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Lamar County Multi- Jurisdictional Hazard Mitigation Plan <br />Chapter Three <br />3. Extent <br />The most extensive damage from expansive soils can occur to bridges, highways and streets. <br />Homes, buildings and other structures can have extensive damage resulting in sticking doors, <br />uneven floors and cracks in the foundation, floors, walls, and ceilings. The greatest damage <br />occurs when structures are constructed when clays are dry (such as during a drought) and then <br />subsequent soaking rains swell the clay. Damage can become so severe that the cost of repair <br />can exceed the value of the building. <br />Both public and private structures can develop extreme foundation problems during times of <br />shrink -swell events. The most common signs of damage are cracks in foundations, brick <br />exteriors, drywall interiors, sidewalks and other concrete structures within the building. <br />Sewer and water lines are also affected by shrink swell soils. The action of the movement of the <br />soils can snap water and sewer lines, producing a minimum of area discomfort, and a maximum <br />of a serious health and welfare risk. <br />4. Previous Occurrences <br />Since this hazard develops gradually and seldom presents a threat to life, problems may not be <br />recognized as being related to expansive soils or may be considered only nuisances and <br />therefore never repaired or reported. No records of specific incidences of structure loss due to <br />expansive soils in Lamar County were found. <br />5. Probability of Future Events <br />Since no records of specific incidences of loss associated with expansive soils were found and <br />no specific areas of expansive soils were identified within the county, Probability of Future <br />Events cannot be determined at this time. However, according to public opinion, the probability <br />of future events of loss due to expansive soils within the county is possible. <br />6. Vulnerability <br />The effects of expansive soils are most prevalent when periods of moderate to high precipitation <br />are followed by drought and then again by periods of rainfall. Other cases of damage result from <br />increases in moisture volume from such sources as broken or leaking water and sewer lines. <br />Dry clays are capable of absorbing water and will increase in volume in an amount proportional <br />to the amount of water absorbed. Areas capable of these changes in soil volume present a <br />hazard to buildings, slabs, concrete, asphalt and other structures built over them and to the <br />pipelines buried in them. Houses and one -story commercial buildings are more apt to be <br />damaged by the expansion of swelling clays than are multi -story buildings, which are usually <br />heavy enough to counter swelling pressures. However, if constructed on wet clay, multi -story <br />buildings may also be damaged by clay shrinkage when moisture levels are substantially <br />reduced. <br />141 <br />