The USGS monitors flood and high-flow conditions at more than 300 streamgages across Montana and Wyoming. Water level and flow information are used by the National Weather Service (NWS) to make accurate flood forecasts. High-flow conditions are expressed as percentiles comparing current (within the past few hours) instantaneous flow to historical daily mean flow for all days of the year.
A percentile is a value on a scale of one hundred that indicates the percent of a distribution that is equal to or below it.
- "<95" indicates that the estimated streamflow is less than the 95th percentile for all days of the year,
- "95-98" indicates that the estimated streamflow is between the 95th and 98th percentiles for all days of the year,
- ">=99" indicates that estimated streamflow is greater than the 99th percentile, and
- "Not ranked" indicates that a flow category has not been computed. Common reasons for a "Not ranked" category are insufficient historical data or no current streamflow estimates.
Flood stages are determined by the NWS; not all USGS streamgages have flood stages. A depiction of other streamgages at or above flood stage is available the NWS River Conditions Map.

Current Flooding and High-Flow Conditions:
(Current-conditions data are provisional and subject to change)
Wyoming:
- Map: Flood and high flows
- Data table: Locations above flood stages
- Map: Current streamflow conditions vs historical streamflows
- Flood of August 1, 1985 in Cheyenne, WY
- Floods of May 1978 in southeastern Montana and northeastern Wyoming

Montana:
- Map: Flood and high flows
- Data table: Locations above flood stages
- Map: Current streamflow conditions vs historical streamflows
- Floods of May 1981 in west-central Montana
- Floods of May 1978 in southeastern Montana and northeastern Wyoming
- Floods of June 1964 in northwestern Montana
Video Transcript
How can a 100-year flood strike twice in 15 years? This is a downloadable poster discussing the meaning and use of probability language in flood characterization.
Poster: 100-Year Flood--It's All About Chance
Below are other science projects associated with floods and high-flows in Wyoming and Montana.
Black Hills Area Floods - 1921 to 1930
Black Hills Area Floods - 1961 to 1970
Black Hills Area Floods - 1931 to 1940
Black Hills Area Floods - 1901 to 1910
Black Hills Area Floods - 1941 to 1950
Black Hills Area Floods - 1951 to 1960
Black Hills Area Floods - 1911 to 1920
Black Hills Area Floods - 1971 to 1980
Black Hills Area Floods - 1877 to 1890
Black Hills Area Floods - 1891 to 1900
The 1972 Black Hills-Rapid City Flood
Below are data or web applications associated with floods and high-flows in Wyoming and Montana.
USGS Peak Streamflow Data
The National Water Information System (NWIS) is the USGS water data portal where you can find a wealth of historic and real-time data related to floods. The NWIS website also is where you can query peak streamflow data by station, state (Wyoming or Montana), or region.
FloodWatch - View flood and high-flow conditions.
The USGS FloodWatch website is a map-based resource from USGS WaterWatch that gives users hourly visual updates for flood conditions at over 3000 locations across the United States (Wyoming or Montana). Learn how to use FloodWatch.
Surface-water data for Wyoming
Real-time, daily, peak-flow, field measurements, and statistics of current and historical data that describe stream levels, streamflow (discharge), reservoir and lake levels, surface-water quality, and rainfall in Wyoming. Surface-water data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders.
Surface-water data for Montana
Real-time, daily, peak-flow, field measurements, and statistics of current and historical data that describe stream levels, streamflow (discharge), reservoir and lake levels, surface-water quality, and rainfall in Montana. Surface-water data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders.
Below are publications associated with floods and high-flows in Wyoming and Montana.
Montana StreamStats
The effects of Missouri River mainstem reservoir system operations on 2011 flooding using a Precipitation-Runoff Modeling System model
1976 Big Thompson flood, Colorado — Thirty years later
1976 Big Thompson flood, Colorado
Summary of significant floods in the United States and Puerto Rico, 1994 through 1998 water years
The world's largest floods, past and present: Their causes and magnitudes
Large floods in the United States: where they happen and why
Peak-flow characteristics of Wyoming streams
The National Flood Frequency Program, version 3 : a computer program for estimating magnitude and frequency of floods for ungaged sites
Water-surface profile and flood boundaries for the computed 100-year flood, lower Salt River, Lincoln County, Wyoming
Summary of significant floods in the United States, Puerto Rico, and the Virgin Islands, 1970 through 1989
Below are data or web applications associated with floods and high-flows in Wyoming and Montana.
Below are news stories associated with floods and high-flows in Wyoming and Montana.
Study Links Major Floods in North America and Europe to Multi-Decade Ocean Patterns
The number of major floods in natural rivers across Europe and North America has not increased overall during the past 80 years, a recent study has concluded. Instead researchers found that the occurrence of major flooding in North America and Europe often varies with North Atlantic Ocean temperature patterns.
- Overview
The USGS monitors flood and high-flow conditions at more than 300 streamgages across Montana and Wyoming. Water level and flow information are used by the National Weather Service (NWS) to make accurate flood forecasts. High-flow conditions are expressed as percentiles comparing current (within the past few hours) instantaneous flow to historical daily mean flow for all days of the year.
A percentile is a value on a scale of one hundred that indicates the percent of a distribution that is equal to or below it.
- "<95" indicates that the estimated streamflow is less than the 95th percentile for all days of the year,
- "95-98" indicates that the estimated streamflow is between the 95th and 98th percentiles for all days of the year,
- ">=99" indicates that estimated streamflow is greater than the 99th percentile, and
- "Not ranked" indicates that a flow category has not been computed. Common reasons for a "Not ranked" category are insufficient historical data or no current streamflow estimates.
Flood stages are determined by the NWS; not all USGS streamgages have flood stages. A depiction of other streamgages at or above flood stage is available the NWS River Conditions Map.
Sources/Usage: Public Domain. Visit Media to see details.Current Flooding and High-Flow Conditions:
(Current-conditions data are provisional and subject to change)Wyoming:
- Map: Flood and high flows
- Data table: Locations above flood stages
- Map: Current streamflow conditions vs historical streamflows
- Flood of August 1, 1985 in Cheyenne, WY
- Floods of May 1978 in southeastern Montana and northeastern Wyoming
Sources/Usage: Public Domain. Visit Media to see details.Montana:
- Map: Flood and high flows
- Data table: Locations above flood stages
- Map: Current streamflow conditions vs historical streamflows
- Floods of May 1981 in west-central Montana
- Floods of May 1978 in southeastern Montana and northeastern Wyoming
- Floods of June 1964 in northwestern Montana
Video Transcript
Sources/Usage: Public Domain.Devastating floods across much of the U.S. were severe and unrelenting during the spring and summer of 2011. When floods happen, USGS crews are among the first-responders. Often working in dangerous conditions, USGS scientists measure streamflow and river levels, repair and install streamgages, measure water quality and changes in sediment flow, and assess river changes. From flood forecasts to difficult decisions about flood management, science is critical for flood preparations and response. How can a 100-year flood strike twice in 15 years? This is a downloadable poster discussing the meaning and use of probability language in flood characterization.
Poster: 100-Year Flood--It's All About Chance - Science
Below are other science projects associated with floods and high-flows in Wyoming and Montana.
Black Hills Area Floods - 1921 to 1930
Black Hills Area Floods - 1921 to 1930Black Hills Area Floods - 1961 to 1970
Black Hills Area Floods - 1961 to 1970Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1931 to 1940
Black Hills Area Floods - 1931 to 1940Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1901 to 1910
Black Hills Area Floods - 1901 to 1910Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1941 to 1950
Black Hills Area Floods - 1941 to 1950Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1951 to 1960
Black Hills Area Floods - 1951 to 1960Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1911 to 1920
Black Hills Area Floods - 1911 to 1920Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1971 to 1980
Black Hills Area Floods - 1971 to 1980Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1877 to 1890
Black Hills Area Floods - 1877 to 1890Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.Black Hills Area Floods - 1891 to 1900
Black Hills Area Floods - 1891 to 1900Look under the Multimedia table for pictures and more information regarding the event date and location, flow data (if available), a brief summary of the event, and links to available photographs or scanned newspaper articles.The 1972 Black Hills-Rapid City Flood
The 1972 Black Hills-Rapid City Flood Revisited - Data
Below are data or web applications associated with floods and high-flows in Wyoming and Montana.
USGS Peak Streamflow Data
The National Water Information System (NWIS) is the USGS water data portal where you can find a wealth of historic and real-time data related to floods. The NWIS website also is where you can query peak streamflow data by station, state (Wyoming or Montana), or region.
FloodWatch - View flood and high-flow conditions.
The USGS FloodWatch website is a map-based resource from USGS WaterWatch that gives users hourly visual updates for flood conditions at over 3000 locations across the United States (Wyoming or Montana). Learn how to use FloodWatch.
Surface-water data for Wyoming
Real-time, daily, peak-flow, field measurements, and statistics of current and historical data that describe stream levels, streamflow (discharge), reservoir and lake levels, surface-water quality, and rainfall in Wyoming. Surface-water data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders.
Surface-water data for Montana
Real-time, daily, peak-flow, field measurements, and statistics of current and historical data that describe stream levels, streamflow (discharge), reservoir and lake levels, surface-water quality, and rainfall in Montana. Surface-water data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders.
- Publications
Below are publications associated with floods and high-flows in Wyoming and Montana.
Montana StreamStats
About this volumeMontana StreamStats is a Web-based geographic information system (http://water.usgs.gov/osw/streamstats/) application that provides users with access to basin and streamflow characteristics for gaged and ungaged streams in Montana. Montana StreamStats was developed by the U.S. Geological Survey (USGS) in cooperation with the Montana Departments of Transportation, Environmental QuaFilter Total Items: 50The effects of Missouri River mainstem reservoir system operations on 2011 flooding using a Precipitation-Runoff Modeling System model
In 2011 the Missouri River Mainstem Reservoir System (Reservoir System) experienced the largest volume of flood waters since the initiation of record-keeping in the nineteenth century. The high levels of runoff from both snowpack and rainfall stressed the Reservoir System’s capacity to control flood waters and caused massive damage and disruption along the river. The flooding and resulting damage1976 Big Thompson flood, Colorado — Thirty years later
In the early evening of Saturday, July 31, 1976, a large stationary thunderstorm released as much as 7.5 inches of rainfall in about an hour (about 12 inches in a few hours) in the middle reaches of the Big Thompson River Basin and to a lesser extent in parts of the Cache la Poudre River Basin. In steep mountain terrain with thin or no soil, this large amount of rainfall in such a short period of1976 Big Thompson flood, Colorado
In the early evening of July 31, 1976, a large stationary thunderstorm released as much as 7.5 inches of rainfall in about an hour (about 12 inches in a few hours) in the upper reaches of the Big Thompson River drainage. This large amount of rainfall in such a short period of time produced a flash flood that caught residents and tourists by surprise. The immense volume of water that churned down tSummary of significant floods in the United States and Puerto Rico, 1994 through 1998 water years
This volume is a compilation of significant floods that occurred at streamgages throughout the United States and Puerto Rico from October 1, 1993, through September 30, 1998. A significant flood in this report refers to a peak-flow discharge(instantaneous or time averaged) that is in the top 5 percent of all the annual peak flows recorded at streamgages during their total period of record. Most ofThe world's largest floods, past and present: Their causes and magnitudes
Floods are among the most powerful forces on earth. Human societies worldwide have lived and died with floods from the very beginning, spawning a prominent role for floods within legends, religions, and history. Inspired by such accounts, geologists, hydrologists, and historians have studied the role of floods on humanity and its supporting ecosystems, resulting in new appreciation for the many-faLarge floods in the United States: where they happen and why
The spatial distribution of large gaged floods throughout the United States shows that the locations of most of the largest flows are related to specific combinations of regional climatology, topography, and basin size. Key factors include the general northward trend of decreasing atmospheric moisture, proximity to oceanic moisture sources such as the Pacific Ocean and the Gulf of Mexico, and oriePeak-flow characteristics of Wyoming streams
Peak-flow characteristics for unregulated streams in Wyoming are described in this report. Frequency relations for annual peak flows through water year 2000 at 364 streamflow-gaging stations in and near Wyoming were evaluated and revised or updated as needed. Analyses of historical floods, temporal trends, and generalized skew were included in the evaluation. Physical and climatic basin characteriThe National Flood Frequency Program, version 3 : a computer program for estimating magnitude and frequency of floods for ungaged sites
For many years, the U.S. Geological Survey (USGS) has been developing regional regression equations for estimating flood magnitude and frequency at ungaged sites. These regression equations are used to transfer flood characteristics from gaged to ungaged sites through the use of watershed and climatic characteristics as explanatory or predictor variables. Generally, these equations have been develWater-surface profile and flood boundaries for the computed 100-year flood, lower Salt River, Lincoln County, Wyoming
The water-surface profile and flood boundaries for the computed 100-year flood were determined for a part of the lower Salt River in Lincoln County, Wyoming. Channel cross-section data were provided by Lincoln County. Cross-section data for bridges and other structures were collected and compiled by the U.S. Geological Survey. Roughness coefficients ranged from 0.034 to 0.100. The 100-year flood wSummary of significant floods in the United States, Puerto Rico, and the Virgin Islands, 1970 through 1989
This volume is a compilation of significant floods that occurred throughout the United States, Puerto Rico, and the Virgin Islands during 1970 through 1989. A summary of most devastating floods according to amount of damage and lives lost is provided for each year. State-by-state compilations include a description of the general hydroclimatology and conditions that produce significant floods, a de - Web Tools
Below are data or web applications associated with floods and high-flows in Wyoming and Montana.
- News
Below are news stories associated with floods and high-flows in Wyoming and Montana.
Study Links Major Floods in North America and Europe to Multi-Decade Ocean Patterns
The number of major floods in natural rivers across Europe and North America has not increased overall during the past 80 years, a recent study has concluded. Instead researchers found that the occurrence of major flooding in North America and Europe often varies with North Atlantic Ocean temperature patterns.