Water Damage

The Dual Threat: Why Merced Homes Face Water Damage From Above and Below

• 7 min read • By Indoor-Restore Services
Deeply cracked clay soil typical of the San Joaquin Valley floor beneath Merced, CA
The Merced series clay loam expands when wet and contracts in summer heat, placing constant stress on foundations and underground pipes.

Living in Merced comes with a water damage risk profile that is genuinely different from most California cities. Our location on the floor of the San Joaquin Valley means we are caught between two distinct forces: powerful atmospheric rivers that can push Bear Creek past its flood stage in a matter of hours, and the slow, relentless movement of the expansive clay soil on which most of our homes are built. Each threat is serious on its own. Together, they make water damage one of the most pressing concerns for Merced homeowners.

The Threat From Above: Atmospheric Rivers and Bear Creek

The term "atmospheric river" describes a narrow corridor of concentrated water vapor in the atmosphere, stretching thousands of miles from the Pacific Ocean toward the California coast. When these systems make landfall over the Central Valley, they can deliver a month's worth of rainfall in just a few days. Merced, with an average annual precipitation of only about 12 inches, is not built for that kind of intensity.

The consequences became undeniable in January 2023. A series of atmospheric rivers struck California in rapid succession, and Bear Creek—the waterway that winds through the heart of Merced—bore the brunt of the runoff. At the NOAA gauge on McKee Road, the creek crested at a record 26.18 feet, well above its flood stage of 23 feet. Water escaped its banks at East South Bear Creek Drive between Glen Avenue and Cameron Lane, and the surge reached the top of the levee system at the north end of Morse Drive and Thurman Court. Neighborhoods that had felt protected by existing flood infrastructure found themselves inundated.

The flooding was not limited to properties immediately adjacent to the creek. Fast-moving water pushed into streets, garages, and ground-floor living spaces across a wide area. Cars were lifted and displaced. Drywall, insulation, flooring, and personal property were destroyed. For many residents, it was the first time they had experienced direct flood damage—and the first time they realized that standard homeowners insurance does not cover losses from a natural waterway overflow. A separate National Flood Insurance Program (NFIP) policy is required for that protection.

What made 2023 particularly alarming was that it was not a once-in-a-generation event. Bear Creek's second-highest recorded crest occurred in 2006, and significant flooding was also recorded in 2011 and 2018. The historical record suggests that major flood events are a recurring feature of life in Merced, not a rare anomaly. For homeowners near the creek and in low-lying areas, the question is not whether flooding will happen again, but when.

The Threat From Below: Merced's Expansive Clay Soil

While flood damage from Bear Creek is dramatic and visible, the second threat is quieter and often goes unrecognized until it has caused serious harm. The ground beneath most of Merced is composed of what soil scientists classify as the Merced series: a clay loam dominated by montmorillonite, a mineral with an unusually high capacity to absorb and release water.

The United States Department of Agriculture's official soil series description characterizes this soil as having "slow permeability" and notes that under natural conditions, it was "subject to overflow and at times was under water for considerable periods." The same document describes the soil's structure as "very hard, very firm, plastic and very sticky" when moist—and notes that the soil becomes dramatically drier and more contracted in summer. This is the definition of an expansive, or shrink-swell, soil.

For a home built on this type of ground, the seasonal cycle creates a persistent mechanical stress. In winter, the soil absorbs rainfall and swells, pushing upward against foundations. In summer, it dries and contracts, pulling away from those same foundations. Over years and decades, this movement can produce:

  • Cracks in concrete slab foundations, which provide pathways for groundwater to enter living spaces
  • Differential settlement, where one part of a foundation sinks faster than another, causing uneven floors and cracked walls
  • Fractures in rigid underground supply lines and drain pipes, leading to slow leaks beneath the slab
  • Gaps around exterior penetrations like conduit and plumbing stacks, allowing moisture to wick into wall cavities

A slab leak is a particularly insidious form of water damage. The water escapes slowly, often for weeks or months, saturating the soil beneath the floor and wicking upward through the concrete. By the time a homeowner notices warped flooring, a musty odor, or an unexplained spike in their water bill, mold may already be established in the subfloor or wall base plates.

A Compounding Factor: Aging Homes and Aging Infrastructure

The dual threat of flooding and soil movement is made worse by the age of much of Merced's housing stock. A significant share of the homes in the city were built between the 1950s and the 1970s. These properties were constructed with galvanized steel water supply pipes, which have a typical service life of 40 to 70 years. Many of those pipes are now at or beyond that threshold.

Galvanized steel corrodes from the inside out. As the zinc coating erodes, rust builds up on the interior walls of the pipe, restricting flow and creating weak points. The combination of internal corrosion and the external mechanical stress imposed by Merced's expansive soil makes these pipes particularly prone to failure. A burst galvanized pipe inside a wall or beneath a slab can release hundreds of gallons before it is detected.

The city's broader infrastructure faces similar pressures. Merced manages over 260 miles of sewer pipes, portions of which date back decades. During heavy rainfall events, stormwater infiltrates these aging lines, overwhelming their capacity and forcing sewage backward into homes through floor drains and toilets. Sewage backflow is not just a water damage problem—it is a Category 3 contamination event that requires specialized remediation to address safely.

Practical Steps to Protect Your Merced Home

Understanding these risks is the foundation of a sound protection strategy. For homeowners near Bear Creek or in flood-prone areas, the most important step is verifying your insurance coverage. If you do not have an NFIP flood policy, contact your insurance agent. The City of Merced participates in the NFIP, meaning policies are available to local property owners. Keep in mind that there is typically a 30-day waiting period before a new flood policy takes effect, so do not wait until a storm is forecast to act.

For the soil-related risks, regular inspection is your best defense. Walk your foundation perimeter each spring and fall and note any new cracks, especially horizontal ones in block walls or step-pattern cracks in brick. Inside, watch for doors that suddenly stick, floors that feel springy or uneven, or baseboards that have separated from the wall. Any of these signs can indicate foundation movement or a hidden moisture problem beneath the slab.

If your home was built before 1975 and still has original plumbing, consider having a licensed plumber perform a pipe inspection. A camera inspection of the main sewer line is also worthwhile, particularly if you have mature trees whose roots can infiltrate older clay or cast-iron sewer pipes.

When water damage does occur—whether from a Bear Creek flood, a slab leak, or a storm-driven roof failure—the response time matters enormously. Mold can begin to colonize wet building materials within 24 to 48 hours. Structural drying must begin quickly to prevent secondary damage from compounding the original loss.

For more information on how water damage is assessed and restored, visit our water damage restoration service page, where we explain the full process from emergency extraction through structural drying and final repairs.

Merced's clay soil was formed in basin areas and depressions that were historically subject to overflow. The same conditions that made this valley so productive for agriculture also make it uniquely challenging for the homes built on top of it.

The dual threat facing Merced homeowners is real, but it is manageable with the right knowledge and the right team. Whether you are dealing with the aftermath of a Bear Creek flood or have just discovered a slow leak beneath your slab, Indoor-Restore Services is here to help. We are based in Merced and understand the specific challenges our soil, our creeks, and our aging housing stock create. Call us any time at (209) 451-2288 for immediate assistance or a free consultation. We serve all of Merced, CA and the surrounding communities.