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The Dissertation Committee for Judith L - The University of Texas at ...

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springs in <strong>Texas</strong>. While the spring flow varies year to year, the daily average flow from<br />

the Comal Springs is 184 million gallons and per minute minimum flow <strong>of</strong> 112,500<br />

gallons and a maximum <strong>of</strong> 157,000 gallons. 15 <strong>The</strong>se w<strong>at</strong>er sources pulled other groups <strong>of</strong><br />

people to settle the area long be<strong>for</strong>e the arrival <strong>of</strong> the Germans and Southern Anglos.<br />

Archeological evidence shows human habit<strong>at</strong>ion in both areas d<strong>at</strong>ing back to 9,200 years<br />

ago. 16<br />

<strong>The</strong>se two communities are found in the Cwd 17 clim<strong>at</strong>e type <strong>of</strong> a modified<br />

Köppen clim<strong>at</strong>e classific<strong>at</strong>ion. 18 (See Figure 1.3) 19 New Braunfels and San Marcos<br />

occupy a mesothermal region where the majority <strong>of</strong> time the years are humid and<br />

experience a mean annual temper<strong>at</strong>ure <strong>of</strong> 73.2 degrees Fahrenheit. Winter is the dry<br />

season though seasonal variability is not all th<strong>at</strong> gre<strong>at</strong>. Within this zone there are also<br />

occasional years where desert-like conditions are experienced. <strong>The</strong> reason <strong>for</strong> this is th<strong>at</strong><br />

the two communities exist not far from the 100 th meridian, the traditional dividing line<br />

between the humid, wetter clim<strong>at</strong>e <strong>of</strong> the eastern half <strong>of</strong> the United St<strong>at</strong>es from the dry<br />

clim<strong>at</strong>e <strong>of</strong> the western half <strong>of</strong> the country. 20 <strong>The</strong> proximity to this transition zone<br />

accounts<br />

15 U.S. Dept. <strong>of</strong> Agriculture, Soil Survey, 3.<br />

16 Hugh Williamson, “San Marcos, River Town.” <strong>Texas</strong> Parade, Vol. 12, No. 7 (December 1951), 15-19;<br />

and “San Marcos, <strong>Texas</strong> (Hays County), “ n.d., n.p., Vertical files, Center <strong>for</strong> American History, <strong>The</strong><br />

<strong>University</strong> <strong>of</strong> <strong>Texas</strong> <strong>at</strong> Austin.<br />

17 <strong>The</strong> Köppen classific<strong>at</strong>ion <strong>of</strong> “C” represents mesothermal clim<strong>at</strong>e zones. A mesothermal clim<strong>at</strong>e is one<br />

where coolest-month temper<strong>at</strong>ures average between 32 and 64.4 degrees Fahrenheit. <strong>The</strong> lower case “w”<br />

represents a dry winter season and the “d” indic<strong>at</strong>es occasional dry years. For a more detailed discussion <strong>of</strong><br />

the Köppen system as applied to <strong>Texas</strong> see Richard Joel Russell’s article “Clim<strong>at</strong>es <strong>of</strong> <strong>Texas</strong>,” Annals <strong>of</strong><br />

the Associ<strong>at</strong>ion <strong>of</strong> American Geographers 35 (June 1945), 37-52.<br />

18 <strong>The</strong> modified Köppen system referred to here is found in the article “Clim<strong>at</strong>es <strong>of</strong> <strong>Texas</strong>.” <strong>The</strong><br />

modific<strong>at</strong>ions were made by Russell, the author <strong>of</strong> the article.<br />

19 Terry Jordan, <strong>Texas</strong>: A Geography, 25.<br />

20 Ibid., 44-47.<br />

11

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