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3 edition of Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado found in the catalog.

Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado

Stanley G. Robson

Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado

by Stanley G. Robson

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  • 27 Currently reading

Published by U.S. Dept. of the Interior, U.S. Geological Survey in [Reston, Va.?] .
Written in English

    Subjects:
  • Aquifers -- Front Range (Colo. and Wyo.),
  • Front Range (Colo. and Wyo.)

  • Edition Notes

    Other titlesStatus of shallow aquifer mapping in the Northern Front Range Area, Colorado.
    StatementS.G. Robson.
    SeriesUSGS fact sheet -- 069-00., Fact sheet (Geological Survey (U.S.)) -- FS-00-069.
    ContributionsGeological Survey (U.S.)
    The Physical Object
    Pagination[2] p. :
    ID Numbers
    Open LibraryOL16330945M
    OCLC/WorldCa48214868

    Colorado Foundation for Water Education Logan St., Suite • Denver, CO • Colorado’s water supply future. CN - JA - 72nd Society for Range Management International Meeting PB - Society for Range Management Meeting Abstracts CY - Minneapolis, Minnesota ER - TY - JOUR T1 - Digital mapping of ecological land units using a nationally scalable modeling framework JF - Soil Science Society of America Journal Y1 - A1 - Maynard, Jonathan J. A1.

    PROCEEDINGS of the NATIONAL GROUND WATER QUALITY SYMPOSIUM Cosponsored by the Environmental Protection Agency and the National Water Well Association August , Denver, Colorado Dedicated to C. E. Jacob () Contract No. Project # GRB For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, B.C. - . into them. As shown in Figure , headwater streams are classified as first order, with order number increasing in a downstream ter networks of very small streams accumulate rainfall, overland flow, snowmelt, or aquifer discharge, sending variable amounts of water downstream to increasingly larger channels.

    Upon receipt of a proper deed from the State of North Dakota, executed under authority of the act of its legislative assembly, approved February 5, , reconveying to the United States title to sect township north, range 81 west, fifth principal meridian, the Secretary of the Interior is authorized to issue patents to said State. Coping with Flash Floods book & chapters Kluwer Academic Publishers, Dordrecht, , edited collection Based on the findings from the NATO Advanced Study Institute held in Ravello, Italy, November , (w. J. Handmer) Gruntfest, E., and C. Huber, Status Report on Flood Warning Systems in the United States.


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Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado by Stanley G. Robson Download PDF EPUB FB2

Mapping of shallow aquifers in the northern Front Range area of Colorado has been completed as part of the U.S. Geological Survey Front Range Infrastructure Resources Project. The aquifer mapping was undertaken as part of a comprehensive effort to better define the mineral, energy, cartographic, biological, and water resources that are critical to the support and development of the area's.

Get this from a library. Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado. [Stanley G Robson; Geological Survey (U.S.)]. Status of Shallow-Aquifer Mapping in the Northern Front Range Area, Colorado -s.c.

Robson INTRODUCTION Mapping of shall ow aquifers in the northern Front RAuthor: Stanley G. Robson. 2 Ground-Water-Quality Assessment of Shallow Aquifers in the Front Range Urban Corridor, Colorado, –98 Figure 1. Locations of the study area and water-quality wells in. Monitoring earthquake shaking in buildings to reduce loss of life and property.

Format Online Resource Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado. Robson, Stanley G. I «Previous. Anderson, S. W., Suzanne Anderson, Robert S. Anderson Exhumation by debris flows in the Colorado Front Range storm.

Geology, 43(5): DOI: /G Eve-Lyn Hinckley Fate of sulfur fungicide in the vineyard and beyond. Practical Winery and Vineyard, May issue. Stratigraphy and water levels in the Arapahoe aquifer, Douglas County area, Denver Basin, Colorado Article in Mountain Geologist 41(4) October with Reads How we measure 'reads'.

Shallow groundwater in the Atankwidi Catchment of the White Volta Basin: Current status and future sustainability. Colombo, Sri Lanka: International Water Management Institute. 30p. Geological Survey (U.S.): Analysis of the Augrainstorm and storm runoff to the South Platte River in the southern Denver metropolitan area, Colorado / (Lakewood, Colo.: U.S.

Dept. of the Interior, Geological Survey ; Denver, CO: For sale by Open-File Services Section, U.S. Geological Survey, MSWestern Distribution Branch.

Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado / ([Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, []), by Stanley G Robson and Geological Survey (U.S.) (page images at HathiTrust). The study area is located at the Bérchules River watershed, within the limits of the Sierra Nevada National Park, in southern Spain ().The region, called La Alpujarra, is formed by two main relief elements: (1) Sierra Nevada, the highest mountain range in the Iberian Peninsula (Mulhacén, m a.s.l.) and (2) the Alpujarra Corridor, an E-W valley parallel to the mountain range at its Cited by: Nevada Petroleum Society Publicat Cenozoic geology of the northern Colorado River extensional corridor, Nevada and Arizona: economic implications of extensional segmentation structures, Nevada Petroleum Society Field Trip, October, by J.

Faulds (editor), p. plus 2 large color plates; copyrighted. Newsletter of the Water Center of Colorado State University May/June Vol Issue 3. Theme: Student Research. Co-Sponsored by Colorado Water Institute, Colorado State University. Rehabilitating slash pile burn scars in upper montane forests of the Colorado Front Range.

Natural Areas Journal. 31(2): Giardina, C.P. and C.C. Rhoades. Clear cutting and burning affect nitrogen supply, phosphorus fractions and seedling growth in soils from a Wyoming lodgepole pine forest. Forest Ecology and Management inputs. MAR is the largest input of salt mass in the northern Shallow Aquifer (HSU-1), even though the concentration of the recharge water is relatively low and acts to improve groundwater quality.

Agricultural and municipal irrigation return flow together comprises the second largest salt input in the northern Shallow Aquifer (HSU-1). PROCEEDINGS OF THE SECOND NATIONAL GROUND WATER QUALITY SYMPOSIUM Cosponsored by the Environmental Protection Agency and the National Water Well Association, September, Denver, Colorado Contract No.

TABLE OF CONTENTS 2 Ground Water and Politics Jay H. Lehr 4 C. McGuinness - Hydrogeologist, Writer, Teacher Gerald Meyer 7. Colorado Water Resources Research Institute Project on Grant Number 01HQGR, Project CO6B.

The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or.

Plummer, L.N., and Busenberg, E.,CFC's--Tools for age-dating and tracing shallow ground water, in U.S. Geological Survey Yearbook, Fiscal Yearp. Kenski, D.M., and Risch, M.R.,Calculated back trajectory coordinates for air masses contributing to five selected precipitation-mercury deposition episodes at a National Atmospheric Deposition Program monitoring site in.

According to the U.S. Census Bureau, the county has a total area of 2, square miles (6, km 2), of which square miles (1, km 2) is land and 1, square miles (4, km 2) (80%) is water.

It is the largest county in Wisconsin by total area. The county also has miles (, m) of shoreline. The county covers the majority of the Door Peninsula.

The third section (Monitoring/Response) includes a paper that models range expansion of the Northern Snakehead in the southeastern USA based on occurrence data and environmental conditions.

Also included in this section is a paper summarizing an environmental DNA study to assess the status and range of the Bullseye Snakehead C. marulius in. An abundant supply of fish culture water is supplied by five shallow aquifer wells ( feet in depth) capable of pumping a combined 2,+ gallons per minute.

The well water is a constant F, pH oftotal hardness of 2, ppm, and total dissolved solids of 3, ppm. Water rights, allocated through.Considering River-Scale Ecological Improvements within Flood Management Planning: The Lower Menomonee River Watercourse Status Report; Developing Linkages between Biological Impairment and Stream Siltation: A Case Study in the Northern Great Plains Ecoregion.Proceedings of the World Environmental and Water Resources Congress, held in Kansas City, Missouri, MaySponsored by the Environmental and Water Resources Institute of ASCE.

This collection contains papers focusing on the engineering challenges of balancing environmental and development issues while achieving a sustainable.