Deflation basins, called blowouts, are hollows formed by the removal of particles by wind.
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Saucer blowouts indicate a deceleration of wind flow along the deflation basin as the structure widens over time by reversing flows eroding the sides and expanding upwind.
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In troughs, the structure s topography can accelerate flows and form jets that result in maximum erosion along the deflation basin floor and laterally expand the slopes of the blowout.
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Even though they re more influences blowout structures have on their morphology, both types basically tend to have deflation basins eroded until they reach their non-erodible base level.
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