Thirty-four small thrust faults provide analogs for larger cross-section or seismic-scale thrusts.

Thrust fault system formed without developing floor or roof thrusts.

Max. displacements are in limestone beds where they nucleated and tip into mudrock.

Displacements diminish up into hanging wall anticlines and down into footwall synclines.

Décollement layers may be a consequence rather than cause of thrust ramps.