Been invested since 2015. Watched one financial investing guru talk-up Redstar to investors--many who proceeded to put $10,000 USD chunks into the stock--which was the time it went to .12 cents/USD. Then the bottom fell out with Ball's drilling: which doubled the district scale size, but delivered small grams/ton AU results. Then those same investors dumped it when it went to .06 before settling near ,02 cents per share NYSE.
Anyways, these are to me stellar starting poings of the new drilling program. Just my opinion. Reminds me of Continental when I was in on the ground floor before the Chinese bought it out and I sold. That one went from .40 cents to $4.10 USD at the buy-out close.
Vancouver, Canada, January 25, 2021 – Heliostar Metals Limited (TSX.V: HSTR, US: RGCTF, FRA: RGG) ("Heliostar" or the "Company") is pleased to announce results from the first two of nine holes completed at the SH-1 Zone in its 2020 exploration program at the Unga project in Alaska.
Heliostar CEO, Charles Funk, commented “These excellent results demonstrate the high gold grades contained within the SH-1 zone at Unga. SH-1 is the most advanced target at Unga with 384,318 ounces of gold at 13.8g/t and is open to expand. Assays are pending for the remaining seven holes completed at SH-1 in 2020 and the resource is expected to grow. Unga received very little exploration in the last 40 years. However, it has several exciting, high-grade gold targets. Heliostar will continue to aggressively explore the property in 2021 with a goal of defining resources in excess of one million ounces.”
Drilling Highlights
SH20-01A
· 7.74 grams per tonne (g/t) gold and 27.0 g/t silver over 11.65 metres (m) from 12.95 m downhole including;
· 16.06 g/t gold and 37.7 g/t silver over 4.0 m from 12.95 m downhole
SH20-02
· 18.66 g/t gold and 11.5 g/t silver over 1.98 m from 50.75 m downhole
Note: All numbers are rounded and widths represent downhole lengths. True thickness is estimated at 80-85% of downhole thickness.
SH-1 Zone
SH-1 is a priority target at Unga. It holds a high-grade inferred resource containing 384,318 ounces gold at a grade of 13.8 g/t and has significant potential for expansion with high grade intercepts open along strike and at depth. The resource is centred on the Main Shoot, which is well defined by tightly spaced drilling, but is loosely defined by widely spaced drilling outside of this zone.
A 100-metre vertical gap existed between surface and the first historical vein intercepts and in 2020, seven holes were completed to fill the blanks in our understanding of the rocks around the upper portions of the Main Shoot. The reported holes are 50 metre step outs on previously completed drilling. Based on previous drilling, it was possible to interpret both steep and shallow plunges to mineralization. These first results suggest a steeper orientation is more likely which emphasizes the potential for further resource expansion at depth.
The company also completed two deeper holes in 2020 to test depth extensions in areas of widely spaced drilling. The deepest completed hole to date at SH-1 intersected 23.99 g/t gold over 5.48 metres in hole BM-01 and the company will continue to infill these areas and expand to depth where the system remains open.
Drilling along strike from the Main Shoot indicates parallel zones of mineralization that remain open and will be tested when drilling recommences in late March.
SH-1 is one of multiple epithermal gold targets along the 8.4km long Shumigan vein corridor. It is the most advanced prospect at Unga with a high-grade inferred resource but has considerable potential for expansion.
The SH-1 inferred resource sits at the eastern end of the Shumagin vein corridor below an elongate hill formed by quartz veining and alteration associated with gold mineralization. At SH-1 the vein forms between rhyolite in the hanging wall to the southeast and andesite in the footwall to the northwest. The vein occurs as a multi-episodic quartz vein, with a core of competent brecciated quartz veining grading outwards through an intense to weak zone of quartz alteration. Gold and lesser silver mineralization is carried within the veins and strongly silicified zones and is usually found associated with the zinc and lead sulphides, sphalerite and galena.