LOCATION COVING             TX
Established Series
Rev. CMT:CAB
04/2003

COVING SERIES


The Coving series consists of deep, somewhat poorly drained, moderately slowly permeable soils that formed in deep loamy and
sandy sediments. These soils are on wide, shallow, somewhat
concave drainageways. Flooding, of brief duration, is rare to common. Slopes range from 0 to 3 percent.

TAXONOMIC CLASS: Loamy, siliceous, superactive, thermic Aquic Arenic Paleustalfs

TYPICAL PEDON: Coving loamy fine sand--idle cropland.
(Colors are for dry soil unless otherwise stated.)

Ap--0 to 7 inches, brown (7.5YR 5/4) loamy fine sand, dark
brown (7.5YR 4/4) moist; weak coarse blocky structure parting to
fine granular structure; soft, very friable; many fibrous roots; common very dark brown stains; neutral, clear smooth boundary. (6
to 11 inches thick)

A2--7 to 28 inches, pink (7.5YR 7/4) loamy fine sand, light brown (7.5YR 6/4) moist; massive; loose, very friable; common very dark brown stains; many fine roots; neutral; gradual smooth
boundary. (14 to 29 inches thick)

B21t--28 to 46 inches, common coarsely mottled brown (7.5YR 5/4), reddish brown (5YR 5/4), and gray (10YR 5/1) loam; moderate coarse subangular blocky structure; soft, very friable, sticky;
many fine roots; clay films on surface of peds; medium acid;
gradual wavy boundary. (12 to 22 inches thick)

B22t--46 to 66 inches, mottled very dark grayish brown (10YR 3/2), light yellowish brown (10YR 6/4), and gray (10YR 5/1) clay loam; moderate coarse subangular blocky structure; very friable;
clay films on surface of peds; common black concretions; neutral. (15 to 25 inches thick)

B3--66 to 75 inches, light olive gray (5Y 6/2) sandy clay
loam, olive gray (5Y 5/2) moist; many medium distinct reddish
yellow (7.5YR 6/8) and strong brown (7.5YR 5/8) mottles moist;
weak coarse subangular blocky structure; very friable; few fine roots; ped surfaces have thin coatings of sand and silt; few black concretions; mildly alkaline.

TYPE LOCATION: Hill County, Texas; about 15 miles northwest of Hillsboro and 6 miles northeast of Whitney. About 4.5 miles north
of Whitney and Farm Road 933 to second road to east, then 2.7
miles east. The site is on north side of road in wide drain.

RANGE IN CHARACTERISTICS: Solum thickness ranges from 60 to more than 80 inches. Clay content of the upper 20 inches of the Bt horizon ranges from 18 to 30 percent.

The A horizon ranges from 20 to 40 inches thick. The Ap or A1 horizon is brown (7.5YR 5/4; 10YR 5/3), light brown (7.5YR 6/4),
or pale brown (10YR 6/3) and ranges from slightly acid Through neutral. Color of the A2 horizon is brown (7.5YR 5/4; 10YR 5/3), pale brown (10YR 6/3), light brown (7.5YR 6/4), or pink (7.5YR
7/4), with mottles of light brown (7.5YR 6/4) and grayish brown
(10YR 5/2) in some pedons. Reaction ranges from slightly acid through mildly alkaline.

The B21t horizon is mottled brown (7.5YR 5/2, 5/4; 10YR 5/3),
light gray (10YR 7/1), gray (10YR 5/1, 6/1), pale brown (10YR
6/3), brownish yellow (10YR 6/6), yellow (10YR 7/8), red (2.5YR
5/6), or reddish brown (5YR 5/4). Texture ranges from loam to
clay loam. Reaction ranges from medium acid to mildly alkaline.

The B22t horizon is mottled gray (5Y 6/1; 10YR 5/1, 6/1), light
olive brown (2.5Y 5/4), olive yellow (2.5Y 6/6), light gray (10YR 7/1), very dark grayish brown (10YR 3/2), light yellowish brown
(10YR 6/4), brownish yellow (10YR 6/6, 6/8), yellow (10YR 7/8), reddish yellow (7.5YR 7/6), or red (2.5YR 5/8). Texture is sandy clay loam or clay loam; reaction ranges from slightly acid to
mildly alkaline.

The B3 horizon is generally mottled with a combination of light
olive gray (5Y 6/2), gray (5Y 5/1; 10YR 6/1), brown (10YR 5/3),
light gray (10YR 7/1), brownish yellow (10YR 6/6, 6/8), and
reddish yellow (7.5YR 6/8) and contains few to common pockets, streaks, and coatings of uncoated sand and silt. Texture is sandy clay loam or clay loam. Reaction ranges from neutral through moderately alkaline.

COMPETING SERIES: These are the Alum, Catilla, Demona, Heatly, Heaton, Meno, Nimrod, Nobscot, Patilo, Silstid, Styx, and Tremona series. Alum, Demona, and Tremona soils have fine textured
control sections and Alum soils lack gray mottles. Catilla and Patilo soils have sandy epipedons more than 40 inches thick.
Heatly, Heaton, Nobscot, Silstid, and Styx soils lack gray mottles
in the upper Bt horizon. Meno soils have a solum thickness of
less than 60 inches and have mixed mineralogy. The B2t horizon of Nimrod soils is strongly or medium acid throughout.

GEOGRAPHIC SETTING: The Coving series are on nearly level to
gently sloping uplands. These soils occur in wide, shallow,
concave drainageways in the East Cross Timbers MLRA. The soil
formed in deep loamy and sandy sediments, probably reworked by
wind. Slopes range from 0 to 3 percent. Climate is moist
subhumid. Mean annual rainfall ranges from 28 to 35 inches. Mean annual temperature ranges from 64 degrees to 69 degrees F. Thornthwaite P-E indices range from 48 to 62.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Eufaula, Gasil, Silstid, and Vaughan series. Eufaula, Gasil, and Silstid soils
lack gray mottles in the upper B2t horizon. In addition, Eufaula soils have a sandy control section and Gasil soils have A horizons less than 20 inches thick. Vaughan soils have A horizons less
than 20 inches thick.

DRAINAGE AND PERMEABILITY: Somewhat poorly drained; slow runoff; moderate permeability. A perched water table is at the top of the B2t horizon for short periods following heavy rains. Unless protected, flooding by shallow, slow moving water occurs during periods of high rainfall.

USE AND VEGETATION: Used mainly for pasture. Areas that are
cropped are used mostly for peanuts, small grains, and truck
crops. Native vegetation includes sedges, vines, briers, switchgrass, broomsedges, indiangrass, and shrubs. Trees consist
of cottonwood, willows, pecan, and oak.

DISTRIBUTION AND EXTENT: Central Texas in small drains in the
East Cross Timbers. These soils are of minor extent

MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Temple, Texas

SERIES ESTABLISHED: Hill County, Texas; 1975.

REMARKS: These soils were formerly classified in the Red-Yellow Podzolic great soil group and have been included in the Nimrod series.


National Cooperative Soil Survey
U. S. A.