Ore Mineral Security (AQA A Level Geography)

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Robin Martin-Jenkins

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Sources, distribution and trade of copper

  • A mineral is a naturally occurring inorganic solid with a crystalline structure
  • Ores are concentrations of minerals in rock high enough to be economically extracted for use
  • Deposits of copper are found in the Earth’s crust
  • Copper was first extracted and used in around 8000 BCE
    • One of the few metals that can occur naturally in a usable form
  • Copper deposits are found in many regions worldwide, but significant concentrations are focused in a few areas
    • The largest copper-producing countries are Chile, Peru, China, the United States, and Australia
    • Chile is the world's leading copper producer, with vast reserves and numerous mining operations
  • USA and Canada have significant copper deposits, with notable mines in Arizona, Utah, and British Columbia
  • Asia is a significant copper producer
    • Within Asia, China is the biggest producer and consumer of copper.
  • The distribution of copper deposits is influenced by geological processes, tectonic activity, and the presence of specific mineralised zones

Estimated copper production

Estimated copper production, 2017 (in thousand metric tonnes)

  • Copper has various characteristics which gives it many uses in industrial and domestic settings
    • Conducts heat and electricity 
    • Malleable and ductile
    • Durable
      • Copper oxidises by developing a green protective layer on its surface, called patina
      • This can preserve the inside of copper for thousands of years.
    • Anti-Bacterial
    • Recyclable
      • Over 80 percent copper ever mined and manufactured is still in use today

Uses of Copper

Category

Examples of uses

Electrical

Wiring for circuits, circuit boards, micro-cips, semiconductors, internet cable, electromagnets, solar panels

Building construction

Piping for water and heating, heat exchangers in thermal power stations, irrigation systems, light fittings, door handles

Transport

Vehicle radiators, oil coolers, heating systems, electric vehicle, aircraft control systems, shipping hulls

  • The components of demand for copper include:
    • Technological advancements
    • Population change
    • Global economic conditions
  • Copper is traded around the world but two-thirds of copper concentrates are processed in their region of origin
    • Cheaper and easier
    • Copper content of ore is often low, with large percentage of waste rock
    • Refined in situ to save transport costs
  • Copper concentrate and processed copper products are traded as they are required by most countries
    • Supply of copper is often not in the same location as the major demand
  • Of the concentrate that is traded, the biggest flows are from South America to Asia

Trade flows of Copper

Major trade flows of copper concentrate (average per year in thousand tonnes)

  • Recent trends in the global copper trade include:
    • Over 60% of global copper consumption is in Asia
      • In 1990 USA was the largest consumer of copper
      • By 2015 China had overtaken USA as the world's largest consumer of copper, accounting for nearly 40% of global demand
      • The biggest source of China’s copper imports is Chile
        • Almost 9 million tons from Chile in 2021
    • Driven by China’s economic growth and policies:
      • Rapid industrialisation
      • Infrastructure development
      • Urbanisation
      • China’s own copper reserves are plentiful but confined to small and medium sized mines
    • Increasing demand for electric vehicles (EVs)
      • Due to use in electrical wiring and components
    • Sustainable and responsible mining practices
      • Increasing focus on sustainable and responsible mining practices in the copper industry

Physical Geography of Ore

Physical geography of copper ore

Sources of Copper Ore and Key Aspects of Physical Geography

Ore mineral source

Description

Geological formation

Location 

Porphyry ore deposits

Most common type of copper ore (60% of all supply)


Low-grade - 1-2% copper content


Often found alongside other minerals e.g. zinc and gold, so economically viable despite low content


Extracted in open-cast pits

Formed in tectonic subduction zones


Hydrothermal fluids escape from magma chambers into rock layers above to form mineral deposits

Along destructive plate margins


E.g. Andes and Rockies mountain ranges

Massive sulphide deposits 

Higher grade - 2-5% copper content


Less widespread than porphyry

Hydrothermal release of magma on seafloor as two plates pull apart


Deposits merge with sediment and become embedded


Over millions of years tectonic uplift of seabed above the sea level exposes deposits as land

Constructive plate margins along mid-ocean ridges


Former ocean ridges now uplifted into land

E.g. Otavi sediments of northern Namibia



Strata bound copper deposits

Least widely distributed


Richest in copper content - up to 6%

Copper-rich sea water interacts with sedimentary rocks, leading to chemical reactions and the deposition of copper in specific layers in ocean basins


Over millions of years tectonic uplift of seabed above the sea level exposes deposits as land

The Copper Belt of the southern Katanga Province of the Democratic Republic of the Congo

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Robin Martin-Jenkins

Author: Robin Martin-Jenkins

Robin has taught Geography at a number of UK secondary schools over the past 13 years, alongside various pastoral roles. He fell in love with Geography whilst at school and has been a passionate advocate of its importance and relevance ever since. He currently works in an independent secondary school where his teaching is combined with mentoring of younger teachers.