188 
FLORIDA STATE GEOLOGICAL SURVEY. 
depth of 260 feet. The well is cased 100 feet and the principal 
supply of water comes from a depth of 200 feet. The water is 
reported to rise five feet above the surface. 
ESPANOLA. 
A few wells occur in or near Espanola. The wells immedi¬ 
ately in the town do not flow. Flowing wells are obtained, how¬ 
ever, from one to five miles south, along Flaw Creek. 
FEDERAL POINT. 
Federal Point lies within the flowing area bordering the St. 
Johns River. A considerable number of wells have been drilled 
in the vicinity of this place. The material encountered here, to 
the depth of about 125 feet, consists largely of clays. Water is 
obtained at a depth of from 200 to 250 feet, the wells terminating 
in limestone. 
The following is a partial log of the well of Messrs. Hubbard 
and Hart, one-fourth mile northwest of Federal Point. This is 
a six-inch well drilled by Lloyd Crary in 1889. The well has a 
total depth of 225 feet and is cased 60 feet. The water is re¬ 
ported to rise twenty feet above the surface or about thirty feet 
above sea level. The principal supply is obtained at a depth of 
two hundred feet. 
Feet. 
Record incomplete, said to consist largely of clays, 
bluish in color except where oxidized yellow at surface 0-128 
A sample from the depth of 128 feet consists of frag¬ 
ments of dark-colored rock, more or less water 
worn, including small sharks’ teeth, fragments of 
bones, occasional shining black phosphatic pebble's.128-130 
Yellowish sandy clays .130-145 
Dark fossiliferous rock. Fragments of this rock are 
of grayish color and contain inclusions of a dark- 
colored mineral similar in character to rock, found 
at St. Augustine at a depth of 178 feet. Sharks’ 
teeth and black phosphatic pebble's also occur as 
well as numerous shell fragments . 145-130' 
