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.













