3379 days ago,
1443 views
3379 days ago,
1443 views
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. Retrn to message. . . . . . . Thick BEHAVIOR. Ceaseless stream at steady stressLinear, or Newtonian, thick conduct is communicated as:e = (s*t)/visc, where visc = viscosityTypical viscosities for rocks are between 1020 to 1028 Poise. 1 Poise = 1 Pa*secViscous stream happens in the strong earth beneath liquefying temperaturesRate is to a great degree moderate and requires 106 yrs or moreTypical strain rates, e/t =
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