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This is the complete list of all Homes for Sale on Centralia Flowage WI!
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Wisconsin Hobby Farms & Horse Properties For Sale
There are several requests for Hobby Farm and Horse Listings in Wood. Wisconsin has zoning restrictions when it comes to horses. As a result, if you plan to have horses upon the property, you’ll want to be certain to locate a estate that is zoned for horses. Many of these Properties may have stalls, arenas, pastures, etc. Some may be zoned for horses but not have all of these features. Search our Horse Property & Equestrian Real Estate Buyer’s Guide
Wisconsin Hunting Land For Sale
See our Wisconsin Hunting Land Portal! Updated hourly, it is the complete hunting property for sale in Wisconsin portal!
Wisconsin School Districts Homes For Sale
Looking in purchasing a home in a certain school district? See our Homes for Sale by School District!
Homes for Sale on Centralia Flowage
Homes for Sale on Centralia Flowage is your one stop place for current property information about Homes for Sale Centralia Flowage and listings for sale in Wood County. Listings including Homes for Sale on Centralia Flowage WI are updated instantly with direct feed from the MLS. Even if you are looking for that one special Homes for Sale Centralia Flowage WI! You can also create your own specialized searches including Homes for Sale on Centralia Flowage or reach out to us to create your customized search and have new Centralia Flowage WI homes for sale listings emailed to you instantly!
At Realty Solutions Group, we are committed and seasoned real estate professionals, dedicated to providing truly exceptional care and service. We are a full service real estate agency assisting buyers and sellers with the buying and sale of properties, land, condominiums, commercial properties in Wood County and across Wisconsin. Allow us to show you what we can do![su_divider]
Wood County has a 19-member board of supervisors, each believer representing a district.
According to the U.S. Census Bureau, the county has a total area of 809 square miles (2,100 km2), of which 793 square miles (2,050 km2) is house and 16 square miles (41 km2) (2.0%) is water. The geographic center of Wisconsin is in Wood county, nine miles southeast of Marshfield.
Wood County spans two of Wisconsin’s five geographical regions. The northern allowance of the county is in the Northern Highlands, with mostly rich cropland gone heavy clay soil, used for corn, soybeans, hay and dairy. In the northwest corner the Marshfield moraine runs from Marathon County through Marshfield, Bakerville and Nasonville into Clark County. The south and central areas from Babcock through Cranmoor and Wisconsin Rapids are in the Central Plain, flat and marshy – one of the major cranberry-producing centers of the United States. The Wisconsin River cuts across the southeast corner, a corridor of sand flats, islands and oxbows. The river falls nearly 120 feet as it flows through the county, driving several capacity dams. The remainder of the county is drained by smaller streams and rivers, punctuated by only hills next Powers Bluff.
The flat, sandy southern third of the county was largely shaped by the last glacial advance. The ice didn’t achieve Wood County, but it approached from the east into Portage County and butted up against the Baraboo Hills to the south. This blocked the Wisconsin River, damming it as a result that it backed up, forming Glacial Lake Wisconsin, a frigid lake that stretched from the Baraboo Hills north to the sites of Babcock and Wisconsin Rapids, submerging that allocation of the county. This area is generally flat and marshy now because meltwater rivers from the glacier and streams from house to the north carried sand and silt out into the glacial lake, where the sediment established beneath its still waters. After the glacial dam melted ample to drain Glacial Lake Wisconsin vis-Ð°-vis 13,000 years ago, the Wisconsin River cut new channels through the lake-bottom sands in the southeast corner of the county. In a later dry period, wind blew the sand into dunes. One dune in the town of Saratoga is eight meters thick. Later still, the area became wet and peat formed in places upon top of the sand. The first surveyors in 1852 found a great marsh, like a Wisconsin Everglades. Here is their story of what is now Cranmoor:
The north of the county was shaped by earlier glaciers, which deposited glacial till, the basis for the stifling soil there. The Marshfield moraine in the northwest corner is probably a terminal moraine from one of these earlier glaciers, or from a series of them. Its age is unclear, but its relatively mild surface indicates that it has eroded for a much longer become old than the choppy terminal moraines left 13,000 years ago, like the Perkinstown moraine near Medford.
Much of the county except for the northeast corner is underlain by a buildup of Cambrian sandstone, formed long before the last ice age. Most of the native sandstone addition has been eroded away and the remainder is usually buried below glacial till, but it can be seen in gravel pits and a few bluffs. The Lindsey bluffs (a.k.a. the Marshfield School Forest) and Birch Bluff and South Bluff in the Town of Remington are difficult spots in this sandstone which have resisted erosion.
Powers Bluff is alternative from the sandstone bluffs, much older, with a hard core of Precambrian quartzite and a summit of chert. A marker upon the bluff says it is a “worn down zenith of an ancient mountain range which behind covered northern Wisconsin.”