What is Verdigris soil and how does it affect Oklahoma foundations?
In short: Verdigris is a very deep, well-drained silty soil that forms on stream flood plains in northeastern Oklahoma, including the Tulsa area. It has a thick, dark silty topsoil and averages 15 to 33 percent clay, but its official description states that it is subject to flooding. For buildings on Verdigris, flood exposure and soft, water-laid layers are the main foundation considerations.
Where does Verdigris soil occur?
The USDA Natural Resources Conservation Service (NRCS) maintains an Official Series Description (OSD) for each named soil. The Verdigris OSD lists the series in Major Land Resource Areas 76, 112, 116 and 118 and LRU 84A, across southeastern Kansas, northeastern Oklahoma and southwestern Missouri, and calls it extensive 1. Its type location is on the flood plain west of the Verdigris River near Elk City, Kansas 1.
Verdigris forms on flood plains with 0 to 3 percent slopes, in silty alluvium (sediment laid down by streams) 1. That ties it to the Quaternary alluvium along streams in the Tulsa Metro and the Northeast. Most Verdigris land is cultivated for corn, sorghum, alfalfa and wheat 1.
What are its key properties?
| Property | Verdigris (from the OSD) 1 |
|---|---|
| Classification | Fine-silty, mixed, superactive, thermic Cumulic Hapludolls |
| Parent material | Silty alluvium |
| Depth | Very deep |
| Drainage | Well drained |
| Water movement (Ksat) | Moderately high to high |
| Topsoil (A) | Silt loam or silty clay loam, 28-86 cm (11-34 in) thick |
| Control-section clay | 15-33% |
| Below 40 in | May range to sandy loam, loam, clay loam or silty clay |
| Flooding | Subject to flooding |
| Slopes | 0-3% |
| Mean annual rainfall | About 41 in (35-47 in) |
"Cumulic" is a soil-taxonomy term for an unusually thick dark topsoil, which on flood plains typically builds up as floods add sediment. Below 40 inches, textures range from sandy loam to silty clay 1.
Wynona is a closely related flood-plain soil that is somewhat poorly drained, and Osage is an associated clayey bottomland soil with high shrink-swell 12.
What do the properties mean for foundations?
Flood exposure
The OSD states plainly that Verdigris soils are subject to flooding, though it does not give a frequency 1. Official flood hazard maps for a specific address are published through FEMA's Flood Map Service Center 5. The Oklahoma Geological Survey notes that Oklahoma floods tend to occur in spring and fall, and that flood-prone areas are mapped to show land with about a 1-in-100 chance of flooding in a given year 6. See creeks and flood history.
Soft, layered sediment
Verdigris formed in stream-laid silty alluvium, and its textures below 40 inches range from sandy loam to silty clay 1. Layered alluvium is the setting for soft soil consolidation, where wet, compressible layers settle under load. Where a lot was raised with placed soil, fill consolidation settlement is a separate factor.
Shrink-swell and water
NRCS rates shrink-swell by linear extensibility: under 3 percent is low and 3 to 6 percent moderate 4. Verdigris has a fine-silty control section with 15 to 33 percent clay, while neighboring Osage has a clayey (fine) control section and high shrink-swell 12. The rated value is in Web Soil Survey 3. The ASCE homeowner guide recommends at least 3 inches of fall over the first 5 feet and downspouts that discharge at least 3 feet from the foundation 7.
Related
Common questions
Does Verdigris soil flood?
The official description states that Verdigris soils are subject to flooding; they form on flood plains. Flood maps for a specific address are available from FEMA's Flood Map Service Center.
Is Verdigris soil expansive?
Verdigris is a silty soil whose control section averages 15 to 33 percent clay, so it is not a heavy clay. The rated shrink-swell for a map unit is listed as linear extensibility in Web Soil Survey.
Where is Verdigris soil found?
Verdigris is extensive in southeastern Kansas, northeastern Oklahoma and southwestern Missouri along streams. Its type location is on the Verdigris River flood plain near Elk City, Kansas.
How is Verdigris different from Wynona soil?
Both form in silty alluvium on flood plains. Verdigris is well drained, while Wynona is somewhat poorly drained with a seasonal perched water table.
Sources
- Official Series Description - VERDIGRIS Series USDA Natural Resources Conservation Service
- Official Series Description - WYNONA Series USDA Natural Resources Conservation Service
- Web Soil Survey - Home USDA Natural Resources Conservation Service
- Physical Properties of the Soils (Field Office Technical Guide, Section II) USDA Natural Resources Conservation Service
- FEMA Flood Map Service Center Federal Emergency Management Agency
- Geologic Hazards in Oklahoma (GSA South-Central Section abstract) Oklahoma Geological Survey / Geological Society of America
- Living With Shrink/Swell Soils: A Homeowners' Guide to Maintenance of Shallow Foundations American Society of Civil Engineers, Geo-Institute
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