Memorandum of Meeting at which Mr. H. T. Johnson, Assistant Secretary of the Navy, Installations and Environment (ASN (I&E)), met with Mr. Chris Paul, Military Legislative Advisor to Senator John McCain (R. Ariz.), at 1315 in Room 4E523 at the Pentagon. Commander Edward W. Brown, USN, Legislative Liaison; Commander Fred Latrash, USN, Office of Senator John McCain (R. Ariz); Commander Robert E. Vincent 11, JAGC, USN, IAT Recorder; and Captain James A. Noel, USMC, IAT Recorder, were present as well.

Executive Correspondence - Letters from State of Arizona Governor Janet Napolitano to the Commissioners regarding the relocation of the Air Force Lab in Mesa Arizona

Executive Correspondence – Letter dtd 08/10/2005 to Chairman Principi from Lee Wegner, Chair of the Dept of Laboratory Medicine & Pathology urging the BRAC Commission to remove the AFIP from the list of military facilities slated for closure.

DISREGARD RESTRICTION HEADER AND FOOTER - Yuma Proving Grounds Installation Familiarization Briefing

Abstract: Structure drilling under Contract No. AT(05-l)-120 was begun May 13, 1951, and was suspended June 30, 1951, at Red Rock, Arizona with the completion of 12 holes and 2,390.5 feet of drilling. No mineralization was disclosed in the widely spaced holes. The structure and rock composition was found favorable for a potential drilling area.

Abstract: A drilling program was conducted by the Atomic Energy Commission on Cove Mesa, Arizona to further develop uranium and vanadium ore reserves that are vital to the National Defense. The drilling was performed by the Minerals Engineering Company of Grand Junction, Colorado. Uranium and vanadium ore horizons are found in the Salt Wash member of the Morrison formation on Cove Mesa.

The tabulations on these pages include all of the known areas in Colorado, Utah, New Mexico, and Arizona having economically important uranium-vanadium deposits of the type which are generally referred to by the terms roscoe-lite and/or carnotite. Though similar deposits are known to exist in other areas they are to be viewed as being little more than mineralogical curiosities.

From abstract: Mesa V of the Lukachukai area is capped by Morrison sediments which dip gently eastward from the mountains to the mesa tip, where the strata are tilted sharply to the opposite dip by the Lukachukai monocline. The Salt Wash of Mesa V contains ore outcrops which indicate favorable intensity of mineralization at one horizon along a 2000-foot outcrop interval. Other scatted exposures indicate the existence of ore under much of the mesa surface.