Over the Creek and Through the Woods

…. To Barton Springs we go!

For our first of many field trips this summer, our REU group visited Barton Springs, a natural groundwater fed pool in the city of Austin. This is a prime spot of interest for those looking to escape the heat of the day as the pool’s water is around 68°F yearlong.

Barton Springs Creek

However, we weren’t there just to swim. Barton Springs is an interesting case study in biodiversity and climate effects on a karst (characterized by a lot of limestone) region. Through this trip we explored both of these aspects in person. Curious to learn more? Prior to the trip we read these three articles on the Barton Springs area and some of the issues impacting it.

After arriving in the Barton Springs complex, we hiked along the greenbelt trail to the upper springs area to explore the geologic formations in a karst region. We then went to the Old Mill Spring on the other side of the complex to discuss biodiversity. The final exploration of the day was a comparison between the surface water in the springs area, as compared to the groundwater in the Barton Springs Pool.

Barton Springs- Edwards Aquifer

The four springs in the Barton Springs Complex act as the discharge points for water from the Edwards Aquifer. These springs are part of an artesian system which means the water is under high pressure, causing its discharge to be seen at the surface in the form of a spring. There are three important features that make up this unique ecosystem, the karst nature of the site, the wide biodiversity, and the springs themselves.

1. Karst Regions

Fault Line in Campbell’s Hole Outcrop

While many karst regions do tend to be characterized by the presence of limestone, it is more correctly defined as a landscape formed by a dissolution of soluble rock material such as limestone or gypsum. At the end of our hike along the greenbelt, we crossed the creek and arrived at an area of exposed limestone from which we could examine the material that characterized this region and also to explore the rock layers in the nearby Campbell’s Hole Outcrop. One of the defining features of this outcrop— besides the easily differentiated layers—is the noticeable fault line. After our exploration of the rock layers and material, we hiked a little ways up the cliff front to the exposed fault line which is shown in the picture I took on the right.

Drought and wet conditions are especially impactful in karst regions because an increase in surface water can rapidly affect the groundwater quality because of the easily soluble nature of the rocks. Spring flow and groundwater levels can change rapidly in a short amount of time in these regions, and thus they are more susceptible to climate change.

2. The Springs

There are four springs in the Barton Springs complex: Old Mill Spring, Eliza Spring, and Upper and Main Barton Springs. These streams are connected by an intricate network of dams and other structures. It is difficult to describe the exact nature of this system from a single visit, but I think this description from edwardsaquifer.net does a great job.

Main Spring, also known as Parthenia Spring, feeds the 900′ long swimming pool. There is a dam at each end of the pool; the upper dam directs flow from Upper Spring and Barton Creek into a bypass culvert so that stormwater flows do not enter the swimming area.  Old Mill Spring, sometimes called Walsh or Zenobia Spring, is just south of Barton Creek about 450′ below the lower dam and is surrounded by a round limestone enclosure built by the Works Progress Administration.  Upper Spring occurs about 1,200′ above the swimming pool. The fourth spring, Eliza Spring, is adjacent to the swimming pool and also surrounded by a WPA structure, a deep concrete ampitheatre that used to be a swimming hole.

As a part of our field trip, we visited Old Mill Spring which is now closed to the public as can be seen by the bars in the photo on the right below. This space, along with Eliza Springs, are being preserved for their historical value but are also being reserved as habitat for the diverse range of species that take residence in the springs.

Old Mill Spring

Old Mill Spring

3. Biodiversity

Barton Springs Salamander (Photo By: Lisa O’Donnell, City of Austin)

The unique nature of the spring ecosystem makes it an ideal home for a wide range of species. Two species of concern are the Barton Springs Salamander and the Austin Blind Salamander, which are both federally listed endangered species. This spring complex is the only known home for these two salamanders, and dams and other uses of the springs have greatly reduced their numbers. As mentioned above, Old Mill Spring and Eliza Spring are being reserved as habitat for these and other species.


Overall, I would deem this a very successful field trip with interesting ties to the project I am working on this summer. My research looks at modeling non-residential indoor water demand in Austin. So it was very fascinating to explore Barton Springs, particularly in regard to the recreational water demand aspect to see how that use compares to the usage I am tracking in my research. Many of the patterns experienced by the springs during drought and wet conditions can be similarly modeled to match indoor water demand and usage over those same time periods, especially for irrigation. I highly recommend visiting Barton Springs, both to swim in the cold groundwaters of the pool and to have a chance to experience all that this unique ecosystem has to offer.

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