Chico is the regional centre of the northern Sacramento Valley and it has a genuinely old core for a city this far north. Founded in the 1860s, the downtown and the neighbourhoods around it hold housing from the late nineteenth century through the 1920s, and those laterals are cast iron and the earliest vitrified clay, in some cases original. A pipe that went into the ground when this was a new town is well past any reasonable service life, and the usual finding is a bore substantially narrowed by a century of corrosion and deposit, presenting as a whole house that drains slowly and has done so for years.
The ground here is distinctive. The eastern side of the city sits against the Tuscan formation, volcanic mudflow deposits washed off the southern Cascades, which gives hard, cobbly, cemented material quite unlike the fine valley sediments further south. Excavation through that is slow work, and depth matters a great deal to the cost of a repair. Toward the valley floor and west the ground softens into alluvium along Big Chico Creek and the Sacramento River plain, with a higher water table and infiltration becoming the mechanism instead.
Chico's tree canopy is exceptional, with very large valley oaks, sycamores and other mature species through the older neighbourhoods and around Bidwell Park, one of the largest municipal parks in the country. Those root systems are substantial, and in a climate with a long completely dry summer a sewer lateral is a dependable moisture source. Where a joint has opened, roots find it.
Hot dry summers and wet winters give a real annual soil cycle, and the surrounding foothill country has a serious wildfire history with the consequences that follow for buried utilities on burned slopes.
Around Chico
We regularly work near:
- 📍Bidwell Park
- 📍Bidwell Mansion
- 📍Downtown Chico
- 📍California State University, Chico
Main Sewer Line Cleaning in Chico — Local Notes
- •Founded in the 1860s, so the downtown and surrounding neighbourhoods carry original cast iron and earliest clay
- •Eastern side sits on hard cobbly Tuscan formation volcanic mudflow deposits, making excavation slow and costly
- •Valley floor and western ground is softer alluvium with a higher water table, where infiltration takes over
- •Exceptional mature tree canopy including very large valley oaks provides substantial root systems
- •A long completely dry summer makes a lateral the most dependable moisture source in the ground
