The Water Infrastructure Finance Authority of Arizona is an independent entity authorized to finance the construction, rehabilitation and/or improvement of drinking water, waste water, waste water reclamation, and other water quality facilities/projects. As a “Bond Bank”, WIFA is authorized to issue water quality bonds on behalf of communities for basic water infrastructure. Generally, WIFA offers borrowers below market interest rates on loans for 100% of eligible project costs.

The Water Infrastructure Finance Authority of Arizona implements three types of technical assistance:
1. Project Technical Assistance – Planning and Design Assistance Grants assist an individual drinking water or wastewater system to conceive, plan, design, or develop an infrastructure project.
2. Policy Technical Assistance – Policy TA includes studies, surveys and other types of reports that provide benefit to a range of drinking water and wastewater systems statewide.
3. Operational Technical Assistance – The Arizona Department of Environmental Quality manages this program to provide assistance to individual drinking water and wastewater systems to improve facility operations.

The Drinking Water State Revolving Fund IUP describes WIFA’s plan to utilize various sources of funds to finance drinking water infrastructure and support related program activities during the State FY funding cycle from July 1 through June 30. This plan is a required element of the grant application documentation to obtain the grant award. Arizona herewith submits its IUP for the funds available to Arizona for the purposes of continuing the development, implementation and administration of the DWSRF program in Arizona.

The Intended Use Plan describes WIFA’s plan to utilize various sources of funds to finance clean water infrastructure and support related activities during the State FY funding cycle from July 1 through June 30. This plan is a required element of the grant application documentation to obtain the grant award for the purposes of continuing the development, implementation and administration of the Clean Water State Revolving Fund program in Arizona.

The Water Infrastructure Finance Authority of Arizona is an independent agency of the state of Arizona established to finance the construction, rehabilitation, and improvement of drinking water, wastewater, wastewater reclamation, and other water quality projects. WIFA operates as a “bond bank” and has the authority to issue bonds on behalf of communities for basic water infrastructure.

Some of the richest helium-bearing gas in the world was produced in Arizona. Helium concentrations range from trace amounts up to ten percent in the Holbrook Basin and Four Corners. Both areas have good potential for additional discovery and production of helium. Includes metadata for the monthly, annual, and cumulative summary reports of oil, gas and helium production by Arizona drilling fields.

The purpose of this research project is to determine the origin of the materials used to construct the Black Hills Dam in order to restore the landscape to pre-dam conditions. The Black Hills Dam site is located in northern Scottsdale, Maricopa County, at 33.75° North, 111.80° West. The goals of this project are to characterize the surficial deposits and local geology of the dam site. This report presents our findings, interpretations and conclusions based on background research, a site visit to the dam site, and technical discussions with the City of Scottsdale engineer and planners.

This open-file report describes the carbon-sequestration potential at the site of the 1 Alpine-Federal geothermal test drill hole, which is located south of Springerville in central eastern Arizona near the New Mexico border. A previous report, Arizona Geological Survey (AZGS) Open-File Report OFR 94-1, version 2.0, describes the subsurface geology encountered in the 1 Alpine-Federal well in much more detail than this new report.

This report details geothermal resource exploration done for Arizona Public Service and the U.S. Department of Energy in 2005 to evaluate the geothermal resources of the Clifton Hot Springs area in Greenlee County, eastern Arizona for electric power production. The intent of the evaluation was to determine the local geologic controls of the geothermal system and, using publicly available data and original mapping performed for this project, to recommend locations for Controlled Source Audiomagnetotelluric (CSAMT) cross sections. The results of the geophysics were then combined with the geologic mapping to site three gradient holes, two of which were drilled to depths of 635 feet and 1,000 feet, respectively.

To provide insight into provenance relations for multiple mid-Oligocene to mid-Miocene subbasins
(typically half-grabens) dissected by erosion in uplands lying north of the Catalina core complex and west of the San Pedro trough, 136 outcrop counts were made of clast types in tilted conglomerates of the Cloudburst and San Manuel Formations and their lateral equivalents in exposures as far north as the Gila River near Kearny. Clast counts were not made for younger conglomerates of the post-mid-Miocene Quiburis Formation, which fills the San Pedro trough and onlaps flanking uplands (Dickinson, 1998), because Quiburis clast assemblages in all cases match bedrock sources exposed uphill on the modern landscape. By contrast, paleotopography during Cloudburst and San Manuel deposition can only be inferred from local paleocurrent indicators (clast imbrications; figure 39 of Dickinson, 1991, p. 70-71) and clast assemblages in tilted strata. Areas included in this study were the Guild Wash allochthon between the Tortolita and Suizo Mountains, the Star Flat allochthon on the east flank of the Black Mountains, the
Black Hills (west of Mammoth), Camp Grant Wash (and Putnam Wash) between the Black Mountains and the Black Hills, multiple drainages of the Tortilla Mountains (Eagle Wash, Jim Thomas Wash, Hackberry Wash, Indian Camp Wash), and Ripsey Wash on the west flank of the Tortilla Mountains (Figs. 1-4).