Gold producer Mexico with Starcore.com? Storing physical gold has the same security threats as any cash in our house. It is equally vulnerable to theft as anything else in our house and thus, the investors have to be more cautious for their assets when investing into gold. although going for some other form of gold investment like gold ETF or fund of fund is a better way to go but this way too, you are not totally secure, you are vulnerable to internet security attacks but the difference here is that this security is threat is equally likely to happen to anyone or even everyone and even other investments too like mutual funds etc.
Deflation is defined as a period in which prices decrease, when business activity slows and the economy is burdened by excessive debt, which has not been seen globally since the Great Depression of the 1930s (although a small degree of deflation occurred following the 2008 financial crisis in some parts of the world).. During the Depression, the relative purchasing power of gold soared while other prices dropped sharply. This is because people chose to hoard cash, and the safest place to hold cash was in gold and gold coin at the time.
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. Find more details on best gold investment.
The Ajax Property occurs along the western margin of the Stikinia Terrane of the North America Cordillera, immediately adjacent to the eastern margin of the Coast Plutonic Complex. The property is underlain by Jurassic Hazelton Group rocks consisting primarily of argillaceous sediments and minor interbedded andesite tuffs that locally has been intruded by four closely spaced stocks of quartz monzonite porphyry. The Ajax deposit occupies a rectangular area approximately 650 m x 600 m that ranges in elevation from 425 masl to 1050 masl. The mineralization is predominantly pyrrhotite and lesser molybdenite that typically comprises less than 2% of the rock by volume. Molybdenite is typically associated with quartz and occurs in pyrrhotite-bearing veinlets, in thin stringers and on fracture and shear surfaces. Areas of elevated molybdenite grades (>0.060% Mo) are characterized by a high fracture density where quartz vein stockwork is well developed. Lower grade material (0.030 to 0.060 % Mo), is found in areas of weaker fracturing and forms a broad halo around the higher grade zones, especially below the 762 m elevation contour.
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. Find more details on https://starcore.com/.