Water work across the Delta, the White River Ozarks and the river valley

Water is bought in four of the five counties on this line: Crittenden, Baxter, Crawford and Franklin. Craighead County is not among them. Those four counties sit in three regions that share nothing, and the water arrives by a different route in each one, which is what decides how a house is dried.

Where water calls are taken

Craighead County does not appear in that table. Fire is what is purchased in Craighead, and a water call from Jonesboro, Bay, Bono, Brookland, Caraway, Lake City or Monette cannot be routed here no matter how the loss happened.

1. You callOne number per county. The dispatcher takes the address, the ZIP and a short description of what happened.
2. A local crew calls backAn independent restoration contractor already working that county rings you directly and sets a time.
3. They look, then scope itNothing is priced from a phone call. The crew walks the building, takes readings, and writes a scope you can hand to your adjuster.

Crittenden County: flat ground and heavy clay

The county lies entirely on Mississippi River bottomland with alluvial sediment more than a hundred feet thick, and the soil that matters most for drying is Sharkey clay, a dark heavy slack-water deposit that farmers call buckshot. It is productive and it is dense, and it does not let water go anywhere quickly. A slab poured on it sits over ground that stays wet after the sky has cleared.

The mainline levees have held since 1927. In May 2011, when the Mississippi crested at Memphis at 48.03 feet, the second-highest on record, the county's levees came through it; a few homes near the river flooded, fields and roads went under, and the countywide damage total came to about $500,000. Most Crittenden County water calls are not river calls at all. They are rain that had nowhere to drain, of the kind that dropped twelve inches on West Memphis on December 25, 1987, or sewer that backed up when the system could not shed it. West Memphis stands roughly eleven feet above river level, which is why the city won a federal grant in 2024 to restore riverfront wetlands as a buffer for I-40 and I-55.

Baxter County: karst under the floor

Open-river flooding is largely a historical problem here. Norfork Dam went into service in 1944 and Bull Shoals was dedicated in 1952, and the Norfork project alone is credited with cutting the eighteen highest crests on the lower river by an average of 3.31 feet. What replaced it is lake level and flash flood. Norfork Lake reached its 580-foot flood pool in 2011 and buried County Road 806 under about eighteen feet of water, and after repeated flooding there the Weather Service posted permanent high-water signs in October 2011. In May 2020, Mountain Home logged 9.36 inches of rain by mid-month and Bull Shoals rose to 693 feet, two feet below its flood pool.

Inside a building, the local complication is karst. The Central Plateau around Mountain Home is limestone with sinkholes, shallow irregular bedrock and dissolved voids near the surface, which lets surface and storm water disappear underground and reappear at a spring with little natural filtering. A crawl space over that ground can stay damp for reasons that have nothing to do with the pipe that failed, and drying it without understanding why it is wet is how the same call happens twice. Cotter has a different problem again: the town sits at 620 feet directly on the White River below limestone bluffs, with a housing stock that goes back to its 1905 railroad years.

Crawford and Franklin: the river and everything that drains into it

The Arkansas River forms Crawford County's entire southern border and cuts Franklin County in two. In late May and early June 2019 it crested at 40.79 feet at Van Buren, 18.79 feet over the 22-foot flood stage and above the 1945 record of 38.1 feet, with peak flow near 570,000 cubic feet per second; the Weather Service called it near catastrophic, and about twenty-five homes in the Crawford County area were damaged. At Ozark the same flood reached 374.99 feet on May 30, the second-highest crest on record, and inundated thousands of acres of farmland.

The creeks do their own damage and do it faster. Lee Creek runs through the west side of Van Buren into the Arkansas and crested at a record 417.5 feet in late December 2015, taking Rena Road and its campground; it came up again three times in 2019. Frog Bayou drains the Boston Mountains north of Van Buren, Little Frog Bayou runs through Alma into Lake Alma, and the Mulberry River comes seventy miles out of the Ozarks to meet the Arkansas just south of Mulberry, where floods in 1923 and 1927 wrecked the surrounding farmland. Ozark Lake sits behind the Ozark-Jeta Taylor Lock and Dam, but that dam was built for navigation, and being upstream of it is not flood protection.

What changes about the drying

Category matters before anything else. Clean water from a supply line is a different job from river water or sewer water, and the last two bring silt and contamination that turn parts of a drying job into a removal job. That is why a dispatcher asks where the water came from before anything about square footage.

The building matters next. A pre-1920 house in the Van Buren Main Street district holds moisture in plaster and old framing that modern wallboard does not; a slab house on Crittenden County buckshot has no crawl space to work in at all; a Baxter County house over karst may have a wet crawl space that predates the loss. The equipment is largely the same everywhere. What differs is where the moisture hides, how long it takes to come out, and what has to be opened up before drying can even start.

What people ask before calling

Call while the damage is still doing whatever it is doing. It gets easier, not harder, to fix early.