Gold producer in Mexico and investing in gold advantages: Although the U.S. dollar is one of the world’s most important reserve currencies, when the value of the dollar falls against other currencies as it did between 1998 and 2008, this often prompts people to flock to the security of gold, which raises gold prices . The price of gold nearly tripled between 1998 and 2008, reaching the $1,000-an-ounce milestone in early 2008 and nearly doubling between 2008 and 2012, hitting around the $1800-$1900 mark. The decline in the U.S. dollar occurred for a number of reasons, including the country’s large budget and trade deficits and a large increase in the money supply.
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.
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. Discover more details at best gold investment.
Mineralization is generally made up of breccia that commonly is concordant with a limestone/shale contact (in the San Martin and San Jose areas) which forms the relatively steeply dipping tronco deposits, these troncos contact the younger volcanic flows (dacite and ignimbrite) where they have formed the more horizontal manto portions of the deposit. The mineralized economic breccia grades from 30 g Ag/t to 250 g Ag/t. Exploration has been concentrated along the NE trending breccia zone however evidence of a northerly trend in area 30 leads us to suspect possible other structures together with 2.0 g Au/t to 30 g Au/t over widths that vary from 1.0 to 17.0 m but average 4.0 m.
Starcore International Mining and El Creston Property development news: Most of the work completed on the Creston property has been concentrated on the evaluation of the El Creston Main and Red Hill Zones which together make up the Creston Deposit. Overall the Creston Deposit is up to 1100 metres long x up to 1000 metres wide. The work to date includes mapping, geochemical sampling, geophysical surveying and the completion of the following: In 2010 SRK Consulting completed Resource Inventory calculations based on the results 28 diamond drill holes completed by AMAX between 1974 to 1978 and 109 holes drilled by Creston Moly Corp representing 36,151 metres of core. The resources are summarized below. See more details on this website.