Point Loma Formation
|Point Loma Formation
Stratigraphic range: Late Cretaceous
Typical exposure of the Point Loma Formation at Sunset Cliffs
|Unit of||Rosario Group|
|Primary||sandstone, shale, siltstone|
|Extent||San Diego to La Jolla|
|Named for||Point Loma|
|Named by||Kennedy and Moore, 1971|
The Point Loma Formation was first described as the middle formation of the Rosario Group by Kennedy and Moore in 1971. Their description is that the lower half is composed of interbedded fine-grained, dusky yellow sandstone and olive-gray clay shale in ledgy graded beds about 20 cm thick, which grades into massive grayish-black siltstone in the top half of the formation.
Dinosaur remains have been recovered from this formation. In 1967 Brad Riney found a single hadrosaur neck vertebra in a sea cave in La Jolla. In 1983 he found a femur of a hadrosaur in Carlsbad and in 1986 thirteen cervical vertebrae of another hadrosaur. In 1987 Riney discovered teeth and fragments of the postcranium of the ankylosaur Aletopelta coombsi. In about 1980 Leon Case found the midsection of a right dentary with teeth of a hadrosaur while walking along a beach in San Diego County.
- Kennedy, M.P., and Moore, G.W., 1971, Stratigraphic relations of Upper Cretaceous and Eocene formations, San Diego coastal area, California: American Association of Petroleum Geologists Bulletin, v. 55, no. 5, p. 709-722. article
- Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. ISBN 0-520-24209-2.
- "Table 17.1," in Weishampel, et al. (2004). Page 368.
- Hilton (Dinosaurs and Other Mesozoic Reptiles of California, 2003), pp. 233-36.
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