Answer: Troposphere
Explanation:
Clouds form in the troposphere, which is the layer of the atmosphere that is closest to Earth.
The process of cloud formation starts with warm, moist air that rises because warm air rises. This air cools as it rises. The temperature of the rising air drops until the air can no longer rise further and it expands into the troposphere. The water vapor in the air then condenses to form water droplets which form clouds.
Answer:
Explanation:
The Brahmin Varna consists of priests, and individuals of this specific Varna are separated into sub-castes called gotras
Answer:
a gypsum.
Explanation:
On the moh's scale of hardness, minerals that are above another can be scratched by the one below.
The moh's scale is used to measure the hardness of a substance.
- Hardness increases upward on the scale
- Since gypsum and talc are found below the hardness of fingernail.
- They can easily be scratched by the fingernail.
Answer:
The convergence of tectonic plates, forming a mountain range.
Explanation:
On the diagram, we can see the Eurasian plate and Indian plate, as well as the movement of the Indian plate over time relative to the Eurasian plate. The Indian plate has been moving over the course of millions of years from the southern hemisphere toward the northern hemisphere and has eventually hit the Eurasian plate. The two plates have collided and formed a convergent plate boundary.
The convergence occurs between continental crusts. With the crust constantly creating an enormous amount of pressure along the plate boundary, the crust in this part has started to bend and lift up, gradually creating a mountain range. The mountain range that has formed here is actually the highest and most massive mountain range in the world, the Himalayas.
At some point in an earthquake, solid rock produces more shaking and building damage than loose, water-saturated soils. Stresses purpose rocks to deform; earthquakes arise as the rock can now not deform and ruptures
While earthquake surprise takes place in waterlogged soils, the water-filled pore spaces fall apart, which decreases the general volume of the soil. This technique increases the water pressure between character soil grains, and the grains can then move freely within the watery matrix.
But, earthquake shaking can disrupt the shape, the soil particles do not guide all the weight, and the groundwater strain starts offevolved to rise. The soil debris can circulate farther, and come to be entrained within the water--the soil flows. Liquefied soil will pressure open floor cracks so one can get away from the floor.
Learn more about earthquakes here:
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