The yellow raft of SCREE expedition leader, Tom Minckley, floating through calm waters of Browns Park National Wildlife Refuge, Colorado. The far bank in the midground of the photo are the exposed sediments of the pre-dam floodplain of the Green River. The layers of rock in the background are the exposed layers of the red Uinta Mountain Group quartzite.
Jason S. Alexander (Former Employee)
Science and Products
Wyoming Landscape Conservation Initiative: Water Resources
Characterizing Hydrologic and Geomorphic Processes in a Spring-Fed, Cold-Desert Headwater Stream
Peak-Flow Frequency Analysis for Selected Montana Streamgages
Geologic Map of the valley corridor of the Niobrara National Scenic River, Nebraska
Digitized datasets used in channel stability study in the Colorado River headwater arroyo system of Muddy Creek, Wyoming
Data from Lab Experiments to Support Interim Guidance for Performing Calibration Checks on the Sequoia Scientific LISST-ABS Acoustic Backscatter Sensor
Peak-flow frequency analyses for selected streamgages on the Bighorn, Tongue, and Lower Yellowstone Rivers and tributaries and Home Creek, Montana, based on data through water year 2021
Peak-flow frequency analyses for selected streamgages in and near Teton County, Montana, based on data through water year 2019
Peak-flow frequency analyses for selected streamgages in and near Powell County, Montana, based on data through water year 2019
Peak-flow frequency analyses for selected streamgages in and near the Milk River Basin, Montana, based on data through water year 2018, Part 1
The yellow raft of SCREE expedition leader, Tom Minckley, floating through calm waters of Browns Park National Wildlife Refuge, Colorado. The far bank in the midground of the photo are the exposed sediments of the pre-dam floodplain of the Green River. The layers of rock in the background are the exposed layers of the red Uinta Mountain Group quartzite.
View looking downstream at the red sandstone walls of Swallow Canyon. This small canyon is one of two canyons that divide Browns Park into series of intermittent alluvial-meandering and bedrock canyon segments. Unlike Red Canyon and Lodore Canyon, the slope of Swallow Canyon is not controlled by debris flows, and thus does not have any rapids.
View looking downstream at the red sandstone walls of Swallow Canyon. This small canyon is one of two canyons that divide Browns Park into series of intermittent alluvial-meandering and bedrock canyon segments. Unlike Red Canyon and Lodore Canyon, the slope of Swallow Canyon is not controlled by debris flows, and thus does not have any rapids.
View looking upstream from a raft on the Green River at the downstream end of Swinging Bridge Canyon, near Flynn Bottom. The eastern end of the Unita Mountains lie in the background. A pump station supplying water to the flooded wetlands of Brown's Park National Wildlife Refuge can be seen on the right near the edge of water.
View looking upstream from a raft on the Green River at the downstream end of Swinging Bridge Canyon, near Flynn Bottom. The eastern end of the Unita Mountains lie in the background. A pump station supplying water to the flooded wetlands of Brown's Park National Wildlife Refuge can be seen on the right near the edge of water.
View looking at a shallow side channel of the Green River in Brown's Park, Colorado. The picture is taken looking downstream from the left bank of the river. In the foreground and on the opposite bank are stands of sandbar willow (Salix exigua). Further beyond, are stands of Fremont cottonwood (Populus fremontii).
View looking at a shallow side channel of the Green River in Brown's Park, Colorado. The picture is taken looking downstream from the left bank of the river. In the foreground and on the opposite bank are stands of sandbar willow (Salix exigua). Further beyond, are stands of Fremont cottonwood (Populus fremontii).
The photo shows the SCREE Powell 150 expdition camp at Big Pine Campground in Red Canyon of the Green River, Utah. The large green tarp was set up to keep the kitchen area and campers dry. Two very large ponderosa pines are in the center of camp, and surely were witness to the 1869 Powell expedition.
The photo shows the SCREE Powell 150 expdition camp at Big Pine Campground in Red Canyon of the Green River, Utah. The large green tarp was set up to keep the kitchen area and campers dry. Two very large ponderosa pines are in the center of camp, and surely were witness to the 1869 Powell expedition.
This photo demonstrates one of the challenges of down-river boating in the Colorado River system.
This photo demonstrates one of the challenges of down-river boating in the Colorado River system.
This photo displays the contrast between the clear, sediment-starved waters released from a large dam, and the murky, sediment-rich waters of natural tributaries. The tributary is just one of many that gradually re-supply the river with sediment.
This photo displays the contrast between the clear, sediment-starved waters released from a large dam, and the murky, sediment-rich waters of natural tributaries. The tributary is just one of many that gradually re-supply the river with sediment.
This photo demonstrates the typical set up of the so-called 'bat-and-bug' citizen science data collection platform used on the SCREE - Powell 150 expedition. The UV light attracts bugs to the pool of ethanol, where they land and are preserved for identification, while the touchpad device has an untrasonic microphone to collect bat calls.
This photo demonstrates the typical set up of the so-called 'bat-and-bug' citizen science data collection platform used on the SCREE - Powell 150 expedition. The UV light attracts bugs to the pool of ethanol, where they land and are preserved for identification, while the touchpad device has an untrasonic microphone to collect bat calls.
Yellowstone River fish bypass channel physical and hydraulic monitoring, Montana
Interim guidance for calibration checks on a submersible acoustic backscatter sediment sensor
Using continuous measurements of turbidity to predict suspended-sediment concentrations, loads, and sources in Flat Creek through the town of Jackson, Wyoming, 2019−20 — A pilot study
Testing the potential of streamflow data to predict spring migration of an ungulate herds
U.S. Geological Survey science for the Wyoming Landscape Conservation Initiative—2018 annual report
Deposition potential and flow-response dynamics of emergent sandbars in a braided river
Spectrally based bathymetric mapping of a dynamic, sand‐bedded channel: Niobrara River, Nebraska, USA
Effects of streamflows on stream-channel morphology in the eastern Niobrara National Scenic River, Nebraska, 1988–2010
Characteristics of sediment transport at selected sites along the Missouri River, 2011–12
The influence of controlled floods on fine sediment storage in debris fan-affected canyons of the Colorado River basin
Monitoring and research to describe geomorphic effects of the 2011 controlled flood on the Green River in the Canyon of Lodore, Dinosaur National Monument, Colorado and Utah
Sediment transport and deposition in the lower Missouri River during the 2011 flood
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Wyoming Landscape Conservation Initiative: Water Resources
Characterizing Hydrologic and Geomorphic Processes in a Spring-Fed, Cold-Desert Headwater Stream
Peak-Flow Frequency Analysis for Selected Montana Streamgages
Geologic Map of the valley corridor of the Niobrara National Scenic River, Nebraska
Digitized datasets used in channel stability study in the Colorado River headwater arroyo system of Muddy Creek, Wyoming
Data from Lab Experiments to Support Interim Guidance for Performing Calibration Checks on the Sequoia Scientific LISST-ABS Acoustic Backscatter Sensor
Peak-flow frequency analyses for selected streamgages on the Bighorn, Tongue, and Lower Yellowstone Rivers and tributaries and Home Creek, Montana, based on data through water year 2021
Peak-flow frequency analyses for selected streamgages in and near Teton County, Montana, based on data through water year 2019
Peak-flow frequency analyses for selected streamgages in and near Powell County, Montana, based on data through water year 2019
Peak-flow frequency analyses for selected streamgages in and near the Milk River Basin, Montana, based on data through water year 2018, Part 1
The yellow raft of SCREE expedition leader, Tom Minckley, floating through calm waters of Browns Park National Wildlife Refuge, Colorado. The far bank in the midground of the photo are the exposed sediments of the pre-dam floodplain of the Green River. The layers of rock in the background are the exposed layers of the red Uinta Mountain Group quartzite.
The yellow raft of SCREE expedition leader, Tom Minckley, floating through calm waters of Browns Park National Wildlife Refuge, Colorado. The far bank in the midground of the photo are the exposed sediments of the pre-dam floodplain of the Green River. The layers of rock in the background are the exposed layers of the red Uinta Mountain Group quartzite.
View looking downstream at the red sandstone walls of Swallow Canyon. This small canyon is one of two canyons that divide Browns Park into series of intermittent alluvial-meandering and bedrock canyon segments. Unlike Red Canyon and Lodore Canyon, the slope of Swallow Canyon is not controlled by debris flows, and thus does not have any rapids.
View looking downstream at the red sandstone walls of Swallow Canyon. This small canyon is one of two canyons that divide Browns Park into series of intermittent alluvial-meandering and bedrock canyon segments. Unlike Red Canyon and Lodore Canyon, the slope of Swallow Canyon is not controlled by debris flows, and thus does not have any rapids.
View looking upstream from a raft on the Green River at the downstream end of Swinging Bridge Canyon, near Flynn Bottom. The eastern end of the Unita Mountains lie in the background. A pump station supplying water to the flooded wetlands of Brown's Park National Wildlife Refuge can be seen on the right near the edge of water.
View looking upstream from a raft on the Green River at the downstream end of Swinging Bridge Canyon, near Flynn Bottom. The eastern end of the Unita Mountains lie in the background. A pump station supplying water to the flooded wetlands of Brown's Park National Wildlife Refuge can be seen on the right near the edge of water.
View looking at a shallow side channel of the Green River in Brown's Park, Colorado. The picture is taken looking downstream from the left bank of the river. In the foreground and on the opposite bank are stands of sandbar willow (Salix exigua). Further beyond, are stands of Fremont cottonwood (Populus fremontii).
View looking at a shallow side channel of the Green River in Brown's Park, Colorado. The picture is taken looking downstream from the left bank of the river. In the foreground and on the opposite bank are stands of sandbar willow (Salix exigua). Further beyond, are stands of Fremont cottonwood (Populus fremontii).
The photo shows the SCREE Powell 150 expdition camp at Big Pine Campground in Red Canyon of the Green River, Utah. The large green tarp was set up to keep the kitchen area and campers dry. Two very large ponderosa pines are in the center of camp, and surely were witness to the 1869 Powell expedition.
The photo shows the SCREE Powell 150 expdition camp at Big Pine Campground in Red Canyon of the Green River, Utah. The large green tarp was set up to keep the kitchen area and campers dry. Two very large ponderosa pines are in the center of camp, and surely were witness to the 1869 Powell expedition.
This photo demonstrates one of the challenges of down-river boating in the Colorado River system.
This photo demonstrates one of the challenges of down-river boating in the Colorado River system.
This photo displays the contrast between the clear, sediment-starved waters released from a large dam, and the murky, sediment-rich waters of natural tributaries. The tributary is just one of many that gradually re-supply the river with sediment.
This photo displays the contrast between the clear, sediment-starved waters released from a large dam, and the murky, sediment-rich waters of natural tributaries. The tributary is just one of many that gradually re-supply the river with sediment.
This photo demonstrates the typical set up of the so-called 'bat-and-bug' citizen science data collection platform used on the SCREE - Powell 150 expedition. The UV light attracts bugs to the pool of ethanol, where they land and are preserved for identification, while the touchpad device has an untrasonic microphone to collect bat calls.
This photo demonstrates the typical set up of the so-called 'bat-and-bug' citizen science data collection platform used on the SCREE - Powell 150 expedition. The UV light attracts bugs to the pool of ethanol, where they land and are preserved for identification, while the touchpad device has an untrasonic microphone to collect bat calls.
Yellowstone River fish bypass channel physical and hydraulic monitoring, Montana
Interim guidance for calibration checks on a submersible acoustic backscatter sediment sensor
Using continuous measurements of turbidity to predict suspended-sediment concentrations, loads, and sources in Flat Creek through the town of Jackson, Wyoming, 2019−20 — A pilot study
Testing the potential of streamflow data to predict spring migration of an ungulate herds
U.S. Geological Survey science for the Wyoming Landscape Conservation Initiative—2018 annual report
Deposition potential and flow-response dynamics of emergent sandbars in a braided river
Spectrally based bathymetric mapping of a dynamic, sand‐bedded channel: Niobrara River, Nebraska, USA
Effects of streamflows on stream-channel morphology in the eastern Niobrara National Scenic River, Nebraska, 1988–2010
Characteristics of sediment transport at selected sites along the Missouri River, 2011–12
The influence of controlled floods on fine sediment storage in debris fan-affected canyons of the Colorado River basin
Monitoring and research to describe geomorphic effects of the 2011 controlled flood on the Green River in the Canyon of Lodore, Dinosaur National Monument, Colorado and Utah
Sediment transport and deposition in the lower Missouri River during the 2011 flood
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.