To determine the average outflow velocity of water from the cylindrical soil sample, we can use the formula for velocity, v, which is given by:
v = Q/A
where Q is the volumetric flow rate and A is the cross-sectional area of the tube.
First, calculate the cross-sectional area, A, of the tube. The formula for the area of a circle is:
A = π(d/2)2, where d is the diameter of the tube.
Here, d = 100 mm.
Thus, A = 3.14 × (100/2)2 = 3.14 × 502 = 3.14 × 2500 = 7850 mm2.
Now, calculate the volumetric flow rate, Q. Given that 1000 mm3 of water is collected every 10 seconds, Q = 1000 mm3 per 10 sec = 100 mm3/sec.
Substitute Q and A into the velocity formula:
v = 100/7850
v ≈ 0.012738.
Rounded to three decimal places, the average outflow velocity is approximately 0.013 mm/sec.
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) 
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 )
Which of the following stereographic projections represent(s) an upright plunging fold? 
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) 
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) 
The shaded region (P) in the given ACF diagram represents the compositional range of mafic rocks that have undergone granulite facies metamorphism. Which of the following equilibrium mineral assemblages is/are identified in these mafic rocks? 
Match the stratigraphic units in Group I with their corresponding basins in Group II.
| Group I | Group II |
|---|---|
| P. Kajrahat Limestone | 1. Cuddapah |
| Q. Shahabad Limestone | 2. Pranhita-Godavari |
| R. Chanda Limestone | 3. Vindhyan |
| S. Narji Limestone | 4. Bhima |
The schematic diagram given below shows textual relationship among garnet, muscovite, biotite and kyanite in a metapelite. Biotite defines S1 foliation and muscovite defines S2 and S3 foliations. S1, S2, and S3 fabrics were developed during distinct deformation events D1, D2, and D3, respectively. Which one of the following represents the pre-D3 mineral assemblage? 