San Antonio, Texas

Blue Hole at Headwaters Sanctuary

Visit the traditional headwaters of the San Antonio River, then follow the story of a sacred spring, a growing city, and the aquifer beneath them both.

Address4503 Broadway
Setting53-acre sanctuary
HoursDawn to dusk, daily
Known ForSan Antonio River headwaters

How to Visit

Blue Hole is part of a wildlife sanctuary on the University of the Incarnate Word campus—not a swimming hole. Come for a quiet walk, living history, and a close look at the river’s traditional beginning.

  • ParkingUIW requires an online visitor parking permit Monday–Friday during fall and spring semesters. Weekend parking generally does not require one.
  • The WalkExplore on foot and stay on marked trails. The sanctuary welcomes walking, nature study, photography, and quiet observation.
  • Protect the SanctuaryNo bikes or motorized vehicles. Do not collect plants or wildlife, litter, swim, or enter protected restoration areas.
  • Check Before You GoReview current directions, parking instructions, trail maps, events, and closures on the official Headwaters website.

Set expectations: Blue Hole is an intermittent spring. In dry conditions the stone basin may hold little or no visible water, but the place remains historically, culturally, and hydrologically significant.

History of Blue Hole

People have gathered around these springs for millennia. Each event below includes a direct source so the chronology can be followed beyond this guide.

~12,000 years ago

Archaeological evidence places people around the San Antonio Springs for nearly 12,000 years. Indigenous communities depended on and regarded the springs as sacred.

Headwaters history ↗
Before colonization

Blue Hole was the largest outlet in a network of Edwards Aquifer springs. Traditional accounts describe a sacred gathering and pilgrimage place for the Payaya and other Indigenous peoples.

San Antonio Report ↗
1691

On June 13, Domingo Terán de los Ríos and Father Damián Massanet’s expedition camped near the headwaters with Payaya people. The Spanish named the place San Antonio de Padua.

Edwards Aquifer history ↗
1745–c. 1776

The Spanish built the Alamo Madre acequia in 1745, then the Upper Labor dam and acequia around 1776, diverting spring and river water for settlement and irrigation.

Edwards Aquifer history ↗
1857

Frederick Law Olmsted saw the spring before extensive aquifer pumping and wrote that “the whole river gushes up in one sparkling burst from the earth.”

Olmsted quotation and context ↗
1869–1880s

Isabella Brackenridge purchased the estate in 1869. Beginning in 1877, the San Antonio Water Supply Company used spring flow to operate a pumping plant and supply the city.

Edwards Aquifer history ↗
1891

Concerned that spring flow was unreliable, George W. Brackenridge drilled large artesian wells into the Edwards Aquifer for municipal water. Numerous additional wells followed.

Edwards Aquifer history ↗
Late 1890s

Artesian pumping and prolonged drought dramatically reduced Blue Hole’s flow. Brackenridge reportedly lamented that the river was “dying” and attributed it to the wells.

Headwaters history ↗
1897

Brackenridge sold approximately 280 acres, including the springs, to the Sisters of Charity of the Incarnate Word.

Handbook of Texas ↗
1940s–1970s

Increasing groundwater withdrawals made the spring intermittent. Blue Hole entered roughly three decades of dormancy before returning during exceptionally wet conditions in the 1970s.

Edwards Aquifer history ↗
1978–1989

Blue Hole became part of the National Register-listed Source of the River Historic District in 1978. The present octagonal limestone wall and walkway were installed in 1989.

Cultural Landscape Foundation ↗
1992

The Edwards Aquifer reached a recorded high of 703.3 feet at the J-17 index well. Blue Hole flowed, though at only a fraction of the nineteenth-century volume.

Edwards Aquifer history ↗
1999–2000

San Antonio began using highly treated recycled water to conserve aquifer water and support dependable river flow during dry periods. It supplements the river downstream; it does not refill Blue Hole.

SAWS recycled water program ↗
2015 & 2018

Wet periods raised the aquifer enough for Blue Hole to flow again temporarily. In September 2018, its water crossed the formerly dry channel and mixed with Olmos Creek water.

San Antonio Report ↗
Today

Blue Hole is an intermittent spring. Sources place its approximate flowing threshold around 670–676 feet above mean sea level at the J-17 index well.

Cultural Landscape Foundation ↗

What Happened to the Water?

Blue Hole is an artesian outlet of the Edwards Aquifer, not a conventional pond that was drained. Visible flow depends on underground water rising high enough to reach the spring opening.

01

Rain recharges limestone

Rain over the Edwards Aquifer recharge zone enters cracks, caves, and porous limestone.

02

Pressure raises the spring

When the aquifer rises high enough, groundwater pressure pushes water naturally through Blue Hole.

03

Wells share the source

Since the 1890s, regional wells have drawn from the same aquifer, reducing pressure and water level.

04

Drought lowers recharge

Dry periods reduce the water entering the aquifer while pumping continues across the region.

05

The outlet falls dry

Below Blue Hole’s outlet elevation, the water remains underground or is withdrawn through wells elsewhere.

06

Rain can wake it again

After sustained rainfall raises the aquifer, Blue Hole can flow into the river channel once more.

Downstream is different: Water visible in Brackenridge Park or downtown is not necessarily from Blue Hole. In dry conditions, SAWS uses highly treated recycled water to help maintain the river’s base flow. Blue Hole remains the river’s traditional and cultural headwater, while the Olmos Basin’s technical hydrology includes multiple springs and channels.

Sources

Visitor requirements and spring conditions can change. Check the official Headwaters site before making a special trip.

Hero image: an AI-generated visual interpretation made for this guide, not documentary evidence of current spring conditions.