Undervalued gold company in Mexico and investing in gold advantages: Return rates of physical gold are never profitable if you invest in the gold jewellery. The reason being that the price of jewellery is not only determined by the gold rates but it also includes the making charges and this is the just the half story i.e. when you purchase the gold. Now, when you sell the gold, the story is totally different, the making charges are not considered and you get the money only for the pure gold based on the gold rates of that particular day. Take for example; the gold rate in Mumbai during December 2015 was 27000 Indian rupees for ten grams of 24 karat gold and assuming that you bought a gold necklace of 20 grams for about 60,000 Indian rupees which include the making charges too. Now, due to some reason you want to sell it and you go to a shop who quotes the price only for the gold that necklace contains and not for the stones it has or the copper which weighs it down to only 13grams and the cost of 13 grams of pure gold in 2020 is only 40000 Indian rupees in 2020, obviously, it is a loss deal for you and thus, poor return rates are one of the downsides to keep in mind while investing in physical gold.
Starcore International Mining and El Creston Property development news: The Red Hill Deep Zone refers to a 750 metre long x up to 400 metre wide and open zone of molybdenum and copper mineralization hosted within Laramide intrusive breccia and quartz monzonite porphyry located at depth below the eastern half of the Red Hill Zone. The top of the zone is in part above the bottom of the proposed open pit. Eight drill holes have tested the zone. Results include a 241.35 metre section averaging 0.088% Mo commencing at a downhole depth of 253.15 metres. Find additional details at How to invest in gold.
Lower plate carbonate rich sediments are exposed below the Roberts Mountain Thrust within an area called the Cortez window. These lower plate sediments host over 90% of the gold found within the Carlin and Battle Mountain- Eureka trends. In the Toiyabe project area gold mineralization is hosted within a similar geologic setting. The stratigraphy, structure and alteration are analogous to that found at nearby Cortez, Cortez Hills, Pediment, Horse Canyon and Pipeline deposits.
High grade mineralization was discovered at San Martin in the 18th Century, and is reported to have been mined over a period of 40 years; however, no production records exist. Between 1900 and 1924, an estimated 250,000 tonnes grading 15 g Au/t and 100 g Ag/t was reportedly mined. Mineralization occurs in Upper Cretaceous black limestone and calcareous shales of the Soyatal Mexcala Formation as electrum, and silver selenide minerals principally associated with quartz and to a lesser degree with calcite. The deposit is an epithermal, probably high sulphidation precious metal (Ag-Au) type (metal ratio Au:Ag at 1:10), related to a Tertiary dacitic/andesitic intrusive dome. Read additional details on starcore.com.