The Arizona notary law was amended in 1996, 1997, 1999, 2000, and 2004. The 1996 amendments comprised the first major revisions of the notary law in Arizona in more than 50 years. Rules, effective August 25, 2004, are included in this manual which contains:

* A question and answer section
* Notary laws
* Rules
* Instructions for completing a notary application form
* An application form
* Name/Address form
* An index

This publication contains lobbying definitions, statutes, and lobbyist forms for those interested in how to register as a lobbyist and file with our office. This booklet helps explain how to register and file lobbyist reports with the Election Services Division. Included are deadlines, instructions and reporting requirements – all at your fingertips for quick reference.

The Secretary of State’s Office publishes this manual as a guide for Arizona notaries. Revisions to this manual include concise explanations of how to apply with our office, how to purchase a notary bond, information about your commission, duties as a public official, samples of notarial acts, and the laws and rules that govern Arizona notaries. Arizona notaries are required to have a copy of this manual and keep it as a reference.

This handbook is chiefly intended to help political committees at the state level to understand and comply with the laws of the state relating to campaign finance reporting and to provide some technical assistance and practical guidance on how to use the Secretary of State's campaign finance software to facilitate such reporting. Much of this handbook may be useful to political committees in other Arizona jurisdictions as well.

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.