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Which of the following is not considered a stage in the capital budgeting process?
Synclines
Geological folds that dip towards each other from opposite sides, often forming a trough-like structure.
Joints
Natural fractures or separations in rocks that occur without the rock moving apart.
Normal Faults
A type of fault where the hanging wall moves down relative to the footwall due to tensile (pulling apart) stress in the Earth's crust.
Oblique-Slip Faults
Faults that exhibit both vertical (dip-slip) and lateral (strike-slip) movement, combining features of normal, reverse, and transform faults.
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