O30 Princeton Hydro Report Dated 9 3 25

3/31/25, 1:10 PM Official Series Description - HASBROUCK Series more. Texture is loam or silt loam in the fine-earth fraction. The E or Eg horizon has hue of 2.5YR through 10YR, value of 3 through 6, and chroma of 1 or 2. Mottles with higher value and chroma are few or common. Texture ranges from sandy loam to silt loam in the fine-earth fraction. The BEg horizon, where present, has hue of 2.5YR through 10YR, value of 3 through 6, and chroma of 1 or 2. Redoximorphic features with higher chroma are common or many. Texture ranges from fine sandy loam to silt loam in the fine-earth fraction. The Btg horizon has hue of 2.5YR through 10YR, value of 3 through 7, and chroma of 1 or 2. Redoximorphic features with higher chroma are common or many. Texture is loam, clay loam, or sandy clay loam in the fine-earth fraction. Clay content dominantly is between 20 and 30 percent. The Bx horizon has hue of 2.5YR through 10YR, value of 3 through 7, and chroma of 1 through 8. Texture is commonly loam, loam, fine sandy loam, or sandy loam. Clay content dominantly is between 10 and 20 percent. Structure is weak or moderate, medium or thick platy, and may be within weak coarse prisms. Ped coat colors are one or two units of value higher than ped interiors. The C horizon has hue of 10R through 10YR, value of 3 through 7, and chroma of 0 through 6. Texture is dominantly sandy loam but ranges from loamy sand to loam in the fine-earth fraction. Clay content is less than 10 percent. The C horizon is massive, but may have weak, very thick platy layers in the upper 60 cm. Consistence is friable or firm. COMPETING SERIES: This is the Frenchtown series. Frenchtown soils have rock fragments that are dominantly sandstone gravel. GEOGRAPHIC SETTING: Hasbrouck soils are in nearly level or gently sloping depressions, drainageways, and areas adjacent to narrow floodplains of minor streams on uplands. Slope ranges from 0 to 8 percent. The soils formed in eroded and redeposited glacial materials on till of Wisconsin Age. The till materials are composed primarily of red shales, red sandstone, and basalt. GEOGRAPHICALLY ASSOCIATED SOILS: These include the well to moderately well drained Boonton soils and the somewhat poorly drained Haledon soils which formed in till and are on the adjacent uplands. The well drained Netcong soils, which do not have a fragipan, are on sideslopes of uplands.

on soils and the somewhat poorly drained Haledon soils which formed in till and are on the adjacent uplands. The well drained Netcong soils, which do not have a fragipan, are on sideslopes of uplands. The well drained Holyoke and Yalesville soils are shallow and moderately deep soils on hills and ridges. The poorly or very poorly drained Preakness soils are on adjacent outwash plains and terraces. DRAINAGE AND PERMEABILITY: Poorly drained. Runoff is negligible to high. Permeability is moderately rapid or moderate in the solum above the fragipan, slow or very slow in the fragipan, and moderately rapid or moderate in the C horizon. Saturated hydraulic conductivity is moderately low to high in the solum and substratum and very low to moderately low in the fragipan. USE AND VEGETATION: Most of the areas are wooded. A few of the gently sloping areas are used for recreation. Native vegetation is dominated by red maple, ash, pin oak, and swamp white oak. DISTRIBUTION AND EXTENT: Northern New Jersey. The soil is of limited extent with approximately 5,000 acres mapped. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Amherst, Massachusetts SERIES ESTABLISHED: Bergen County, New Jersey 1986. REMARKS: The Hasbrouck series replaced those soils which were previously correlated as Haledon Variant in Middlesex and Passaic Counties, New Jersey. Cation exchange activity class determined from a review of associated soils. Geographical location and coordinates could not be reliably determined from the described location. Diagnostic horizons and features recognized in this pedon include: 4. Ochric epipedon - the zone from the surface to a depth of 14 inches (A, Eg and BEg horizons). 2. Argillic horizon - the zone from 14 to 24 inches (Btg horizon). 3. Fragipan - the zone from 24 to 42 inches (Bx horizon). https://soilseries.sc.egov.usda.gov/OSD_Docs/H/HASBROUCK. html 213