Q. The soils most susceptible to liquefaction are:

A
Saturated dense sand
B
Saturated fine and medium sands of uniform particle size
C
Saturated clays of uniform size
D
Saturated gravel and cobbles
Solution:
  • Liquefaction is a phenomenon in which the strength and stiffness of a soil is reduced by earthquake shaking or other rapid loading.
  • Poorly drained fine-grained soils such as sandy, silty, and gravelly soils are the most susceptible to liquefaction.
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