An update to the Flagstaff Regional Plan 2030 (FRP30), to bring its Road Network Illustration (Map 25) into compliance with Arizona Revised Statute requirements and to resolve inconsistencies between Map 25 and parts of the Flagstaff City Code. This update does not alter the intent of FRP30; it is only concerned with correcting errors, removing legal vulnerability, and improving the readability of FRP30.

This report is a result of the "2002 Equitable Treatment of Minority Youth" report produced by the Arizona Supreme Court Commission on Minorities in the Judiciary. One of the recommendations issued in that report was to create an annual report card to assess progress on the reduction of over-representation of minority youth in the juvenile justice system. The decision has been modified to produce a report card every other year. The first report serves as a baseline for the second, third and fourth report cards. The intent is to illustrate the current situation, provide a basis for future comparison, highlight areas of special concern and compare these results with the prior report card.

This report represent the efforts of the Commission since its reactivation under a new mandate in May of 1994. The goal of this work group is to develop policies and programs that will facilitate the growth of minority applicants seeking appointments as judges, commissioners, judges pro tempore, special masters, clerkships, and internships.

Shortly after selecting Judge Roxanne Song Ong as Commission Chair and reconstituting its membership, Chief Justice McGregor directed the Commission to develop a strategic plan with projects that seek to enhance fairness and equity in the judiciary and present a report at the December 2006 meeting of the Arizona Judicial Council.

The conference looked beyond the juvenile justice system proper to examine the roots and potential solutions to the over representation of minority youth in Arizona’s juvenile justice system. Through this important undertaking and the dedication of the Commission on Minorities, Arizona demonstrated once again its important role as a leader in shaping the future of the juvenile justice system.

A series of small earth movements occurred along the slopes of State Route 87 at about mile marker 224 (between the Bush Highway and Route 188) throughout the winter of 2007‐2008, culminating with a landslide on Friday, 21 March 2008. This landslide buckled the southbound lanes, displaced the northbound lanes, and closed the highway for nearly a week. The mass movements occurred on slopes that were constructed with re‐vegetated, laid back slopes; soil nail walls; and rip rap‐lined channels. However, our reconnaissance mapping indicates that most, if not all, of the slope movements are located within a much larger, older landslide adjacent to, and cut by, SR‐87. No specific trigger for the landslides was immediately apparent, although a combination of factors (e.g., precipitation, groundwater levels, etc.) may have contributed to conditions for the slope failure. Headscarps of various types of landslides are present along both sides of the highway. Results from our preliminary investigation indicate that up to three other paleo‐landslides may be present in the immediate vicinity. The full extent and nature of these landslides are unknown and require further investigation to evaluate their potential to be reactivated and risk they pose to the highway.

This field trip guide was created for a Project WET conference held in Tucson, Arizona, June, 2007. This guide discusses the general geology of the Santa Catalina Mountains in Sabino Canyon, and points out evidence of the July 2006 floods and debris flows. There are stops in the first few miles of canyon, and towards the end of the tram road, where the most spectacular debris flows are located.

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.