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The debate involving how cuspate forelands form is ongoing.
Over time, a cuspate foreland forms as a result of continued accretion and progradation.
Point Scott is a cuspate foreland along this lakeshore that has formed from the gradual accumulation of sand and gravel.
Where marine action is relatively stronger deltas tend to be cuspate with concave outlines in plan, for example the Tiber, though one wonders whether these differences in plan might not be due primarily to the frequency and location of distributaries: the Tiber has only one.
Orford Ness is a cuspate foreland shingle spit on the Suffolk coast in Great Britain, linked to the mainland at Aldeburgh and stretching along the coast to Orford and down to North Wier Point, opposite Shingle Street.
Yanoconodons name is composed of two elements: 'Yan' is taken from the Yan Mountains in the north of the Hebei Province near where the holotype of Yanoconodon was found; 'Conodon' is an often used as a mammalian taxonomic suffix meaning 'cuspate tooth'.