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Sialolithiasis of Parotid Gland

Parotid sialolithiasis is calculus formation in the parotid gland or the Stensen duct. It accounts for 10 to 20 percent of salivary stones; the stones are usually smaller, softer and less often radiopaque than submandibular stones.

  • The saliva is serous and low in calcium, so stones form less often.
  • Dehydration, diuretics, anticholinergic drugs, Sjogren syndrome and poor oral hygiene contribute.
  • Stones may sit at the duct opening, at the masseter bend or inside the gland.

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