86 FLORIDA GEOLOGICAL SURVEY-TWELFTH ANNUAL REPORT 
Geol. Surv. Bull. 84, p. 125, 1892) fossils of Vicksburg age [prob¬ 
ably Upper Ocala] were observed at St. Augustine at a depth of 
224 feet. This would fit into the gap in the samples I have had 
and would account for the. Lepidocyclina already noted. This 
also coincides with the data from other adjacent areas. 
There is no record of whether a horizon characterized by 
abundant thick Nummulites occurs here or not. 
The Lower Cretaceous of Fredericksburg age is indicated by 
the sample from 440 feet and occurs below, but probably orig¬ 
inated from about the same general level. How much above 440 
feet the. Lower Cretaceous extends cannot be determined, from 
lack of material. 
According to the description of the samples, a dense, light 
brown limestone is encountered from 495-520 feet. This may be 
similar to the hard, brown limestone occurring below the conical 
Orbitolina at various places. 
In the very limited material from below, none of the large, low 
forms of Orbitolina were met with but are in all probability 
there. Fossiliferous limestones are. recorded in the descriptions 
from 1,293-1,390 feet but no samples from this range were avail¬ 
able except at 1,351 feet, which had nothing of value. 
The well records show that both the. Ocala and the Lower Cre¬ 
taceous are much nearer the surface here than at Jacksonville. 
WELL OF CAMPAGNIE GENERALE DES PHOS. DE LA 
FLORIDE, AT ANTHONY, MARION COUNTY, 
FLORIDA. 
Samples are available from depths between 50 and 500 fee.t. 
No records of the casing are available, but from the condition of 
the samples it must be very complete for at least the. upper por¬ 
tion. Samples examined show the following: 
50 feet. No Lepidocyclina but very abundant large ‘Nummulites. 
75 feet. Few Nummulites. 
100 feet. Few Nummulites. 
no feet. Numerous small 1 foraminifera —Miliolidae and Orbitolina. 
130 feet. Mostly hard rock fragments. No foraminifera. 
