Noble Mineral Exploration Inc. announced that it has acquired 677 claims through staking, to cover the Nagagami Carbonatite/Alkalic Complex, located about 65 kilometers Northwest of Hearst Ontario The staked area is equivalent to about 1,400 hectares or 140 square kilometers. Recent research by Noble indicated remarkable similarities between the niobium producing Niobec Mine and the Nagagami Complex. The Niobec Mine now owned by IAMGOLD started commercial production of niobium pentoxide in 1976. It is one of the major sources of niobium in the world and North America's only source of pyrochlore. It currently produces around 7%- 8% of the niobium used globally. Niobec also has a resource in rare earth metals. A study of the magnetic data for the Nagagami Complex and the Niobec Mine both indicate a donut shaped structures with syenitic rocks forming the circular magnetic high with carbonatitic rocks forming the central magnetic low. At Niobec, it is in the central magnetic low where the Niobium and Rare Earth mineralization is hosted. Recently the Ontario Government, along with the Canadian and World governments have implemented policies in order to stimulate the search for strategic and critical metals that are in short supply due to the worldwide push for clean energy, battery, and communication technology. To promote this, the Ontario Government has launched the Ontario Junior Exploration Program to help Mining companies explore for these metals in Ontario through grants. Noble will apply for the Ontario grant on the Nagagami project. Previous work in the Nagagami area has been spotty due in part to the fact that the complex is not exposed on surface. Algoma Ore Properties performed the original airborne magnetic survey in the area that Identified the complex. Limited drilling was aimed at the magnetic ring structure in search of iron deposits. Despite drilling in the wrong geology for niobium and rare earth metals, one of the Algoma drillholes returned an assay of 0.3% Nb205 from a grab sample of syenite taken at 230 feet. Fluorite was noted in one drill hole as red-brown, waxy hydronephelite (an alteration form of nepheline) comprising 5-10% of the rock. The existence of fluorite is characteristic of carbonatite style mineralization. About 4.5 kilometers south of the Nagagami Complex, Zenyatta Ventures is developing the Albany graphite deposit. The Albany deposit is classed as one of the larger known hydrothermal graphite deposits in the world. Hydrothermal graphite is the purest, but also the rarest, form of graphite. The graphite mineralization here appears to be related to the emplacement of the Nagagami complex resulting in the possible occurrence of similar mineralization and geology on the Noble property.