In 2019, the U.S. Geological Survey, in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two longitudinal hydrophone profiles were carried out at different streamflows to collect underwater acoustic data using hydrophones throughout the study area on June 6-8, 2019 (June 6-8 longitudinal profile) and June 18-19, 2019. The June 6-8 longitudinal profile began at the Pumphouse Recreation Area and ended at the Dotsero boat launch located at Dotsero, Colo. For the June 6-8 longitudinal profile, one of the mobile hydrophone systems, consisting of two H2a-XLR hydrophones (Aquarian Audio, 2013) and a recording system, was attached to a 16-foot Hyside inflatable raft and mounted about 1 foot below the water line (one on the port side of the raft and the second on the starboard side of the raft). A second mobile hydrophone system, consisting of one H2a-XLR hydrophone (Aquarian Audio, 2013) and a recording system, was attached to a 16-foot Down River Equipment inflatable cataraft and mounted about 1 foot below the water line on the stern of the raft.

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two longitudinal hydrophone profiles were carried out at different streamflows to collect underwater acoustic data using hydrophones throughout the study area on June 6-8, 2019 and June 18-19, 2019 (June 18-19 longitudinal profile). The June 18-19 longitudinal profile began at the Pumphouse Recreation Area and ended at the Catamount Bridge boat launch located at the USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo. For the June 18-19 longitudinal profile, a mobile hydrophone system, consisting of two H2a-XLR hydrophones (Aquarian Audio, 2013) and a recording system, was attached to a 16-foot Hyside inflatable raft and mounted about 1 foot below the water line (one on the port side of the raft and the second the starboard side of the raft).

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two longitudinal hydrophone profiles were carried out at different streamflows to collect underwater acoustic data using hydrophones throughout the study area on June 6-8, 2019 and June 18-19, 2019 (June 18-19 longitudinal profile). The June 18-19 longitudinal profile began at the Pumphouse Recreation Area and ended at the Catamount Bridge boat launch located at the USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo. For the June 18-19 longitudinal profile, a mobile hydrophone system, consisting of two H2a-XLR hydrophones (Aquarian Audio, 2013) and a recording system, was attached to a 16-foot Hyside inflatable raft and mounted about 1 foot below the water line (one on the port side of the raft and the second the starboard side of the raft).

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two stationary hydrophone systems were installed on April 23, 2019 at the above Catamount Bridge stationary hydrophone site (above Catamount Bridge site), and two were installed on April 24, 2019 at the Radium stationary hydrophone site (Radium site). These four systems recorded underwater sounds related to bed movement until all the stationary hydrophone systems were removed on August 26, 2019. The upstream location and downstream location at the Radium site were located on the right streambank 400 feet (ft) and 2,000 ft downstream from the Grand County Road 11 Bridge, respectively. The upstream location and downstream location at the above Catamount Bridge site were located on the right streambank 16,800 ft (3.2 miles) and 18,200 ft (3.4 miles) upstream from the Catamount Bridge, respectively. At each of the four monitoring reach locations (an upstream and downstream location at both sites), a stationary hydrophone system with two Aquarian H2a-XLR hydrophones and one recording computer was deployed. The stationary hydrophone systems were programmed to collect a 1-minute audio recording at 15-minute intervals, which is equivalent to the time stamp of the stage and streamflow data collected at the streamgages in the study area (USGS streamgage 09058000 Colorado River near Kremmling, Colo. and USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo.). The audio data were recorded as 44.1 kilohertz, 16-bit stereo (2-channel) .wav files for 1 minute at 15-minute intervals. Debris was found on the hydrophones during each routine servicing, which caused nonsediment background noise in the recordings.

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two stationary hydrophone systems were installed on April 23, 2019 at the above Catamount Bridge stationary hydrophone site (above Catamount Bridge site), and two were installed on April 24, 2019 at the Radium stationary hydrophone site (Radium site). These four systems recorded underwater sounds related to bed movement until all the stationary hydrophone systems were removed on August 26, 2019. The upstream location and downstream location at the Radium site were located on the right streambank 400 feet (ft) and 2,000 ft downstream from the Grand County Road 11 Bridge, respectively. The upstream location and downstream location at the above Catamount Bridge site were located on the right streambank 16,800 ft (3.2 miles) and 18,200 ft (3.4 miles) upstream from the Catamount Bridge, respectively. At each of the four monitoring reach locations (an upstream and downstream location at both sites), a stationary hydrophone system with two Aquarian H2a-XLR hydrophones and one recording computer was deployed. The stationary hydrophone systems were programmed to collect a 1-minute audio recording at 15-minute intervals, which is equivalent to the time stamp of the stage and streamflow data collected at the streamgages in the study area (USGS streamgage 09058000 Colorado River near Kremmling, Colo. and USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo.). The audio data were recorded as 44.1 kilohertz, 16-bit stereo (2-channel) .wav files for 1 minute at 15-minute intervals. Debris was found on the hydrophones during each routine servicing, which caused nonsediment background noise in the recordings.

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two independent and complementary lines of evidence were collected to detect incipient bed movement. Two stationary hydrophone systems were installed on April 23, 2019 at the above Catamount Bridge stationary hydrophone site, and two were installed on April 24, 2019 at the Radium stationary hydrophone site. These four systems recorded underwater sounds related to bed movement until all the stationary hydrophone systems were removed on August 26, 2019. Two longitudinal hydrophone profiles were carried out at different streamflows to collect underwater acoustic data using hydrophones throughout the study area on June 6-8, 2019 (June 6-8 longitudinal profile) and June 18-19, 2019 (June 18-19 longitudinal profile). The June 6-8 longitudinal profile began at the Pumphouse Recreation Area and ended at the Dotsero boat launch located at Dotsero, Colo. The June 18-19 longitudinal profile began at the Pumphouse Recreation Area and ended at the Catamount Bridge boat launch located at the USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo. Pebble counts of coarse surface particles were performed in the wadeable areas adjacent to the stationary hydrophones to provide general estimates of the size of the material that could be mobilized and recorded near the hydrophones.

In 2019, the U.S. Geological Survey (USGS), in cooperation with the Upper Colorado River Wild and Scenic Stakeholder Group, studied the magnitude and recurrence interval of streamflow needed to initiate bed movement of gravel-sized and finer sediment in a segment of the Colorado River in Colorado to better understand sediment movement and its relation to flow regimes of the river. Bed movement occurred more frequently and at lower streamflows from State Bridge to Catamount Bridge compared to the study area upstream from State Bridge. Two independent and complementary lines of evidence were collected to detect incipient bed movement. Two stationary hydrophone systems were installed on April 23, 2019 at the above Catamount Bridge stationary hydrophone site, and two were installed on April 24, 2019 at the Radium stationary hydrophone site. These four systems recorded underwater sounds related to bed movement until all the stationary hydrophone systems were removed on August 26, 2019. Two longitudinal hydrophone profiles were carried out at different streamflows to collect underwater acoustic data using hydrophones throughout the study area on June 6-8, 2019 (June 6-8 longitudinal profile) and June 18-19, 2019 (June 18-19 longitudinal profile). The June 6-8 longitudinal profile began at the Pumphouse Recreation Area and ended at the Dotsero boat launch located at Dotsero, Colo. The June 18-19 longitudinal profile began at the Pumphouse Recreation Area and ended at the Catamount Bridge boat launch located at the USGS streamgage 09060799 Colorado River at Catamount Bridge, Colo. Pebble counts of coarse surface particles were performed in the wadeable areas adjacent to the stationary hydrophones to provide general estimates of the size of the material that could be mobilized and recorded near the hydrophones.

These data were compiled to determine the rate and magnitude of channel-planform change, and the topographic change of the channel and floodplain in Echo, Island, and Rainbow Parks within Dinosaur National Monument between the 1990s and 2019. The objective(s) of our study were to analyze geomorphic change within Echo, Island, and Rainbow Parks to determine the magnitude and style of channel change with respect to the past two decades of combined streamflow from Flaming Gorge Dam and the relatively unregulated Yampa River. These data represent river channel planform delineations made within a geographic information system, and topographic channel and floodplain data collected using total stations, depth sounders, Real-Time Kinematic GNSS, and multibeam sonar. These data were collected in June 2019.

These data were compiled to determine the rate and magnitude of channel-planform change, and the topographic change of the channel and floodplain in Echo, Island, and Rainbow Parks within Dinosaur National Monument between the 1990s and 2019. The objective(s) of our study were to analyze geomorphic change within Echo, Island, and Rainbow Parks to determine the magnitude and style of channel change with respect to the past two decades of combined streamflow from Flaming Gorge Dam and the relatively unregulated Yampa River. These data represent river channel planform delineations made within a geographic information system, and topographic channel and floodplain data collected using total stations, depth sounders, Real-Time Kinematic GNSS, and multibeam sonar. These data were collected in June 2019.

These data were compiled to determine the rate and magnitude of channel-planform change, and the topographic change of the channel and floodplain in Echo, Island, and Rainbow Parks within Dinosaur National Monument between the 1990s and 2019. The objective(s) of our study were to analyze geomorphic change within Echo, Island, and Rainbow Parks to determine the magnitude and style of channel change with respect to the past two decades of combined streamflow from Flaming Gorge Dam and the relatively unregulated Yampa River. These data represent river channel planform delineations made within a geographic information system, and topographic channel and floodplain data collected using total stations, depth sounders, Real-Time Kinematic GNSS, and multibeam sonar. These data were collected in June 2019.