Whittier was founded in 1887 and its Uptown district and surrounding older neighbourhoods carry housing from the 1890s through the 1920s, which makes this some of the oldest sewer stock in the Gateway area. Those laterals are cast iron and early vitrified clay, often original, and cast iron of that age has typically built a crust of corrosion and scale narrowing the bore until the whole house drains slowly.
There is a specific seismic history worth knowing here. The Whittier Narrows earthquake of 1987, a magnitude 5.9 event centred nearby, caused considerable damage in this city and particularly to the older masonry buildings of the Uptown district. Ground motion of that order displaces rigid buried pipe, and a joint knocked slightly out of alignment does not necessarily fail at once. It admits roots, catches solids, and deteriorates quietly for decades. On older Whittier laterals we look specifically for sideways offsets at joints and cracks running across the pipe, which are motion signatures rather than soil-movement ones.
The northern and eastern parts of the city climb into the Whittier Hills, and that terrain brings its own mechanism. Expansive clay on slope moves both vertically with the annual wet and dry cycle and steadily downhill with slope creep, which shears a rigid lateral across its section. Those hillside lots also have deeper laterals, so defect depth has a real effect on repair cost.
Between the historic core and the hills, the postwar tracts on the flatter ground carry mid-century clay and some Orangeburg following the standard pattern of opened joints and root entry.
Around Whittier
We regularly work near:
- 📍Uptown Whittier
- 📍Whittier College
- 📍Hellman Park
- 📍Pio Pico State Historic Park
Main Sewer Line Cleaning in Whittier — Local Notes
- •Founded in 1887, so Uptown and the older neighbourhoods carry 1890s to 1920s cast iron and early clay
- •The 1987 Whittier Narrows earthquake, magnitude 5.9 and centred nearby, damaged the city substantially
- •Ground motion leaves sideways joint offsets and transverse cracks that then deteriorate quietly for years
- •Whittier Hills neighbourhoods have expansive clay on slope, which shears laterals and sits deeper
- •Postwar tracts on the flats carry mid-century clay and some Orangeburg with standard joint and root failure
