Silver is found in a native form very rarely as nuggets in placer deposits and veins. It is more commonly combined with sulfur, arsenic, antimony, or chlorine and in various ores such as argentite (Ag2S), chlorargyrite ("horn silver," AgCl), and galena (a lead ore often containing significant amounts of silver). As silver is often found in conjunction with these or alloyed with other metals such as gold, it usually must be further extracted through amalgamation or electrolysis.
Silver mining has been undertaken since as early as the 5th century BCE. As silver is a precious metal often used for coins and bullion, its mining has historically often been lucrative. As with other precious metals such as gold or platinum, newly discovered deposits of silver ore have sparked silver rushes of miners seeking their fortunes. In recent centuries, large deposits were discovered and mined in the Americas, influencing the growth and development of Mexico, Andean countries such as Bolivia, Chile, Argentina and Peru, as well as Canada and the United States.
Silver has been known since ancient times. Silver is mentioned in the Book of Genesis, and slag heaps found in Asia Minor and on the islands of the Aegean Sea indicate that silver was being separated from lead as early as the 4th millennium BC. The silver mines at Laurium were very rich and helped provide a currency for the economy of ancient Athens, where the process involved mining the ore in underground galleries, washing and then smelting it to produce the metal. Elaborate washing tables still exist at the site which used rain water held in cisterns and collected during the winter months.
The Roman took over silver mining in Spain from Carthage after their acquisition of Carthaginian territories there following the Second Punic War. Extraction of silver from lead ore was widespread in Roman Britain very soon after the Roman conquest of the first century AD.
Vast amounts of silver were brought into the possession of the crowns of Europe after the conquest of the Americas from the now Mexican state of Zacatecas (discovered in 1546) and Potosí (Bolivia, also discovered in 1546), which triggered a period of inflation in Europe. Silver mining required large amounts of mercury to extract the metal from ore. In the Andes, the source was the Huancavelica mercury mine; Mexico was dependent on mercury from the Almadén mercury mine in Spain. Mercury had a very high and adverse environmental impact. Silver was extremely valuable in China, became a global commodity, contributing to the rise of the Spanish Empire. The rise and fall of its value affected the world market.
In the first half of the 19th century Chilean mining revived due to a silver rush in the Norte Chico region, leading to an increased presence of Chileans in the Atacama desert and a shift away from an agriculture based economy. The country of Argentina was named after its silver resources by Spanish conquistadors; Argentina is a Spanish adjective meaning "silvery".
Silver mining was a driving force in the settlement of western North America, with major booms for silver and associated minerals (lead, mostly) in the galena ore silver is most commonly found in. Notable silver rushes were in Colorado; Nevada; Cobalt, Ontario; California and the Kootenay region of British Columbia; notably in the Boundary and "Silvery" Slocan. A silver rush in Idaho produced mines in an area known as Silver Valley, a handful of which are still active today. The first major silver ore deposits in the United States were discovered at the Comstock Lode in Virginia City, Nevada, in 1859.
Silver-bearing ore typically contains very little silver, with much higher percentages of copper and lead. As such, most silver produced is refined from sulfide ores such as galena (lead) or chalcopyrite (copper) which contain small amounts of silver. Many of these ores are mined for their value as sulfide ores, and silver is extracted as a valuable by-product, however, some ores are mined explicitly for their silver value. Flotation separation is a key step in this complicated process. Silver mineralizes most commonly as argentite, polybasite and proustite, Ag2S, (Ag, Cu)16Sb2S11 and Ag3AsS3 respectively 
Methods for mining silver vary between mines depending on factors related to the ore body, such as the grade of the ore, its depth, host rock, and economic factors. Commonly, silver is extracted in open pit mines, and underground drifts and shafts. One of the most challenging aspects of silver mining is extraction of the ore, as silver and its host rock can be very heavy. Explosives are frequently used to shatter veins into manageable pieces, which are transported via mine cars and then lifted to the surface. This is a dangerous process that can lead to rapid structural failure of the mine known as rock bursts, which can occur without warning.
In recent history, there have been global silver deficits as a result of greater demand than supply. To combat this silver scrap mining became more prevalent. A significant amount of silver can be harvested from scrap materials, 1,700 tons were recovered in the United States in the year 2000. Silver scrap has a much lower value than other metals, and as a result of this traditional techniques that work for many materials do not work for silver. Jewelry is commonly re-alloyed as opposed to being refined, although this silver is less pure. The same process is undertaken for recovering silver from dental alloys and silverware. Photographic film is another source of economic scrap, as silver can be extracted from spent film via leaching of burnt film ashes.
Once silver ore has been removed from a mine, it is crushed into a fine powder. Silver is commonly extracted from the powdered ore by smelting or chemical leaching. Silver's melting point occurs at 962oC (1764oF, 1,235.15K). As such, industrial metallurgic processes are needed to prepare silver for commercial purposes. Ore treatment by mercury amalgamation, such as in the patio process or pan amalgamation was widely used through the 1800s, but is seldom used today.
Parting is a common process by which metallic silver can be extracted. This is done by dissolving a gold alloy (less than 30% gold) and boiling with 30% nitric acid. Affination is the process of boiling silver and gold with concentrated sulfuric acid. This separates the silver and gold.
Silver is also produced during the electrolytic refining of copper and by application of the Parkes process on lead metal obtained from lead ores that contain small amounts of silver. Commercial grade fine silver is at least 99.9 percent pure silver and purities greater than 99.999 percent are available.
Silver processing has led to significant environmental impacts. As patio amalgamation became widespread in the Americas, more mercury was needed, as it is a key component in the process. It is estimated that 90% of the mercury consumed in the United States from 1850 to 1900 was used to extract silver and gold. An estimated 257, 400 tonnes of mercury were lost to the environment in this process in the Americas since the patio process was first used. 60-65% of this is likely released into the atmosphere, being the single largest contributor to the global mercury cycle. Mercury poisoning has severe health effects and can be deadly.
Contaminants are also known to enter drinking water in and around abandoned silver mines. Well water in South Morelos State, Mexico, was found to have high concentrations of toxic metals including arsenic, iron, manganese, lead, and fluorine. This is attributed to the abandoned and flooded silver mine at Huautla. Groundwaters flooded the mine-shafts after they were abandoned in the early 1990s, which allowed for oxidation and mobilization of these dangerous contaminants.