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Reading Time: 7 min
Last Updated: September 15, 2026
Main Ideas: 5
Reading Time: 7 min
Last Updated: September 15, 2026
Main Ideas: 5

Topic 6.4 Notes – Distribution of Natural Energy Resources

Verified for 2027 AP® Environmental Science Exam
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Natural energy resources are not spread evenly around Earth. In APES, this topic is about where coal, oil, natural gas, and uranium ore occur, and why geology, especially ancient environments and rock structures, controls that pattern.

What the Distribution of Natural Energy Resources Means

When APES says distribution, it means the physical pattern of where a resource occurs in Earth’s crust. That is different from how much is extracted or used.

Keep these terms straight:

  • Distribution = where the resource exists
  • Deposit = a natural concentration in one location
  • Reserve = the recoverable part of a known deposit with current technology and economics
  • Production = how much is extracted
  • Consumption = how much is used
  • Access = whether people can actually obtain and use it

This distinction gets tested a lot. A country can have a big deposit but low production if extraction is expensive, difficult, or restricted. A production map or reserve map is not the same as a map of geologic occurrence.

The biggest idea here is simple. Uneven distribution comes from geologic history, not from today’s political borders or present climate.

Why Geologic History Controls Where Resources Are Found

Resources form through a chain of geologic events, and that chain only happened in certain places.

  1. Source material forms or collects in a particular environment.
  2. Burial, heat, pressure, chemical change, tectonics, or fluids transform it.
  3. Rock structures preserve, trap, or concentrate it.
  4. Those conditions were uneven across Earth, so deposits are uneven too.

Major controls include:

  • Ancient environments such as swamps, shallow seas, lakes, and sedimentary basins
  • Burial history over time, including depth, heat, and pressure
  • Rock type such as source rock, reservoir rock, and cap rock
  • Tectonic activity such as folding, faulting, uplift, volcanism, and basin formation
  • Erosion and exposure, which can bring deposits closer to the surface

For fossil fuels, those controls often show up as geologic traps that let oil and natural gas accumulate in certain rock layers instead of spreading out everywhere.

Study guide illustration

Common petroleum traps

Current surface conditions can fool you. A desert today may contain oil from an ancient shallow sea. A cold region today may contain coal from ancient equatorial wetlands.

Where the Major Energy Resources Occur

Coal

Coal forms from plant material in ancient wetlands and swamps. Low oxygen slows decomposition, then burial and pressure turn peat into coal. Coal usually occurs in sedimentary layers called coal seams.

  • Standard example: Appalachian coalfields
  • Major regions: China, India, Russia, Australia, South Africa, eastern United States

Crude oil

Crude oil forms mainly from marine microorganisms such as algae and plankton in low-oxygen seas, lakes, or coastal areas. After burial, hydrocarbons form and migrate into porous rock, then get trapped under cap rock.

  • Standard example: Persian Gulf region
  • Major regions: Middle East, Russia, United States, Venezuela, Canada, North and West Africa, North Sea, Central Asia
  • Heavy oil and bitumen examples: Alberta oil sands and Venezuela’s Orinoco Belt

Natural gas

Natural gas is mostly methane. It forms from buried organic matter, often in the same sedimentary basins as oil. In a trap, gas usually sits above oil because it is less dense. It can also occur in shale or separate reservoirs.

  • Major regions: Russia and Central Asia, Middle East, United States, Canada, parts of Africa and Europe

Uranium ore and other ores

An ore is rock with enough useful material to recover economically. Uranium matters here because it fuels nuclear power. Ores form through magma cooling, hydrothermal fluids, sedimentary concentration, weathering and erosion, and metamorphism with tectonics.

  • Major uranium regions: Kazakhstan, Canada, Australia, Namibia, parts of the United States and Central Asia

How to Read Resource Maps and Cross-Sections

Always identify what a map shows first. Is it deposits, reserves, or production?

Good map reading does three things:

  • Describe the pattern
    Resource locations usually appear clustered, not uniform.
  • Explain the geology
    Connect coal to ancient swamps, and oil and gas to sedimentary basins and traps.
  • State a human consequence
    Export potential, import dependence, or unequal access.

For cross-sections, remember:

  • Oil and gas: source rock deep below, porous reservoir rock, cap rock above, gas over oil over water, traps made by folds or faults
  • Coal: seams follow sedimentary layers, then folding, faulting, or uplift may distort or expose them

Why Uneven Distribution Matters for Human Energy Systems

Uneven deposits create unequal domestic energy availability.

  • Resource-rich countries may export
  • Resource-poor countries may import
  • Access also depends on technology, wealth, pipelines, ports, infrastructure, trade routes, and policy

A large deposit does not guarantee high production or energy independence. The chain to remember is:

geologic history → deposits → availability → use shaped by economics and technology

Key Takeaways

A reserve can change when technology or prices change, even if the geology stays the same.
A production map cannot prove where a resource does or does not geologically occur.
Coal points to ancient terrestrial wetlands, while oil and many gas deposits point to ancient aquatic environments.
In a conventional petroleum trap, gas sits above oil and oil sits above water because of density.
Present-day climate does not tell you the original environment where a fossil fuel formed.
When a map question asks “why there,” the best answer is geologic history, not political borders.

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