Shoal Creek, Austin, Texas


Shoal Creek is a stream and an urban watershed in Austin, Texas, United States.
Shoal Creek has its headwaters near The Domain and runs in a southerly direction, soon reaching the intersection of Texas State Highway Loop 1, locally known as "MoPac Expressway" or simply "MoPac," and Highway 183. It continues south, partly along Shoal Creek Boulevard and Lamar Boulevard, through the western part of downtown Austin to its end at Lady Bird Lake.
Shoal Creek is the largest of Austin’s north urban watersheds, encompassing approximately 8,000 acres. About 27% of the watershed is over the Edwards Aquifer Recharge Zone. Its length is approximately 11 miles. It runs parallel to and between Waller Creek to its east and Johnson Creek to its west.
The creek is notable for its links to the history of Texas and Austin, its floods, and its scenery and parks just a few minutes from the Texas Capitol.

Course and tributaries

Shoal Creek has its origin on the west side of MoPac, with two springs, one called MCC/UT Spring and the other reportedly without a name. It runs eastward from there, crossing MoPac, and then enters a culvert that runs south. It then turns into a swampy area at MoPac and 183, and goes under 183 through a culvert, and Shoal Creek Boulevard begins to follow the course of the creek on its west side.
About a mile or more later, the creek crosses Anderson Lane and the Spicewood Springs/Foster Branch joins it from the west.
Perhaps a mile farther, the creek goes to the west of Beverly S. Sheffield Northwest Park, which is an important flood control facility, and it is joined from the west by the outflow from the Great Northern Dam, which is another one of the City of Austin’s Watershed Protection Department’s flood control projects. A minor tributary runs through the park from the east. At the downstream end of the park, Shoal Creek Boulevard crosses the creek and the street now follows the creek on the east side.
More than 2 miles later, north of 45th Street, the Hancock Branch, which has already been joined by the Grover Tributary, enters from the east. This is the largest tributary of Shoal Creek and drains about 2 square miles of residential areas, the Brentwood, Abercrombie and Crestview neighborhoods.
When the creek reaches 38th Street, Shoal Creek Boulevard ends, and the output of two springs enters the creek: the Beth Israel Temple Spring, just north of 38th, and Seiders Springs, just south. The year-round output of these springs creates a permanent pond north of 34th Street, which is the home of terrapins and fish.
The creek now heads southeast to Lamar Boulevard, which it follows on the west for the next two miles. Big Boulder Spring, just south of 29th Street, is the next permanent source of creek water. There is also a seep or spring on the other side of Lamar Boulevard that drains into the creek through a culvert.
Near 14th Street the creek goes under Lamar Boulevard and runs to the east of it for the rest of its course. At about 5th Street the creek makes a nearly right-angle bend to the east. The downtown part of the creek is channeled and many downtown streets run over it on bridges. Near 4th Street, the “lost” tributary, Little Shoal Creek, joins the main stream from the east. Little Shoal Creek was completely covered over by downtown development in 1917 and its outlet into Shoal Creek was always there to see, and it was not forgotten.,
The creek flows into Lady Bird Lake between Nueces Street and West Avenue, after running past the Central Branch of the Austin Public Library.
The difference in elevation from its source to its mouth is approximately 320 feet.

History

Arrowheads and other artifacts indicate that Native Americans occupied the Shoal Creek watershed 11,400 years ago. There are also stories of attacks by the native people on early settlers. One Gideon White, who lived at Seiders’ Springs before the Seiders family settled there, was killed near his home in 1842 by a band of Native Americans. A Mrs. Sarah Hibbins, who had been captured by natives when crossing the Colorado River in 1836, escaped them by night and followed the channel of Shoal Creek back to the Colorado, where she obtained help. Her two children, or perhaps only one of them, were rescued but her husband had already been killed. At that time, the village that would become Austin was called Dewitt’s Colony.
There is supposed to be a Native American burial mound “near the old McCall Spring just west of the street now called Balcones Trail.” Neither the spring nor the street exist now by those names.
In 1838, a few settlers lived along the creek’s mouth in the village of Waterloo when Mirabeau B. Lamar, later the second president of the Republic of Texas, arrived there. Lamar was looking for places that would be suitable for Texas’s new capital. He shot a buffalo and admiring the area’s scenic beauty, returned to Houston. The next year, when Lamar was president, a commission appointed by him recommended Waterloo as the capital of Texas. Lamar wanted the capital to be on the “frontier” and have room to expand. He considered Shoal Creek to be the frontier and the land west of it to be Comanche territory.
Shoal Creek was named by Edwin Waller and was the original western boundary of the city of Austin, then called Waterloo, when it was established in 1839. In the "Bird's-Eye View" map by Augustus Koch, Shoal Creek is the large canyon on the left side.
When founded, the city issued land patents to several people, and others bought tracts of land. The Hancock brothers, beginning around 1845, owned a huge tract spanning the creek, which stretched from what is now 45th street north about 2 miles to include the Allandale neighborhood. George Hancock apparently owned the southern and eastern part and John’s half was on the other side of the creek and to the north. This land was far outside the city limits at that time. John Hancock was a congressional representative. After he died, his family moved “into town” and sold the land, about 1896.
In 1846, Louisa Maria White, the daughter of Gideon White, who as mentioned above was killed by Native Americans, married Edward Seiders, who was in the livery and grocery business. They took up residence in the cabin by the springs where her father had lived. The springs thereafter started to be called Seiders Springs, and the nearby oak grove was known as Seiders Oaks.
In the 1850s, Governor Elisha M. Pease acquired a 365-acre tract west of downtown, including some of the Shoal Creek watershed, which he named Woodlawn Plantation. After the Civil War, General George Armstrong Custer, commanding the 2nd Wisconsin and the 7th Indiana Cavalry, was assigned to Austin in late 1865 and early 1866 as part of Reconstruction and intended to use Governor Pease’s house, named Woodlawn, as his headquarters. Pease was out of the state at the time. The citizens of the city did not allow it. Custer’s men camped on the banks of Shoal Creek in the area that would become Pease Park. Some of them died of cholera and were buried by the creek.
Pease Park, originally twenty-four acres and part of Woodlawn Plantation, was given to the city in 1875 by former Governor Pease.
Austin's first bridge was built on Pecan Street across Shoal Creek in 1865. It was a narrow iron footbridge, built by the United States Army, and could not carry wagon traffic. In 1887, a new, larger bridge across Shoal Creek was built to match the full 80-foot width of Sixth Street and permit wagons to cross; this West Sixth Street Bridge is still in use today, and has since been added to the National Register of Historic Places.
In the 1870s, Edward Seiders still owned the property around Seiders Springs but had moved back into Austin. Seiders Springs had become an important recreation destination and Seiders built bath houses, picnic tables, and a dance pavilion there. He provided transportation to and from Austin for those who wanted to visit the springs.
In the 1890s, there were rumors of buried treasure along the creek. Lights and digging in Pease Park at night was reported. Legend had it that Spanish gold was buried here.
“Split Rock” was said to be used as a hiding place by outlaws, and there were also rumors of treasure buried in the vicinity. Split Rock is between 29th and 31st Streets. It was supposedly a hangout for children skipping school, who would go swimming at “Cat Hole” nearby or “Blue Hole” farther down the creek. Split Rock was the subject of a painting, “Split Rock on Shoal Creek”, oil on academy board, by Hermann Lungkwitz.
The area to the west of the creek remained largely undeveloped into the 1920s. There were no bridges crossing the creek north of 12th Street for many years, probably due to the width of the canyon there and the steepness of its sides. The 24th Street bridge was built in 1928, in less than a month by private parties, and widened in 1938. It is a Texas Historic Landmark.
The city adopted a plan in 1927 that provided for ample parkland along Shoal Creek. This was prudent since the regular flooding makes it unwise to construct buildings along the creek. Nevertheless, a number of homes and businesses are within reach of the creek's floods. The entire watershed of Shoal Creek is now developed. This is labeled “urban stream syndrome” by the City of Austin on its website. “The impervious cover created with new buildings and roads prevents rainfall from soaking into the ground. Then we need to get all of this stormwater out of the way so our buildings and roads don’t flood. So we collect the water at inlets and concrete pipes and send it straight to the creek.”
The City of Austin, perhaps in the 1950s, moved a "honeymoon cottage" that had belonged to O. Henry from the east side of downtown to a location along Shoal Creek near Gaston Avenue. This meant that the cottage was just down the hill from the exclusive neighborhood of Pemberton Heights. Apparently the City had plans to move the O. Henry house to this location as well. The honeymoon cottage burned to the ground on Dec. 23, 1956. Arson was suspected as this was the third fire in the cottage since it had been moved.
In the 1950s, Janet Long Fish obtained the approval of the Austin City Council to construct a hiking trail from Pease Park to 39th Street, on her own time and using her own money. She walked the trail, leading a bulldozer, for four years.
As of 2018, downtown development near the creek is proceeding quickly. Ballet Austin, at 501 West 3rd Street, once a landmark, is now surrounded by office and residential towers. The Austin Music Hall, 208 Nueces Street, was torn down and a 28-story office building took its place. Office buildings and mixed-use towers are still being constructed. The “tallest residential tower west of the Mississippi” is here. The new central public library, near the mouth of the creek, is complete, and landscaping along the creek makes the waterway look more attractive.
Population in the watershed was 59,011 in 2000 and is projected to be 78,759 in 2030. Impervious cover was estimated to be 52% in 2017. Austin's current codes allow up to 64% of impervious cover in the watershed. Another source estimated impervious cover to be about 55% in 1996.

Geology

The Shoal Creek watershed has three main types of rocks: the Georgetown Formation, the Del Rio Claystone, and the Buda Limestone.
The bottommost of these, and hence the oldest, is the Georgetown Formation. It consists of alternating beds of thin, fine-grained limestone or limestone with marl. It is patchily or discontinuously distributed, with the patches separated by faulting. It varies from 13 meters in thickness to about 20 meters in different parts of Austin. The top of the Georgetown Limestone can be observed in Shoal Creek at Martin Luther King Jr. Boulevard. Georgetown Limestone represents a number of open-shelf, subtidal environments of the early Cretaceous with varying faunas.
The Del Rio Claystone is also more or less discontinuous in areas along Shoal Creek. The Del Rio is about 25 meters of dark olive to bluish-gray to yellow-brown pyritic clay containing gypsum. The clay contains illite, montmorillonite, and kaolinite. Fossils of Ilymatoqyra arietina, also known as Exogyra arietina, an extinct species of oyster from the Cretaceous, are common in this layer. Many very small species also are present, and the clay "lacks a normal bottom assemblage." This led Young et al. to conclude that it had been deposited in a lagoon with abnormal bottom conditions, which would account for the large amounts of pyrite. Upon weathering, the pyrite in the claystone reacts with water to produce sulfuric acid, which in turn reacts with calcite to produce the selenite found in Austin and elsewhere in Texas.
The lower boundary of the Del Rio is “gradational” with the Georgetown Limestone, and the transition occurs through one to two meters. The upper boundary in the Austin area is sharply defined from the basal beach limestone of the Buda Formation.
The Buda Limestone consists of 11.5 to 16 meters of nodular, soft and hard limestone. The bottom of this layer is a hard limestone composed of oyster shell fragments. Most of the other beds are mollusk limestones, softer in the lower part and harder in the upper part.
This limestone in the Austin area represents shallow subtidal and intertidal deposits. The bottom layer is a shoal or beach that spread across the Del Rio Formation and scoured it at the top. The rest of the formation is shallow subtidal storm deposits; the different beds seem to have been subjected to storms many times, and most of the fossils have been broken. However, there are fossils of burrowing animals present.
The Buda Limestone can be visited at a variety of outcrops along Shoal Creek, especially along the Hike and Bike Trail.
Springs are present all over Austin because porous rock covers thick clays/shales which are more impervious to water. When the limestone over clay layers are exposed from the side, the water that percolates down through the limestone runs out on top of the clay.
Big Boulder Spring shows how the local geology contributes to the formation of a spring. This spring is located on Shoal Creek just south of 29th Street. This is a gravity flow spring, with surface waters migrating down the overlying terrace deposits and Buda limestone, along vertical and horizontal fractures and faults and discharging at an opening where the fractured/faulted Buda Formation sits on top of the Del Rio Clay. Similar springs are present on the banks of Shoal Creek from the Pease Park area to near Koenig Lane.
Seiders Springs is another spring near the banks of the creek. This spring may actually be two springs, obtaining their water from different sources, that are close to each other. One of the two springs is an "ebb-and-flow" spring which varies from 2 to 7 gallons per minute to between 50 and 62 gallons per minute.
“The Balcones Fault is visible from the 34th street intersection, which was once a creek crossing for the early Native Americans and later one of Austin’s first public highways.” Many outcrops and fault lines are visible in the Shoal Creek area. The elevation on the west side of the creek is higher than on the east, as West Austin is the beginning of the uplift of the Edwards Plateau, of which the Balcones Fault is the eastern boundary. Although the escarpment of the Balcones Fault is more likely to be gradual than sudden, there are places where it, or part of it, is well-defined.
University of Texas students discovered a fossil ichthysaurus on upper Shoal Creek near Northwest District Park during an archaeological dig. The ichthysaurus is now on display at the UT Natural History Museum.

Water Chemistry

A study of samples taken up and down the watershed from September 1994 to April 1995 found that, as expected in a creek running mostly on a limestone bottom, calcium bicarbonate is present in the water. The investigators showed that there is a lower concentration of nitrate and other dissolved solids during “stormflow” events, compared to “base-flow” samples. Nitrate was from 0.19 to 0.75 mg/L in stormflow and 0.02 to 1.9 mg/L during base-flow. Total dissolved solids were from 16 to 187 milligrams per liter for stormflow samples, and from 213 to 499 milligrams per liter for base-flow samples.
By analyzing oxygen and nitrogen isotopes, they concluded that the nitrate in stormflow samples came from the atmosphere, and from soil nitrate and ammonium fertilizer. Nitrate from base-flow samples had a different ratio of isotopes, suggesting an origin of soil nitrate, ammonium fertilizer, sewage and animal waste. The researchers decided that sewer lines in the creek corroborated this finding. Old sewer lines might leak, they said, and the excess of chlorine relative to sodium indicated sewage: a mixture of human waste and chlorinated water.
They found fecal coliform bacteria, ranging from 1 to 84,000 colonies/100mL during stormflow, and less than 1 to 1,600 colonies/100mL during baseflow. The investigators compared this with fecal streptococci and interpreted this to mean that the fecal bacteria came mostly from animal wastes, washed into the creek by rain.

Ecology

The Shoal Creek watershed contains steep limestone slopes, thin soils, sparse vegetation and impervious cover. About 30% of the watershed has tree canopy cover.
Shoal Creek has ecological issues in common with most urban creeks: reduced vegetation, elevated streambank erosion, and impaired water quality. Nevertheless, the wildlife in and along the creek is varied because Austin itself is located at the intersection of four major ecological regions, and is very diverse ecologically and biologically. The City of Austin now has a program of creating “grow zones” in the watershed to re-establish plant life, which also benefits animal life. This creates a healthier “riparian buffer,” with benefits to the public as well.
Shoal Creek is often referred to as an intermittent stream. However, there are places where it flows all year long, and pools that are present all year. When the creek appears to be dry, in reality there is water trickling through the limestone gravel that has piled up. Where the creek appears to have a bed of limestone rock and there is no water trickling on the surface, a porous layer of rock underneath may have water trickling through. Numerous springs and seeps along the course of the creek contribute to a constant flow, which may be small but is always present except perhaps in years of severe drought.

Species lists

Plants

The organization iNaturalist, a joint initiative by the California Academy of Sciences and the National Geographic Society, posts online lists of species observed or collected in or near Shoal Creek. The lists have been combined here, and not all of the species are named.
Plants: Trees include Ulmus crassifolia, Quercus fusiformis, Ungnadia speciosa, Melia azedarach, Acer negundo, Ipomopsis rubra, Prosopis glandulosa, Sophora secundiflora, Platanus occidentalis, Sapindus saponaria, Juniperus ashei, Taxodium distichum, Cercis canadensis, Eriobotrya japonica, Magnolia grandiflora, Triadica sebifera, Punica granatum, Quercus stellata, Quercus muehlenbergii, Albizia julibrissin, Morus rubra, Ulmus americana, Ailanthus altissima, Morus alba, Quercus phellos, Cordia boissieri, Prunus mexicana, Quercus falcata, Diospyros texana, and Quercus shumardii.
Shrubs, bushes and small trees include Vachellia farnesiana, Berberis trifoliolata, Lantana montevidensis, Parkinsonia aculeata, Lantana camara, Nandina domestica, Ilex vomitoria, Maclura pomifera, Sabal minor, Ligustrum quihoui, and Ptelea trifoliata.
Vines include Lonicera japonica, Campsis radicans, Passiflora lutea, and Parthenocissus quinquefolia.
Water plants include Arundo donax and Cyperus involucratus.
Cacti include Opuntia engelmannii and Cylindropuntia leptocaulis.
The list assembled by iNaturalist includes many wildflowers, notably Rudbeckia hirta, Gaillardia pulchella, Monarda citriodora, Coreopsis tinctoria, Solanum elaeagnifolium, Lupinus texensis, Lindheimera texana, Callirhoe involucrata, Oenothera speciosa, Verbena halei, and Malvaviscus arboreus.
The list of plants also includes the epiphytes Tillandsia recurvata and Tillandsia usneoides.
The lists do not include any aquatic plants or algae, but the City of Austin has a list, with photos, of wetland plants in the Austin area.
At the creek’s junction with Lady Bird Lake, there are numerous non-native elephant ears.
The vegetation in the creek area is typical of Austin. Large live oaks provide year-round shade on the hike-and-bike trail. One group of oaks in Pease Park is festooned with Spanish moss. Other native trees include sycamore, pecan, hackberry and juniper. Bamboo, a non-native pest, has a large stand south of 29th Street on the hike-and-bike trail. There is a program in the works to eradicate the bamboo with herbicide.

Animals

Invertebrates
Crustaceans:
Aquatic animals include Procambarus clarkii and the amphipod Talitroides topitotumv.
Armadillidium vulgare, the Common Pillbug is listed.
Insects
Butterflies and moths:
Papilio polyxenes, Hylephila phyleus, Agraulis vanillae, Libytheana carinenta, Strymon melinus, Zerene cesonia, Hyphantria cunea, and Petrophila jaliscalis, the "Jalisco Petrophila." The larvae of the last species are aquatic, living within a silken web in the water. They are associated with intermittent streams. .
Walkingsticks:
Anisomorpha ferruginea
Hymenoptera:
Polistes exclamans, Sceliphron caementarium, Apis mellifera, Xylocopa virginica, Pseudomyrmex gracilis, Solenopsis invicta.
Beetles:
Diabrotica undecimpunctata, Harmonia axyridis, Hippodamia convergens, Euphoria sepulcralis.
Grasshoppers:
Chortophaga viridifasciata.
Leafhoppers:
Homalodisca vitripennis, Oncometopia orbona.
Shoal Creek has an abundance of dragonflies and damselflies. iNaturalist lists these:
Libellula croceipennis, Pachydiplax longipennis, Argia immunda, Argia plana, Argia sedula, and Argia translata.
Other insects include Labidura riparia, Stagmomantis carolina, Panorpa nuptialis, and Parcoblatta americana.
Arachnids:
The only arachnid listed by iNaturalist is Anasaitis canosa, the Twinflagged Jumping Spider.
Vertebrates
Fish: iNaturalist lists Herichthys cyanoguttatus.
The creek also has sunfish, and Micropterus salmoides near its mouth. These fishermen also found Mexican tetra and the Texas cichlid.
Another fisherman specifically mentions “Redbreast”, and Bluegill. He also mentions “bass” and describes the spawning beds of the Rio Grande Cichlid, with a picture of one that he caught. This fish is also called the “Rio Grande Perch.”
A fish common from the lower to the upper reaches of Shoal Creek is the Texas mosquitofish, Gambusia affinis. The City of Austin introduces it for mosquito control and it also occurs naturally.
Amphibians: Listed by iNaturalist: Incilius nebulifer and Eleutherodactylus cystignathoides, Acris blanchardi and Eleutherodactylus marnockii.
“The Jollyville Plateau Salamander is found in the Spicewood Springs tributary of Shoal Creek. It is listed as a threatened species under the Endangered Species Act." The health of this species is strongly affected by the flow of the springs in which they live. There was a drought in 2011, but salamander populations increased in 2014 when rainfall resumed
A species of amphibian that is likely to be present is the Bullfrog.
Reptiles:
Listed by iNaturalist: Anolis carolinensis, Hemidactylus turcicus, Sceloporus olivaceus, Rena dulcis, Haldea striatula, Nerodia erythrogaster, Thamnophis marcianus, Tropidoclonion lineatum, Trachemys scripta, Thamnophis proximus, Apalone spinifera, Nerodia rhombifer, Tantilla gracilis, Storeria dekayi, Scincella lateralis, Pseudemys texana, Pantherophis obsoletus, and Chelydra serpentina.
Birds: Listed by iNaturalist: Butorides virescens, Quiscalus mexicanus, Mimus polyglottos, Egretta thula, Ardea alba, Cardinalis cardinalis, Columba livia, Zenaida asiatica, Cyanocitta cristata, Sturnus vulgaris, Passer domesticus, Cardinalis cardinalis, Thryothorus ludovicianus, Nyctanassa violacea, Lanius ludovicianus, Melanerpes carolinus, Aix sponsa, Corvus brachyrhynchos, Myiopsitta monachus, Bombycilla cedrorum, and many others.
The Shoal Creek Nature Conservancy conducted a bird walk in 2014 and saw or heard the following species: Wood Duck, Green Heron, Red-shouldered Hawk, Red-tailed Hawk, Spotted Sandpiper, Rock Pigeon, White-winged Dove, Mourning Dove, Chimney Swift, Red-bellied Woodpecker, Great Crested Flycatcher, Blue Jay, Barn Swallow, Carolina Chickadee, Tufted Titmouse, Carolina Wren, Blue-gray Gnatcatcher, Northern Mockingbird, European Starling, Cedar Waxwing, Orange-crowned Warbler, Nashville Warbler, Clay-colored Sparrow, Lincoln’s Sparrow, Summer Tanager, Northern Cardinal, Great-tailed Grackle, Lesser Goldfinch, House Sparrow.
Mammals:
Listed by iNaturalist: Sciurus niger, Odocoileus virginianus, Canis latrans, Didelphis virginiana, Procyon lotor, Mephitis mephitis, Otospermophilus variegatus, Oryctolagus cuniculus, and Rattus norvegicus.

Flooding

The City of Austin is located in "Flash Flood Alley," an area of Texas that may be subject to intense rain caused by moisture from the Gulf of Mexico, cold fronts from the north and masses of air from the west.
Since Shoal Creek runs through the downtown area of a major city, it has the potential to cause enormous damage by flooding. This is exacerbated by the flatness of downtown Austin, which is the flood plain of the Colorado River after it descends from the Edwards Plateau. As a result of erosion by the Colorado River, Shoal Creek’s large canyon does not exist south of 12th Street. The Colorado River has eroded and flattened this terrain. There is still an elevation to the west of the creek, but there is little to the east, where the center of downtown lies. Downtown, the creek runs in a channel 30 to 50 feet wide and 15 to 20 feet deep, which takes a sudden bend to the east at 4th Street. The canyon walls upstream constrain a flood but this small channel is not adequate to keep the creek from overflowing into the streets.
There are 339 flood detention basins in the watershed, and 100 water quality treatment basins. They manage only about 21% of the impervious cover, however. In the 100-year floodplain, there are 274 "inundated" structures. In the 25-year floodplain, there are 127; in the 10-year floodplain, 67; and 6 in the 2-year floodplain. In all, there are 655 structures within the 100-year floodplain. Most of the watershed, 71%, was developed before the 1991 Urban Watersheds Ordinance regulations. There are 54 roadways within the 100-year floodplain with 46 inundated by the 100-year, 41 inundated by the 25-year, 35 inundated by the 10-year, and 11 by the 2-year floods.
Shoal Creek has had numerous floods throughout Austin’s history. A major one occurred in 1869. A flood in 1915 killed 23 people along Shoal Creek, and another 12 along Waller Creek.
On Memorial Day, May 24, 1981, the rain that had begun the day before started falling much more heavily after dark. Parts of the Shoal Creek watershed received 11 inches of rain in 3 hours. The water flow in the creek, normally about 90 gallons per minute, increased to 6.55 million gallons per minute. Thirteen people lost their lives, many had to be rescued, hundreds of houses were destroyed, and Shoal Creek washed dozens of cars into its channel, many from car dealerships next to it on 5th and 6th Streets. This was called a “100-year flood.”
As a result of this flooding, voters approved a drainage fee and millions of dollars in bonds in 1981, 1982, and 1984 to fund flood control and drainage improvement projects. Since the 1981 Memorial Day Flood, the City of Austin has spent over $65 million to construct detention ponds, make channel modifications, and construct other flood mitigation solutions in the Shoal Creek watershed. Millions more have been spent to purchase properties.
The flood control measures did not significantly change the creek downtown. Following heavy rains, a second large Memorial Day Flood struck in 2015. The damage was “depressingly similar” to the flood in 1981.
Any larger-than-ordinary rain is too much for the capacity of the creek’s channel downtown. Two low-water crossings on 9th and 10th streets between Lamar Blvd. and West Ave. have been closed nine times between 2010 and 2016.
Six hundred and fifty-seven structures are within Shoal Creek’s 100-year floodplain. This is 15% of all structures in floodplains city-wide.
Ninety-six structures near the Hancock Branch and Grover Tributary are at risk during a 100-year flood. The Brentwood neighborhood was developed during the 1940s and 1950s. The drainage infrastructure that was constructed is inadequate. Undersized channels, culverts, and storm drains result in street and structure flooding on a frequent basis.
"As the Hancock Tributary is directly downstream of the Brentwood neighborhood, any solution to the localized flooding in Brentwood must be carefully designed so as not to worsen flooding in this area." Actually, as one can see on a map, the Hancock tributary originates in the Crestview neighborhood north of Brentwood, and flows through the Brentwood neighborhood. The Hancock Branch runs down the median of a street named Arroyo Seco. Heavy rains will flood the entire street. The Grover Tributary joins the Hancock Branch from the east near Koenig Lane and Arroyo Seco.
Development of the neighborhood also altered the erosion patterns of Hancock Branch and Grover Tributary. Particularly, the Grover Tributary runs through underground drains through much of its length, or constructed channels as shown in the picture. The danger area along Joe Sayers Street is southwest of the place the tributaries meet. In fiscal year 2017, the city began a preliminary engineering study for a project to correct multiple defects in the drainage infrastructure in this area.
Although this is serious, the City of Austin says that Lower Shoal Creek between 15th Street and Lady Bird Lake is the worst flooding problem in the city.
Besides the loss of lives and property, flooding erodes the banks of the creek. On Friday, May 4, 2018, heavy rains caused part of the canyon to collapse near the 2500 block of North Lamar along the west bluff of Shoal Creek. The landslide damaged part of the Shoal Creek Trail and some homes on the bluff lost part of their backyards, which fell down the slope. This occurred just 2 weeks after an official celebration, on April 20, of the completion of the City’s Shoal Creek Restoration Project.
There were no injuries. The landslide damaged city parkland at Pease Park and about 300 feet of the hike-and-bike trail. It also “buckled” a city wastewater line beneath the trail. Crews put in pumps to redirect wastewater flow to a working part of the sewer system until there is a permanent solution. Mike Kelly, Austin Watershed managing engineer, said that the bluff above Shoal Creek is made of Buda limestone over an unstable Del Rio clay formation. When the clay moves beneath the limestone, it causes fractures that can eventually lead to slope failures. On that day, Shoal Creek crested at about 12.37 feet around noon, according to the Lower Colorado River Authority.
On April 16, 2019, after spending $1 million on a year-long study of the landslide, the City of Austin estimated that repairing the damage and stabilizing the slope would cost $8 to $16 million. The top of the slope had moved again just a few weeks before the announcement.
Soon after the City released the repair estimate, floods in early May 2019, damaged more of the trail, causing it to slide into the creek. The landslide area was considered so dangerous that it was not possible to do any work to repair it. In addition, a man who was bathing in the creek at 9th Street was swept away by the flood and drowned. His body was found in Lady Bird Lake.
Following the flooding in May 2019, a new repair estimate was $12.5 million for design and construction costs and $7.5 million in contingency funding.
In January 2020, the City of Austin announced that it was unable to reach agreement with the landowners whose backyards partially fell into the creek bed. As a result, the City was unable to acquire easements to stabilize the cliff and maintain it. The city has four goals now: to clear the debris from the creek and allow the water to flow more freely, to widen the creek in places, to replace the wastewater line that was damaged by the landslide, and to construct a new segment of the hike-and-bike trail, about 500 feet long, to replace the part that was destroyed.

Flood control

As mentioned earlier, the 1981 Memorial Day flood was the impetus for Austin voters to approve bonds and spend millions to control flooding. In addition to rebuilding bridges, increasing the size of culverts and ditches and turning flooded properties into open space, the city built some large projects.
Great Northern Dam, between MoPac and Shoal Creek Boulevard, impounds a retention pond for all of the watershed to the west of Shoal Creek up to the Spicewood tributary. This includes rain that falls on MoPac itself and is collected in the ditches to the side of the highway. The land rises steeply west of the impoundment—this is the edge of the Balcones Fault. The dam and its impoundment are on a minor tributary of Shoal Creek that is usually dry. The dam was first constructed at an unknown date. It was considered "high-hazard" and was modernized after studies between 2003 and 2008.
Beverly S. Sheffield Northwest District Park was renovated by the City’s Watershed Protection Department after the 1981 flood. Its tennis courts, parking lot, a grassy field, and a baseball field, totaling approximately 10 acres, are for flood control. When the creek rises to approximately 10 feet, the water runs over a wall into the park and then drains back at a slower rate.
The park is the site of an old quarry, from which came the limestone blocks for the first Texas Capitol building, constructed in 1853. Since it was already an excavation, it was not hard to adapt it to retain floodwaters by building the wall in the picture and levees.
In 2014, the Watershed Protection Department, based on a study proposal made by the Army Corps of Engineers in 1991, suggested a 26-foot diameter tunnel that would run 6,000 feet from 19th Street to the lake at an estimated cost of $133 million. Its proposed inlet was to be within Pease Park. The City of Austin has used this means of flood control before. A tunnel routes flood waters in Barton Creek around the Barton Springs Pool. As of 2018, the City is completing a similar tunnel to prevent flooding on Waller Creek, and it has problems.
The Pease Park Conservancy opposed the tunnel. In a 2016 press release, it urged the City Council to “only consider solutions that do no alienate any dedicated parkland” and to not waste taxpayer dollars on “studying a flood control system that will be dead on arrival and never built.”
The Conservancy noted that the land was stipulated to be a park, so therefore “taking portions of the park for other divergent uses could violate the terms of that deed and be certain to subject the City to costly litigation.”
Another way to control floods would be to retain the floodwaters upstream. The flood control measures at Northwest District Park and at Great Northern Dam did not prevent flooding in 2015. Greater retention capacity would be hard to create. The properties in the neighborhoods around Shoal Creek are deemed very desirable and would be costly to obtain.
Another possibility is to make areas that are floodable, i. e. designing and contouring areas such as parking lots, recreational sports fields, parks, etc. to accept periodic inundation. Downtown, it seems that this is recognized as a solution, as office buildings are built to the edge of the channel of the creek. Presumably these buildings, which have open-air cafes and mixed-use spaces on the banks of the creek, expect to be flooded from time to time. House Park, a football field near the creek at 15th Street, floods regularly.
The State of Texas owned a 75-acre tract along the creek south of 45th Street. This was sold to developers in 2014, and Austin approved a development plan in 2018. The major issue brought up by the City in setting requirements for development was the creation of “affordable housing,” not flood control. This was despite some warnings that more development and impervious cover in the watershed would make flooding worse. As a result, the final plan has little or no flood control facilities: neither retention nor lowered floodable areas. However, buildings are set well away from the creek, which runs through the park that is part of the development.
The development plan approved by the City did propose “No modification to the existing 100-year floodplain” and “Direct storm water runoff from impervious surfaces to a landscaped area at least equal to the total required landscape area." It is not clear what effect these requirements will have.
Two other possible solutions to flooding are cisterns to take overflow water during flooding and the possibility of storing water underground in aquifers, perhaps by creating enormously deep dry wells. This would raise the issue of pollution of the aquifer, but might solve flooding and recharge the aquifer at the same time.
The City of Austin is establishing “flood cameras” to have some idea of when roads should be closed to protect people. Most of these cameras will be on rural low-water crossings, but four points along Shoal Creek are identified on the map: The ramp from Northbound 183 to MoPac, MoPac at Steck, Shoal Creek at Lamar and West 9th Street at North Lamar.
The webpage for the continuing study of these options (officially called the Shoal Creek Flood Mitigation Study, is maintained by the City of Austin, Watershed Protection Department.

Pollution

Shoal Creek’s water quality is rated as fair on the City’s Environmental Integrity Index.
As noted above, the City of Austin, back when little attention was paid to environmental issues, laid sanitary sewer lines in the creek. The flooding on May 4, 2018, caused “buckling” in the sewer line near the 2500 block of North Lamar. It is not clear how much sewage escaped.
While chronic pollution in the creek is perhaps not a tractable problem due to its location in an urban area, the City's Watershed Protection Department attends to reports of spilled substances quickly.
Construction near the creek is a potential source of pollution, and the city investigates after someone reports changes in the water. In one instance, the water was reported to be “murky.”
In another case of murky water, the City filed a Class C misdemeanor complaint against a contractor. This time, the project manager and the contractor were apparently aware of problems and did not correct them. The court record says that 'crews tried a "number of ways to contain and clean it" but efforts have "continually failed."'
The City’s Watershed Protection Department’s Shoal Creek Restoration Project is not only establishing “grow zones,” reducing erosion and planting vegetation, but also fighting pollution that enters the creek in storm runoff. The Department is installing rain gardens, biofiltration ponds and meadows, and vegetated swales to improve water quality.
In 2016, the project was expected to be complete by summer of that year.
Besides sewers, construction and miscellaneous spills, there is the problem of trash.

Recreation

Shoal Creek’s Hike-and-Bike Trail is the oldest trail in Austin. It was started by Janet Fish in the late 1950s, who hired a bulldozer and operator and made a trail through Pease Park. More of it was built by volunteers in the 1960s and improved by the City in the 1970s. Parts were rendered impassable by the flooding on May 4, 2018. At one time it was possible to walk from 38th Street to Lady Bird Lake on the trail, with the exception of one block on 31st Street where steep canyon sides and private property force a hiker to use the street.
Pease Park is the site of the annual Eeyore’s Birthday Party which is traditionally held on a Saturday near the beginning of May. When the date is announced, a rain date is also announced.
The trail is used daily by walkers and bicyclists, some of whom use it to commute to jobs downtown. The plan of the Shoal Creek Conservancy is to extend the trail to the Domain, where the creek has its headwaters. There, eventually, it would connect to the Walnut Creek Trail and form a 30-mile trail loop with much of the City of Austin inside.
The construction of Austin's new Central Library and the redevelopment of downtown Austin presented an opportunity to make Lower Shoal Creek into a "signature urban green space." The Task Force's report noted that near Lady Bird Lake, the creek is usually confined to its channel, and also that there is room for significant improvement in the stream's appearance. They proposed removing obsolete infrastructure, standardizing the appearance of the banks using large limestone boulders for a natural look, and planting vegetation. The Central Library was completed and opened in 2017.

Notable people associated with the creek