantle and crust. To solve this, we need to use the formula for the volume of a sphere: \[ V = \frac{4}{3} \pi r^3 \] The core radius is roughly 3,500 km, and the total Earth radius is around 6,371 km. We need to calculate the volume of the core and the total volume of the Earth.
Step 2: Calculate the volume of the Earth and the core.
The total volume of the Earth: \[ V_{\text{Earth}} = \frac{4}{3} \pi (6371)^3 \approx 1.08321 \times 10^{12} \, \text{km}^3 \] The volume of the core: \[ V_{\text{Core}} = \frac{4}{3} \pi (3500)^3 \approx 1.7764 \times 10^{11} \, \text{km}^3 \]
Step 3: Calculate the volume percentage.
The volume percentage of the core relative to the total volume of the Earth is: \[ \text{Volume \% of Core} = \left( \frac{V_{\text{Core}}}{V_{\text{Earth}}} \right) \times 100 = \left( \frac{1.7764 \times 10^{11}}{1.08321 \times 10^{12}} \right) \times 100 \approx 16.4\% \]
Step 4: Conclusion.
The volume percentage of the core relative to the total volume of the Earth is 16.4%.
A magma having density of 2900 kg m\(^-3\) just reaches the surface through a two-layered crust as shown in the figure below. Assuming isostatic equilibrium, its depth of melting is .......... km. (Round off to one decimal place) 
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)


Two boreholes A and B, both inclined towards 270°, penetrate a dipping coal bed at the same point and pass through it entirely in the sub-surface as shown in the figure below. The bed dips towards 270°. The thickness of the coal bed, measured along the borehole A is 10 m and along borehole B is 8 m. The angle between the two boreholes is 20°. The orthogonal thickness \( x \) of the coal bed is ........ m. (Round off to one decimal place) 
A well-developed succession of laminated shale is bound by two volcanic ash beds that were precisely dated as shown in the schematic diagram given below. Assuming a constant sedimentation rate, the age of the fossiliferous limestone bed 65 m above the basal volcanic ash bed is ............ Ma. (Round off to nearest integer) 
The data tabulated below are for flooding events in the last 400 years.
The probability of a large flood accompanied by a glacial lake outburst flood (GLOF) in 2025 is ........... \(\times 10^{-3}\). (Round off to one decimal place)
| Year | Flood Size | Magnitude rank |
|---|---|---|
| 1625 | Large | 2 |
| 1658 | Large + GLOF | 1 |
| 1692 | Small | 4 |
| 1704 | Large | 2 |
| 1767 | Large | 2 |
| 1806 | Small | 4 |
| 1872 | Large + GLOF | 1 |
| 1909 | Large | 2 |
| 1932 | Large | 2 |
| 1966 | Medium | 3 |
| 2023 | Large + GLOF | 1 |
A satellite launching vehicle is carrying a lander for Moon mapping.
As shown in the figure below, P is the position where the gravitational forces exerted by Earth and Moon on the vehicle balance out.
The distance \( P \) from the center of the Earth is ........... \(\times 10^5\) km. (Round off to two decimal places)
The isobaric temperature-composition (T–X) phase diagram given below shows the phase relation between components M and N. The equilibrium melting undergone by the rock R to generate the liquid of composition L is .............. % (In integer )