27.08.2013 Views

Jefferson County - East-West Gateway Coordinating Council

Jefferson County - East-West Gateway Coordinating Council

Jefferson County - East-West Gateway Coordinating Council

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

4<br />

<strong>Jefferson</strong> <strong>County</strong> – Section 1<br />

predominantly limestone and cherty limestone. The limestone weathers easily and<br />

produces deep cherty soils (in the northeastern part of the county). The Pennsylvanian<br />

system consists of reddish-brown sandstone and bluish-gray to purple shale found in<br />

sinkholes and vertical bedrock joints. Geologic units consist of flat to gently dipping<br />

bedrock dominated by dolostone, sandstone and limestone formations. Northwestsoutheast<br />

trending folds and faults where bedrock dip is over ten degrees has altered a<br />

slight regional dip of one to two degrees to the northeast. Several zones of high angle<br />

faults that are downthrown are considered to be extensions of the Ste. Genevieve Fault<br />

System. They are the Crystal City anticline, the Plattin Creek anticline, the Roselle<br />

lineament, the Rugley School fault block, the Summit Park structure and the Valles Mines-<br />

Vineland fault zone. A structure known as the Eureka-House Springs anticline has been<br />

traced from the Mississippi River to near Wright City (McCracken, 1971). The potential for<br />

landslide or slump occurs in areas of the Maquoketa and Warsaw shales. Sinkholes are<br />

numerous in the Kimmswick limestone. Refer to Figure J3 below.<br />

FIGURE J3 GEOLOGIC MAP OF MISSOURI<br />

Source: Missouri Department of Natural Resources<br />

Soils - There are a total of six soil associations in <strong>Jefferson</strong> <strong>County</strong> including the Haynie-<br />

Tice-Waldron Association, the Sonsac-Useful Association, the Wrengart-Goss Association,<br />

the Menfro-Gasconade Association, the Minnith-Pevely Association, and the Haymond-<br />

Freeburg-Horsecreek-Bloomdale Association.<br />

The Haynie-Tice Waldron Association includes zero to two percent slopes, formed in<br />

Mississippian River alluvium. It covers one percent of the county and is present mainly on<br />

natural levees, bottomlands and old meanders. It consists of 48 percent well drained<br />

Haynie soils (silty loam), 29 percent somewhat poorly drained Tice soils (silty loam), 20<br />

percent somewhat poorly drained Waldron soils (silty loam) and three percent minor soils.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!