Submandibular Gland (Wharton's Duct)
The submandibular gland, which drains through Wharton's duct located beneath the tongue, is the gland from which a salivary stone would emerge. 1, 2
Anatomical Location and Stone Distribution
The submandibular gland accounts for 80-84% of all salivary stones, making it by far the most common site for sialolithiasis. 2, 3
Within the submandibular system, 90% of stones are located in Wharton's duct itself (the duct that runs beneath the tongue), rather than in the gland parenchyma. 3, 4
The duct opening can be visualized intraorally at the floor of the mouth, where stones may sometimes be directly palpable or even visible. 1, 2
Clinical Recognition
The hallmark presentation is pain and swelling of the submandibular region that begins just before or during meals, as salivary flow is stimulated but blocked by the stone. 1, 5
Bimanual palpation of the floor of the mouth allows direct detection of calculi within Wharton's duct, making physical examination a critical diagnostic tool. 1, 6
Intraoral inspection with adequate lighting enables visualization of the duct opening and assessment of reduced or absent salivary flow from the affected side. 1
Why the Submandibular Gland Predominates
The submandibular gland's susceptibility to stone formation relates to several anatomical and physiological factors, though the exact etiology remains incompletely understood. 7 The duct's upward course against gravity, higher calcium concentration in submandibular saliva, and more viscous secretions all contribute to stone formation. 3