RCMAP - Roaring Fork River at Basalt, Colorado Completed
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.
The Roaring Fork River at Basalt, Colorado, is a single-thread, high-gradient, cobble/boulder-bed river that presents a natural hazard to the town, nearby residential structures, several bridges and roadways, and the municipal waste-treatment facility. The Roaring Fork has a frequently mobile streambed composed of gravel, cobbles, and boulders. The hazard originates from high velocity snowmelt runoff and a high bedload-transport rate that cause intermittent channel realignment as well as scour and deposition of coarse-grain bars and islands.
Recent urban, highway, and recreational development on the flood plain, earlier attempts to realign and confine the Roaring Fork channel with retaining walls and levees, and flow obstructions such as bridge openings and piers have altered the hydrology, hydraulics, sediment transport, and sediment deposition areas of the Roaring Fork. Entrainment and deposition of coarse sediment on the streambed and in large alluvial bars have reduced the flood-conveying capacity of the river. Engineering studies identified flood-prone areas and hazards related to inundation and high streamflow velocity (Matrix Design Group, 2000; McLaughlin Water Engineers, 2000). A USGS study (Elliott, 2002) evaluated the potential response of the channel to discharges that entrain the coarse streambed and identified several subreaches where bed-material entrainment or deposition potentially could create problems.
Location:
The monitoring reach is a 0.8 mile (4,200 ft) segment of the river extending from approximately 1,200 ft upstream from the Highway 82 Upper Bypass Bridge, east of the town of Basalt, downstream to the Emma Bridge near the confluence of the Fryingpan River in downtown Basalt. This reach includes parts of sections 17, 18, and 7, T8S, R86W, Pitkin County. Streamflow gaging station 09081000 Roaring Fork River near Emma, Colorado is approximately 2.9 miles downstream from the Emma Bridge.
Streamflow Data:
Current streamflow: USGS 09081000 Roaring Fork River near Emma
View peak streamflow: 09081000 Roaring Fork River near Emma
Photographic History:
Cross Section Images:
- Cross Section 3.2
- Below Cross Section 3.6
- Cross Section 6.1
- Cross Section 8.2
- Cross Section 10
- Cross Section 10.9
- Cross Section 13
- Cross Section 17 (left hand bank)
- Cross Section 17 (right hand bank)
Sediment Surveys
See: Sediment Distribution Charts for Roaring Fork River at Basalt
Channel Surveys
See: Cross Section Data for sites on Roaring Fork River at Basalt
Below are other science projects associated with the RCMAP project at the Roaring Fork River at Basalt, Colorado.
Reconfigured Channel Monitoring and Assessment Program (RCMAP)
RCMAP - Muddy Creek below Wolford Mountain Reservoir near Kremmling, Colorado
RCMAP - Lake Fork of the Gunnison near Lake City, Colorado
RCMAP - North Fork Gunnison River at Hotchkiss, Colorado
RCMAP - Gunnison River at the Hartland Dam near Delta, Colorado
RCMAP - Gunnison River at Spann Diversion at Gunnison, Colorado
RCMAP - Uncompahgre River at Ridgway, Colorado
RCMAP - Lake Fork at Gateview, Colorado
- Overview
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.
The Roaring Fork River at Basalt, Colorado, is a single-thread, high-gradient, cobble/boulder-bed river that presents a natural hazard to the town, nearby residential structures, several bridges and roadways, and the municipal waste-treatment facility. The Roaring Fork has a frequently mobile streambed composed of gravel, cobbles, and boulders. The hazard originates from high velocity snowmelt runoff and a high bedload-transport rate that cause intermittent channel realignment as well as scour and deposition of coarse-grain bars and islands.
Sources/Usage: Public Domain. View Media DetailsRoaring Fork River at Basalt, Colorado on May 17, 2001. Discharge: 1130 ft3/s Recent urban, highway, and recreational development on the flood plain, earlier attempts to realign and confine the Roaring Fork channel with retaining walls and levees, and flow obstructions such as bridge openings and piers have altered the hydrology, hydraulics, sediment transport, and sediment deposition areas of the Roaring Fork. Entrainment and deposition of coarse sediment on the streambed and in large alluvial bars have reduced the flood-conveying capacity of the river. Engineering studies identified flood-prone areas and hazards related to inundation and high streamflow velocity (Matrix Design Group, 2000; McLaughlin Water Engineers, 2000). A USGS study (Elliott, 2002) evaluated the potential response of the channel to discharges that entrain the coarse streambed and identified several subreaches where bed-material entrainment or deposition potentially could create problems.
Location:
The monitoring reach is a 0.8 mile (4,200 ft) segment of the river extending from approximately 1,200 ft upstream from the Highway 82 Upper Bypass Bridge, east of the town of Basalt, downstream to the Emma Bridge near the confluence of the Fryingpan River in downtown Basalt. This reach includes parts of sections 17, 18, and 7, T8S, R86W, Pitkin County. Streamflow gaging station 09081000 Roaring Fork River near Emma, Colorado is approximately 2.9 miles downstream from the Emma Bridge.
Streamflow Data:
Current streamflow: USGS 09081000 Roaring Fork River near Emma
View peak streamflow: 09081000 Roaring Fork River near Emma
Photographic History:
Sources/Usage: Public Domain. View Media DetailsCross Section Images:
- Cross Section 3.2
- Below Cross Section 3.6
- Cross Section 6.1
- Cross Section 8.2
- Cross Section 10
- Cross Section 10.9
- Cross Section 13
- Cross Section 17 (left hand bank)
- Cross Section 17 (right hand bank)
Sediment Surveys
See: Sediment Distribution Charts for Roaring Fork River at Basalt
Channel Surveys
See: Cross Section Data for sites on Roaring Fork River at Basalt
- Science
Below are other science projects associated with the RCMAP project at the Roaring Fork River at Basalt, Colorado.
Reconfigured Channel Monitoring and Assessment Program (RCMAP)
Channel reconfiguration to mitigate a variety of riverine problems has become an important issue in the Western United States. Reasons cited for channel reconfiguration include restoration to more natural or historical conditions, improved water conveyance in flood-prone areas, mitigation of unstable streambed and streambanks, increased sediment transport, and enhancement of riparian habitat or...RCMAP - Muddy Creek below Wolford Mountain Reservoir near Kremmling, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - Lake Fork of the Gunnison near Lake City, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - North Fork Gunnison River at Hotchkiss, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - Gunnison River at the Hartland Dam near Delta, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - Gunnison River at Spann Diversion at Gunnison, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - Uncompahgre River at Ridgway, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach.RCMAP - Lake Fork at Gateview, Colorado
The U.S. Geological Survey was engaged in a program to monitor and assess the long-term geomorphic behavior of selected river and stream reaches that previously had undergone some physical modification. These modifications included natural channel adjustments to floods as well as intentional channel reconfigurations to alter the function or appearance of a river reach. - Multimedia
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