OCKLOCKNEE AND AUCILLA RIVERS. 115 
Calcium Chloride - 3.213 
Sodium Sulphate - 8.407 
Magnesium Sulphate - 4-441 
Calcium Sulphate - 3.213 
Calcium Carbonate - 20.475 
Ferrous Carbonate--- 0.882 
Magnesium Carbonate _:_ 1.051 
Silicic Acid (Si 0 2 ) - 0.893 
Alumina - Traces 
Organic Matter (Loss on Ignition) _ 3.210 
Total _:_198.118 
Spring Number 2. 
Sodium Chloride_ 
Magnesium Chloride 
Calcium Chloride_ 
Potassium Chloride 
Sodium Sulphate — 
Magnesium Sulphate 
Calcium Sulphate — 
Iron Carbonate _ 
Calcium Carbonate _ 
Alumina _ 
Silica _ 
Total - 
23.664 
— .IS 
0.870 
1-452 
2.307 
3770 
0.382 
0.672 
6.656 
0.197 
0.348 
58.398 
55.083 
144.128 
76.136 
55.083 
■ 351.021 
15.120 
18.018 
15.309 
Traces 
55-031 
33.96415 
405.693 
258.532 
14-915 
24.892 
39.550 
64.632 
6.548 
11.520 
114.109 
3-377 
5.966 
1001.169 
In addition to the springs that have been mentioned, there are 
numerous smaller springs entering the creeks and rivers which flow 
into the Gulf. Some of these springs enter the Gulf below tide 
water and are known only by the “boil” of water through the salt 
water. Others form an important source of supply to the creeks 
and rivers. Among these are springs entering and making up 
Spring Creek, near Shell Point, in Wakulla County, and those en¬ 
tering the St. Marks River. 
