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This is the complete list of all Homes for Sale on Biron Flowage WI!
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Wisconsin Hobby Farms & Horse Properties For Sale
There are several inquiries for Hobby Farm and Horse Listings in Wood. Wisconsin has zoning laws when it comes to horses. As a result, if you wish to have horses upon the property, you’ll want to be positive to locate a estate that is zoned for horses. Some of these Properties may have stalls, arenas, pastures, etc. Some may be zoned for horses but not have all of these items. Search our Horse Property & Equestrian Real Estate Buyer’s Guide
Wisconsin Hunting Land For Sale
Check out our Wisconsin Hunting Land Portal! Updated instantly, it is the total hunting land for sale for Wisconsin portal!
Wisconsin School Districts Properties For Sale
Interested in purchasing a property in a particular school district? See our Homes for Sale by School District!
Homes for Sale on Biron Flowage
Homes for Sale on Biron Flowage is your only portal for real time property information about Homes for Sale Biron Flowage and listings for sale in Wood County. Listings including Homes for Sale on Biron Flowage WI are updated in real time with direct feed from the MLS. Even if you are looking for that one special Homes for Sale Biron Flowage WI! You can also create your own specialized searches to include Homes for Sale on Biron Flowage or contact us to setup your customized search and have new Biron Flowage WI homes for sale listings sent to you instantly!
At Realty Solutions Group, we are committed and experienced real estate professionals, dedicated to giving truly exceptional care and service. We are a full service real estate brokerage helping buyers and sellers with the purchase and selling of homes, land, condominiums, commercial properties in Wood County and across Wisconsin. Let us demonstrate you how we can help![su_divider]
Wood County has a 19-member board of supervisors, each supporter 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 home 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 portion of the county is in the Northern Highlands, with mostly rich cropland subsequent to 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 about 120 feet as it flows through the county, driving several skill dams. The remainder of the county is drained by smaller streams and rivers, punctuated by solitary hills next Powers Bluff.
The flat, sandy southern third of the county was largely shaped by the last glacial advance. The ice didn’t accomplish Wood County, but it approached from the east into Portage County and butted up neighboring the Baraboo Hills to the south. This blocked the Wisconsin River, damming it hence 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 share of the county. This Place is generally flat and marshy now because meltwater rivers from the glacier and streams from home to the north carried sand and silt out into the glacial lake, where the sediment granted beneath its yet waters. After the glacial dam melted tolerable to drain Glacial Lake Wisconsin around 13,000 years ago, the Wisconsin River clip new channels through the lake-bottom sands in the southeast corner of the county. In a later teetotal 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 version 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 serene 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 close Medford.
Much of the county except for the northeast corner is underlain by a layer of Cambrian sandstone, formed long since the last ice age. Most of the native sandstone growth 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 vary from the sandstone bluffs, much older, with a difficult core of Precambrian quartzite and a pinnacle of chert. A marker on the bluff says it is a “worn down peak of an ancient mountain range which similar to covered northern Wisconsin.”