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Entisols: Young Soils with No Diagnostic Horizons

Entisols are what soil looks like before it has had time to develop: fresh sediment with little more than a topsoil.[1] Below: what keeps a soil in this order, the suborders NRCS describes and how they’re used, how wet or dry they run, and where USDA’s survey maps them.

Is your soil an Entisol?

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Entisols are soils with no diagnostic horizons, many of them sandy or very shallow, often formed where sediment arrives faster than a soil can develop. USDA maps about 251.3 million acres, 12.5% of US soil acres with an order and the fourth most of any order.

What makes a soil an Entisol

The rule is an absence: Entisols have no diagnostic horizons. Many have an ochric epipedon and a few an anthropic one, many are sandy or very shallow, and some sit on steep slopes that are actively eroding.[2]

The Soil Science Society of America describes little to no development beyond an identifiable topsoil. These soils form on recently deposited sediment, often where deposition outpaces soil development: active flood plains, dunes, landslide areas and ground left by retreating glaciers. The name comes from “recent”, and worldwide they are the second largest group after Inceptisols, about 16% of the land.[1]

Entisols form on recently deposited sediment, such as active flood plains and dunes, where deposition outpaces soil development.[1]

Mostly an A horizon over C material

In the survey, the most common Entisol sequence is A–C, a topsoil straight over C material, on 54.1% of described acres. A B horizon turns up on only 20.9%, while C material is in 90.2% of the profiles.[3]

AtopsoilClayered sediment
An Entisol in A–C, the survey’s most common Entisol sequence: a topsoil (A) straight over C material, here the layered sediment of a flood plain, with no B horizon between. Not to scale.[3][1]

The next sequences are A–B–C (18.8 million acres), O–A–C (10.5 million acres) and C (10.2 million acres). The A horizon has a median thickness of 5.1 inches (13 cm), thinner than the 6.3 inches (16 cm) of all US soils, and bedrock appears in 12.5% of profiles, at a median 11.8 inches (30 cm) where it does.[3]

Where a parent material is recorded, it’s most often alluvium (40.2%), residuum (17.0%) and eolian (wind-blown) sand (15.7%). The first mineral layer is most often sandy loam (21.0%), sand (20.0%), silt loam (15.6%), loam (14.3%) and loamy sand (13.0%); sand and loamy sand alone make up 33.0%.[3]

Typical properties of the first mineral layer

Median, with the middle half of the acres in brackets.

PropertyMedian (middle half)Components
Water held (in per ft)1.3 (0.96–2.0)117,934
Ksat (µm/s)28 (9–91.7) · High119,434
Bulk density (g/cm³)1.45 (1.33–1.53)118,604
pH7.4 (6.5–7.9) · slightly alkaline119,300
Organic matter (%)1.2 (0.75–2.0)119,485

The median pH of the first mineral layer, 7.4, is slightly alkaline.[3][4]

Entisol suborders and how they’re used

NRCS describes these Entisol suborders:

  • Aquents are the wet Entisols, and they’re widely distributed. They support vegetation that tolerates permanent or periodic wetness and are used mostly as pasture, cropland, forest or wildlife habitat.
  • Arents have no diagnostic horizons because they’ve been deeply mixed by plowing. They’re important soils for irrigated crop production in California.
  • Orthents are mainly in the Western States, commonly on recent erosional surfaces, and are used mostly as rangeland, pasture or wildlife habitat.
  • Psamments are sandy in all layers. In some arid and semiarid climates they’re among the most productive rangeland soils, but some that are nearly bare are subject to soil blowing and drifting and give wheeled vehicles poor support. Some of the largest areas are in Nebraska, California, Minnesota, Wisconsin, Michigan, Arizona and Florida.[2]

Fluvents, the Entisols of recent water-laid sediment on flood plains, have their own section on our alluvial soil page.[2] The survey data doesn’t record suborders, so none of them gets an acreage here.

Wet and droughty Entisols

Entisols run to both ends of the drainage scale. 33.2% of their acres are excessively or somewhat excessively drained, and 10.3% are poorly or very poorly drained.[3][5] The wet end has its own suborder in NRCS’s scheme, the Aquents.[2]

Drainage classShare of Entisol acresMillion acres
Excessively drained18.9%47.2
Somewhat excessively drained14.2%35.4
Well drained43.7%108.8
Moderately well drained5.7%14.3
Somewhat poorly drained6.8%17.0
Poorly drained5.7%14.2
Very poorly drained4.6%11.4
Subaqueous0.3%0.8

35.4% of Entisol acres are in hydrologic soil group A, the group where water soaks in fastest, the largest share of any order.[3][6]

Are Entisols good for farming?

Another 6.0% would be prime if drained, irrigated or protected from flooding, and 6.9% is farmland of statewide or local importance. Most of the rest sits in land-capability Classes VI–VIII (72.7% of rated acres); 22.0% is in the cultivable Classes I–IV.[3][7][8]

NRCS lists the uses suborder by suborder: Orthents are used mostly as rangeland, pasture or wildlife habitat; some Psamments are among the most productive rangeland soils in arid and semiarid climates; Aquents serve as pasture, cropland, forest or wildlife habitat; and Arents are important for irrigated crops in California.[2]

Check one address with the prime farmland checker.

Entisols vs Inceptisols

The two orders differ by how far development has gone. Entisols show little to none beyond a topsoil; Inceptisols show a moderate degree of development but haven’t built up much clay in the subsoil.[1] The University of Nebraska–Lincoln’s PASSEL lessons sum them up as “little, if any horizon development” against “beginning of horizon development”.[9]

In the survey that gap shows up as the B horizon: 88.6% of described Inceptisol acres have one, against 20.9% of Entisol acres.[3]

Where Entisols are in the US

California25.0MNebraska22.0MAlaska20.0MMontana17.9MArizona16.4MNevada14.2MWyoming13.7MColorado11.4MNew Mexico11.0MUtah9.9M
  1. 1. California: 25.0M
  2. 2. Nebraska: 22.0M
  3. 3. Alaska: 20.0M
  4. 4. Montana: 17.9M
  5. 5. Arizona: 16.4M
  6. 6. Nevada: 14.2M
  7. 7. Wyoming: 13.7M
  8. 8. Colorado: 11.4M
  9. 9. New Mexico: 11.0M
  10. 10. Utah: 9.9M
Top 10 states by Entisol acres (USDA survey).

California has the most Entisol acres, 25.0 million, and they’re the leading order in California and Wyoming. As a share of each state’s own soil acres they peak in Nebraska:[3]

StateShare of the state’s soil acresMillion acres
Nebraska45.2%22.0
California29.9%25.0
Utah28.7%9.9
Wyoming28.2%13.7
Arizona27.5%16.4
Florida24.1%8.0
Nevada23.3%14.2
Montana21.1%17.9

Most widespread Entisol series

SeriesAcresMost inSurvey areas
Valentine10,802,220Nebraska66
Valent3,524,504Colorado66
Cabbart2,680,209Montana65
Bibb2,292,057Alabama213
Cabba2,092,237Montana64
Lakeland1,970,348Florida106
Sheppard1,395,900Arizona27

Valentine (Nebraska) covers 10.8 million acres, more than any other series of any order in our data; Valent (Colorado) and Cabbart (Montana) come next. Each name links to its official USDA description.[3][10]

Download the Entisols data (CSV)

Entisols compared with other orders

Among the twelve orders, Entisols rank fourth by US acres, and only five orders (Andisols, Aridisols, Gelisols, Histosols and Spodosols) have a smaller prime-farmland share.[3][7]

OrderShareMedian ASurface pHPrime farmland
Alfisols14.9%7.1 in6.220.6%
Andisols1.6%8.3 in5.81.8%
Aridisols8.7%3.5 in7.90.1%
Entisols12.5%5.1 in7.43.0%
Gelisols6.3%3.9 in5.30.0%
Histosols2.4%——0.0%
Inceptisols13.8%5.1 in5.65.3%
Mollisols23.6%9.8 in7.023.2%
Oxisols0.0%5.9 in5.120.7%
Spodosols4.5%3.9 in4.82.2%
Ultisols9.6%5.9 in5.324.0%
Vertisols2.1%7.1 in7.332.2%

Histosols show a dash: their surface is organic material (peat or muck), so a topsoil (A) or surface pH median would describe mineral soil beneath it.

Frequently asked questions

What are Entisols?
Soils with no diagnostic horizons. Many are sandy or very shallow, and some are on steep, actively eroding slopes.[2]
Why are Entisols called young soils?
They form on recently deposited sediment, often where deposition is faster than soil development, so they show little development beyond a topsoil. The name comes from “recent”.[1]
What are the types of Entisols?
NRCS describes Aquents (wet), Arents (deeply mixed), Orthents (on recent erosional surfaces, mainly in the West), Psamments (sandy in all layers) and Fluvents (on flood-plain sediment).[2]
Are Entisols good for farming?
Few are prime farmland: 3.0% of their acres, against 12.5% nationally. NRCS lists rangeland, pasture and wildlife habitat among the main uses of its suborders, and irrigated crops for California’s Arents.[3][7][2]
Where are Entisols found in the US?
California, Nebraska and Alaska have the most acres, and they make up 45.2% of Nebraska’s soil acres with an order.[3]
What is the difference between Entisols and Inceptisols?
Development. Entisols show little to none beyond a topsoil; Inceptisols show a moderate degree but little clay buildup in the subsoil. 88.6% of described Inceptisol acres have a B horizon, against 20.9% of Entisol acres.[1][3]
What does ‘Entisol’ mean?
It comes from “recent”: these are soils of newly laid sediment.[1]

How we calculate this

Acres come from USDA SSURGO via Soil Data Access, weighted by each soil component's share of its map unit (USDA's representative percent) and summed across 3,386 detailed USDA soil surveys; shares are of the US acres that have a recorded order. Surface medians (pH, organic matter, water held, Ksat and bulk density) are of each component's first mineral layer below any organic (O) layer. Topsoil thickness, horizon sequences, farmland class and parent material come from a matching read of one profile per soil component. Data generated 2026-10-07.

Drainage class, hydrologic soil group, pH class, land capability, shrink-swell and in-state shares come from our soil-order profile aggregation of the same surveys (data generated 2026-10-30); in-state shares rank the 50 states and DC with at least 1,000,000 acres that have an order.

Sources

  1. Soil Science Society of America (soils4teachers), The Soil Orders Simplified (D. Lindbo)
  2. USDA NRCS, Entisols
  3. USDA NRCS, Soil Survey Geographic Database (SSURGO), via Soil Data Access
  4. USDA NRCS, National Soil Survey Handbook, Part 618, section 618.53: Reaction (pH) classes
  5. USDA NRCS, Soil Survey Manual (Agriculture Handbook 18), Ch. 3: drainage classes
  6. USDA NRCS, National Engineering Handbook, Part 630, Chapter 7: Hydrologic Soil Groups (January 2009)
  7. USDA NRCS, Farmland Protection Policy Act (7 U.S.C. 4201): definitions of prime, unique and statewide or local farmland
  8. USDA Soil Conservation Service, Land-Capability Classification (Agriculture Handbook 210; Klingebiel and Montgomery, 1961)
  9. University of Nebraska–Lincoln, PASSEL, Soil Orders
  10. USDA NRCS, Official Soil Series Descriptions (OSD) fact sheet

Marko Visic · MPharm, BSc Physics · Last reviewed November 13, 2026