Carolyn J. Kraus Revocable Trust 154.32 ± Acres

Ceresco Township, Blue Earth County

Listing Agent: Darrell Hylen, ALC Office: 507-345-LAND (5263)Toll Free: 800-730-LAND (5263) Direct: 507-381-3843 Auctioneer #07-17-01 Darrell.Hylen@WingertRealty.com www.WingertRealty.com

We are pleased to present

For Sale at $825,000.00

State Highway Map

SUBJECT PROPERTY

Minneapolis

Mankato

Blue Earth County Minnesota

SUBJECT PROPERTY

Ceresco TownshipBlue Earth County

SUBJECT PROPERTY

FSA Aerial View

NOT NOT INCL- INCL- UDEDUDED

Building Site Survey Excluded from Sale

DESCRIPTION: 154.32± Acres. NE¼ ex Beg 1889.85’W of NE Cor W430.68’ S572.63’ E406.97’ N581.18’ Section 1, T106N-R29W (not to be used on legal documents) (Ceresco Township, Blue Earth County, Minnesota)

TAX PID #: R33.16.01.200.003 BUILDINGS: None

REAL ESTATE TAXES: 2020 Ag Non Hmstd taxes = $5,722.00 FSA INFORMATION: Total acres = 154.32 ± acres FSA Tillable acres = 144 ± acres Corn base acres = 85.54 ± acres Corn PLC Yield = 168 ± bushels Soybean base acres = 37.44 ± acres Soybean PLC Yield = 45 ± bushels 2014-2018 Farm Program Info - Enrolled into Agricultural Risk Coverage (ARC) County *This parcel is being split from a larger tract. FSA will recalculate bases attributed to each parcel after sale if parcels are sold separate. SOIL DESCRIPTION: Granby, Litchfield, Grogan, Clarion, Estherville, Fieldon, Storden, Dickinson, Estherville, Nicollet . See Soils Map.

CPI: Crop Productivity Index = 58.5

TOPOGRAPHY: Level to rolling

DRAINAGE: Private mains, substantial system tiling. See Tile Map.

NRCS CLASSIFICATIONS ON TILLABLE ACRES: Exempt from conservation compliance provisions. NHEL - Non-Highly Erodible Land

Property Information

WINGERT REALTY & LAND SERVICES, INC. stipulates that they are representing the seller exclusively in this transaction.

The information gathered for this brochure in its entirety is from sources deemed reliable, but cannot be guaranteed by Seller, Wingert Realty & Land Services, Inc., or its staff. Package is subject to prior sale, price change, correction or withdrawal. The buyer must make their own independent investigation of the property. The buyer is purchasing the property “as is”.

Tile Map

Tile lines supplied by seller.

This tile map is an approximation.Wingert Realty & Land Services, Inc. does not guarantee tile maps, footage, tile condition, location, size, grade or depth.

Soils Map

Soil Descriptions

GRANBY SERIES - Soil # 178

The Granby series consists of very deep, poorly drained or very poorly drained soils formed in sandy outwash or sandy glaciolacus-trine deposits on outwash plains, lake plains, and glacial drainage-ways. Permeability is rapid. Slope ranges from 0 to 3 percent. Mean annual precipitation is about 35 inches, and mean annual temperature is about 50 degrees F

TYPICAL PEDON: Granby loamy sand, on a 1 percent slope in a cultivated field at an elevation of 624 feet.

GEOGRAPHIC SETTING: The Granby soils are on outwash plains, lake plains, and glacial drainageways. The soils formed in sandy outwash or sandy glaciolacustrine deposits. Slope gradients range from 0 to 3 percent. Mean annual precipitation ranges from 30 to 42 inches, mean annual temperature ranges from 48 to 53 degrees F., frost-free period ranges from 130 to 180 days, and elevation ranges from 600 to 1,150 feet above sea level.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Chelsea, Gilford, Oakville, Pipestone, Spinks, Tedrow, and Wat-seka soils, and the competing Gumz soils. The excessively drained Chelsea and Oakville soils and the well drained Spinks soils are on nearby beach ridges and moraines. The poorly drained or very poorly drained Gilford and Gumz soils are on similar landforms. The some-what poorly drained Pipestone soils are associated with Granby soils at the northern extent of its range and are on swells. The somewhat poorly drained Tedrow and Watseka soils are on higher positions on the landscape.

DRAINAGE AND PERMEABILITY: Poorly drained or very poorly drained. The potential for surface runoff is negligible. Perme-ability is rapid. Depth to an apparent seasonal high water table ranges from 1 foot above the surface to 1 foot below the surface for some time in normal years.

LITCHFIELD SERIES - Soil # 181, 946 Complex

The Litchfield series consists of very deep, moderately well drained soils that formed in glacio-fluvial deposits on outwash plains, ter-races, or deltas. Permeability is moderately rapid or rapid. Slopes range from 0 to 3 percent. Mean annual temperature is 48 degrees F. Mean annual precipitation is 28 inches.

TYPICAL PEDON: Litchfield loamy fine sand in a bromegrass pasture.

GEOGRAPHIC SETTING: These soils are on nearly level to gently sloping outwash plains, stream terraces or deltas. Slopes range from 0 to 3 percent. The soils formed mostly in sandy glacio-fluvial deposits that have finer textured layers. These materials generally range from 5 to 10 feet thick and overlie medium textured drift or lacustrine deposits and are late Wisconsinan in age. Mean annual precipitation is 26 to 30 inches. Mean annual temperature is 45 degrees to 50 degrees F. Frost free days range from 124 to 165. El-evations above sea level range from 700 to 1400 feet.

GEOGRAPHICALLY ASSOCIATED SOILS: The most com-mon associated soils are the Darfur, Dassel and Sparta soils. The poorly drained Darfur soils are on flats. The very poorly drained Dassel soils are in depressions. The excessively drained Sparta soils are on more sloping positions and/or are on higher lying terrain.

DRAINAGE AND PERMEABILITY: Moderately well drained. Permeability is moderately rapid or rapid. Surface runoff is slow.

GROGAN SERIES - Soil # 128

The Grogan series consists of deep, well and moderately well drained soils that formed in calcareous silty lacustrine sediments on glacial lake plains. These soils have moderately rapid permeability. They have slopes with gradient of 0 to 15 percent. Mean annual precipita-tion is about 26 inches, and mean annual temperature is about 47 degrees F.

TYPICAL PEDON: Grogan silt loam with a 3 percent convex east-facing slope on a delta in a glacial lake plain in a cultivated field.

GEOGRAPHIC SETTING: These soils have plane or convex slopes with gradients of 0 to 15 percent primarily in deltaic portions of glacial lake plains. They formed in calcareous, silty lacustrine sedi-ments of the Des Moines lobe of the Late Wisconsinan glaciation. Mean annual temperature is 45 to 48 degrees F, and mean annual precipitation if 24 to 30 inches.

GEOGRAPHICALLY ASSOCIATED SOILS: The Grogan soils are the dominant soils in their area of occurrence. The poorly drained Darfur soils and the somewhat poorly drained Yahara soils are associated in a few places. These soils formed in somewhat similar sediments.

DRAINAGE AND PERMEABILITY: Well or moderately well drained. Surface runoff is slow to medium. Permeability is moder-ately rapid.

CLARION SERIES - Soil # 102B, 920D Complex, 920B Complex

The Clarion series consists of very deep, well drained, moderately permeable soils formed in glacial till on uplands. Slopes range from 1 to 9 percent. Mean annual air temperature is about 47 degrees F. Mean annual precipitation is about 29 inches.

TYPICAL PEDON: Clarion loam on a convex upland slope of 4 percent gradient - in a cultivated field.

GEOGRAPHIC SETTING: Clarion soils typically are on convex slopes in the relatively undissected, gently undulating to rolling Late Wisconsin till plain. The topography is hilly in some places. Slopes commonly are short and irregular with gradients typically from 2 to 5 percent but range from 1 to 9 percent. The soils formed in calcareous glacial till of the Des Moines Lobe advance. Mean annual air tem-perature is 45 to 50 degrees F. Mean annual precipitation is 27 to 32 inches. Annual frost free days range from 120 to 180 days. Elevation above sea level ranges from 700 to 1400 feet.

Soil Descriptions

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Nicollet, Omsrud, Storden, and Webster series. Nicollet and Webster soils, which form a drainage sequence with Clarion soils, are the most common associates in undulating to gently rolling landscapes. Oms-rud and Storden soils are often associated in rolling or hilly land-scapes and are on the steeper or more strongly convex slopes. Storden soils do not have a cambic horizon free of carbonates and Omsrud soils do not have saturation in the lower part of the profile.

DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is medium. Permeability is moderate. The seasonal high water table is at depths of 4 to 6 feet during November to July in most years.

ESTHERVILLE SERIES - Soil # 920D Complex, 920BComplex

The Estherville series consists of very deep, somewhat excessively drained soils that formed in glacial outwash sediments, which consist of a loamy mantle and underlying sandy and gravelly sediments. They are on outwash plains, stream terraces, valley trains, and kames. They have moderately rapid permeability in the upper part and rapid or very rapid permeability in the underlying sediments. Slopes range from 0 to 70 percent. Mean annual precipitation is about 28 inches. Mean annual temperature is about 46 degrees F.

TYPICAL PEDON: Estherville sandy loam with a plane slope of about 1 percent on a glacial outwash plain in a cultivated field.

GEOGRAPHIC SETTING: Estherville soils have plane or convex slopes ranging from 0 to 70 percent. They formed in sandy and grav-elly outwash on broad outwash plains, stream terraces, valley trains, and on kames in glacial moraines. Mean annual temperature is about 45 to 55 degrees F. Mean annual precipitation is about 25 to 36 inches. The frost free days range from 124 to 190. Elevation above sea level ranges from 700 to 1600 feet.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hawick, Linder, Biscay, and Mayer soils The excessively drained Hawick soils primarily are on steeper slopes. The somewhat poorly drained Linder soils are on nearby lower lying or less sloping terrain. The poorly drained Biscay and Mayer soils are on nearby lower lying terrain. The Salida, Cylinder, Hanska, Lemond, and Talcot soils are associates in some places.

DRAINAGE AND PERMEABILITY: Estherville soils are some-what excessively drained. Runoff is very low to medium. Permeability is moderately rapid in the upper part and rapid or very rapid in the lower part.

FIELDON SERIES - Soil # 160

The Fieldon series consists of deep, poorly drained soils that formed in loamy and sandy glacial outwash or deltaic sediments on glacial lake and outwash plains. These soils have moderate and moderately rapid permeability in the upper part and rapid permeability in the

lower part. Their slopes are less than 2 percent. Mean annual pre-cipitation is about 28 inches, and mean annual temperature is about 48 degrees F.

TYPICAL PEDON: Fieldon loam with a plane level slope on a delta in glacial lake plain in cultivated field.

GEOGRAPHIC SETTING: These soils have plane to slightly convex slopes with gradients of less than 2 percent primarily on the deltaic portions of glacial lake plains. They are on a few outwash plains. The Fieldon soils formed in loamy and sandy lacustrine or outwash sediments that are dominated by fine and very fine sand and that are commonly stratified. Loamy glacial till or silty lacustrine sediments commonly underlie these sediments at depths ranging from 40 to 120 inches. These sediments are of the Des Moines lobe of the Late Wiscon-sinan glaciation. Mean annual precipitation is 26 to 30 inches, and mean annual temperature is 45 to 48 degrees F.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Dassel, Darfur, and Grogan soils which formed in sediments similar to those of the Fieldon soils and which are in a drainage sequence with the Fieldon soils. The very poorly drained Dassel soils are in depressions and swales. The poorly drained Darfur soils are on ter-rain that is similar to that of the Fieldon soils. The moderately well and well drained Grogan soils are on slight rises. The moderately well and somewhat poorly drained, sandy Litchfield soils and the somewhat excessively drained, sandy Lasa soils are associated in some places.

DRAINAGE AND PERMEABILITY: Poorly drained. Surface runoff is slow. Permeability is moderate and moderately rapid in the upper part and rapid in the lower part.

STORDEN SERIES - Soil # 961

The Storden series consists of very deep, well drained soils that formed in calcareous loamy glacial till on glacial moraines. These soils have moderate permeability. Slopes range from 4 to 70 percent. Mean annual precipitation is about 26 inches. Mean annual air tem-perature is about 48 degrees F.

TYPICAL PEDON: Storden loam with an 8 percent convex slope on a ground moraine in a cultivated field.

GEOGRAPHIC SETTING: These soils have convex slopes with gradients of 4 to 70 percent. They are on glacial moraines. They formed in calcareous loamy Des Moines Lobe glacial till of Late Wisconsinan Age. Mean annual air temperature ranges from 45 to 50 degrees F. Mean annual precipitation ranges from 25 to 32 inches. Frost free days ranges from 124 to 165. Elevation ranges from 700 to 1600 feet.

Soil Descriptions

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Swanlake, Clarion, Omsrud, Nicollet, Delft and Webster soils. The well drained Swanlake soils have a mollic epipedon. The well drained Clarion and Omsrud soils have a mollic epipedon and are not calcar-eous in the upper part. Delft and Webster soils are poorly drained and on footslopes and swales. Nicollet soils are on lower summits or sideslope positions and are somewhat poorly drained.

DRAINAGE AND PERMEABILITY: Well drained. Surface runoff is moderately slow to very high. Permeability is moderate.

DICKINSON SERIES - Soil # 27B

The Dickinson series consists of very deep, well drained soils formed in glacial or alluvial deposits that have been reworked by wind on uplands and stream terraces. Permeability is moderately rapid in the upper part and rapid in the lower part. Slopes range from 0 to 30 per-cent. Mean annual temperature is about 50 degrees F. Mean annual precipitation is about 31 inches.

TYPICAL PEDON: Dickinson fine sandy loam with a convex slope of 3 percent - cultivated.

GEOGRAPHIC SETTING: Dickinson soils are on convex slopes of the uplands and to a lesser extent on stream terraces and outwash areas. Slopes range from 0 to 30 percent. Dickinson soils formed in moderately coarse-textured glacial or alluvial sediments reworked by wind. Differences in texture in the material with depth are related to sorting of material rather than soil development. Mean annual tem-perature ranges from 47 to 54 degrees F. Mean annual precipitation ranges from 25 to 34 inches. Frost free days range from 145 to 180. Elevations above sea level range from 600 to 1500 feet.

GEOGRAPHICALLY ASSOCIATED SOILS: In the uplands they are on landscapes with Clarion, Kenyon, Ostrander, Ocheye-dan, and Fostoria soils. These soils contain less sand in the subsoil and substratum. Near major stream valleys the loess-derived Tama, Marshall, Sharpsburg, and Otley soils are adjacent to small areas of Dickinson soils. These loess-derived soils have a lower sand content and contain more clay in the solum than Dickinson soils. They are associated with the Sparta soils and the Lamont soils on uplands and on stream terraces. Other associated soils on terraces are the Dakota and Waukegan soils. Dickinson soils form a biosequence with the Lamont soils. Dakota and Waukegan soils have sand and gravel at depths less than 40 inches. Lamont, Dakota, and Waukegan soils are on similar landscape positions or at slightly lower elevations than the Dickinson soils. Sparta soils tend to be at slightly higher elevations.

DRAINAGE AND PERMEABILITY: Well drained. Runoff is medium. Permeability is moderately rapid in the upper part and rapid in the substratum.

NICOLLET SERIES - Soil # 946 Complex

The Nicollet series consists of very deep, moderately well and some-what poorly drained soils that formed in calcareous loamy glacial till on till plains and glacial moraines. These soils have moderate permeability. Their slopes range from 0 to 5 percent. Mean annual precipitation is about 28 inches. Mean annual temperature is about 48 degrees F.

TYPICAL PEDON: Nicollet clay loam on a 2 percent plane slope in a cultivated field.

GEOGRAPHIC SETTING: Nicollet soils have slightly convex or plane slopes. They are on till plains, ground moraines, and terminal moraines. Their slopes range from 0 to 5 percent. They formed in friable, calcareous loam and clay loam glacial till of Late Wisconsinan age. The climate is humid continental with warm summers and cold winters. Mean annual temperature ranges from 45 to 55 degrees F. Mean annual precipitation ranges from 26 to 32 inches.

GEOGRAPHICALLY ASSOCIATED SOILS: These are the Canisteo, Clarion, Glencoe, Okoboji, Storden, Swanlake, and Webster soils which are members of a hydrosequence with Nicollet soils. The well drained Clarion, Storden and Swanlake soils are generally on the more convex slopes and higher in the landscape. Poorly drained Can-isteo and Webster soils are on broad nearly level areas. Very poorly drained Glencoe and Okoboji soils are in depressions and swales.

DRAINAGE AND PERMEABILITY: Moderately well and somewhat poorly drained. Permeability is moderate. Runoff is slow.

Property PhotosEast side facing south.

East side facing southwest.

East side looking northwest.

East side looking north.

Photos taken 6/2018

Property PhotosSouthwest corner looking east.

Southeast corner looking west.

Overflow intake near bern east edge of farm.

East side of farm, berm to control erosion along creek.

Photos taken 6/2018

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Additional Notes

WINGERT REALTY & LAND SERVICES, INC.Serving Minnesota and Northern Iowa

Mankato Office: Toll Free 800-730-LAND (5263) • Local 507-345-LAND (5263) www.WingertRealty.com

All are licensed MN REALTORS®

THE LAND REPORT, the magazine of the American Landowner, has named Wingert Realty & Land Services, Inc.

“America’s Best Brokerages” 2010-2016 and “Top Auction Houses” 2011-2016 in the U.S.A.!

Auctioneer # 07-18-01

Charles Wingert, alC Past national President of realtors land institute (2013)Broker Direct Line: 507-381-9790Charles@WingertRealty.com

Auctioneer # 07-16-10

darrell hylen, alC Real Estate Sales & Lease Negotiation Direct Line: 507-381-3843Darrell.Hylen@WingertRealty.com

Redwood Falls Office: 507-637-8178riChard hauge, alC & araReal Estate Sales & Appraisals Direct Line: 507-829-5227Rick@WingertRealty.com

Auctioneer # 64-002

david hanson Real Estate Sales Direct Line: 507-525-7510 David@WingertRealty.comAuctioneer # 07-17-09

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