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Physical Process

Peat Formation

Biogeochemical and Pedological Processes

The gradual accumulation of partially decomposed plant material in waterlogged, oxygen-poor conditions, where decomposition proceeds far more slowly than the rate of new plant growth, allowing organic matter to build up over centuries and millennia rather than fully breaking down. Peatlands formed by this process store an outsized share of the world's soil carbon relative to the land area they cover.

Facts
Timescale
Timescale (category)
Thousands of Years 1
Process Type
Biogeochemical or Pedological 2
Connections

Shaped

Bog, Landforms
Source Bog (Wikipedia)
Sources
1. Peat (Wikipedia)
Wikipedia infobox 'Lead section' = 'Peat is an accumulation of partially decayed vegetation or organic ...' on 'Peat'View the Source
2. Peat Formation (Wikipedia)
Wikimedia FoundationIntroduction
Quote, Introduction
Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs.
View the Source
Bog (Wikipedia)
Shaped: Bog, Lead
Quote, Shaped: Bog, Lead
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials
View the Source
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