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Lithosphere

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Total cards: 24•Content version: v4•Public deck•Updated: 8/1/2026

Card preview (24)

#1
Front (Question)

Stock

Back (Answer)

All Minerals that exist in the lithosphere

#2
Front (Question)

Resource

Back (Answer)

All the material theoretically exploitable

#3
Front (Question)

Reserve

Back (Answer)

Proportion of minerals that can be exploited now

#4
Front (Question)

Lasky’s Principle

Back (Answer)

The amount of Ore you find in 1m3 of rock

#5
Front (Question)

Resistivity

Back (Answer)

Use electricity to locate deposits on the basis that water conducts electricity

#6
Front (Question)

IR Spectroscopy

Back (Answer)

Use IR waves to locate deposits using knowledge of mineral characteristics - will they absorb/deflect

#7
Front (Question)

Magnetometry

Back (Answer)

Using magnetic pull to locate deposits - used for nickel, cobalt and iron

#8
Front (Question)

Gravimetry

Back (Answer)

Measures the density of rock and can then be used to identify deposit - igneous are dense

#9
Front (Question)

Seismic Surveys

Back (Answer)

Using sound to locate deposits by assessing reflection

#10
Front (Question)

Igneous processes

Back (Answer)

Processes by which rocks and minerals are created by the cooling and hardening of magma or molten lava.

#11
Front (Question)

Sedimentary processes

Back (Answer)

Processes that cause minerals to settle and build up to produce layers of deposited sediment

#12
Front (Question)

Metamorphic processes

Back (Answer)

The alteration of exisiting rocks with high temperatures and pressures without melting them - often caused by igneous processes or tectonic movement

#13
Front (Question)

6 examples of metal ores deposited by hyrothermal processes

Back (Answer)

• Tin • Copper • Lead • Silver • Gold • Arsenic

#14
Front (Question)

Proterozoic marine sediments

Back (Answer)

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.

#15
Front (Question)

How long ago were proterozoic marine sediments formed?

Back (Answer)

2.5 to 1.8 billion years ago

#16
Front (Question)

Alluvial deposits

Back (Answer)

Formed by materials being carried and seperated by flowing water in order of density

#17
Front (Question)

Evaporites

Back (Answer)

Crystallised minerals, such as halite, leftover from evaporation

#18
Front (Question)

Secondary enrichment

Back (Answer)

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

#19
Front (Question)

Biological sediments

Back (Answer)

Those where living organisms form mineral deposits

#20
Front (Question)

Inferred reserves

Back (Answer)

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

#21
Front (Question)

Probable reserve

Back (Answer)

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

#22
Front (Question)

Proven reserves

Back (Answer)

Sufficient exploration has been carried out, including trial drilling, to accurately estimate the amount of the mineral that can be economically extracted

#23
Front (Question)

What are the impacts of mining a low ore grade? (4)

Back (Answer)

• 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

#24
Front (Question)

How does chemical form impact mine viability?

Back (Answer)

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