Edwards Aquifer

Barton Springs

Water makes its long journey through the Edwards Aquifer and gushes forth at Barton Springs. The primary springs are located near the diving board on the east side of the pool.

Bubbling with a life of its own, the cold and crystal-clear waters of Barton Springs give us only a hint of the vast subterranean world no mortal may hope to see. These pristine waters flow to the Springs from the caverns of the Edwards Aquifer, an underground reservoir of billions of gallons of water.

The Edwards Aquifer – lifeblood of Barton Springs and the subject of decades-long debates – curves from Bell County in the north to Kinney County in the southwest, and is divided into three sections. The Southern Edwards includes much of south central Texas, and provides drinking water for San Antonio and other cities. The Northern Edwards extends from Austin, through Georgetown, to Salado and supplies drinking water to Round Rock and Georgetown. The Barton Springs section, which encompasses 155 square miles of Travis and Hays counties, delivers water to Barton Springs. In addition, this federally designated Sole Source Aquifer supplies drinking water to over 50,000 rural residents.

Surface boundaries of the Barton Springs section are well defined: Town Lake on the north, the Mount Bonnell Fault on the west, a line paralleling Highway 150 in Hays County on the south and a line roughly paralleling IH 35 on the east. Barton Springs is near the northeast corner of the Aquifer at 435 feet above sea level.

The Aquifer is the legacy of a shallow sea that covered much of Texas during the Cretaceous period, about 100 million years ago. Austin was part of a reef system then, littered with shelled sea creatures whose names often were longer than the animals themselves.

Over millions of years, thick beds of limestone formed from the decomposing shells of these creatures. The Aquifer takes its name from these limestone beds, called the Edwards Formation. The Georgetown Formation also forms part of the Aquifer. Water has dissolved millions of holes in the limestone, from large caves to tiny pockets that give the rock a honeycomb appearance.

Other layers capped the Edwards, until powerful earthquakes sheared the rock, exposing sections of the formation in the hills south and west of town. Through cracks in these exposed layers, water filtered to the bottom of the Edwards, cutting a latticework of caverns that form today’s Edwards Aquifer.

About 300,000 acre-feet of water are stored in this maze of underground chambers – enough to fill the world’s largest building 60 times with plenty to spare.

Of the total recharge water, about 85 percent flows out at Barton Springs and 15 percent is pumped from wells. Most of the well-water is so pure that many people drink it without any chemical treatment.

During the relatively dry winter months, Barton Springs supplies significant water flow into Lady Bird Lake.

Barton Springs groundwater movement in the Edwards AquiferBarton Creek, because it is the closest creek to Barton Springs, has the greatest impact on the Springs. Some of the water entering Barton Creek takes only a few hours to enter the Aquifer and emerge from the Springs. Barton Creek provides about 28 percent of the flow from Barton Springs each day. Onion Creek provides another 34 percent, although the recharge water from that creek takes much longer – perhaps several years – to reach the Springs.

Water quality at Barton Springs is directly affected by water quality in these creeks. It’s like the old computer programmer’s saying: garbage in, garbage out. Fecal coliform bacteria (found in the digestive tracts of humans and animals), pesticides, nitrogens (found in fertilizers), and other pollutants that wash into creeks in the recharge zone – particularly Barton Creek – quickly find their way into the Barton Springs Pool. This is particularly true after heavy rains, when layers of pollutants that might have accumulated for weeks pour into the Aquifer in large doses. This frequently results in closings of the Pool after a rainfall because bacteria levels are too high, or visibility is too low.

Increased urban development damages the quality of water in the Aquifer. Paved areas reduce the amount of soil and vegetation, which filter some pollutants from runoff water before it enters the Aquifer. Additional houses, apartment complexes and businesses generate more pollutants – from spilled motor oil, antifreeze and gasoline to pesticides, herbicides and fertilizers. Rains wash these compounds into the recharge zone, and hence into the Aquifer – and Barton Springs.

The Aquifer is recharged from the watersheds of six creeks. A watershed is a drainage basin; rain falling in a given watershed is carried by a network of tributaries t0 the parent creek.

As these creeks – Barton, Williamson, Slaughter, Bear, Little Bear and Onion – flow above the Aquifer, water percolates through cracks in the creekbeds to the Aquifer itself.

Once underground, the water follows the topography, flowing from the higher southwest corner of the Aquifer (about 850 feet above sea level), to the lowest level at Barton Springs.

Surface water → groundwater, “Now you see it → now you don’t.”

 

Flooded creek

Hill Country creeks change dramatically with weather. Heavy rains quickly flood the rocky creek beds. Stream flow is usually short-lived, since any water present is quickly recharged to the Aquifer. A period with little or no rainfall soon results in dry creeks.

Dry creek

Windmill

Whether you call it a windmill, papalote, or high lonesome, it has provided rural areas with water for domestic, agricultural and livestock needs since the 1800’s.

Erosion controls

Erosion and sedimentation controls at construction sites are important to Aquifer protection.

Soil erosion

Throughout the watershed, livestock waste, soil erosion, pesticides and fertilizers contaminate rainfall runoff. These examples of non-point source pollution in turn pollute local creeks and eventually the Aquifer and Barton Springs.

Creek flowing

The water we see flowing in area creeks may become the unseen water of the Aquifer. We can only expect the groundwater to be as clean as the water going into it.

Karst limestone

The highly porous and fractured karst features of the Edwards limestone provide easy pathways for rapid groundwater flow.

Many factors affect water quality

Click the picture for a larger image.

Edwards aquifer graphic