O30 Princeton Hydro Report Dated 9 3 25

3/31/25, 1:09 PM Official Series Description - HALEDON Series LOCATION HALEDON NJ+NY Established Series Rev. CFE-RAS-SMF 01/2013 HALEDON SERIES The Haledon series consists of very deep, somewhat poorly drained soils in low positions on undulating uplands. They formed in glacial till. Slope ranges from 0 to 15 percent. Saturated hydraulic conductivity is moderately high or high above the fragipan and very slow or slow in in the fragipan and densic materials. Mean annual temperature is about 13 degrees C and mean annual precipitation is about 1258 mm. TAXONOMIC CLASS: Coarse-loamy, mixed, active, mesic Aquic Fragiudalfs TYPICAL PEDON: Haledon cobbly loam at an elevation of about 140 m. (Colors are for moist soil.) Ap--0 to 20 cm; very dark grayish brown (10YR 3/2) cobbly loam, gray (10YR 6/1) dry; moderate medium granular structure; very friable; many roots; common fine pores; 25 percent rock fragments of stones, cobbles and gravel; moderately acid; clear wavy boundary. (15 to 25 cm thick) Bt1--20 to 41 cm; yellowish brown (10YR 5/4) cobbly loam; moderate medium subangular blocky structure; friable, slightly sticky; common roots that decrease in number with depth; common fine tubular pores; few faint brown (7.5YR 4/4) clay films on faces of peds and in sand and pebble niches; 20 percent rock fragments, dominantly cobbles and coarse gravel and some stones; common coarse and medium distinct brown (7.5YR 4/4) masses of iron accumulation, common fine and medium faint brown (10YR 5/3) iron depletions, and few fine distinct strong brown (7.5YR 5/8) masses of iron accumulation; moderately acid; gradual wavy boundary. (10 to 46 cm thick) Bt2--41 to 76 cm; yellowish brown (10YR 5/4) and brown (7.5YR 4/4) cobbly loam; moderate medium subangular blocky structure; friable; few fine roots; few fine tubular pores; brown (7.5YR 4/4) clay films on faces of peds and common bridging with semi-waxy clay films; 20 percent rock fragments, dominantly cobbles and gravel; common coarse distinct dark brown (7.5YR 3/2) iron depletions, common fine faint pale brown (10YR 6/3) masses of iron accumulation, few fine distinct strong brown (7.5YR 5/8) masses of iron accumulation, and few to common fine distinct light brownish gray (10YR 6/2) masses of iron accumulation and grayish brown (10YR 5/2) iron depletions that increase in number with depth; moderately acid; abrupt smooth

d few to common fine distinct light brownish gray (10YR 6/2) masses of iron accumulation and grayish brown (10YR 5/2) iron depletions that increase in number with depth; moderately acid; abrupt smooth boundary. (0 to 41 cm thick) Bx1--76 to 97 cm; brown (7.5YR 4/4) gravelly sandy loam streaked and splotched with yellowish brown (10YR 5/4); weak very thick platy structure; very firm; brittle; few fine roots between peds or in structures; very few fine vesicular pores; very few distinct waxy and semi-waxy clay and silt coats on plate surfaces; common faint silt and clay bridging between sand grains; few fine black (10YR 2/1) manganese stains on ped surfaces; 20 percent rock fragments, dominantly gravel; moderately acid; clear smooth boundary. (15 to 51 cm thick) Bx2--97 to 114 cm; variegated brown (7.5YR 4/4), light brownish gray (10YR 6/2), strong brown (7.5YR 5/6), yellowish brown (10YR 5/6), and brown (10YR 5/3) gravelly sandy loam; moderate very thick platy structure; very firm; brittle; very few fine vesicular pores; very few distinct clay films on faces of peds; few fine black (10YR 2/1) manganese stains on ped surfaces; 20 percent rock fragments, dominantly gravel; moderately acid; abrupt smooth boundary. (0 to 51 cm thick) Cd--114 to 183 cm; brown (10YR 4/3) gravelly sandy loam; massive; very firm; few fine vesicular pores; 30 percent rock fragments, dominantly gravel; slightly acid. TYPE LOCATION: Passaic County, New Jersey; Township of Wayne, 10 feet west of unimproved dirt road, 1,000 feet north of junction of dirt road with Patterson-Hamburg turnpike. Junction of dirt road with turnpike is 1,600 feet east of entrance to north Jersey Country Club; USGS Paterson quadrangle, longitude 40 degrees 57 minutes 20 seconds N., latitude 74 degrees 12 minutes 45 seconds W, NAD 27. RANGE IN CHARACTERISTICS: Thickness of the solum ranges from 102 to 152 cm. Depth to the fragipan is 61 to 90 cm. Depth to bedrock is greater than 2 m. Rock fragments of mostly gravel, cobbles, and stones of basalt, shale, sandstone and gneiss range from 5 to 25 percent in the solum and from 15 to 35 percent in the substratum. Mineralogy is dominated by quartz, feldspar, amphibole and mica. Reaction ranges from extremely acid to moderately acid in the upper part of the solum, from strongly acid to slightly acid in the lower part of the solum and upper part of the C

r, amphibole and mica. Reaction ranges from extremely acid to moderately acid in the upper part of the solum, from strongly acid to slightly acid in the lower part of the solum and upper part of the C horizon, https://soilseries.sc.egov.usda.gov/OSD_Docs/H/HALEDON. htm! 113,