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Clean Energy Transition Inc V.TRAN

Alternate Symbol(s):  GCRIF

Clean Energy Transition Inc. is focused on opportunities to generate positive cash flow, across the energy transition. The Company includes a Quartz division focused on advancing its silica/quartz business with the Snow White Project in Ontario and the Silicon Ridge Project in Quebec. The silica in high-quality quartz can be used to make silicon metal, a key component in solar energy panels. The Snow White project is located in northern Ontario, 500km north-northwest of Toronto, 105km west of Sudbury. It is just over 40km by road from the town of Massey- 25km on highway and 15km on logging roads. The property comprises ten claim units within three staked unpatented mining claims totaling approximately 160 hectares. The Silicon Ridge Project is located approximately 40km north of the City of Baie-Saint-Paul, which borders the north shore of the Saint Lawrence River in central Quebec. Baie-Saint-Paul is about 100km northeast of Quebec City and approximately 350km northeast of Montreal.


TSXV:TRAN - Post by User

Bullboard Posts
Post by LeMarcuson Sep 11, 2017 3:07pm
144 Views
Post# 26681217

Joburke Mine : (produced 430Kt @ 3.63gpt)

Joburke Mine : (produced 430Kt @ 3.63gpt)
Joburke gold mine (MacKeith Lake mine), Keith Township, Cochrane District, Ontario, Canada
[url=https://www.google.com/maps/place/48%C2%B008'50.0%22N+82%C2%B017'00.0%22W/@48.1477161,-82.2873137,16z/data=!4m5!3m4!1s0x0:0x0!8m2!3d48.1472222!4d-82.2833333]Joburke Mine on a Map: That around 5 km west of Radio Hill iron formation (on strike with PDFZ)[/url]

ttp://www.geologyontario.mndmf.gov.on.ca/mndmfiles/mdi/data/records/MDI42B01NW00002.html

About Joburke
The property is underlain by a diverse array of metavolcanic rocks and interbedded metasediments and iron formation. Rock units dip steeply to the north and strike northeast, north of the MacKeith Lake fault and southeast, south of the fault. The stratigraphy consistently faces north. The fault zone surrounding the MacKeith Lake fault contains brecciated fragments of chert, iron formation, lamprophyre and talc chlorite schist
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