SITE ASSESSMENT AND SEPTIC EVALUATION FOR JASON & JANET THATCHER 201 N. SPRAGUE AVED KINGSTON, PA 18704

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1 DATE: December 13, 2010 N.H. LICENSED DESIGNER OF SUBSURFACE DISPOSAL SYSTEMS 216 Hill Road Phone & Fax: Franklin, NH Cell: SITE ASSESSMENT AND SEPTIC EVALUATION FOR JASON & JANET THATCHER 201 N. SPRAGUE AVED KINGSTON, PA Lot#: 99-2 Tax Map#: 407 Mt Cardigan Road, Alexandria, NH

2 State of New Hampshire DEPARTMENT OF ENVIRONMENTAL SERVICES Subsurface Systems Bureau 29 Hazen Drive, PO Box 95, Concord, NH FAX Site Assessment Form RSA 485-A:39 A. Property 1. Seller's Name: BLACK BROOK REALTY TRUST Street: 264 EASTMAN HILL ROAD City/Town: SANBORNTON State: NH Zip: Tel #: 2. Agent's Name: FRAN SANDERSON - BEANGROUP REALTORSStreet: MAIN STREET City/Town: FRANKLIN State: NH Zip: Tel #: Assessor's Name: TOM Designer Permit #: ANGE Street: HILL ROAD City/Town: FRANKLIN State: NH Zip: Tel #: Lot Location: City/Town: ALEXANDRIA Lot #: 99-2 Tax Map #: 407 Street: MT. CARDIGAN ROAD Subdivision Name: (not known) 5. Brief Description of Property and Structures (incl. # bedrooms): 3.49 ACRE LOT 6. Abutters, if known (attach additional sheet if necessary): Name: N/A Mail Address: Name: Mail Address: Name: Mail Address: B. Lot Characteristics 1. Lot Size: Slope: E - APPROX 25% 3. Loading Capacity (calculated): 1,454 GPD (A 4-BR HOUSE IS 600GPD) 4. Water Supply: Well on Lot: (FUTURE) Municipal N/A (name) Community: N/A (name) Other: N/A 5. Soil Type*: BECKET 6. Estimated Seasonal High Water Table*: (TBD) 7. Scope of Review (e.g., written record only, on-site investigation, etc.): VISITED SITE AND PULLED SOIL CORES WITH AUGER. 8. Designer=s Assessment of Site for Current Use of System: THERE IS NO SYSTEM CURRENTLY ON THE LOT. THE SOIL IS A MODERATELY WELL DRAINED SOIL OF GLACIAL TILL. THE SOIL AND ESTIMATED PERC WILL SUPPORT A 3 OR 4 BEDROOM SEPTIC SYSTEM. *From US Natural Resources Conservation Service maps or actual data, if available Distribution: Original with listing, then to Buyer; 1 copy to Assessor

3 C. Present Sewage Disposal System 1. Does the property currently have any sewage disposal system? Yes No 2. If yes, is the system state approved? Yes No If YES, a copy of the approved plan, construction approval and operational approval must be attached to the original of this form. Also, an 8-1/2" x 11" sketch to scale or with dimensions shown of the lot, approximate property lines and approximate locations of abuttors' septic systems and wells (with 75' well radius), if known, must be attached. If NO, supply all available information on the type, capacity, age and location of the system, and include an 8-1/2" x 11" sketch to scale or with dimensions shown of the property and the location of the system. Also, an 8-1/2" x 11" sketch to scale or with dimensions shown of the lot, approximate property lines and approximate locations of abuttors' septic systems and wells (with 75' well radius), or if known, must be attached. NOTE: Env-Ws PROVIDES THAT "HOLDING TANKS SHALL NOT BE APPROVED EXCEPT AS A REPLACEMENT FOR AN EXISTING SYSTEM IN FAILURE WHEN NO OTHER MEANS OF DISPOSAL IS PRACTICAL." HOLDING TANKS ARE NOT APPROVED FOR NEW CONSTRUCTION OR FOR EXPANSION OF EXISTING STRUCTURES. THE ASSESSOR MUST STAMP AND DATE BELOW Assessment Date: THE STATEMENT BELOW MUST BE SIGNED AND DATED BY THE BUYER The undersigned certify that we have reviewed this Site Assessment Form and understand the information contained herein and that we have received a copy of this Site Assessment Form. Buyer: Date: Buyer: Date: Revised 10/99

4 Soil Map Grafton County, New Hampshire 43 38' 29'' 43 38' 3'' ' 21'' 71 51' 22'' D 57E Brock Brook Brook Rd 559C C B Map Scale: 1:5,650 if printed on A size (8.5" x 11") sheet. Meters Kummerer Rd C ,200 1,800 57D Feet B Mud Hill Rd Hutchins Hill Rd D 559B 90C Shin Valley Rd D 61D 559C ' 29'' ' 28'' ' 30'' 43 38' 5'' Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey Page 1 of 3

5 Soil Map Grafton County, New Hampshire MAP LEGEND MAP INFORMATION Area of Interest (AOI) Area of Interest (AOI) Soils Soil Map Units Special Point Features Blowout Borrow Pit Clay Spot Closed Depression Gravel Pit Gravelly Spot Landfill Lava Flow Marsh or swamp Mine or Quarry Miscellaneous Water Perennial Water Rock Outcrop Saline Spot Sandy Spot Severely Eroded Spot Sinkhole Slide or Slip Sodic Spot Spoil Area Stony Spot Very Stony Spot Wet Spot Other Special Line Features Gully Short Steep Slope Other Political Features Cities Water Features Oceans Streams and Canals Transportation Rails Interstate Highways US Routes Major Roads Local Roads Map Scale: 1:5,650 if printed on A size (8.5" 11") sheet. The soil surveys that comprise your AOI were mapped at 1:24,000. Please rely on the bar scale on each map sheet for accurate map measurements. Source of Map: Natural Resources Conservation Service Web Soil Survey URL: Coordinate System: UTM Zone 19N NAD83 This product is generated from the USDA-NRCS certified data as of the version date(s) listed below. Soil Survey Area: Grafton County, New Hampshire Survey Area Data: Version 13, Oct 23, 2009 Date(s) aerial images were photographed: 9/8/2003 The orthophoto or other base map on which the soil lines were compiled and digitized probably differs from the background imagery displayed on these maps. As a result, some minor shifting of map unit boundaries may be evident. Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey Page 2 of 3

6 Soil Map Grafton County, New Hampshire Map Unit Legend 57C 57D 57E Grafton County, New Hampshire (NH009) Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI Becket fine sandy loam, 8 to 15 percent slopes, very stony Becket fine sandy loam, 15 to 25 percent slopes, very stony Becket fine sandy loam, 25 to 35 percent slopes, very stony 61D Tunbridge-Lyman-Rock outcrop complex, 15 to 25 percent slopes % % % % 90C Tunbridge-Lyman complex, 8 to 15 percent slopes % 90D Tunbridge-Lyman complex, 15 to 25 percent slopes % 255D Monadnock and Hermon soils, 15 to 25 percent slopes, very stony % 558B Skerry fine sandy loam, 3 to 8 percent slopes % 559B 559C Skerry fine sandy loam, 3 to 8 percent slopes, very stony Skerry fine sandy loam, 8 to 15 percent slopes, very stony % % 613 Croghan loamy fine sand % 711D Monadnock-Hermon association, hilly, very stony % Totals for Area of Interest % Natural Resources Conservation Service Web Soil Survey National Cooperative Soil Survey Page 3 of 3

7 Official Series Description - BECKET Series Page 1 of 3 LOCATION BECKET NH MA ME NY VT Established Series Rev. RJK-SHG-SWF 03/2010 BECKET SERIES The Becket series consists of very deep, well drained soils that formed in a loamy mantle overlying dense, sandy till on drumlins and glaciated uplands. They are moderately deep to a densic contact. Saturated hydraulic conductivity is moderately high through very high in the mineral solum and moderately low or moderately high in the dense substratum. Slope ranges from 3 through 60 percent. Mean annual precipitation is about 40 inches and mean annual temperature is about 43 degrees F. TAXONOMIC CLASS: Coarse-loamy, isotic, frigid Oxyaquic Haplorthods TYPICAL PEDON: Becket fine sandy loam, on a 9 percent west-southwest facing slope in a stony, forested site. (Colors are for moist soil.) Oi-- 0 to 2 inches; slightly decomposed plant material. (The combined thickness of the O horizon is 0 to 5 inches thick.) E-- 2 to 4 inches; pinkish gray (7.5YR 6/2) fine sandy loam; weak fine granular structure; very friable; many medium and fine roots; 5 percent gravel; very strongly acid; abrupt wavy boundary. (0 to 3 inches thick.) Bhs-- 4 to 5 inches; dark reddish brown (5YR 3/2) fine sandy loam; weak fine granular structure; very friable; many medium and fine roots; 10 percent gravel; very strongly acid; abrupt wavy boundary. (Combined thickness of the Bhs and Bh horizons is 0 to 11 inches thick.) Bs1-- 5 to 7 inches; reddish brown (5YR 4/4) fine sandy loam; weak fine granular structure; very friable; many medium and fine roots; 10 percent gravel; very strongly acid; abrupt irregular boundary. Bs2-- 7 to 14 inches; strong brown (7.5YR 5/6) fine sandy loam; weak fine granular structure; very friable; common medium and fine roots; 10 percent gravel; very strongly acid; clear irregular boundary. Bs to 24 inches; yellowish brown (10YR 5/6) gravelly sandy loam; weak medium granular structure; friable; common fine roots; 15 percent gravel; very strongly acid; clear wavy boundary. (Combined thickness of Bs horizons is 4 to 25 inches.) BC-- 24 to 33 inches; light olive brown (2.5Y 5/4) gravelly sandy loam; moderate medium granular structure; friable; few fine roots; 20 percent gravel, 5 percent cobbles; strongly acid; abrupt smooth boundary. (0 to 24 inches thick.) Cd-- 33 to 67 inches; mixed olive (5Y 4/3) gravelly sandy loam and olive yellow (2.5Y 6/6) sand, composite texture of gravelly loamy sand; massive; firm and brittle; few medium prominent strong brown (7.5YR 5/8) masses of iron accumulation; 20 percent gravel, 10 percent cobbles; horizon consists of firm gravelly sandy loam with horizontally oriented lenses and pockets of loose sand; rock fragments

8 Official Series Description - BECKET Series Page 2 of 3 coated with olive yellow (2.5Y 6/6) sand; strongly acid. TYPE LOCATION: Cheshire County, New Hampshire; town of Rindge, 2,200 feet south of NH Rte. 119, 3,000 feet southwest of the intersection NH Rte. 119 and U.S. Rte 202, in a logging road cut. USGS Monadnock, NH 15 minute quadrangle; Latitude 42 degrees, 45 minutes, 35 seconds N. and Longitude 72 degrees, 03 minutes, 00 seconds W., NAD 83. RANGE IN CHARACTERISTICS: Mineral solum thickness ranges from 20 through 36 inches. Reaction ranges from extremely acid through slightly acid in the mineral solum, and from very strongly acid through neutral in the substratum. Rock fragment are dominantly gravel and range from 5 through 30 percent in the solum and from 5 through 40 percent in the substratum. Rock fragments constitute less than 35 percent of the particle-size control section. Ortstein ranges from 0 through 20 percent of the spodic horizon. The O horizon is neutral or has hue of 2.5YR through 10YR, value of 2 through 4, and chroma of 0 through 4. It is slightly, moderately or highly decomposed plant material. Some pedons have an A horizon that has hue of 5YR through 10YR, value of 2 through 4, and chroma of 1 through 3. It is up to 6 inches thick. Disturbed areas have an Ap horizon with hue of 7.5YR or 10YR, value of 3 or 4, and chroma of 2 through 4. The A and Ap horizons are dominantly fine sandy loam, but include loam and sandy loam in the fine-earth fraction. Structure is granular. The E horizon has hue of 5YR through 2.5Y, value of 4 through 7, and chroma of 1 or 2. Texture is fine sandy loam, sandy loam, or loamy sand in the fine-earth fraction. Structure is granular or subangular blocky or the horizon is massive. The Bhs horizon has hue of 2.5YR through 7.5YR, value of 2 through 3, and chroma of 1 through 3. Texture is dominantly fine sandy loam, but includes loam and sandy loam in the fine-earth fraction. Structure is granular or subangular blocky or the horizon is massive. Some pedons have a Bh horizon has hue of 2.5YR through 10YR, value of 2 through 3, and chroma of 1 through 4. Texture range is the same as the Bhs horizon. The Bs horizon has hue of 2.5YR through 10YR, value of 3 through 8 and chroma of 2 through 8. Texture is fine sandy loam or sandy loam in the fine-earth fraction. Structure is granular or subangular blocky or the horizon is massive. The BC horizon has hue of 10YR through 5Y, value and chroma of 3 through 6. Texture is fine sandy loam, sandy loam, loamy fine sand, or loamy sand in the fine-earth fraction. Structure is granular, platy, or subangular blocky or the horizon is massive. The Cd horizon has hue of 10YR through 5Y, value of 4 through 7, and chroma of 2 through 6. It is comprised of loamy layers and sandy pockets and lenses with horizontal orientation, with a composite texture of loamy sand, loamy fine sand, sandy loam, fine sandy loam, or their gravelly analogues. The lenses are coarse, medium, or fine sand and are 1/8 through 3 inches thick. They make up 20 percent or more of the horizon. They are massive, with or without plate-like divisions. Consistence is firm or very firm. Some pedons have friable C horizons up to 8 inches thick. COMPETING SERIES: These are the Marlow, Mundal, Mundalite and Plaisted series. Marlow soils have loamy substrata with less than 20 percent sand lenses or pockets. The duration of saturation in the

9 Official Series Description - BECKET Series Page 3 of 3 subsoil is greater in Mundal soils which are moderately well drained. Mundalite soils have spodic horizons greater than 18 inches. Plaisted soils have greater than 50 percent silt in the particle-size control section. GEOGRAPHIC SETTING: Becket soils are on drumlins and glaciated uplands. Slope is dominantly 3 through 35 percent, but ranges from 3 through 60 percent. The soils formed in stony till of Wisconsin age derived principally from granite, gneiss, and schist on drumlins and glaciated uplands. Mean annual temperature ranges from 38 through 45 degrees F. and mean annual precipitation ranges from 30 through 50 inches. The frost-free growing season ranges from 90 through 160 days. GEOGRAPHICALLY ASSOCIATED SOILS: These are the Berkshire, Lyman, Lyme, Monadnock, Peru, Pillsbury, Skerry, and Sunapee soils. The moderately well drained Skerry soils are in a drainage sequence with Becket soils. The well drained Marlow soils and moderately well drained Peru soils have densic materials with less than 20 percent sand lenses. The somewhat excessively drained Hermon soils, the well drained Berkshire and Monadnock soils, and the moderately well drained Sunapee soils have friable substrata. The somewhat excessively drained Lyman soils are on bedrock controlled landforms and have bedrock within 20 inches. The somewhat poorly drained and poorly drained Pillsbury and Lyme soils are in depressions and drainageways. DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Well drained. Potential for surface runoff is low to high. Saturated hydraulic conductivity moderately high to very high in the mineral solum and moderately low or moderately high in the dense substratum. USE AND VEGETATION: Mostly forested. Principle species include sugar maple, yellow birch, paper birch, eastern white pine, eastern hemlock, balsam fir, and white spruce. Areas cleared of trees and stones are used mostly for hay and pasture with a few apple orchards and cultivated crops. DISTRIBUTION AND EXTENT: Maine, New Hampshire, and northern New York. MLRA's 142, 143, 144B and 145. The series is extensive. MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Amherst, Massachusetts. SERIES ESTABLISHED: Berkshire County, Massachusetts, Becket is a Hall of Fame series. REMARKS: The use of the Becket series in MLRA 145 is in question. Becket has a Frigid temperature regime which is unlikely in MLRA 145. Diagnostic horizons and features recognized in this pedon are: a. Albic horizon - the zone from 2 through 4 inches (E horizon). b. Spodic horizons - the zone from 4 through 14 inches (Bhs, Bs1, and Bs2 horizons). c. Densic contact - at 33 inches. d. Densic materials - the zone from 33 through 67 inches (Cd horizon). National Cooperative Soil Survey U.S.A.

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