The HSM conductance anomaly is approximately 1,400 m in length by 350 m in width or approximately 45 hectares in size and is located 1 km south of the Robin’s Place kimberlite (news release of November 24, 2020). As per the image in this news release, the new HSM kimberlite, along with the Paradis Pond and Robin’s Place kimberlites are spatially associated with the Cross Lake Fault Structure, while the Gleeson kimberlite appears to be associated with a SW/NE fault structure.

Three drill holes were completed to test this anomaly, all of which returned kimberlite intersections. Drill hole HSM- 20-01 intersected 14.45 m of kimberlite. Drill hole HSM-20-02 was located 325 m to the northwest of hole HSM-20-01 and intersected 48.2 m of kimberlite before being lost due to difficult drilling conditions. Drill hole HSM-20-03 was located 340 m to the north-west of drill hole HSM-20-02 and intersected 18.1 m of kimberlite. The HSM kimberlite is a tuffisitic kimberlite breccia with a monticellite-rich microcrystal matrix with accessory concentrations of phlogopite and ilmenite xenocrysts.

Additional in-fill drilling is required to further define the boundaries of each of these conductance anomalies.

Glenn Kasner, President of RJK stated, “The discovery of a fourth kimberlite on the Bishop property, in addition to the Kon kimberlite discovered earlier in the year, is remarkable. All members of our team had a geology professor some 45 years ago named Dan Atchinson, who first told us about the Nipissing Diamond. It was his hope that a graduate would find the source kimberlite pipe. RJK’s management are all graduates of the Haileybury school of Mines (HSM), and so we have named this new discovery the HSM Kimberlite.”

Mr. Peter Hubacheck, P. Geo., Project Manager for RJK and the Qualified Person as defined by National Instrument 43-101 has approved the geotechnical disclosure in this release.

Contact Information:

Glenn Kasner, President

Mobile: (705) 568-7567

info@rjkexplorations.com

Web Site: https://www.rjkexplorations.com/

Company Information: Tel: (705) 568-7445

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Forward Looking Information

This news release includes certain forward-looking statements, which may include, but are not limited to, statements concerning future mineral exploration and property option payments. Any statements contained herein that are not statements of historical facts may be deemed to be forward-looking, including those identified by the expressions “will”, “anticipate”, “believe”, “plan”, “estimate”, “expect”, “intend”, “propose” and similar expressions. Forward-looking statements involve known and unknown risks and uncertainties that could cause actual results, performance, or achievements to differ materially from those expressed or implied in this news release. Factors that could cause actual results to differ materially from those anticipated in this news release include, but are not limited to, the financial resources of the Corporation being inadequate to carry out its stated plans. RJK assumes no obligation to update the forward-looking statements or to update the reasons why actual results could differ from those reflected in the forward-looking statements except as required by applicable law.

The post RJK DISCOVERS ITS FOURTH KIMBERLITE AND LARGEST INTERSECT ON THE BISHOP PROPERTY appeared first on RJK Explorations Ltd..

Notes:

1. This map includes results from the 2019 KIM sampling program only. The results confirmed the sampling reports completed by the Bishop family south of Grassy Lake between 2014 and 2018, which returned abnormally high amounts of KIMs in concentrate. Select grains from that concentrate confirmed presence of KIMs in probing.
2. Two kimberlite boulder samples were discovered down-ice from the Grassy Lake target, both nearby the KIM sample locations.

G9 & G10 Garnets

Notes:

1. Traditionally, G9 and G10 garnets have been used to determine the potential for diamonds in their kimberlite sources.  Like Ilmenites, their chemistry is very important, as specific types are generally correlated with diamondiferous pipes.

Eclogitic Garnets

Notes:

1. Discovery of Eclogitic Garnets was an important step in determining that De Beers’ Victor kimberlite pipe contained economic diamonds. Eclogitic garnets are believed to originate very deep within the earth’s mantle, where larger diamonds are believed to be formed.
2. The Victor Mine won a “Mine of the Year” award in 2008, paying back its entire $1 Billion Capex in year one.  It was previously in production for 12 years, producing very high quality diamonds.

Chrome Diopsides

Notes:

1. Chrome Diopsides generally disintegrate the fastest of all KIMs, and therefore historically tend to indicate proximity to a kimberlite source.

Ilmenites

Notes:

1. Ilmenite chemistry is very important when determining the odds of diamonds in the kimberlite origin, as specific chemistry types are highly correlated world-wide with diamondiferous kimberlite pipes.

Chromites

Forsterite

KIMS Over Geology

Notes:

1. Rocks in two locations down-ice from Grassy Lake were found and are believed to be kimberlite.
2. The red dot locations indicate where samples were taken, but in the field, they’re not weighed.  The samples are normalized in the lab to 10kg for consistency, and sometimes multiple till samples close to each other are combined to total 10kg of till.

KIMs Over Topography

Notes:

1. Rocks in two locations down-ice from Grassy Lake were found and are believed to be kimberlite.
2. The red dot locations indicate where samples were taken, but in the field, they’re not weighed.  The samples are normalized in the lab to 10kg for consistency, and sometimes multiple till samples close to each other are combined to total 10kg of till.

The post Bishop North Lorrain KIM Maps appeared first on RJK Explorations Ltd..