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Epipedon Surface Descriptor: Mollic
Thick, dark colored, high base saturation, strong structure (A)
Epipedon Surface Descriptor: Umbric
Thick, dark colored, low base saturation, strong structure (A)
Epipedon Surface Descriptor: Ochric
Too light colored, low OM, may be hard or massive when dry, Low base saturation, thin light (A)
Epipedon Surface Descriptor: Melanic
Thick, black, High OM, common in volcanic ash (A)
Epipedon Surface Descriptor: Histic
very high in OM, wet during some part of year, peat bog (O)
Epipedon Surface Descriptor: Anthropic
Human modified molliclike horizon, high in available P (A)
Epipedon Surface Descriptor: Plaggen
Human made sodlike horizon created by years of manuring (A)
Epipedon Subsurface Descriptor: Argillic
Silicate clay accumulation
Epipedon Subsurface Descriptor: Natric
argillic, high in sodium, columnar or prismatic structure
Epipedon Subsurface Descriptor: Spordic
OM, Fe, and Al oxides accumulation
Epipedon Subsurface Descriptor: Cambric
Changed or altered by physical movement or chemical reactions, generally nonilluvial
Epipedon Subsurface Descriptor: Argic
Organic and clay accumulation just below plow layer resulting from cultivation
Epipedon Subsurface Descriptor: Oxic
Highly weathered, primarily mixture of Fe, Al oxides and non sticky-type clays
Epipedon Subsurface Descriptor: Duripan
Hard pan, strongly cemented by silica
Epipedon Subsurface Descriptor: Fragipan
Brittle pan, usually loamy textured, dense
Epipedon Subsurface Descriptor: Albic
light colored, clay, Fe and Al oxides mostly removed
Epipedon Subsurface Descriptor: Calcic
Accumulation of gypsum
Epipedon Subsurface Descriptor: Salic
Accumulation of salts
Epipedon Subsurface Descriptor: Kandic
Accumulation of low activity clays
Alfisols: Distribution & Characteristics
Dominate in Ohio, Indiana, Michigan, Wisconsin, Minnesota, Pennsylvania, NY (Humid to subhumid climate) Subsurface diagnostic horizon in which silicate clay has accumulated by illuviation; >35% base saturation, argillic horizon, natric and kandic horizon
Andisols: Distribution & Characteristics
Volcano areas, Washington Cascade in US, Japan, NZ and Chile rapid weathering of volcanic ash to produce amorphous or poorly crystallized silicate minerals: allophane and Fe oxy-hydroxide; melanic epipedon; high OM; dark color
Antisols: Distribution and Characteristics
S. California, Nevada, AZ, Central NM & Northern Mexico Dry, light in color, low in OM; Orchric epipedon; argillic and natric (sometimes); Rich in Calcic, gypsic, salic or natric; Argillic horizon
Entisols: Distribution & Characteristics
Rocky Mountainous Regions, NW Nebraska, SE Coastal Plain; River flood plains, river valley, riverbanks, floodplains and deltas Little Morphological developement, weakly developed mineral soils, unaltered from plant material, oorchic epipedon
Gelisols: Distribution & Characteristics
N. Russia, Canada, Alaska permafrost layer; cryoturbation; developed accumulations of Organic Parent Materials = Histels; young soils; little profile development
Histosols: Distribution & Characteristics
Wet areas of Alaska; Canada, Finland, Iceland,Ireland, Scotland, FL everglades, LA bayou Little profile development b/c of anaerobic environment; no permafrost; one or more thick layers of OSM; High OM; low bulk density
Inceptisols: Distribution & Characteristics
Mountains from S. NY through Carolinas Steep topography; low temperatures; resistant parent materials; low precipitation; thin surface horizons (ochric and umbric); slow development b/c of fast erosion; overlaying erosion resistant bedrock
Mollisols: Distribution & Characteristics
Large grassland areas; Great Plains of North America Dark soils; deep A horizon; mollic; <50% base saturation
Oxisols: Distribution & Characteristics
South America and Africa Highly weatered soils; hot climate with year round moisture; deep oxic horizon; ochric or umbric epipedon; uniform appearance with depth
Spodosols: Distribution & Characteristics
N. Europe and Russia, Central and Eastern Canada; NE US; N. Michigan; Wisconsin; S. Alaska; Cool mountainous areas of temperate regions Coarse textured and acid parents subject to leaching; occur only in moist areas; spodic horizon; subsurface accumulation of illuviated OM; accumulation …
Ultisols: Distribution & Characteristics
SE US; Hawaii; W. California; Oregon; Washington (Tropical - subtropical climate) Highly leached, clay accumulation n B horizon, argillic or kandic horizon; acidic B horizon; <35% base saturation; iron rich mottled material called plinthite
Vertisols: Distribution & Characteristics
India; Ethiopia; Sudan; N. & E. Australia; E. Mississippi; W. Alabama; SE Coast of Texas 30% of sticky swelling clays; forms deep cracks when soil is dry; dark (blackish) in color; OM is 1-6%; OM-clay complexes make OM oxidation slow; Develop from limestone

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