Northern Freegold Resources Ltd. announced results from the 2013 exploration program on the Freegold Mountain Project. The project is 100% owned by the company and is road accessible, located 70 km west of Carmacks in the Dawson gold belt of southwestern Yukon. The discovery zone consists of a number of porphyry, skarn, and epithermal showings and targets which collectively cover an area encompassing approximately seven square kilometres.

The objective of the 2013 program was to assess an area within the Discovery Zone historically known as the Northwest Zone. Geochemical surveys have previously identified a 150-250 metre wide by 1,700 metre long gold in soil anomaly (90th percentile) which is centered on the historic Melissa Showing. The geochemical surveys and trenching activities completed during 2013 were designed to ground truth historic soil values, provide multi-element geochemistry, and trench high priority geochemical targets.

The 2013 geochemical survey from the Discovery area has successfully delineated a 150 to 300 metre wide by 900 metre long west-northwest trending zone of coincident anomalous gold-silver-arsenic-bismuth-lead-antimony in soil east of the existing geochemical grid completed in 1986 and west of the geochemical grid completed in 2011. The total strike length of the anomalous gold zone (90th percentile) is currently defined up to 1,700 metres. This zone has never been drill tested.

Initial data analysis completed prior to 2014 field activities included compilation of historic drill hole assays and surface rock samples to identify elemental correlations with gold mineralization. These correlations were then used to determine which pathfinder elements would be used to delineate prospective exploration zones during post-field data analysis. The data analysis concluded that silver (Ag), bismuth (Bi), and arsenic (As) are strong pathfinder elements for gold mineralization, whilst lead (Pb) and antimony (Sb) are moderate pathfinder elements for gold mineralization, within the Northwest or Seymour Zone.

A total of 14.7 line kilometres of geochemical surveys totalling 590 B-horizon soil samples were collected during the program using soil augers. The 2013 geochemical survey from the Discovery area has successfully delineated a 150 to 300 metre wide by 900 metre long west-northwest trending zone of coincident anomalous gold (90th - 99th percentile), silver (90th - 99th percentile), arsenic (90th - 99th percentile), bismuth (75th - 99th percentile), lead (90th - 99th percentile), and antimony (75th - 99th percentile) in soil east of the existing geochemical grid completed in 1986 and west of the geochemical grid completed in 2011. The total strike length of the anomalous gold zone (90th percentile) is currently defined up to 1700 metres and has never been drill tested.

Two grab samples of quartz vein material, CRFGR003 and MMFGR036, collected from historic workings at the Melissa showing returned 1.72 gpt Au/13.7 gpt Ag and 0.43 gpt Au/9.9 gpt Ag respectively. These results are consistent with historic assays. A 5.0 metre chip sample of silicified etasediments collected from TR13-008 located 35 metres northwest of the Melissa showing returned 0.14 gpt Au and 6.0 gpt Ag.

The chip sample results are also consistent with historic trench results completed in 2004. All samples were submitted to ALS Minerals in Whitehorse for prep and geochemical analysis. The following analytical techniques were used for all rock samples: ME-ICP41, Au-AA23 30 g Fire Assay, and Au-GRA21 30 g Fire Assay for all samples 10 ppm Au.

The following analytical techniques were used for all soil and silt samples: ME-MS41, Au-TL44, and Au-OR44 for all samples 1 ppm Au. The company QAQC measures included insertion of external blanks and standards into the sample stream for all rock chip samples. A minimum of one standard and one blank sample was inserted for each trench containing multiple chip/channel samples.

In addition, the lab was instructed to wet-sieve each sample prior to sample preparation in order to minimize contamination from placer gravels.