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Nevada Exploration Provides Grass Valley Project Update with McEwen Mining Inc.

VANCOUVER, BRITISH COLUMBIA--(Marketwired - Aug. 12, 2013) - Nevada Exploration Inc. (TSX VENTURE:NGE) ("NGE") is pleased to provide an exploration update on the Grass Valley Project and to announce that McEwen Mining Inc. has elected to continue the Project.

Background and Project Description

In February 2012 McEwen Mining and NGE began working together under an Exploration Agreement to generate new gold projects using NGE's proprietary hydrogeochemistry (groundwater chemistry) exploration technology within a 25,000 hectare (95 sq mi) study area in Grass Valley in north central Nevada (the "AOI"), south of Barrick Gold Corp's Cortez Hills Gold Mine. During the year, McEwen Mining and NGE completed a hydrogeochemistry sampling program across the large AOI, and delineated a large, previously unexplored target area on the west side of Grass Valley based on a NNE lineament of upwelling groundwater containing anomalous concentrations of gold and other trace elements associated with Carlin-type mineralization.

When evaluated in the context of the regional geology, the hydrogeochemistry results suggested a possible underlying mineralized fault system projecting northward towards Cortez Hills, and in September 2012 McEwen Mining elected to acquire the Grass Valley Project as a Designated Project under the Exploration Agreement. The Grass Valley Project consists of approximately 59 sq km (23 sq mi) of unpatented mining claims along the west side of Grass Valley.

Exploration Update

Since acquiring the Grass Valley Project, McEwen Mining has advanced the Project by: collecting rock, soil, and vegetation geochemistry samples; mapping the exposed range front geology in the context of the regionally important structural controls; completing a detailed gravity geophysics survey; and acquiring and reprocessing historic seismic geophysical data. During this time, NGE has also completed additional groundwater sampling.

While the spatial extent of the rock, soil, and vegetation geochemistry sampling was limited to several small areas, the results show localized concentrations of elevated gold and trace element chemistry along areas defined by anomalous hydrogeochemistry in patterns that further suggest the presence of NNE trending structural zones beneath the project area.

At the project scale, the geologic mapping along the exposed range front identified upper plate rocks with widely-scattered, small areas of hydrothermal alteration coincident with anomalous gold and trace-elements in the rock geochemistry samples. At the district scale, four miles to the west of the Project, windows through the upper plate have exposed lower plate rocks hosting a small Carlin-type gold deposit at the Toiyabe mine. Several of the SSE trending folds exposed in the mountains surrounding the Toiyabe mine project beneath the Grass Valley Project area, where they intersect the major inferred NNE structural zones. Together, the local and district scale mapping suggest the possibility that the lower plate rocks associated with mineralization at Cortez Hills to the north and Toyiabe to the west could also be present at economic depths at the Grass Valley Project.