
Based on general numismatic knowledge, as the provided context is insufficient for a detailed , the worth of a silver dime is determined by two primary factors: its intrinsic silver value and its numismatic, or collector, value.
The base value for any silver dime is its silver melt value. United States dimes minted in 1964 and earlier are composed of 90% silver and 10% copper. Each of these dimes contains approximately 0.07234 troy ounces of pure silver. This intrinsic value fluctuates daily with the spot price of silver. Therefore, a common silver dime will always be worth at least its weight in silver, which is significantly more than its ten-cent face value.
Beyond the melt value, a dime can carry a numismatic premium. This collector value is based on factors such as rarity, date, mint mark, and physical condition or grade. For example, most silver Roosevelt dimes (1946-1964) and common-date Mercury dimes (1916-1945) in circulated condition are traded primarily for their silver content. However, key-date coins, such as a 1916-D Mercury dime, or any silver dime in pristine, uncirculated condition, can be worth substantially more to collectors, with values ranging from many dollars to thousands of dollars depending on the specific coin.


