Answer:
Explanation:here is the answer for the question u asked
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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<h3><u>Indiana climate change:
</u></h3>
- It has been made clear by several agencies that over the past hundred years the mean temperature of the state of Indiana and the adjacent regions has gone up by 1° F.
- One most important factor that has resulted in this increase in the average temperature is the rapidly increasing emission of the greenhouse gases.
- Indiana has stayed in the list of the top 10 states that produce half of the United States total greenhouse gases.
- Gradual and consistent degradation of the environment due to the greenhouse gases has culminated in frequent flooding and rapid melting of the ice sheets on the Great Lakes.
<span>C) Nucleated town, t-shaped village, linear hamlet</span>
Answer:
Equator is a imaginary line around which the earth rotates