Lithosphere
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Stock
All Minerals that exist in the lithosphere
Resource
All the material theoretically exploitable
Reserve
Proportion of minerals that can be exploited now
Lasky’s Principle
The amount of Ore you find in 1m3 of rock
Resistivity
Use electricity to locate deposits on the basis that water conducts electricity
IR Spectroscopy
Use IR waves to locate deposits using knowledge of mineral characteristics - will they absorb/deflect
Magnetometry
Using magnetic pull to locate deposits - used for nickel, cobalt and iron
Gravimetry
Measures the density of rock and can then be used to identify deposit - igneous are dense
Seismic Surveys
Using sound to locate deposits by assessing reflection
Igneous processes
Processes by which rocks and minerals are created by the cooling and hardening of magma or molten lava.
Sedimentary processes
Processes that cause minerals to settle and build up to produce layers of deposited sediment
Metamorphic processes
The alteration of exisiting rocks with high temperatures and pressures without melting them - often caused by igneous processes or tectonic movement
6 examples of metal ores deposited by hyrothermal processes
• Tin • Copper • Lead • Silver • Gold • Arsenic
Proterozoic marine sediments
These include iron ore deposits such as haematite and magnetite. They were formed when dissolved iron compounds became oxidised by the oxygen released by photosynthesis, producing insoluble iron ore deposits.
How long ago were proterozoic marine sediments formed?
2.5 to 1.8 billion years ago
Alluvial deposits
Formed by materials being carried and seperated by flowing water in order of density
Evaporites
Crystallised minerals, such as halite, leftover from evaporation
Secondary enrichment
When economically important metals can form minerals that are soluble or insoluble depending upon the conditions, especially oxygen availability. They may be transported in solution, by moving water, and then deposited as their oxidation state changes
Biological sediments
Those where living organisms form mineral deposits
Inferred reserves
The presence of the mineral can be predicted from knowledge of the geological structures present but not enough is known to estimate the amount that can be economically extracted
Probable reserve
Sufficient information is known, so the amount of the mineral that can be economically extracted can be estimated with suffient accuracy that further exploration is justified
Proven reserves
Sufficient exploration has been carried out, including trial drilling, to accurately estimate the amount of the mineral that can be economically extracted
What are the impacts of mining a low ore grade? (4)
• More rock will have to be mined • More waste materials will be produced • More energy will be needed for mining and processing • More pollution will be generated
How does chemical form impact mine viability?
It controls the ease of chemical extraction of the metal. For example, aluminium can be extracted from bauxite but not from clay which is more abundant