We cover the Tulsa metro inside about 35 miles of downtown. Each city below has its own page because the soil, the housing stock, and the usual fix are different from one town to the next.
The city itself. Pre war Midtown pier and beam, 1950s east side slabs, South Tulsa subdivisions, and the clay under all of it.
Newer slab subdivisions on red clay. Settlement shows up in years two and three, usually on the south wall.
Heavy clay and drainage trouble off Garnett. Mostly concrete leveling and pier and beam work up here.
Older Riverside homes next to new builds. Two different soils inside a few miles.
Arkansas River splits it. Clay north of the river, sandy loam in the bottoms, clay and sandstone south toward Bixhoma.
Hillside cut and fill lots over sandstone and shale. Keystone releases push the water table around.
Oil boom housing stock on Creek County clay. Pier and beam originals with slab additions bolted on.
Fast growth since 2000 on old oilfield ground. Disturbed fill under a lot of the newer slabs.
Wagoner County prairie clay over hardpan. New builds off Highway 51 moving in their first five years.
Ridge lots on Catoosa silt loam over limestone, bottom lots in Verdigris River alluvium. Different fixes for each.
Limestone close to the surface downtown, shale clay in the flats. Pier and beam old town, slab since the 1960s.
Old coal town with mines near the surface. Sandstone ridges, shale clay flats, cut and fill in the new additions.
Hillside lots over interbedded shale and sandstone. Downhill sides settle first.
Inside Tulsa proper, the neighborhood matters as much as the city. See the Tulsa neighborhood pages for Maple Ridge, Brookside, Florence Park, Midtown, Cherry Street, Kendall Whittier, Lortondale, and South Tulsa.
Not on the list? Call REPLACE_PHONE. If it's within an hour of downtown we probably work it.