Clark Field was a baseball park in Austin, Texas, used primarily by the University of Texas Longhorns. The field was used from 1928 until 1974. It is considered one of the most novel ballparks ever conceived thanks to its location. There was a limestone cliff in the outfield that created havoc for outfielders and made baseball games exciting. It was replaced by UFCU Disch-Falk Field in 1975.CliffClark Field was unusual because there was a 12- to 30ft limestone cliff that ran from left-center to center field that made playing the outfield adventurous. The cliff could only be accessed via a goat path in the left-center field. Center field was nicknamed "Billy Goat Hill." There was a scoreboard on top of the hill in the field in front of the fence that could cause even more weird bounces for outfielders. Clearly, this gave the Longhorns a home field advantage over visiting teams. For example, the Longhorns could easily get an inside-the-park home run when a ball was hit in the direction of the cliff because the opposing outfielders were perplexed by its caroms and how to make plays by using the cliff. Longhorn outfielders could typically hold batters to a double or triple because of their familiarity with the cliff. Half of the team's outfielders purportedly chose to play on top while the other half chose to play in front of the cliff.AtmosphereWhile the ballpark had an irregular outfield, the stadium only sat 2,000. The stadium had an intimate yet palatial feeling that mirrored other jewel box ballparks such as Wrigley Field, Fenway Park, and Tiger Stadium. Once when the Texas A&M Aggies visited Clark Field, the crowd overflowed into right field and rowdiness ensued, which happened regularly when other visiting teams played there as well. In the late 1960s, the Sam Houston State Bearkats regularly opened with weekend doubleheaders in Austin.
