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Saratoga and How to See It

Chapter 30: History.
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About This Book

A practical visitor's guide to the mineral springs and resort community that combines geological and chemical analyses of the waters with descriptions of each spring's history and properties and guidance on drinking and therapeutic use. It maps and explains routes, hotels, accommodations, rail connections, drives, walks, and principal places of interest, and outlines climate notes and local institutions that serve visitors. Practical appendices cover bathing and remedial establishments, suggested routines, entertainments such as balls and races, and other conveniences for travelers, all presented to help health-seekers and tourists plan their stay and understand the springs' reputed effects.

Bases and Acids as actually found
in the Analysis uncombined
Star
Spring.
High
Rock
Spring.
Seltzer
Spring.
Pavilion
Spring.
United
States
Spring.
Hathorn
Spring.
Crystal
Spring.
Congress
Spring.
Geyser
spouting
well.
Potassium 7.496 5.419 0.949 4.931 4.515 5.024 5.326 4.611 13.039
Sodium 160.239 163.216 61.003 182.084 57.259 202.058 132.006 162.324 251.031
Lithium 0.163 0.202 0.093 0.976 0.499 1.179 0.445 0.490 0.720
Lime 43.024 45.540 31.066 41.540 32.189 58.989 35.218 49.569 58.901
Strontia Trace. Trace. Trace. Trace. 0.009 Trace. Trace. Trace. 0.211
Baryta 0.056 0.292 Trace. 0.517 0.537 1.026 0.429 0.549 1.190
Magnesia 16.992 15.048 11.051 20.895 19.968 48.346 20.592 33.358 40.915
Protoiyde of iron 0.491 0.598 0.689 1.040 0.289 0.456 0.824 0.137 0.396
Alumina Trace. 1.223 0.374 0.329 0.094 0.131 0.305 Trace. Trace.
Chlorine 246.357 241.017 82.128 282.723 90.201 314.037 203.292 246.834 352.825
Bromine 0.443 0.568 0.489 0.767 0.656 1.188 0.322 6.645 1.718
Iodine 0.106 0.072 0.026 0.060 0.039 0.166 0.055 0.117 0.208
Fluorine Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace.
Sulphuric acid 2.483 0.739 0.256 0.934 Trace. Trace. 0.992 0.409 0.146
Phosphoric acid Trace. Trace. Trace. 0.004 0.008 0.003 0.004 0.008 Trace.
Boracic acid Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace.
Carbonic acid in carbonates  56.606 62.555 44.984 60.461 50.380 104.928 54.984 80.249 112.880
Carbonic acid for bicarbonates 56.606 62.555 44.984 60.461 50.380 104.928 54.984 80.249 112.880
Silica 1.283 2.260 2.561 3.155 3.184 1.260 3.213 0.840 0.665
Organic matter Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace. Trace.
Water in bicarbonates 23.160 25.591 18.405 24.736 20.613 42.929 22.496 33.828 46.183
Oxygen in KO (SO3). 0.496 0.148 0.051 0.187  ...  ... 0.199 0.082 0.029
Oxygen in LiO (HO2 CO2) 0.187 0.232 0.105 1.116 0.570 1.347 0.509 0.560 0.824
Oxygen in NaO (HO2 CO2) 1.206 3.323 2.803 0.358 0.444 0.408 0.959 1.024 6.785
Oxygen in 2 NaO (HO, PO5)  ...  ...  ... 0.001 0.002 0.001  ... 0.002  ...
Total per U.S. gallon, 231 cu. in. 617.367 630.500 302.007 687.275 331.837 888.403 537.155 700.895 991.546
Total residue by evaporation 537.600 542.350 238.970 602.080 260.840 740.550 439.670 588.818 832.483



Table showing the total quantities of mineral matter left by evaporation, and of some of the more important constituents.
SPRING. Total solids
as left by
evaporation.
Chlorides of
sodium and
potassium.
All other solids
left by evaporation;
carbonates of lime,
magnesia, etc.
Bicarbonate
of lime (CaO,
HO, 2CO2).
Bicarbonate of
magnesia (MgO,
HO, 2CO2).
Bicarbonate
of iron (FeO,
HO, 2CO2).
Geyser Spouting well 832.48   586.71   245.77   170.39   149.34   0.98  
Hathorn spring 740.55   519.55   221.00   170.65   176.46   1.13  
Hamilton spring 611.71   411.00   200.71   144.84   104.80   1.80  
Congress spring 588.82   408.49   180.33   143.40   121.76   0.34  
High Rock spring 542.35   399.10   143.25   131.74   54.92   1.48  
Washington spring 353.23   215.00   138.23   110.23   40.56   2.40  
Excelsior spring 611.05   473.00   138.05   90.38   72.27   2.84  
Pavilion spring 602.08   467.56   134.51   120.17   76.73   2.57  
Putnam spring 354.79   220.50   134.27   110.72   60.01   3.97  
Columbian spring 353.08   219.00   134.08   104.89   78.05   3.26  
Star spring 537.60   408.05   129.55   124.46   61.91   1.21  
Crystal spring 459.67   336.79   122.88   101.88   75.16   2.04  
Eureka spring 280.16   171.00   119.16   94.02   63.75   3.36  
United States spring 260.84   150.49   110.35   93.12   72.88   0.71  
Empire spring 460.32   355.16   105.16   113.54   48.10   1.34  
Seltzer spring 238.97   135.62   103.35   89.87   40.34   1.70  
Red spring 155.53   73.50   82.03   79.80   27.84   2.51  
Village spring, Ballston 153.09   75.00   78.09   65.08   21.59   2.00  



Individuals have their preferences, and opinions may differ in regard to the relative value of the springs, particularly when parties are interested in them. We have no interest in one more than in all, and have brought to our task, we believe, no partiality. The manuscript has been submitted to leading physicians of Saratoga before publication, and is approved by them. The arrangement is alphabetical.

CONGRESS SPRING.

In Congress Park, opposite Grand Central Hotel. Congress and Empire Spring Company are the proprietors. The New York office is at 94 Chambers street.

History.

Congress Spring was discovered in 1792, by a party of three gentlemen, who were out upon a hunting excursion. Among the party was John Taylor Gilman, an ex-member of Congress from New Hampshire. Probably in that day, office conferred more honor than at the present time, and as a compliment to so distinguished a person, the spring was then and there christened the Congress. The attention of the hunters was attracted to the spot by the foot-prints of large numbers of deer, the first patrons, it seems, of the sparkling water. Although more especially esteemed by pretty dears of a different character at the present day, the liquid-eyed fawn, who grace Congress Park, are among those who take their daily rations. At the time of discovery, the low ground about the spring was a mere swamp, and the country in the immediate vicinity a wilderness. The mineral water issued in a small stream from an aperture in the side of the rock, which formed the margin of a small brook, and was caught by pressing a glass to the side of the rock. The flow of water was only about one quart per minute.

From the date of its discovery to the present time this celebrated spring has been the center of attraction at Saratoga. Its name has become a household word through out the land, and the whole civilized world are its customers.

At one time Mr. Putnam had three large potash kettles evaporating the water. The salts thus precipitated were sold in small packages to the amount of several hundred dollars. It was not long, however, before it was discovered that Congress water was not obtained by re-dissolving the salts, as might have been expected if the nature of the water had been considered.

About the year 1820, Dr. John Clarke, the proprietor of the first soda fountain opened in this country, purchased the Congress Spring property. By him the water was first bottled for transportation and sale, and to him the village is indebted for much of its beauty and attractiveness.

The simple and tasteful Doric colonnade over the Congress, and the pretty Grecian dome over the Columbian were erected by him. Dr. Clarke realized a handsome income from the sale of the water. He died in 1846, but the property continued in the hands of his heirs, under the firm name of Clarke & White, until 1865, when it was purchased by an incorporated company, under the title of "Congress and Empire Spring Company." The capital is $1,000,000, and the company is composed of a large number of individual stockholders. The present proprietors of Congress Spring have contributed not a little to the beauty and attractiveness of this favorite watering place.