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Wisconsin State Soil Antigo Silt Loam

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Introduction

Many states have a designated state bird, flower, fish, tree, rock, etc. And, many states also have a state soil – one that has significance or is important to the state. Antigo Silt Loam is the official state soil of Wisconsin. Let’s explore how Antigo is important to Wisconsin.

History

Antigo Silt Loam was named the official state soil of Wisconsin by the State Legislature in 1983, a declaration intended to remind us of the importance of our soil resources. The person instrumental in the process was Dr. Francis D. Hole, soil science professor at the University of Wisconsin in Madison. He Antigo Silt Loam - Wisconsin State Soil logolobbied heavily for a state soil and even made a state soil seal and wrote a song about the Antigo Silt Loam! Antigo is named for the nearby city of Antigo, WI in Langlade County where it was first mapped in 1947. A historical marker is located northeast of Antigo on Highway 52.

It was selected to represent the more than 800 different soils in Wisconsin. It is a productive, well-drained soil with a light-colored surface layer developed under northern hardwood forests. These soils formed in silty material underlain by sand and gravel on glacial outwash plains and versatile soil, supporting mainly dairy, potato, and timber production.

 

“Soil is the hidden, secret friend, which is the root domain of lively darkness and silence.” Francis D. Hole

What is Antigo Soil?

Thousands of years ago, glaciers spread across the Midwest. The last of which is referred to as the Wisconsin Glaciation. When these last glaciers melted around 11,000 years ago they left behind all the mineral debris they had picked up while forming. Sand and gravel from the melting glaciers spread across the land and this was the basis for the Antigo soil which you can still see today in the subsoil (below the surface soil). Found above this sandy horizon, is a layer of clay and silt they blew over the exposed land surface and settled in Wisconsin. Strong winds and glacial meltwaters deposited 2 to 3 feet of silty loess and loamy outwash on top of the sand and gravel. Soil development, under northern hardwood forests, produced an organic enriched surface layer and a clay enriched subsoil. Plants and trees began to grow in the area eventually expanding into great forests. In forests, dead leaves, plants, and other organic matter tend to build up on the surface of the soil. This makes rain slightly acidic as it enters the soil which makes the horizon below the organic matter lighter in color.

A Prime Agricultural Soil, Antigo occurs mostly on nearly level ground, suitable for agriculture.  The organic enriched surface layer provides an excellent seedbed and good tilth. The silty upper layers hold plenty of nutrients and water for plant growth. The underlying sand and gravel layers allow for good drainage. These factors, combined with a favorable climate, make Antigo a Prime Farmland soil, one of the most productive agricultural soils in north central Wisconsin.

Publications

Antigo Soil Profile

 

 

 

 

 

 

 

 

Antigo Silt Loam Song

Francis Hole, former UW Professor of soil science wrote the Antigo Silt Loam song.

Click here to view it full size. Click on the tabs below and explore spatial and tabular data related to Antigo Silt Loam.
These data are based on snapshots of the SSURGO and KSSL databases, as part of the SoilWeb system. Official versions of these data should be consulted for the most up-to-date soils information.