By February of 1998, the Deloitte Consulting firm was under contract with the State of Arizona and had embarked upon what would become an extensive ten-month evaluation of the primary components of Arizona’s Juvenile Justice System. The main focus of the audit from the beginning was the Administrative Office of the Courts, the Juvenile Justice Services Division, the juvenile courts and their probation departments, and the Department of Juvenile Corrections. As part of the audit, both financial and program audits were conducted related to prevention, diversion (early intervention), probation and treatment. In December of 1998, Deloitte Consulting issued its final report to the Committee. The report, which consisted of hundreds of pages of detailed findings, concluded that “It is our assessment that the Arizona Juvenile Justice System is one of the best in the nation.”

The Renewing Arizona Family Traditions program responds to the needs of Arizona's youth and families by providing intensive, family-oriented services to court referred youth. This report reviews the successes as well as the opportunities for growth within the RAFT program and examines the program through a presentation of the data collected by the Administrative Office of the Courts through its contract providers and other sources. The data is recorded by provider agencies and their respective regions and includes intake and discharge/outcome information.

The data for this report are extracted each year from fourteen juvenile courts’ Juvenile On-Line Tracking Systems. JOLTS is the automated juvenile court information management system. After using JOLTS for more than 25 years, July 1, 2008, Maricopa County upgraded to their new Integrated Court Information System. Each juvenile court actively participates in collecting and maintaining the data to ensure quality and accuracy. This report provides an overview of the juveniles processed at various stages of the juvenile justice system statewide.

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.

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.

The goal of this study is to develop a method for identifying potential post-fire debris flow hazard areas prior to the occurrence of wildfires, providing more time for local governments and emergency planners to develop and execute hazard mitigation strategies. This pilot study focuses on the communities of Pine and Strawberry, which are located in forested canyons at the base of the Mogollon Rim in north-central Arizona. Results from this project will provide local agencies, emergency planners and land managers more effective tools for prioritizing watershed treatment areas and implementing mitigation measures to alleviate potential impacts and threats from post-fire debris flows to infrastructure, human life, and property in a timely and cost-effective manner.

In order to begin to assess debris‐flow hazards along the Santa Catalina Mountains in Pima County, we mapped the extent and character of relatively young prehistoric debris‐flow deposits in detail at fifteen
canyon mouths. Mapping was conducted on a scale of 1:6,000 using aerial photographs, detailed
topography, and field relationships. Deposits were classified into relative age categories based on
topographic relationships, soil development and surface characteristics of the deposits. Ages of selected
debris‐flow deposits in four canyons – Soldier, Sabino, Finger Rock and Pima – were estimated using
radiocarbon (14C) and cosmogenic (10Be) isotope methods.

Evidence of past debris flows were found in all fifteen canyons. Relative age dating, corroborated by
10Be, indicates the largest and most extensive deposits in all canyons are late Pleistocene to early
Holocene in age. Events from 2006 show that some potential exists for debris flows to exit the mountain front into developed areas near canyon mouths.