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The Evolution of the Lower Missouri River: National Mapping Discipline Research at Lisbon Bottom

Fact Sheet 126-01 (May 2002)


A color painting showing snages on the Missiori River.

Missouri River Snags by Karl Bodmer (1833-1834)

Introduction

Before 1800, the Missouri River was one of North America's most diverse and dynamic ecosystems.

During the past 200 years, civil engineering has transformed it into a navigation system regulated by reservoirs and confined by bank stabilization and flood control structures. These modifications have reduced seasonal flow variability and sediment load and have disconnected the river from backwater, off-channel, and floodplain habitats.

Flooding along the Lower Missouri River in 1993 and again in 1996 created a side-channel chute across Lisbon Bottom, a well-formed loop bottom near Glasgow, Mo.

The formation and subsequent development of the chute have provided USGS scientists with a glimpse of a preregulated Missouri River.

Knowledge of geologic characteristics and processes in an alluvial setting like Lisbon Bottom provides a scientific basis for floodplain management. This knowledge is also vital to a complete understanding of riverine habitat disturbance, recovery, and rehabilitation.

A critical component of this knowledge is an understanding of the spatial and temporal relationships between riverine habitats and geomorphic processes.


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A section of a color aerial photograph showing the river area.

February 2000 aerial photograph of Lisbon Bottom

Research Questions

This project addresses three specific questions regarding the Quaternary geology of the lower Missouri River Valley and the relationship between the geology of the valley and terrestrial habitat along the river:

  1. What is the Quaternary history of the lower Missouri River Valley?
  2. Can a general model of the lower Missouri River Valley alluvium be developed?
  3. What is the relationship between the valley's alluvial architecture and the hydrogeology of its wetlands?

Determining the architecture of the river's alluvium and the relationship between that architecture and the hydrology of the valley's wetlands will provide a more complete understanding of the relationship between the geology of the river valley and its terrestrial habitats. This will lead to a more complete understanding of habitat recovery and rehabilitation along the lower Missouri River.


More Information

Jeffrey Spooner
US Geological Survey
1400 Independence Road
Rolla, MO 65401
573-308-3526
jspooner@usgs.gov

Phyllis Altheide
US Geological Survey
1400 Independence Road
Rolla, MO 65401
573-308-3813
paltheide@usgs.gov

Information

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For additional information, visit the ask.usgs.gov Web site or the USGS home page at www.usgs.gov.


This document has undergone official review and approval for publications established by the National Mapping Discipline, U.S. Geological Survey. Some figures have been modified or added to improve the scientific visualization of information.


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