Water Protection Program
Division of Environmental Quality
P.O. Box 176
Jefferson City, MO 65102-0176
United States
Water Protection Program
fact sheetDivision of Environmental Quality
Director: Kyra MooreThe present course of the Missouri was formed about 115,000 years ago when streams flowing eastward from the Rocky Mountains encountered the western edge of the Illinoisan ice sheet. These streams were diverted southward until the southern edge of the glacier was reached near present day Kansas City. From there, the river flowed east along the southern border of the glacier, through what is now central Missouri.
From Three Forks, Montana, to St. Louis, the river is 2,300 miles long.
Eighty-seven percent of the basin’s 338.5 million acres was originally prairie. The floodplain of the Missouri and its tributaries were a mixture of grasslands, forests and wetlands.
The river was filled with islands, side channels flowing around islands, quiet backwaters and marshes, as well as the main channel of the river. Today’s river has a nine-foot navigation channel, and at 1,000 feet wide, is roughly half the width it used to be before it was channelized.
Prior to upstream reservoir construction, the Missouri River experienced two general periods of high water. The first, often referred to as the March rise, was caused by snow melt on the plains and the break-up of ice in the main channel and tributaries. The second, called the June rise, resulted from run-off of melting mountain snow and rainfall throughout the basin. The reservoirs were constructed to help minimize the frequent downstream flooding from these rises.
The natural spring rises in river flow often flooded nearby land. The flood waters deposited sediments rich in organic matter. This increased productive plant communities along the river, particularly marshes that produced huge quantities of insects and other small invertebrate animals that served as important food supplies for fish and waterfowl, including ducks and geese.
The first formal exploration of the Missouri River by Lewis and Clark. They saw the value of the river as a convenient avenue of travel into the Great Plains and Rocky Mountains that would help increase fur trading with the American Indians.
Together with the removal of snags, the loss of good habitat has caused an estimated loss of more than 80% of the fish in the river. Changes in habitat and increased water clarity due to the trapping of sediments in the main stem reservoirs has caused an increase in the numbers of species such as skipjack herring, gizzard shad, white bass, bluegill, white crappie and the emerald, river and red shiners. In Missouri, two large river species, the pallid sturgeon and the flathead chub, are in serious decline. In Nebraska, serious declines in seven species of minnow, burbot and sauger have occurred. If trends continue, some of these species may become lost from the Missouri River system. The loss of fish species signifies damage to the river’s ecosystem.
Changes in the river have been accompanied by land use changes as well, particularly on the channelized lower river. Between 1892 and 1982 on floodplain land between Sioux City, Iowa, and St. Louis, cultivated land increased 4300%, while tree cover declined 41%, wetlands declined 40%, sandbars declined 97%, and grasslands declined 12%.
Channelization and dam building have greatly changed the Missouri River. Today, 67% of the Missouri is either channelized for navigation (650 miles) or impounded by dams (903 miles). Most of the remaining free-flowing portions of the river are near the headwaters in Montana. Channelization has resulted in the lower river being about 50% narrower. Most of that loss in width has been in the more biologically productive off-channel backwaters and marshes.
The Missouri Department of Natural Resources does not recommend swimming in the Missouri River. Because of the strong current, the state does not recognize swimming as a protected use of the Missouri River, and wastewater discharges to the river are not required to disinfect. The river has higher bacterial counts than most other surface waters in Missouri, and these higher levels present an increased health risk to those who do swim in the Missouri River.
Although the pesticides DDT, dieldrin and chlordane have been banned from use in the United States, some of their residues are still found in Missouri River fish. While most residues are not in quantities considered harmful, the Missouri Department of Health has advised that no one consume sturgeon caught in the Missouri River due to chlordane and PCBs found in them. The Department of Health has also advised the public to limit consumption of carp, catfish, suckers and buffalo to one pound per week.
There have been several water quality concerns expressed over the use of Missouri River water in the past 200 years. Mark Twain noted when a drinking glass was filled in the river, only about half the glass contained water. The rest was sediment, reflecting the river’s nickname, the Big Muddy. Twain said some people would let the glass set awhile and drink just the water but that most people took the two together. A more serious problem before adequate water treatment was waterborne diseases, such as typhoid. Many river travelers and residents of towns along the river died of typhoid fever after drinking Missouri River water.
River due to chlordane and PCBs found in them. The Department of Health has also advised the public to limit consumption of carp, catfish, suckers and buffalo to one pound per week.
The Missouri Department of Natural Resources recommends that you do not drink untreated water from any surface water, especially an unprotected river, lake, stream or creek. This is because surface water that is used as a drinking water supply is generally treated, including disinfecting, with chlorine before the water is safe for people to drink. This treatment process protects humans against bacteria and other chemical contaminants that might enter an unprotected river, lake, stream or creek. A popular agricultural herbicide, atrazine, is detected frequently in the Missouri River, although not at levels that pose a significant health threat.
Mean annual levels of atrazine in the Missouri River are less than one part per billion; the drinking water standard is three parts per billion. Even though extensive monitoring has shown that the atrazine levels on Midwestern rivers do not exceed drinking water standards, most drinking water suppliers provide extra treatment of drinking waters during spring and summer when atrazine levels are highest.
Yes. Today there are no serious chemical water quality problems on the Missouri River, although there is serious and historical degradation of aquatic habitat. The Missouri Department of Natural Resources is concerned with the management of watersheds of major tributaries and the possible need for additional water treatment to remove contaminants, such as parasitic protozoans like cryptosporidium and chemicals like atrazine. Because of our great reliance on the Missouri River as a drinking water supply, the Missouri Department of Natural Resources is dedicated to protecting and preserving this great natural resource.
Nothing in this document may be used to implement any enforcement action or levy any penalty unless promulgated by rule under chapter 536 or authorized by statute.
Division of Environmental Quality
P.O. Box 176
Jefferson City, MO 65102-0176
United States