Critical taper wedge
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Critical taper concept in geodynamics. A wedge of material with density ρs is pushed over a slope with angle β with a horizontal line, by a force σx (x is the direction parallel to the slope). The wedge makes a slope with a horizontal line with angle α. Forces resisting this push are: 1) the load of an eventual water column above the wedge; 2) the load of the wedge working at the base of the wedge; 3) the shear strength of the base.
- 1) is calculated by multiplying the density of water (ρw) with the height of the water column (D), this is multiplied by the sine of angles α and β to get the component parallel to the base angle β.
- 2) is calculated by multiplying the density of the wedge material (ρs) with the height of the wedge perpendicular to the base slope (H), this is multiplied by the sine of angle β to get the component parallel to the base angle β.
- 3) is given by the Mohr-Coulomb criterion.
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