GAURDIANSHIP REAL ESTATE AUCTION
Sat.....
217.4
Ac. VACANT
Directions: Located on St. Rt. 700 approx.
5.0 mi S. of
Wildlife
Conservancy, Timber, Agricultural, Recreation, Golf Course, or just room to
Relax!!
Property borders
Will be offered in 2 parcels alone and then put back
together and sold whichever way brings the most for the owner. Northern Parcel: Consists of PP# 32-072700
& 32-074201, totaling approx. 117.5 Ac. and a 50 ft. entrance on SR
700. Southern Parcel: Consists of PP#
32.072600 & 32-018330 approx 99.91 Ac. with approx. 725 ft. frontage on SR
700. Bids will be held and totaled on the two offerings and then the entire
217.4 Ac. will be offered.
Terms: Sold by the deed acreage times the price per
acre.
Sold by Order of Atty. Kathryn T. Joseph, Esq., Probate Court Guardian
FIRST QUALITY AUCTION &
REALTY,
Max K. Walton, Real Estate Broker
Auctioneers: The Waltons – Max & Mark
email: wauction@neo.rr.com
**** Note: All photos and maps on this website are taken from the Geauga County Auditor’s “Access Geauga” website and are approximations – They are not to be taken as exact representations. ****
Approximate Acreage for each Parcel
Rivers, Streams, Lakes, Ponds
Contours at 10ft & 2ft intervals
Map of Soils (map key of soil types listed below)
FcA--Fitchville
silt loam, 0 to 2 percent slopes
This
is a deep, nearly level, somewhat poorly drained soil on terraces and in basins
of former glacial lakes. Most areas are oblong, broad, or irregular in shape
and range from 10 to 200 acres in size.
Typically,
the surface layer is dark grayish brown, friable silt loam about 7 inches
thick. The subsoil is yellowish brown and dark yellowish brown mottled, friable
and firm silt loam and silty clay loam about 52 inches thick. The substratum to
a depth of about 69 inches is yellowish brown, friable silt loam.
Included
with this soil in mapping are small areas of moderately well drained Glenford
soils on slight rises and poorly drained Sebring soils in shallow depressions
and along drainageways. The included soils make up about 15 percent of most
areas.
A
water table is perched between depths of 12 and 30 inches in winter and spring
and during other extended wet periods. Permeability is moderately slow. Runoff
is slow. The root zone is deep and the available water capacity is high. The
subsoil ranges from very strongly acid to medium acid in the upper part and
strongly acid to neutral in the lower part.
In
most areas this soil is used as cropland. In drained areas it is well suited to
cultivated crops, hay, and pasture. Row crops can be grown year after year.
Planting is delayed in undrained areas. In undrained areas this soil can be
used for water-tolerant grasses and legumes for hay and pasture. Surface drains
help remove excess surface water and subsurface drains help lower the water
table. This soil is subject to crusting, compaction and hard clodding if
tillage or harvesting is done when the soil is wet. Using crop residue and
planting cover crops improve the content of organic matter and tilth and
increase water infiltration. Because of compaction, grazing should be limited
to periods when the surface is not soft and sticky.
The
soil is well suited to use as woodland. Species selected for planting should be
tolerant of some wetness. Logging and planting can usually be done during the
drier part of the year. Spraying, mowing or disking can reduce plant
competition.
This
soil is not well suited as a site for buildings, recreation uses and most
sanitary facilities because of the seasonal high water table, moderately slow
permeability and low strength. It is better suited to houses without basements
than to houses with basements. Storm sewers and ditches help lower the water
table. Drains at the base of footings and coatings on exterior basement walls
help prevent wet basements. Local roads can be improved by using artificial
drainage and suitable base material to reduce the damage from frost action and
improve soil strength. Play areas and walkways need drainage and in some cases
special surfacing.
This
soil is in capability subclass IIw and in woodland suitability subclass 2o.
Wa--Wabasha
silty clay loam, ponded
This
is a deep, nearly level, very poorly drained soil on flood plains. It is
subject to frequent flooding of long duration and is ponded much of the year.
The depth of the water fluctuates with the level of the Cuyahoga River. Slope
is 0 to 2 percent. Most areas are irregular in shape and range from 5 to 150
acres in size.
Typically,
the surface layer is very dark grayish brown and black, friable silty clay loam
about 8 inches thick. The subsoil is dark gray and gray, mottled, firm silty
clay loam about 37 inches thick. The substratum to a depth of about 65 inches
is light olive brown, mottled, firm silty clay. In some areas the surface layer
is silty clay or mucky silty clay loam. In a few areas organic material is in
the surface layer and the upper part of the subsoil.
Included
with this soil in mapping are small areas of Carlisle soils that formed in
organic material. Also included are small areas of Wallkill soils that have 16
to 40 inches of alluvium over muck. The included soil make up about 20 percent
of most areas.
The
water table is above and near the surface in fall, winter and spring.
Permeability is slow. The depth of rooting of most plants is related to the
depth to the water table. The available water capacity is high. The soil
puddles and clods easily. The shrink-swell potential is high. The subsoil is
slightly acid to mildly alkaline.
In
most areas this soil is used as woodland or pasture. This soil is poorly suited
to use as cropland and woodland. However, it is suited to habitat for wetland
wildlife. Ponding severely limits the use of planting and logging equipment.
Species selected for planting should be tolerant of ponding and flooding.
This
soil is unsuited as a site for buildings, sanitary facilities and recreation
uses. Ponding, flooding, slow permeability and high shrink-swell potential
severely limit this soil for these uses. Very few areas have been artificially
drained and it is difficult or impossible to locate suitable outlets for
drains.
This
soil is in capability subclass Vw and in woodland suitability subclass 5w.
Or--Orrville
silt loam, frequently flooded
This
is a deep, nearly level, somewhat poorly drained soil on flood plains. It is
frequently flooded for very brief to brief periods in fall, winter, and spring.
Slopes are 0 to 2 percent. Most areas are long and narrow and range from 5 to
120 acres.
Typically,
the surface layer is dark, grayish brown, friable silt loam about 6 inches
thick. The subsoil is about 25 inches thick. It is yellowish brown and grayish
brown, friable silt loam and loam that has mottles in the upper part. The
substratum to a depth of about 60 inches is gray, friable and loose fine sandy
loam, loamy fine sand, and gravelly loamy sand that has mottles in the upper
part.
Included
with this soil in mapping and making up about 15 percent of most areas are
narrow strips of poorly drained Holly and very poorly drained Wabasha soils in
slight depressions and old meander channels and well drained Tioga soils on
slight rises.
The
water table is between depths of 12 and 30 inches in winter and spring and
during other extended wet periods. Permeability is moderate. Runoff is slow.
The root zone is deep, and the available water capacity is high. Reaction is
strongly acid to slightly acid in the surface layer and subsoil, except where
lime has been added. The shrink-swell potential is low.
In
most areas this soil is used as pasture or woodland. Flooding and seasonal
wetness limit farming. Wetness delays planting and limits the choice of crops.
Undrained areas can be used for pasture, but maintaining tilth and desirable
forage stands is difficult. Drained areas are suited to row crops, corn for
example. Surface drainage can be used to remove excess surface water.
Subsurface drainage is also needed, but suitable outlets are difficult to
establish in some areas. Growing cover crops helps maintain the content of
organic matter and protect the surface during flooding.
This
soil is well suited to use as woodland. Species selected for planting should be
able to withstand flooding and be tolerant of some wetness. Seedlings grow well
if competing vegetation is controlled or removed by such practices as spraying,
mowing, or disking.
This
soil is unsuited as a site for buildings, septic tank absorption fields and
most recreation uses because of the flooding hazard and seasonal wetness.
During the drier part of the year this soil is suited to some recreation uses,
hiking, for example. The use of dikes to control flooding is difficult. Local
roads and streets can be improved by using fill to raise the road above the
flooding level and a suitable base material to reduce the damage from frost
action. Sloughing is a hazard in excavations.
This
soil is in capability subclass IIw and in woodland suitability subclass 2o.
OsB--Oshtemo
sandy loam, 2 to 6 percent slopes
This
is a deep, gently sloping, well-drained soil on outwash terraces and kames.
Most areas are irregular in shape and range from 3 to 25 acres in size.
Typically,
the surface layer is dark, grayish brown, friable sandy loam about 9 inches
thick. The subsoil is about 43 inches thick. The upper part is dark brown,
friable sandy loam; and the lower part is dark brown, firm sandy clay loam and
loose loamy sand. The substratum to a depth of about 66 inches is brown, loose
loamy sand and gravelly loamy sand. In some areas the surface layer is loam. In
a few areas the subsoil has more gravel and clay.
Permeability
is moderately rapid in the upper part of the subsoil and very rapid in the
substratum. Runoff is slow. The root zone is deep, and the available water
capacity is moderate or low. The surface layer and subsoil are commonly
strongly acid to slightly acid. The shrink-swell potential is low.
In
most areas this soil is used for cultivated crops. It is well suited to small
grains, hay, and early spring pasture. If the soil is irrigated, it is well
suited to cultivated and specialty crops. No-till or minimum tillage is a
suitable practice. Growth of pasture is slow in summer because the soil is
droughty. Deep-rooted plants, for example, alfalfa, make the best growth during
dry periods. Using crop residue, growing cover crops, and other management
practices conserve moisture, improve tilth, reduce erosion, and maintain the
content of organic matter. Because nutrients are moderately rapidly leached,
this soil generally responds better to smaller but more frequent, timely
applications of fertilizer than to one large application.
This
soil is moderately well suited to use as woodland. Machine planting of tree
seedlings is practical on this soil. Spraying, mowing or disking can reduce
plant competition. Species adapted to dry sites should be selected for
planting.
This
soil is well suited as a site for buildings, local roads and streets, and most
recreation uses. It is poorly suited to some sanitary facilities, especially
sewage lagoons and sanitary landfills, because of the possible contamination of
ground water. Sloughing is a hazard in excavations. There may be some
difficulty establishing a lawn because of the moderate or low available water
capacity. This soil is a probable source of sand.
This
soil is in capability subclass IIIs and in woodland suitability subclass 3o.
Wt--Willette
muck, ponded
This
is a deep, very poorly drained, level soil in bogs and swales on lake plains
and uplands. It is ponded much of the year and is subject to frequent flooding.
Slope is 0 to 2 percent. Most areas are oval and range from 3 to100 acres in
size.
Typically,
the surface layer is black, very friable muck about 10 inches thick. The next
layer is black, very friable muck about 12 inches thick. The substratum to a
depth of about 60 inches is gray, firm silty clay. In some areas a thinner
organic layer is above the mineral material and in other areas the organic
layer is thicker.
Included
with this soil in mapping and making up about 15 percent of most areas are
small areas of Wallkill and Canadice soils.
Water
is near the surface and ponds for long periods. Runoff is very slow.
Permeability is moderately rapid in the muck layers and slow in the substratum.
The content of organic matter is very high. The rooting depth of most plants is
related to the depth to the water table. The available water capacity is very
high. The subsoil is medium acid to mildly alkaline.
In
most areas this soil is in natural vegetation, including sedges and some water-tolerant
trees.
This
soil is poorly suited to farming because of the very poor natural drainage and
ponding. Both ditches and subsurface drains can be used to improve drainage;
however, in most areas drainage outlets are difficult to establish. Subsidence
or shrinkage occurs after draining. Controlling drainage so that the water
table can be raised or lowered helps reduce the amount of shrinkage. In drained
areas this soil is suited to some cultivated and specialty crops.
This
soil is poorly suited to use as woodland. In undrained areas the soil supports
some cattails, reeds, sedges and water-tolerant trees. The wetness seriously
limits the selection of trees to plant.
This
soil is unsuited as a site for buildings, sanitary facilities and most
recreation uses because of flooding, ponding, low strength and the slow
permeability and high shrink-swell in the substratum. In undrained areas the
soil provides good habitat for ducks, muskrats and other wetland wildlife.
This
soil is in capability subclass Vw. It is assigned to a woodland suitability
subclass.
Ca--Canadice
silt loam
This
is a deep, nearly level, poorly drained soil in basins of former glacial lakes.
It receives runoff from adjacent higher lying soils and is subject to ponding.
Most areas are irregular in shape and range from 5 to 200 acres in size. Slopes
are 0 to 2 percent.
Typically,
the surface layer is dark gray, friable silt loam about 10 inches thick. The
subsoil is gray and olive brown, mottled, firm silty clay about 30 inches
thick. The substratum to a depth of about 60 inches is light olive brown, firm
silty clay. Some areas in depressions have a very dark gray surface layer and
other areas have less clay in the subsoil and substratum.
Included
with this soil in mapping and comprising about 15 percent of most areas are
small areas of somewhat poorly drained Caneadea and Fitchville soils on slight
rises.
The
water table is perched near or above the soil surface in winter and spring and
during other extended wet periods. Runoff is very slow or ponded. Permeability
is very slow. The root zone is deep. The average water capacity is moderate or
high. The shrink-swell potential is moderate. The subsoil is medium acid to
neutral.
In
most areas this soil is used as woodland or pasture. In a few areas it has been
cleared and is used as cropland. Excessive wetness and very slow permeability
are major limitations for farming. These limitations commonly delay tillage.
Undrained areas can be used for hay and pasture but maintaining tilth and
desirable forage stands is difficult. Drained areas are suited to crops, hay
and pasture. The very slow internal water movement reduces the effectiveness of
subsurface drains. Outlets for subsurface drains are not available in many
areas. Surface drains can be used to remove surface water. This soil is subject
to crusting, compaction and hard clodding if tillage or harvesting is done when
the soil is wet. Using crop residue and planting cover crops increase water
infiltration and improve the content of organic matter and tilth.
The
soil is poorly suited to use as woodland. However, water-tolerant trees grow
well. Use of harvesting and planting equipment is limited during wet seasons.
Reforestation with desirable species is difficult because plant competition is
severe.
This
soil is poorly suited to use as a site for buildings, to recreation uses and to
use for most sanitary facilities because of prolonged wetness, the very slow
permeability and the amount of clay in the subsoil and substratum. Drainage can
be improved with surface drains, storm sewers and open ditches. Building sites
should be landscaped for good surface drainage away from foundations. Local
roads and streets can be improved by providing artificial drainage and a suitable
base material to increase soil strength. Play areas and walkways usually need
special surfacing.
This
soil is in capability subclass IVw and woodland suitability subclass 5w.
FIRST QUALITY AUCTION & REALTY,
Medina, OH (330) 416-3119
Max K. Walton, Real Estate Broker &
Auctioneer
email: wauction@neo.rr.com
