Gold investment advantages and Starcore gold mining company: Much of the supply of gold in the market since the 1990s has come from sales of gold bullion from the vaults of global central banks. This selling by global central banks slowed greatly in 2008. At the same time, production of new gold from mines had been declining since 2000. According to BullionVault.com, annual gold-mining output fell from 2,573 metric tons in 2000 to 2,444 metric tons in 2007 (however, according to Goldsheetlinks.com, gold saw a rebound in production with output hitting nearly 2,700 metric tons in 2011.) It can take from five to 10 years to bring a new mine into production. As a general rule, reduction in the supply of gold increases gold prices.
Speaking of gold, it is easily the oldest form of currency in use on earth. It was used by our ancestors centuries ago and is still used today, its mention can even be found in the epics of Hindu mythology which highlights the position that gold holds in the Indian and especially Hindu culture. It is considered as a carrier of good luck and thus is gifted to the new brides and other important milestones of life as well. Therefore, one of the tools which are popular for this purpose is the financial investment which allows a person to multiply his savings by investing it into one of the multiple options available like mutual funds, real estate, gold etc.
Toiyabe contains at least two strongly mineralized fault zones with strong gold values on surface and in drilling. This evidence demonstrates the potential for gold-mineralizing fluids to travel from a deeper source through reactive, lower plate, carbonate rocks to the shallow mineralization encountered to date at Toiyabe. Several deeper drill holes have encountered low to moderate gold mineralization erratically distributed through comparable stratigraphy in nearby producing mines. Although the necessary structural complexities and traps required to host a large economic gold occurrence have yet to be encountered, a recent re-interpretation of stratigraphy and structure by Paul D. Noland indicates that this environment likely exists within the Toiyabe project boundary and may be responsible for at least some of the mineralization encountered within less favorable, upper plate lithologies. Read more info at leveraged to gold price.
Discovered in 2012 this area has been found to host several veins 1 – 5m thick generally dipping 20 degrees to the east and striking north/south. It has been found within 50 meters of main in the footwall of San Martin structure in the footwall which was previously thought to be exclusively shales. To date at least 4 veins have been found above level 4 in the northeast of San Martin and possibly 2 veins above level 2 further south. Some of the veins are vertical and some are dipping around 40 degrees. In general most are striking parallel to San Martin breccia.
Starcore International Mining and El Creston Property development news: The Alejandra Zone is located approximately 1 k to the northeast of the Creston Deposit. The area is underlain by oxidized and variably sericite altered Proterozoic Creston Granite and Laramide porphyry granite. The >100 ppm Mo in rock chip contour has defined two areas of interest referred to as the Alejandra East and West. In both areas molybdenum values are generally modest, 100-300 ppm, with occasional spot highs. The Alejandra West is up to 500 metres wide x up to 800 metres long. Within it rock chip samples assayed up to 0.102% Mo over 3 metres. The Alejandra East Anomaly is up to 800 metres long with width variable to 700 metres. The best rock chip assayed 0.256% Mo over 3 metres. Copper values are generally low throughout. The zone has not been drilled. Discover additional info at https://starcore.com/.
