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harte gold corp (HRT) Details

Harte Gold Corp., an exploration stage company, acquires, explores, and develops mineral resource properties in Canada. The company primarily focuses on gold properties. It owns 100% interests in the Sugar Zone property comprising 414 contiguous claims covering an area of approximately 29,300 hectares located northeast of the Town of White River, Ontario; and the Stoughton-Abitibi property with 90% interests in 9 claims and 100% interests in 25 claims located to the north-east of Kirkland Lake, Ontario. The company was formerly known as Harte Resources Company and changed its name to Harte Gold Corp. in December 2003. Harte Gold Corp. was incorporated in 1982 and is headquartered in Toronto, Canada.

Founded in 1982

harte gold corp (HRT) Top Compensated Officers

Chairman, Chief Executive Officer, President,...
Total Annual Compensation: --
Chief Financial Officer
Total Annual Compensation: --
Vice President of Exploration and Director
Total Annual Compensation: C$100.0K
Compensation as of Fiscal Year 2013.

harte gold corp (HRT) Key Developments

Harte Gold Corp. Discovers Hemlo Style Sericite Schist Shear Zone Along Contact Zone

Harte Gold Corp. announced the discovery of a new mineralized zone east of the Sugar Zone Deposit and to provide an exploration update on Harte Gold's 100% owned Sugar Zone property located north-east of White River, Ontario. Hemlo style sericite schist shear zone located along Contact Zone west of Sugar Zone Deposit. Bedrock grab samples taken along an 800m strike length east of the Sugar Zone Deposit range from 2.82 g/t Au to 277 g/t Au and from 2.92 g/t Au to 11.5 g/t Au from a potential Sugar Zone Deposit southern extension. Phase 3 Induced Polarization /Magnetic survey completed. Drill program will target Contact Zone and Sugar Zone extension targets and in-fill drilling on Jewelry Box Bulk Sample test area. The recently completed Phase 3 IP/Mag survey extended coverage to the north, south and west of the IP/Mag survey areas completed earlier this year. Five parallel structures have been traced over distances of up to 2 kms within a 600m wide corridor west of the Sugar Zone Deposit. IP anomalies include a trend with anomalous gold, antimony, arsenic and tungsten as well as a Hemlo style sericite schist shear zone with anomalous arsenic values that follows a topographic depression, along the Contact Zone. A recently completed geological mapping and sampling program collected 1,620 rock samples of which 569 samples were sent for assay. Assay results range from trace to 277 g/t Au and located a mineralized quartz vein east of the Sugar Zone Deposit which returned assays ranging from 2.82 g/t Au to 277 g/t Au from surface bedrock grab samples. Additional bedrock samples from an area approximately 800m south returned assays ranging from 2.92 g/t Au to 11.5 g/t. Harte Gold sees potential to add a new lense and increase the strike length of the Sugar Zone Deposit through follow up drilling on these zones. Much of the sampling program covered areas of the property that have not been previously explored. Results are not necessarily representative of the average grade of mineralized zones on the property. Harte Gold conducted a recent site visit with mine contractors to establish the location of the portal and finalize surface infrastructure for its planned Sugar Zone Mine. Underground development lay-outs are currently being completed and final contractor pricing is anticipated prior to year end. Subject to finalizing financial arrangements for the mining program, Harte Gold anticipates underground development to begin in June, 2015. The final holes drilled under the summer 2014 reconnaissance program; DZ-14-38 - DZ 14-45 were focused on parallel structures east of the Middle Zone and Wolf Zone and returned no significant gold values. A Phase 2 diamond drill program of up to 5,000m will test the down plunge extension of the Wolf Zone, Sugar Zone Deposit extension and Contact Zone targets.

Harte Gold Corp. Announces Results from the Phase I Exploration Diamond Drilling Program at its Sugar Zone Property, North-East of White River, Ontario

Harte Gold Corp. announced further results from the Phase I exploration diamond drilling program that commenced August 5, 2014 on Harte Gold's 100% owned Sugar Zone property located north-east of White River, Ontario. A total of 17 shallow holes have been completed with the objective of defining a plunging zone (lens) of gold mineralization within the Wolf Structural Zone (WSZ). Currently estimated at 125 - 175m in length, this lens is open at depth and features a 70 degree westward dip and steep southward plunge. It is anticipated a series of lenses or zones occur along the 2,100m long WSZ. ICP assays confirm similar arsenic levels in the Middle Zone to those seen in the Peacock boulders and parts of the Wolf Zone. Often associated with gold mineralization, arsenic was a key pathfinder element in the Hemlo gold camp. Given the elevated arsenic it is interpreted that a larger gold system is located down plunge from the surface occurrences. Future drilling in Phase 2 will test targets at depth. A recently completed structural geology report and exploration to date confirms the Sugar Zone Deposit, Wolf Zone, and new Middle Zone are situated in a lower volcanic basalt sequence host. The sequence starts with mafic- ultramafic (basalt) rocks on the east side of the Wolf Zone Structure, evolves from basalt to felsic volcanics west of the Wolf Zone Structure before turning into sediments along the eastern shoreline of Lake Dayohessarah. Historical boulders that occur on the western edge of the volcanic package that hosts the Sugar Zone Deposit, Wolf Zone and Middle Zone have been found to have come from a distance of no more than 400m. Harte Gold anticipates the source of boulders in the Contact Zone will be a similar distance. Harte Gold will conduct a 40 km Induced Polarization /Magnetometer ("IP/Mag") survey over the Contact Zone area west of the Wolf Zone Structure in October. The IP/Mag survey, together with mapping and prospecting are intended to locate Hemlo style shear zones that may occur along the sediment-volcanic contact. A Phase 2 diamond drill program of up to 5,000m scheduled for later October, will focus on down - plunge extension drilling on the Wolf Zone, the WSZ and the Contact Zone. The next phase of road work and site development related to the 70,000 tonne bulk sample is underway.  Drill core was logged in Harte Gold's secure core facility in White River, Ontario. Samples were hand delivered to the AGAT preparation lab in Thunder Bay where they were crushed and pulverized and sent to the Mississauga lab for analysis. Samples within the Wolf Zone were fire assayed using a 30 gram representative sample and finished with ICP analysis. Additional ICP analysis was done for pathfinder elements. For quality control and quality assurance a standard sample was inserted every 20 samples during the program and a blank sample was also inserted every 20 samples, however, within the mineralization a blank was also inserted after every sample. Samples exceeding 1 gram /tonne Au were re-assayed, in cases where visible gold is abundant, metallic screen analysis is used. R.S.

Harte Gold Announces Completion of Phase Two IP Survey

Harte Gold Corp. announced the completion of the expanded Phase Two Induced Polarization survey on the Sugar Zone Property, located 60 kilometers east of the Hemlo gold mines currently being operated by Barrick Gold Corporation. Phase Two IP Survey: The survey was successful in identifying significant extensions to the five high priority IP anomalies located 'up- ice' of the Peacock boulder train identified in the Phase One survey. In addition, significant extensions to both the Wolf Zone and the Sugar Zone Deposit were discovered, as well as several new IP anomalies en echelon to each of the Wolf Zone and Sugar Zone Deposit. The five high priority IP anomalies were traced an additional 700 meters to the north. These IP anomalies are now 1,200 meters long while other parallel anomalies are 1,000 meters to 1,600 meters in length. Magnetometer Survey: A detailed ground Magnetometer survey has been completed over the entire grid covered by the two IP surveys. The Mag survey took readings every two meters and will assist in classifying the IP anomalies and help to define structures that are controlling mineralization and/or off-setting zones, as well as locate any younger mafic dikes (diabase dikes) that cut across the stratigraphy. In the course of cutting and traversing the grid, many newly discovered rusty boulders have been located as well as other angular sericitic slabs. A program of detailed mapping, boulder tracing and sampling, and a limited till sampling program will be carried out over the next three weeks prior to drilling in order to properly prioritize drill targets. This occurrence of mineralized boulders suggests there may be a number of bedrock sources for any new mineralization. Every IP anomaly found in the survey area will be tested in order to confirm mineral content.


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