Water damage restoration across Baxter County

Two federal dams sit above this county, and they changed what high water means here. Bull Shoals holds the White River; Norfork holds the North Fork. Open-river floods of the sort that hit in 1927 and 1945 are largely gone. What replaced them is lake rise, flash flooding on small creeks, and pipes that split in a hard freeze.

Water only, and that is worth saying first

Coverage in Baxter County on this line is water damage only. There is no fire or smoke crew attached to it here. If a kitchen fire or a chimney fire is what happened, we will say so on the phone rather than send out a contractor who does the wrong trade, and you will lose a minute instead of a day. Water is the whole of what this county is bought for, and that includes clean supply-line water, rain and lake water, and the dirty side of a drain.

The county seat is Mountain Home, and the two other towns with their own pages here are Cotter and Gassville. Between and around them sit the lake communities — Lakeview and Midway near Bull Shoals, Henderson and Gamaliel on Norfork Lake, Norfork town at the confluence, Clarkridge up toward the Missouri line, and Big Flat down on the Searcy County line. They are all water-side addresses, and the water comes at them from different directions.

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.

The dams rewrote the flood map

Before flood control, the upper White River basin flooded hard and often. The Encyclopedia of Arkansas records several severe floods in the 1910s and 1920s, then the 1927 flood that broke levees and put more than two million acres under water statewide and wrecked businesses at Cotter. The winter 1937 Ohio and Mississippi Valley flood inundated roughly a million acres in Arkansas. The river came up again in 1943. Then in 1945 the White produced the highest stage ever recorded at Calico Rock, downstream of the county, higher even than 1927.

Norfork Dam went operational in 1944 as the first Corps of Engineers flood-control and hydropower dam on the White River system, and Bull Shoals Dam was dedicated by President Truman on July 2, 1952. Together they control roughly 7,800 square miles of drainage above Baxter County, and the Corps credits Norfork alone with cutting the eighteen highest flood crests on the lower river by an average of 3.31 feet. The practical result for a homeowner is that the river below the dams no longer behaves like a river. It behaves like a release schedule. Uncontrolled high water in this county now arrives mainly as lake-level rise and as flash flooding on small creeks and bayous.

Lake level is the number that soaks buildings

Norfork Lake sits at about 22,000 acres with a 380-mile shoreline at its normal 552-foot pool. At its 580-foot flood pool it covers 30,700 acres with 510 miles of shoreline and holds 732,000 acre-feet of flood storage. Bull Shoals runs about 740 miles of shoreline at conservation pool and roughly 1,050 miles at flood-control pool. That difference is the point: several hundred miles of shoreline exist only when the lake is high, and buildings, drives and septic fields sit along a good deal of it.

In the wet spring of 2011 the region took more than twenty inches of rain, the Corps made emergency spills into the White River basin reservoirs, and Norfork reached its full 580-foot flood pool. County Road 806, less than a quarter mile north of the lake near Mountain Home, went under about eighteen feet of water. That road starts flooding once the pool passes roughly 562 feet, and the National Weather Service put permanent Turn Around Don't Drown signs there in October 2011 because drivers kept going around the barricades at night when depth is impossible to judge.

May 2020 made the same point more gently. Mountain Home logged 9.36 inches of rain by mid-month, its tenth-wettest May on record, including 3.95 inches in a single day. Bull Shoals climbed to 693 feet, two feet under its 695-foot flood pool and level with the 2017 high-water mark. The Corps project office in Mountain Home called that kind of high water somewhat normal for this system. Somewhat normal is a useful phrase to keep in mind when deciding where to store what you cannot replace.

The lake addresses, shore by shore

Northwest of Mountain Home the county runs out to Bull Shoals. Midway, 72651, is 5.5 miles out at the junction of Highways 5, 126 and 178, 1,036 residents in a place that filled up while the dam was under construction and now serves lake visitors and retirees. Highway 178 carries on to Lakeview, 72642, a second-class city of 775 people incorporated in 1973 on the lake's southern shore, built around tourism, the 693-acre Bull Shoals-White River State Park where the lake meets its White River tailwater, and a Ranger Boats plant. These two are the closest of the small places to Mountain Home, which counts for more here than it would elsewhere: there is no interstate in this county and one continuous north-south state highway, so travel is two-lane travel and the road, not the straight-line distance, sets the schedule. North Arkansas Electric serves Lakeview, and the split between that cooperative and Entergy Arkansas runs right through this county, so which one holds the pole outside a soaked building is a first-call question rather than a second one.

East and northeast the water is Norfork Lake and the addresses change character. Henderson, 72544, is 309 residents on the east bank along US-62 and US-412, about 9.5 miles east-northeast of Mountain Home and reached across a bridge the WPA built there during the Depression. Gamaliel, 72537, is smaller by an order of magnitude, about 33 people on a ridge with Bennetts Bayou on one side and the Norfork arm of the lake on the other, with the Gamaliel campground roughly three miles southeast on the lake's east arm. Bennetts Bayou and Bennetts River both empty into that same northeast arm, so a heavy rain up in Fulton County reaches Gamaliel as creek water and as lake water in the same week. Clarkridge, 72623, sits north of both at 869 feet near the end of Arkansas Highway 201, close to the Missouri line and about as far from the county seat as this county reaches in that direction. When Norfork rises from its 552-foot pool to the 580-foot flood pool it hit in 2011, the shoreline all three of these look down on grows from 380 miles to 510.

Norfork, 72658, is the most particular case in the county. Its 465 residents live at the confluence of the North Fork and the White, immediately below Norfork Dam and the federal trout hatchery that opened there in 1957, which means the river past the town is less weather-driven than release-driven, sending a 4.8-mile band of cold tailwater downstream on a schedule set at the dam. Two rivers and an operator's decisions meet at that address, and the historic Jacob Wolf House stands in the middle of it. Big Flat, 72617, is the other extreme: 88 residents on State Highway 14 near the Ozark National Forest at the far south end, mostly in Baxter County but straddling the Searcy County line, and on Entergy Arkansas rather than the cooperative that covers the lake towns. Nothing about Bull Shoals or Norfork explains a wet building down there. What gets one wet is rain, a roof and a plumbing line, which is the plainest version of this work and still the most common one.

Limestone changes what a wet floor does

Baxter County sits on the Salem Plateau, and the flatter Central Plateau around Mountain Home is karst country. That means shallow, irregular limestone bedrock with sinkholes and dissolved-rock voids close to the surface. Storm water disappears underground in one place and comes back out at a spring somewhere else with very little natural filtering along the way. Foundations over that ground are exposed to uneven settling and, occasionally, to a void opening under them.

For a crawl space, karst is the whole story. A crawl space dug into deep soil drains slowly and predictably. A crawl space sitting on rock does not drain at all in the places where the rock is solid, and drains straight out of sight in the places where it is not. Water pools in rock hollows, runs sideways along the ledge, and shows up under a room nowhere near the leak. Northern Baxter County is different again — the White River Hills carry steep, rocky, cherty soils and spring-fed streams, so runoff there arrives fast and leaves fast, and the problem is usually what came in the door rather than what sat under the floor.

Winter does more damage here than the rivers

The February 14 to 20, 2021 arctic outbreak dropped eight to ten inches of snow on Mountain Home on the fourteenth and fifteenth and bottomed the temperature out at 6 degrees on the fifteenth, with the wider region running more than thirty degrees below average through the twentieth as two snowstorms bracketed the deep freeze. Pipes do not usually break during the cold. They break on the thaw, and across Arkansas that thaw brought a wave of burst lines heavy enough to overwhelm utilities — Hot Springs counted roughly three thousand homes and businesses with broken pipes, and one water authority saw usage run at 150 to 200 percent of normal.

The January 26 to 28, 2009 ice storm was a different failure. One to two inches of ice, the worst icing in the region since December 2000, snapped at least 30,000 utility poles statewide and cut power to about 350,000 customers at the peak, with roughly 100,000 still dark on February 3. A trained spotter near Mountain Home logged heavy freezing rain and extensive tree and limb damage from about six in the morning on the twenty-seventh. A house without power in that kind of cold has no heat holding its pipes above freezing, which is how an outage becomes a water loss.

Empty houses and the size of a small leak

The county held an estimated 23,105 housing units as of July 2025, with a 75.2 percent owner-occupied rate and a median home value of $174,600. Those numbers describe a place with a large retiree population and a real share of second homes and seasonal lake places. A supply line that fails in an occupied house is heard within minutes. The same line failing in a lake house that nobody will open until spring runs for weeks, and the difference between those two calls is not the plumbing. It is the calendar.

That is the single most useful thing anyone can do here without a contractor: shut the main and drain the lines on any building that will sit empty through a cold stretch, and have someone look at it after a hard freeze. Half the losses on this side of the state would be small if somebody had turned a valve in November.

Smaller places covered here

These are on the coverage list and calls from them route, but they are too small to carry a page that says anything a page about the county does not already say.

Common questions

Photograph what you can, move what is loose, and call the county number.