This form provides that any Party may propose that geoscience operations be conducted on the Contract Area lands. The Party wishing to conduct geoscience operations shall furnish the other Parties with an information notice which generally describes the proposed geoscience operation.
Mississippi Geoscience Operations on the Contract Area
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Multi-State
Control #:
US-OG-705
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Word;
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FAQ
The Upper Mississippi is defined by a range of limestone bluffs that were carved by water from melting glaciers at the end of the last ice age. As the glaciers melted, water stretched from bluff to bluff, forming a glacio-fluvial spillway (known as Glacial River Warren) that cut deeper and deeper into the landscape.
This forest tract on the Mississippi River contains a geologic formation known as Tower Rock. The Tower Rock Natural Area comprises about 32 acres of upland oak-pine and mixed hardwoods. Most of the Natural Area is on the Missouri bank of the Mississippi River.
The geology of Mississippi includes some deep igneous and metamorphic crystalline basement rocks from the Precambrian known only from boreholes in the north, as well as sedimentary sequences from the Paleozoic.
Geologically, the Mississippi embayment is a syncline which plunges to the south and whose axis generally parallels the Mississippi River. The syncline is filled with sedimentary rocks ranging in age from Jurassic to Quaternary and reaching a maximum thickness of about 18,000 feet in the southern part of the region.
Possibly the most recognized bedrock formation, and one that forms relatively flat-topped benches and mesas along the Mississippi River, is the Platteville Limestone (455-454 million years B.P.). In general, the Platteville is a light gray to buff tan, thinly bedded, dolomitic limestone.