I believe that the answer to the question provided above is that <span>If ethnic Russians in Kazakhstan were to agitate for a part of the country to secede based on concentrations of ethnic Russians is yes. They would be affected since natives of Kazakhstan are large in population.</span>
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The faults in which the hanging wall moves down relative to the footwall is called normal fault.
Explanation:
There are several types of faults based on their characteristics. One of them is the normal fault, or normal dip-slip fault. The main characteristic of this fault is that its hanging wall moves down relative to the footwall, while the footwall tends to move up relative to the hanging wall. The force that creates this type of faults is the vertical compression as the crust of Earth is lengthening.
- These faults can be found all over the world, and they are actually the most common type of faults.
- The normal dip-slip faults are bounding big portion of the mountains, as well as rift valleys.
- As these faults progress with their formation, with the footwall going up, and the hanging wall going down, the footwall becomes a hill or a mountain, while the hanging wall becomes a valley.
- The normal dip-slip faults can be found at all types of tectonic plate boundaries.
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Answer:
the mass of the prism is 29.11 g
Explanation:
Given the dimensions of the prism as;
7 mm = 0.7 cm
18 mm = 1.8 cm
35 mm = 3.5 cm
volume of the prism = 0.7 cm x 1.8 cm x 3.5 cm
= 4.41 cm³
density of the prism, ρ = 6.6 g/cm³
The mass of the prism is calculated as;
mass = density x volume
mass = 6.6 g/cm³ x 4.41 cm³
mass = 29.106 g
mass = 29.11 g
Therefore, the mass of the prism is 29.11 g
Answer:
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Explanation:
UHhHh, not enough context. Density = mass/volume.