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Textures: Subsoil Indicator(s)of Saturation: Consistence: c-day S1. Distinct gray or red redox features Loose- Intact specimen not available sic-silty clay 52. Depleted matrix (value >/=4 and chroma </=2) Friable- Slight force between fingers sc-sandy day 53. 5Y chroma </= 3 Firm- Moderate force between fingers cl-clay loam S4. 7.5 YR or redder faint redox concentrations or redox depletio Extremelv Moderate force between hands or slight firm- foot pressure sicl-silty day loam If yes to one of the above indicators then: Ri id- Foot pressure scl-sandy clay loam Topsoil Indicator(s) of Saturation: Slope Shape: si-silt T1. Wetland Vegetation Slope shape is described in two directions: up and down slope sil-silt loam *Sand Modifiers T2. Depressional Landscape (perpendicular to the contour), and across slope (along the l-loam co-coarse T3. Organic texture or organic modifiers horizontal contour); e.g. Linear, Convex or LV'. sl-sandy loam` m-medium T4. N 2.5/ 0 color ls-loamy sand* f-fine T5. Redox features in topsoil s-sand" vf-very fine T6. Hydraulic indicators SoilStructure _��--„ '�� `" `� Grade: �,�. � �� : 'y ��, -� _ .� ._ Massive- No observable aggregates, or no orderly arrangement of natural lines of weakness ' ^ " � ,.� � Weak- Poorly formed, indistinct peds, barely observable in place �� '�; �°-=� °�°� � "'"��°�� , Moderate- Well formed, distinct peds, moderately durable and evident, but not distinct in undisturbed � �� '_�« .�`t �--�.�.�-� ,.�� Durable peds that are quite evident in un-displaced soil, adhere weakly to one another, _.._,,�� - � » , �.-�� Stron - �,,�ithstand displacement, and become separated when soil is disturbed "�, �.`,. ��'� . ',,� ,,`� �� . _. - ,,-- Laudscape Posit[on: __. � _ Loose- No peds, sandy soil --� ;.r.x- . su�nuvc -a� >r�. .. a... . c�,-�.., � . . �� � , «�_,��,. �_._......� 5houlder :."-.• '�.'�•:J, Soil Structure sA�k s.ae Foot sloue Shape: ' Z'oe slope — Granular- The peds are approximately spherical or polyhe . are the small, rounded peds that hang onto roots Platy_ The peds are flat and plate like. They are oriented horizontally and are usually overlapping. Platy structure is commonly found in forested areas Blocky_ The peds are block-like or polyhedral, and are bounded by flat or slightly rounded surface that are casting of the faces of surrounding peds. Blocky Prismatic- Flat or slightly rounded vertical faces bound the individual peds. Peds are distinctly longer vertically, and faces are typically cast or molds of Sin�le Grain-The structure found in a sandy soil. The individual particles are not held together.