186 
‘ GEOLOGY. 
POST-PLIOCENE DEPOSITS OF MONTEREY, SAN PEDRO, AND SAN DIEGO. 
Evidences of a comparatively recent or Post-Tertiary 'elevation of the California coast are 
found at various points from San Francisco south to San Diego. At San Pedro, near the mouth 
of the Los Angeles River, a low bluff, or hank, about thirty feet high, consists of heach-sand 
and shingle, mingled with shells, similar to those now living in the waters of the Pacific. 
Accumulations of the same kind are also found at Santa Barbarg, and San Diego. 
The hank at San Pedro is composed, at the base, of coarse, brown sea-sand, interstratified with 
fragments of shells ; hut the upper portions are formed of coarser materials, in two or three 
layers, from four to six feet thick. The upper layer is of soil and sand, charged with fragments 
of Pecten ; below this, a thick stratum of sand is filled with shells and a layer of fragments of 
a calcareous rock, or soft limestone, perforated in every direction by boring mollusks. Beach- 
shingle and sand, with shells, are found below. These fossils were all remarkably well pre¬ 
served ; hut had evidently been subjected to much wearing upon a beach, as the fragments were 
very abundant, and many of the shells were broken. 
The following species were obtained: Tellina Pedroana , Venerupis cycladiformis, Saxicava 
abrupta, Petricola Pedroana, Schizothoerus Nutt alii, Mytilus Pedroanus, Penitetta spelceum, 
Fissurella crenulata, Nassa inter striata, N. Pedroana , Strepliona Pedroana, Littorina Pe¬ 
droana. These were all determined and described by Mr. Conrad, who observes in his 
letter that “the shells are generally those which live in the adjacent waters, and indicate 
little, if any, change of temperature since their deposition. The littoral character of this form¬ 
ation is very evident. Water-worn shells and fragments show the action of the surf, whilst 
entire specimens of bivalves, and Pnoladidce, and Saxicavce, remaining undisturbed in their self- 
excavated domicils, exhibit the same disposition of marine shells that is familiar to the observer 
on all sandy and argillaceous shores. They burrow in clay, mud, or sand, beyond the ordinary 
action of the surf; whilst some are scooped out by the tempest-driven surge, and others preyed 
upon by fishes and marine animals of various kinds, and are thus broken up and deposited 
among the living species.” 
The action of the surf at the base of this hank has liberated great numbers of the fossils, and 
they are to be found strewed along the beach, mingled with shells recently cast up by the waves. 
A tooth of the mammoth was also obtained from this hank by a brother of Captain Ord, of 
tooth op the mammoth, (lower molar, one-third natural size.) 
the United States Coast Survey. It is a lower molar, weighing eight pounds, and twelve inches 
long. It has a grinding surface five and a half inches long, which exposes the ends of eight 
