This article is free to read. Creating a lesson uses your daily or stored credits; review the language and settings before starting.
How does natural gas form?
Quick answer
Natural gas forms underground when buried remains of plants and tiny marine organisms are heated and compressed over millions of years. This transforms them into kerogen, which cracks into methane and other gases. Some gas also forms at low temperatures when microbes break down organic matter in shallow sediments.
Natural gas forms when buried organic matter is heated underground over millions of years, breaking large molecules into smaller hydrocarbon gases. Most of it is methane, produced either by heat-driven cracking or by microbes in shallow sediments.
Step by step
- Organic matter from dead organisms settles in oxygen-poor mud and is buried by sediment.
- Increasing heat and pressure convert the organic matter into a waxy material called kerogen.
- At about 100–200°C, kerogen cracks into smaller molecules, mainly methane gas.
- The gas migrates upward through porous rock until it meets an impermeable layer.
- Trapped beneath that layer, the gas accumulates in a reservoir over millions of years.
Key things to understand
- Tiny marine organisms and plant matter settle in oxygen-poor mud, where they partly decay without fully breaking down.
- As layers of sediment pile up, heat and pressure rise, and the buried organic material becomes a waxy substance called kerogen.
- At roughly 100–200°C, kerogen cracks into smaller molecules, mainly methane, along with liquid oil and other gases.
- In shallow, cooler sediments, certain microbes also generate methane by breaking down organic matter without high heat.
- The gas migrates upward through porous rock until it is trapped beneath an impermeable layer, forming a reservoir.
Labelled diagram
- Organic matter
Dead plankton and plants settle in oxygen-poor mud on the seafloor.
- Burial
Sediment layers pile up, increasing heat and pressure on the buried material.
- Kerogen
Heat transforms the organic matter into a waxy substance called kerogen.
- Cracking
At 100–200°C, kerogen breaks into methane and other gases.
- Migration
Gas moves upward through porous rock, seeking lower pressure.
- Trap
An impermeable layer stops the gas, forming a reservoir.
Real-world examples
- The Marcellus Shale in the eastern United States holds vast natural gas reserves formed from ancient marine life.
- The onshore Groningen field in the Netherlands, once Europe's largest gas field, supplied the continent for decades.
- Landfills produce biogenic methane as microbes decompose food and paper waste in oxygen-poor conditions.
- Wetlands such as the Amazon basin release methane naturally as waterlogged plants decay without oxygen.
Common mistake
✗ Myth: Natural gas is a clean, green fuel.
✓ Fact: Burning natural gas releases carbon dioxide, a greenhouse gas, though less than coal or oil per unit of energy. Methane leaks during extraction and transport also warm the planet far more than CO₂ over short periods.
People also ask
How long does natural gas take to form?
What is natural gas made of?
Where is natural gas found?
Is natural gas the same as methane?
How is natural gas found and extracted?
Why is natural gas called a fossil fuel?
Can natural gas form without heat?
Part of the guide: Nature & Earth: Living Things and Rocks →

