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Mineral Resources
Mineral resources are mined from concentrations that formed under suitable conditions by geologic processes
-Weathering, sedimentation, volcanism
Suitable conditions are rare, and may take millions of years to form a deposit
Intensive mining, depletion, declining production and dependence on imports can be applied on a local, regional or global scale to estimate the remaining lifetime of a mineral resource
Renewable and Nonrenewable Resources
Renewable resources can be replenished over relatively short time spans
-Examples include plants and animals for food, trees for lumber and paper, energy from the Sun and wind
Nonrenewable resources are deposits that take millions of years to form
-Examples include fossil fuels and metals
Mineral Resources
Mineral resources are the endowment of useful minerals ultimately available commercially
Mineral resources include:
-Reserves—already identified deposits from which minerals can be extracted profitably
→An ore is a useful metallic mineral that can be mined for profit
Known deposits that are not economically or technologically recoverable
Mineral Resources

98% of the continental crust is composed of only eight elements
-A deposit is valuable if the element is concentrated above the level of its average crustal abundance
The profitability of a deposit may change as demand changes