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Driggs soil series

The Driggs series consists of very deep, well drained soils that formed in mixed alluvium with loess influence. Driggs soils are on fan remnants and have slopes of 0 to 30 percent. The mean annual precipitation is about 406 mm and the mean annual air temperature is about 5 degrees C.

 

TAXONOMIC CLASS: Fine-loamy over sandy or sandy-skeletal, mixed, superactive, frigid Calcic Argixerolls

 

Mollic epipedon thickness: 25 to 44 cm.

Control section total clay range: 20 to 30 percent in the upper part and 1 to 8 percent in the lower part

Rock fragments: 2 to 20 percent in the upper part and,35 to 95 percent in the lower part

Depth to argillic horizon: 12 to 29 cm

Depth to calcic horizon: 44 to 86 cm

Calcium carbonate equivalent: 15 to 40 percent in the calcic horizon

Depth to sandy-skeletal material (2Bk horizon): 50 to 89 cm

 

USE AND VEGETATION:

Major uses: irrigated areas are used primarily for small grains, potatoes, hay and pasture; nonirrigated areas are used for pasture and limited production of small grains and hay. Dominant native vegetation: mountain big sagebrush, bluebunch wheatgrass, arrowleaf balsamroot, snowberry, antelope bitterbrush

 

DISTRIBUTION AND EXTENT:

Distribution: Southeastern Idaho, MLRA 13

Extent: the series is not extensive

 

This revision in 2007 changes the type location and classification of this series. It was formerly classified as fine-loamy over sandy or sandy-skeletal, mixed superactive Xeric Argicryolls.

 

For additional information about Idaho soils, please visit:

storymaps.arcgis.com/stories/97d01af9d4554b9097cb0a477e04...

 

For a detailed description, visit:

soilseries.sc.egov.usda.gov/OSD_Docs/D/DRIGGS.html

 

For acreage and geographic distribution, visit:

casoilresource.lawr.ucdavis.edu/see/#driggs

 

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Uploaded on February 5, 2011
Taken in January 2000