How long is the humboldt river

It is just a sickly rivulet compared to rivers back east. Twain commented that one of the pleasantest [sic] and most invigorating exercises one can contrive is to run and jump across the Humboldt River till he is overheated, and then drink it dry. Humboldt is its name today but there for awhile no one really knew what to call it. It is certain that area Indians called it something but that name is lost in the past. He wrote in his journal that it was the Unknown River.

Joseph Paul, one of the trappers, died on December 18, and was buried on the banks of the river. Now it was called Paul's River. During the time Ogden was in the area, the river is also referred to as Mary's River. Mary was Ogden's Indian wife. In the river was used as part of the route of the Central Pacific segment of the Transcontinental Railroad.

In the 20th century, the valley of the river became the route for U. Highway 40 , later replaced by Interstate About 45, people live within 10 miles of the river, roughly a third of the population of the state outside of western Nevada and Southern Nevada. Reno, NV: U. Department of the Interior, U. Geological Survey. Denver, CO: U. Humboldt River — Humboldt River, s. Humboldt River — spr. Humboldt River — River, northern Nevada, U. Rising in Elko county, it flows west and southwest for mi km to Humboldt Lake also called Humboldt Sink.

Named by John C. It is an intermittent stream draining a rugged area on the edge of the Owyhee Desert in the… … Wikipedia. Humboldt River. The timing and magnitude of the effects of groundwater withdrawals on streamflow of the Humboldt River are not well understood.

Although groundwater use in the Humboldt River Basin is primarily for agriculture, a substantial quantity of groundwater has been removed from consolidated rock units and basin fill as part of mining activity in the middle Humboldt River basin.

The contribution to streamflow depletion by mine dewatering is currently thought to be relatively small, largely because much of the water was or continues to be returned to the river or to unconsolidated deposits near the river. However, many Humboldt River water rights holders contend that mine dewatering contributes significantly to streamflow depletion. To evaluate the impacts of groundwater withdrawals on streamflow, three transient, regional-scale flow models will be developed and documented.

The three models will represent the upper, middle, and lower Humboldt River Basins, respectively. Not all completed studies are listed here. Any decisions to further develop the ground-water resources of the upper Humboldt River Basin will have to be balanced against the potential effects of such development on streamflow. County and state water-resource managers need information that will enable them to make informed decisions regarding future use and development of the water resources of the upper Humboldt River Basin.

To address these needs and concerns, the NVWSC has adopted a phased approach for assessing the water resources of the upper Humboldt River basin in northeastern Nevada. Phase one was completed in —08 and describes the hydrogeologic framework and groundwater conditions.

Phase two took place in federal fiscal years — The results from phase two were summarized in USGS Scientific Investigations Report , which describes properties of basin-fill deposits, presents an overall water budget for the period —, and describes interactions of groundwater and streamflow along the mainstem Humboldt River and its main tributaries.

Elko County officials and citizens are concerned about growing demand for groundwater within the county and demands for groundwater that are occurring elsewhere in the state. Because the Humboldt River is fully appropriated, any additional water needed to support growth in the upper Humboldt River Basin will have to come from groundwater. County and state water-resource managers need Some publications between are not yet available electronically.

BackgroundFloods are one of the most costly and frequent natural disasters in Nevada. In , more than 2 miles of Interstate 15 in southern Nevada was heavily damaged by A pesticide is a substance, or mixture of substances, used to kill or control insects, weeds, plant diseases, and other pest organisms.

Commercial pesticide applicators, farmers, and homeowners apply about 1. Although intended Multiple aquifer tests were conducted in Lovelock, Nevada, to determine hydraulic conductivity and storage properties to be used with the numerical groundwater flow model of the lower Humboldt River Basin while accounting for the influence of surface features with a modeling component. The numerical model will ultimately provide the Nevada The impact of groundwater withdrawal on surface water is a concern of water users and water managers, particularly in the arid western United States.

Capture maps are useful tools to spatially assess the impact of groundwater pumping on water sources e. This study was done in cooperation with Elko County, Nevada in response to concerns over growing demand for water within the county and increasing external demands that are occurring statewide.

The upper Humboldt River basin encompasses 4, square miles in northeastern Nevada and includes the headwaters area of the Humboldt River. Nearly all of At the Humboldt site, D. At a location 4 km away during the first year of defoliation, D. The proposal calls for the landfill to receive by rail about 20, tons of waste per week for up to 50 years. On September 22, , the Interior Appropriation S. Geological Survey to The upper Humboldt River basin encompasses 4, square miles in northeastern Nevada, and it comprises the headwaters area of the Humboldt River.

Nearly all flow of the river originates in this area. The upper Humboldt River basin consists of several structural basins, in places greater than 5, feet deep, in which basin-fill deposits of Ground water is abundant in many alluvial basins of the Basin and Range Physiographic Province of the western United States. Water enters these basins by infiltration along intermittent and ephemeral channels, which originate in the mountainous regions before crossing alluvial fans and piedmont alluvial plains.

Water also enters the basins as This study was initiated to expand upon previous findings that indicated concentrations of dissolved solids, arsenic, boron, mercury, molybdenum, selenium, and uranium were either above geochemical background concentrations or were approaching or exceeding ecological criteria in the lower Humboldt River system.